Friday, March 18, 2011

Wind Power and Windmills

http://earthsci.org/mineral/energy/wind/wind.html

aeration windmill animation

Types of Windmills
Aeration Windmill 
Aermotor Windmill The Wind Turbine

Important Factors to Consider When Building A Windmill
Location  
Wind Characteristics  
Terrain Characteristics Windmill Efficiency
The Purpose of Windmill Shrouds Electricity and Storage of Energy
Brakes Windmills Today
Bibliography

Excellent offsite link from our links page  Wind Power (from Denmark)  very detailed source of information 
Types of Windmills


Aeration type

Aeration Windmill
This windmill will aerate a pond or pump water out of your pond or river to water your animals or garden. This windmill will pump out of a shallow (up to 15m) well.
Aermotor type

Aermotor Windmill
They have been manufactured since 1888 and are the old standard of windmills. They will pump out of a well but will not aerate a pond or pump water out of the pond or river. These styles of windmills will not produce electricity! Many people think you can buy a regular windmill to run your air conditioner, freezer, washer, dryer, etc. and you can not. This is all 240 volts A.C.
Many have seen ads "sell electricity back to your utility company." Do you think your local electric company would let you run a line from a windmill, or even a generator, and send electricity to their line? Dream on...
You can make a windmill produce 12 volt D.C. to charge a battery, but you can charge your batteries with solar cells today much cheaper than using a windmill. The big windmills you see in Ravenshoe , Queensland  will produce electricity but they cost thousands and thousands of dollars.
Have you ever seen a windmill at someone's home that produces 240 volt AC? The technology is not here today to produce electricity for homes.
The Wind Turbine
wind turbine
The wind turbine, also called a windmill, is a means of harnessing the kinetic energy of the wind and converting it into electrical energy.  This is accomplished by turning blades called aerofoils, which drive a shaft, which drive a motor (turbine) and ar e connected to a generator.  "It is estimated that the total power capacity of winds surrounding the earth is 1 x 1011 Gigawatts" (Cheremisinoff 6).  The total energy of the winds fluctuates from year to year.  Windmill expert Richard Hills said that the wind really is a fickle source of power, with wind speeds to low or inconsistent for the windmill to be of practical use.  However, that hasn't stopped windmill engineers from trying.  Today, there are many kinds of windmills, some of which serve different functions.  They are a complex alternative energy source.

Persian vertical axis windmill
 There are a number of types of windmills.  They are divided into Horizontal-Axis and Vertical-Axis types. Low speed horizontal-axis windmills are used for water pumping and air compressing.  Southern Cros  windmills  are an example.  Earlier windmills such as the ones in England and Holland build a couple hundred years ago are another
example.  The horizontal-axis was invented in Egypt and Greece in 300 BCE. "It had 8 to 10 wooden beams rigged with sails, and a rotor which turned perpendicular to the wind direction" (Naar 5).  This specific type of windmill became
popular in Portugal and Greece.  In the 1200's, the crusaders built and developed the post-mill, which where used to mill grain. It was first used to produce electricity in Denmark i n the late 1800's and spread soon after to the U.S.  In America, windmills made the great plains.  They were used to pump water and irrigate crops.  During World War I, farmers rigged
windmills to generate 1 kW of DC current.  They mounted their devices on the tops of buildings and towers.  On western farms and railroad stations, the pumping windmill was 6-16m high with a 2-3m wheel diameter"
(45)].  With 15kmh wind speed, a 2m-diameter wheel, a 60cm diameter pump cylinder, a windmill-pump could lift 200L per hour to a height of 12m.  A 4m in diameter wheel could lift  250L per hour to a height of 38m.  (Naar, p. 46).
The growth of wind-electricity in Australia was greatly peaked in the 1930's and 40's .  However, in the 1970's, due to oil shortages, earlier prototypes of high-speed horizontal-axis windmills were developed. High-speed horizontal-axis types are used for many purposes, come in many sizes.  These include the typical windmills on  windmill farm and any other wind turbines in which the shaft turned by the aerofoils is horizontal.  High-speed horizontal types may have 1, 2, 3, 4, or many aerofoils.
Low-speed types such as European ones have much larger aerofoils in relation to their height above the ground. Low speed types such as western Quensland ones are usually a pinwheel, with many small blades encircled with an outer frame like a wheel. Vertical-axis windmills were first developed in the Persians in 1500 BCE to mill corn and were still in use in the 1970's  in the Zahedan region.  Sails were mounted on a boom, which was attached to a shaft that turned vertically.  By 500 BCE, the technology had spread to Northern Africa and Spain.  Low-speed ve rtical-axis windmills are popular in Finland.  They are about 150 years old.  They consist of a 200L oil drum split in half.  They are used to pump water and aerate land.  They are inefficient.
High-speed vertical-axis windmills include the Darrieus models.  These have long, thin, curved outer blades, which rotate at 3 to 4 times the wind speed.  They have a low starting torque and a high tip-speed ratio.  They are inexpensive and are used for electricity generation and irrigation.  There are three types, the delta, chi, and gamma models.  All models are built on a tripod.  The advantages to a Darrieus-windmill are that it can deliver mechanical power at ground level.  The generator, gearbox, and turbine components are on the ground, instead of at the top of a tower as in horizontal-axis windmills.  They cost much less to construct, because there is less material, and the pitch
of the blades does not have to be adjusted.
Another type of HSVAW's are the Madaras and Flettner types, revolving cylinder s which sit on a tracked carriage.  "The motion of a spinning cylinder causes the carriage to move over a circular track and the carriage wheels to drive an electric generator" (Justus).  The Savonius model, which originated in Finland in the 1920's, is a n S-shaped blade, which rotates and turns a vertical shaft.  Today, these types of windmills are very popular with scientists
and their technology is being developed.

Important Factors to Consider When Building A Windmill
 
What to consider when building a windmill In choosing where to build a windmill, there are many important factors to consider. First is the location: 1) Available wind energy is usually higher near the seacoast or coasts of very large lakes and offshore islands. 2) Available wind energy is generally high in the central Austrsalia because of the wide expanses of level (low surface roughness) terrain.
3) Available wind energy is generally low throughout eastern Australia with the exception of mountain passes but higher on the southern and western coasts
Also important to consider the wind characteristics where you are going to build: 1) the mean wind speed (calculated my cubing the averages and taking the mean of the cubes) and its seasonal variations. 2)  The probability distribution of wind speed and of extreme winds. The mean wind speed must be high enough, and the distribution must be so that all the data points are very similar.
3)  The height variation of wind speed and wind direction.  Wind cannot be too high or too low in relation to the ground or it is too difficult to harness.
4) The gustiness of the wind field in both speed and direction.  Gusty winds greatly affect the power output of the windmills and are usually harmful.
5) The wind direction distribution and probability of sudden large shifts in di rection.  The wind must be
unlikely to suddenly shift direction.  It must blow in the same general direction.
6) the seasonal density of the air, and variations of density of the air with height.  The denser the air, the worse it will be for windmills.
7) Hazard conditions such as sandstorms, humidity, and salt-spray, which are bad for windmills.
8)  Trade winds in the subtropics, and the channeled wind through mountain passes are especially beneficial to windmills.
Terrain Characteristics
Once a suitable location is found, the wind is analysed extensively, and the criteria is met, there are still more requisites. 1)  The terrain upon which the windmills are built must be relatively flat.  The elevation
difference between the turbine site and the terrain is no larger than 60 meters over a 12-km radius.  You may have seen windmills such as those in Ravenshoe, Far North Queensland on little hills, but this is because the requirement is met. The hill may be the only one in a mountain pass 2) All hills must have small height to width ratios:  h:l must be < 0.016.
3) The elevation difference between the highest and lowest point must be 1/3 or less of the
height difference between the bottom of the rotor disk and the lowest
point in the terrain strip.  The surface roughness of the terrain upon
which the windmill is to be built must be low.  If it varies by more than
10%, this is no good.  The terrain must be smooth, and consistently so.  A
rough surface has more of a negative effect on the wind than a smooth
surface.  There is a value n, called, which is assigned to the terrain in
terms of its roughness.  This value is used to calculate the height of the
windmill.  For instance, over the sea, the index location, n is 0.14.
Over rough inland country, n is 0.34.
Wind Mill Efficiency Windmills are turbines.  The two names can be used synonymously. Turbines are a means of harnessing the a fluid's power (the wind) by converting the kinetic energy of the fluid (the wind) into mechanical power (the rotating shaft) When the shaft of a w indmill is hooked up to a generator, electrical energy can be formed. The generator can be used to produce either DC or AC current.  Generators that produce DC can be connected to batteries, an inverter to produce AC, or to power DC loads.
Some generators are connected to heating coils.  Generators that produce AC can be hooked up to AC motors such as water pumps.  Windmills are NOT efficient.  At the very most, a windmill can extract only 16/27ths of the kinetic energy from the wind.  This is called the Betz Limit and it can be mathematically proven through calculus.  Most of today's windmills extract about 30 perc ent of the wind's energy.
The Southern Cross farm windmill can only extract 10%. An important equation used to find the wind power density, how much power is available per square meter is the equation
P = .5 pu³ , where P is the wind power density in W/m2, p is the density of the air, and u³ is the cube of the wind velocity.
An equation for the power available is :
(kinetic energy flux) = .5 p V3 A , where p is the kinetic energy density J/m³, V is the velocity of the wind, A is the cross sectional area of the wind on the turbine.
The equation for determining the power of the shaft, (which is
less than the final power output, since gear trains and generators cause
power to be lost) is as follows:
 
Cp = P(0.5 p V ³ (D2)/4

Where Cp is the power coefficient (Power of shaft), p is the air density,
D is the rotor diameter, V is the velocity of the wind and P is the net
power output.
Also Cp = P available/P turbine
The power available is a function of elevation.  At ground level, 100% of
the power is available. At 30m, 97% is available. At 1500m , 86% is available.

The Purpose of Windmill Shrouds
Some turbines are shrouded like jet engines.  The shroud is
a way to channel the wind.
An equation for the power harnessed by a shrouded wind turbine is:
P(Pe) = ( QT ((p + (k)  where P is the power,
Pe is the power extracted, ( is the turbine efficiency, QT is the
volumetric flow rate of air on the turbine, (V/A), ((p + (k) is the change
in pressure energy between the inlet and the exit of the wind turbine, and
k is the cane in kinetic energy of a unit volume of air that passes
through the machine.
Shrouds concentrate and diffuse the wind as it passes through a
horizontal access wind-turbine.  They reduce the turbulence of the wind
and "direct it".
The advantages of shrouds, as told by Cheremisinoff (pg. 61 of Fundamentals of Wind Energy), are: a ) the axial velocity of the turbine increases, meaning that smaller rotors can operate at higher revolutions, b) the shroud can greatly reduce tip-losses, and
c) the aerofoils would not have to be rotated in a direction parallel to the wind if the wind-direction changed.  The cut in speed is the lowest wind speed below which no usable power can be produced by a wind turbine.  This means that the wind must be fast enough to move the aerofoils to drive the shaft
to create enough power, after much is lost, so that the end amount of power is greater than zero.
Rated power is the maximum power output of a
turbine, which is dependent on a number of factors, especially the
generator.  In calculating the height of the windmill, it is important to
keep in mind that the windmill must be high enough to be above
obstructions.  The wind velocity decreases as one approaches the surface.
That means that the higher you build, the better chance
 there will be that the wind speed is higher, however, you must find the
perfect medium--there are often more variables as you increase in
altitude.  In calculating how high a windmill should be the following
equation is used:
 V1/V2 = (H1/H2)n,
Where V1 is the wind speed at the highest point of the highest blade, V2 is the wind speed at the lowest
point of the lowest blade, H1 is the height of the highest point, and H2 is the height of the lowest point.  n is the index location of the site, a va lue that measures the roughness of the terrain.
The support of the windmill is generally made out of steel.  The windshaft is the shaft which carries the windwheel or aerofoils.  It is turned as the aerofoils turn.  It is made of steel or wood.
Aerofoils are the blades on a windmill.  They can be made out of any material.  They were first made of wood or wood composites.  Steel was used after that.  Aluminum is used in the Darrieus windmills because it is
much stronger. Unfortunately, Aluminum fatigues quicker.  Some windmills use fiberglass blades.  New materials such as strong alloys are being used in today's windmills experimentally.
It is important that the blades have a large lift force and a small drag force.  The lift force is the force needed to bend the flow of the (fluid) air.  It is the force perpendicular to the stream of the air.  The drag force is the force parallel to the stream.  The aerofoil must be able to develop a lift force at least 50 times greater than the drag. Torque acts on the aerofoil with a vector from the center of rotation away.
Other forces that act on the blades of windmills are wind shears, wind gusts, which push on the aerofoils, gravity, a pull towards the earth, and shifts in the direction of the wind.  Shifts in the direction of the wind are often accounted for by having a  small blade, called a tailvane, on the backside of a windmill.  The wind blows on a flat side of the tail, which is oriented differently from the aerofoils.  Then, the aerofoils can be rotated to face into the wind.  If the wind is blowing in the directi on of this tail instead of the direction of the aerofoils, the tail rotates a shaft, which rotates the whole windmill in the proper direction so as to orient it towards the wind.
Wind gusts can greatly affect a windmill.  A turbulent gust is a gust greater than two minutes with a certain mean wind speed.  Gusts are analyzed extensively, with magnitudes, one fo r the lull speed, which is the wind speed of a negative gust amplitude, and the peak speed, which is the wind speed for a positive gust amplitude.
The gust amplitude is the difference between the largest speed in the gust and the mean speed.  The gust du ration is the time from the beginning to the end of a gust.  The gust frequency is the number of positive gusts, which occur per unit time. The gust formation time is the time it takes from the beginning of a gust to the time it attains the peak gust spe ed.  The gust decay time is the time it takes for the gust the end after it reaches its highest amplitude.
There is quite a bit of terminology with aerofoils.  The angle of the surface to the fluid flow is the angle of attack, alpha.  The angle of attack must be just right.  If it is too great, the lift will dramatically decrease and the drag will increase, st alling the windmill.  At rest, (when the windmill is not in operation), the angle of attack is 85°.  When in motion, the angle of attack is anywhere from 2-10 degrees.  Newer and more advanced windmills have an angle of attack in the upper end of this range.  The pitch angle, ß is the angle between the chord of the aerofoil
and its plane of rotation.  The pitch angle can be adjusted.  Solidity is the ratio of the blade width (at widest point) to the distance between the centers of the blades.  A typical "pinwheel Southern Cross windmill" might have
a ratio of about 1:1, because the blades are very narrow and very close together, whereas a new two-bladed aerofoil would have a ratio of about 0.03.  There is a transfer of work between the wind stream and the moving
blade.  In order for this transfer to be efficient, a typical blade is usually 1/4 the width of its length.  (If the blade is 3m long, it will be 750mm wide at its widest point).
Aerofoils come in many shapes.  Some blades are made a little wider than this ratio, because it is easier to start such a windmill.  However, blades like this aren't as efficient.  No matter what the shape, "most have a blunt nose and a finely tapering tab le" (Calvert).  A flow must be able to follow the curved surfaces of the aerofoil without being separated.  The mass flow rate is given by the equation:

m = p Vb A
, where p is the air density, Vb is the air speed at the blades and A is the area.
The number of blades on a windmill varies.  There are many different types of windmills.  The following equation helps figure out how fast the a certain-bladed windmill
will rotate in relation to windmills with different numbers of blades:

Speed of windmill = 1 / sq. root of number of blades
 
The aerofoils of a four bladed machine rotate 71% as fast as that of a 2 bladed machine.  A six bladed machine rotates at 58% and an 8 bladed machine rotates at 56% as fast as a 2 bladed machine.
Electricity and Storage of Energy
 
As mentioned previously, the generators in a wind turbine can convert the mechanical energy produced by the rotation of the shaft into electrical energy, DC.  From there, some windmills have synchronous inverters, complex electronic devices which convert  the DC generated by the turbines into AC.  This is an expensive option. There is a loss of power as well through its processes.  Others have induction generators, which produce AC current without a synchronous inverter and less power loss.  The energy extracted from the wind and converted into mechanical energy then electrical energy by the generator must be stored, since it is not used generally used all at once.  It is important to keep a surplus of energy for usage when the wind is not blowing fast enough, despite the corrections that can be made in the pitch of the aerofoil blades and when the windmill is out of service or the demand is especially high.
  Storing the wind's energy effectively is the key to its long-term use.  Windmills used as water pumpers or air-compressors can pump excess water, hydrogen or air into reserve tanks. Today, there are a number of ways to store the wind's energy.  Windmills are used to charge Electrolyte batteries.  Lead-acid or Lead-cobalt car batteries are commonly used as well.  However, batteries may be expensive and inefficient--they may lose 10-25% of the energy stored in them.
Nickel-Iron, Nickel-cadmium, and zinc-air cells are often used as well. These tend to be more efficient.  Some windmills are now using organic electrolyte batteries such as CuCl2, Ni Cl2, and NiF2 batteries as well as sodium-sulfur batteries, which operate at high temperature, are used.
Although uncommon and still in experimental phases, some energy is stored not by being converted directly into electrical energy, but rather by being stored as thermal or electromagnetic energy,
Sound Fluids are elastic.  Pressure waves are constantly being created and propagated by the aerofoils and the turbine as a whole (entire components excepting the support).  We can hear them in the sound given off.  The sound intensity is directly proportional with the speed of the windmill.
The frequency of the waves is directly proportional to the angular speed of the blades on the rotor.  The flutter you hear has aerodynamic and elastic properties.  The higher speed the aerofoils are, the louder the sound a nd the louder the flutter they will make, as more pressure waves are being created and propagated.  The generators are noisy.  They often confuse birds and cause them to fly towards the turbine.
Windmills can be very noisy.  A 300 kW turbine at 1 mile away has a dB level equal to a traffic light 100 feet away (Gipe).  Windmill sound levels are regulated.
The sound level must be kept under 46 dB in a residential area.  Wind turbines can cause interference, disturbances with TV and radio reception (ghost images on TVs), affect microwaves and disrupt satellite communication.  These problems are currently being resolved.  Many have already been fixed.  There is also a .009 probability of a bird or insect being struck by the blades.  Windmill makers must use artificial sound or florescent paint or scents to scare away flying creatures.

Brakes
 
 Mechanical brakes are used to hold windmills at rest when they are not needed, are not functioning, or are under repair.  Greek windmills used sticks or logs jammed into the ground to keep the windmill stopped, but modern brakes are more sophisticated.  Many windmills today use airbrakes like those used in planes.  Other windmills have rope brakes.
Ropes connected to the aerofoils are simply pulled and tethered to a post to keep the aerofoils from turning.  The torque on a rope brake can be calculated by the equation :

(M-m)(R2 + r)g
 
Windmills Today
Many windmills are used today.  They are used to heat water, refrigerate storage buildings or rooms, refrigerate produce, dry crops, irrigate crops, heat buildings, and charge batteries for tr actors on farms (33).  Ever since the energy shortages of the 70's, the growing concern of pollution due to the burning of fossil fuels and the depletion of natural resources, windmills have been greatly studied and developed. Today, Sandia National Laboratories, Alcoa, GE, Boe ing, Grumman, UTC, Westinghouse, and other scientists are researching and developing Darrieuses and new types of windmills.  Today, windmills are used to operate sawmills and oil mills in Europe.  They are used in mining to extract minerals, to pump water , to generate electricity, and to charge
batteries.  "Windmills have been used on buoys moored far out in the ocean, the power being used for the collection and transmission of oceanographic and weather data.  They also work in deserted places as an aid to radio and telephone communications and they are used to work navigation lights on isolated hazards" (Calvert 77).
The Future will likely bring bigger and better things for the wind turbine.  Many new wind turbine models are being built.  The wind turbine holds much promise for energy production in the years to come.
Bibliography
  Calvert, N. G.  Windpower Principles:  Their application on the small scale.  London:  Charles Griffin and Co., Ltd., 1979. Cheremisinoff, Nicholas P.  Fundamentals of Wind Energy.  Ann Arbor:  Ann Arbor Science Publishers, Inc. 1978.
Gipe, Paul.  Wind Energy Comes of Age.  New York:  John Wiley and Sons, Inc. 1995.
Hau, E., J. Langenbrinck, and W. Palz.  Large Wind Turbines.  Berlin:  Springer-Verlag, 1993.
Hills, Richard L.  Power From the Wind:  A History of Windmill Technology.  London:  Cambridge University Press, 1994.
Justus, C. G.  Winds and Wind System Performance.  Philadelphia:  The Franklin Institute Press, 1978.
Naar, Jon.  The New Wind Power.  New York:  Penguin Books, 1982.
Taylor, R. H.  Alternative Energy Sources for the Centralized Generation of Electricity.  Bristol, England:  Adam Hilger, Ltd. 1983.

Biofuels

What is biodiesel?
Technically, biodiesel is Vegetable Oil Methyl Ester. It is formed by removing the triglyceride molecule from vegetable oil in the form of glycerin (soap). Once the glycerin is removed from the oil, the remaining molecules are, to a diesel engine, similar to petroleum diesel fuel. There are some notable differences. The biodiesel molecules are very simple hydrocarbon chains, containing no sulfur, ring molecules or aromatics associated with fossil fuels. Biodiesel is made up of almost 10% oxygen, making it a naturally "oxygenated" fuel.
Biodiesel is the name for a variety of ester-based oxygenated fuels made from soybean oil or other vegetable oils or animal fats. The concept of using vegetable oil as a fuel dates back to 1895 when Dr. Rudolf Diesel developed the first diesel engine to run on vegetable oil. Diesel demonstrated his engine at the World Exhibition in Paris in 1900 using peanut oil as fuel.

Key Advantages of Biodiesel:
1. Biodiesel is the only alternative fuel that runs in any conventional, unmodified diesel engine. It can be stored anywhere that petroleum diesel fuel is stored.
2. Biodiesel can be used alone or mixed in any ratio with petroleum diesel fuel. The most common blend is a mix of 20% biodiesel with 80% petroleum diesel, or "B20."
3. The lifecycle production and use of biodiesel produces approximately 80% less carbon dioxide emissions, and almost 100% less sulfur dioxide. Combustion of biodiesel alone provides over a 90% reduction in total unburned hydrocarbons, and a 75-90% reduction in aromatic hydrocarbons. Biodiesel further provides significant reductions in particulates and carbon monoxide than petroleum diesel fuel. Biodiesel provides a slight increase or decrease in nitrogen oxides depending on engine family and testing procedures. Based on Ames Mutagenicity tests, biodiesel provides a 90% reduction in cancer risks.
4. Biodiesel is 11% oxygen by weight and contains no sulfur. The use of biodiesel can extend the life of diesel engines because it is more lubricating than petroleum diesel fuel, while fuel consumption, auto ignition, power output, and engine torque are relatively unaffected by biodiesel.
5. Biodiesel is safe to handle and transport because it is as biodegradable as sugar, 10 times less toxic than table salt, and has a high flashpoint of about 300 F compared to petroleum diesel fuel, which has a flash point of 125 F.
6. Biodiesel can be made from domestically produced, renewable oilseed crops such as soybeans.
7. Biodiesel is a proven fuel with over 30 million successful US road miles, and over 20 years of use in Europe.
8. When burned in a diesel engine, biodiesel replaces the exhaust odor of petroleum diesel with the pleasant smell of popcorn or french fries.
 
 
Power
One of the major advantages is the fact that it can be used in existing engines and fuel injection equipment (no modification required) without negative impacts to operating performance.
Fuel availability/economy
Virtually the same MPG rating as petrodiesel and the only alternative fuel for heavyweight vehicles requiring no special dispensing and storage equipment.
Storage
Readily blends and stays blended with petrodiesel so it can be stored and dispensed wherever diesel is stored or sold.
Combustibility/Safety
Biodiesel has a very high flash point (300°F) making it one of the safest of all alternative fuels.
Production/Refining
The only alternative fuel that can boast of a zero total emissions production facility
Lubricity
The only alternative fuel that can actually extend engine life because of its superior lubricating properties.
Environmental Impact
The only renewable alternative diesel fuel that actually reduces a major greenhouse gas components in the atmosphere .  The use of biodiesel will also reduce the following emissions:
carbon monoxide
ozone-forming-hydrocarbons
hazardous diesel particulate
acid rain-causing sulfur dioxide
lifecycle carbon dioxide .





Oil Producing Plants
Corn, Cashew, Oat, Palm , Lupine, Rubber seed, Kenaf, Calendula, Cotton
Hemp, Soybean, Rapeseed, Olive tree, Castor bean, Jojoba, Pecan
Oil Palm, Coffee, Linseed, Hazelnut, Euphorbia, Pumpkin seed, Sesame
Safflower, Rice, Sunflower, Peanut, Tung oil tree, Jatropha, Macadamia nut
Brazil nut, Avocado, Coconut, Macuba palm

Oil Exploration and Production in the Marine Environment

http://earthsci.org/mineral/energy/gasexpl/exproil.html  adap
ted to HTML from Australian Institute of Petroleum with permission

Australia's marine environment is special in many ways - it covers an enormous area, over one and a half times larger than Australia's land surface; it extends from the tropics to Antarctica. It includes extensive submarine environments including sea grass beds and unique coral reef systems which support an array of marine creatures from whales, dugongs, dolphins and seals to thousands of species of fish, shellfish, and a myriad of microscopic organisms. According to the Federal Environment Department (State of the Marine Environment Report 1995) our marine environment is in very good condition.

The petroleum industry shares the community's concern for the protection of the marine environment. Conserving biological diversity and maintaining ecological processes and systems are among the core objectives of ecologically sustainable development which have been endorsed by the petroleum industry. The responsible development of petroleum resources from offshore areas is consistent with achieving these objectives. Petroleum resources are not easy to find, nor are they often located in convenient places for oil or gas to be extracted, processed and sent to be used by the community. Most of Australia's petroleum production comes from offshore wells. Exploring for oil and gas under the sea bed, and the production activities which follow a successful exploration program, all involve some risks and potential impacts on the marine environment. Clearly identifying these risks and impacts and developing detailed management plans to avoid, prevent or minimise them is a vital and integral part of planning these exploration and production activities.

 An independent review by eminent scientists of the environmental impacts of offshore oil and gas exploration and production, commissioned by APPEA in 1992, concluded that the Australian offshore petroleum industry has had no significant effects on the marine and coastal environment in over twenty-five years of operation. The industry is committed to maintaining this record and ensuring that the marine environment in which it operates is well managed and able to be enjoyed by future generations, long after the petroleum industry has completed its work. Government approval to explore and produce petroleum
Petroleum, like other mineral resources under the ground, is owned by the Crown, that is Governments own them on behalf of the community. Governments allow companies to explore and produce oil and gas under strict conditions and in return receive all the information collected about the resources and a large share of the pre-tax profits. Currently well over half of the pre-tax profit) from the sale of the petroleum is returned to the government via taxation.

State and Territory Governments are responsible for managing and regulating most activities, including petroleum exploration and production within 3 nautical miles (5.6km) of their coasts. The Federal Government is responsible for the area from 3 -200 nautical miles off the coast (out to the extent of our Exclusive Economic Zone - defined by the United Nations Convention on the Law of the Sea). Similar legislation is implemented by all Australian governments to regulate activities associated with petroleum exploration and production. The key law for offshore activities is the Petroleum (Submerged Lands) Act 1967, but there are many other Acts that can affect industry operations includingthe Endangered Species Act 1992, Environment Protection (Impact of Proposals) Act1974 , Sea Installations Act 1987, Whale Protection Act 1980, Protection of the Sea (Prevention of Pollution from Ships) Act 1983 and variousState/Territory and Commonwealth Environment Protection Acts. The Industry's Code of Environmental Practice lists almost 80 main Acts that potentially affect environmental management planning.
These laws are aimed at protecting one or more aspects of the marine environment, including cultural and historic values, as well as biodiversity and air and water quality. Controls are placed on all aspects of offshore operations, and licences defining limits are required for various discharges. Strict limits are imposed on discharges to the air and ocean environment.
Types of risks and potential impacts

The industry recognises that various risks and consequences are associated with petroleum exploration and production activities. These are carefully identified and minimised as activities may take place in, or near, environmentally important areas. Environmental impact assessments are undertaken to identify areas of environmental concern and provide the basis for the development and implementation of an environmental management strategy. Baseline studies are usually conducted to accurately describe the environment before any work commences. Direct and indirect environmental effects are monitored. Direct effects are those which may affect the ecology of a particular site or area and whose source is easily identified, while indirect impacts are those which do not affect a localised area (Table 1). The risk and consequence of oil spills is of greatest environmental concern however, dredging, the physical effects of equipment and ship movement including anchoring, drilling, routine discharges including kitchen wastes, noise, artificial lights, and air emissions are all matters that are carefully considered. Table 1: Management of Direct and Indirect Environmental Impacts
 


Direct Potential Impact or Risk Indirect Potential Impact or Risk Comment
Ship movements
The risk of an oil spill is directly related to: a) frequency of ship movement;
b) physical and mechanical condition of a ship and its equipment; and 
c) performance of crews.
Oil spill risk is minimised through achieving appropriate standards and adequate training.
Impacts of an oil spill may be severe on sensitive organisms and/or habitats.
In the event of an oil spill, sophisticated oil spill contingency plans aim to prevent, contain and minimise impacts.
Open ocean impacts likely to be less than coastal impacts.
Dredging navigation channels, if necessary, may disturb and modify the sea floor. Dredge spoil is dumped under permit in locations of minimal impact.
Noise, lights and physical presence of ships may affect the movement of sensitive species. Effects are of short duration and impacts are likely to be minimal.
Seismic surveys
Air based energy sources in seismic arrays generate sounds and may have potential impacts on organisms within range. To avoid adverse impacts, surveys are adapted or scheduled to avoid seasonal migrations or key breeding locations.
Avoidance behaviour by some species may affect feeding. Impacts are likely to be of short duration
APPEA is funding a 3 year research project commencing in 1996 to provide better information on potential impacts and environmental effects in Australian conditions 
Drilling rig placement
Physical placement of drilling rig may cause localised damage, depending on the nature of the sea floor, however the area, if affected, is very small. 

Anchoring
Localised physical damage may be observed.
Minimised by avoiding seabed structures of environmental or other significance.
Drilling
When drill cuttings are discharged overboard impacts are limited to the immediate area surrounding the drill site. Drilling fluids are comprised of clays, and include metals such as barium, and a range of additives depending on the type of rock being drilled.
Harmful constituents are generally recycled or removed before discharge to the ocean.
Monitoring of drilling impacts reveals only minor adverse impact beyond the immediate discharge zone.
Suspended sediment in the water column may reduce the amount of light reaching the sea floor. This may reduce plant growth until the particulate material settles. Effects of short duration.
Localised effects may be impact on the food chain. Such effects can be minimised by reducing levels of toxic components, and/or removing or recycling fluids before discharge.
Generally, no toxic oil-based drilling fluids are used in Australia, hence discharges of these substances to the marine environment are very rare. Drilling is undertaken for a relatively short period of an oil filed operation, eg. 3 months to 3-4 years.
Ocean environments facilitate the rapid dispersion, resulting in minimal seabed impact.
In very sensitive environments, waste from drilling operations may be collected and stored onboard for disposal on land.
Platform placement
Habitat disturbance can be minimised through careful placement. A site is chosen after an environmental impact assessment has been undertaken.  Platforms often attract marine life and can act as artificial reefs. They often become important resting points for seabirds and seals.
Produced formation water (PFW)
Hydrocarbon traces in PFW may have localised impacts. Although PFW is of low toxicity, it is often warmer than the ocean when discharged and may cause possible local effects when organisms make inadvertent contact.
Cumulative and/or sublethal impacts may occur from long exposure to low levels of particular hydrocarbons. PFW may have a salt content greater or less than sea water causing localised transient salinity levels which are unlikely to affect nearby organisms.
Low regulatory limits for hydrocarbons and rapid dispersion ensures that impacts are within metres of discharge. APPEA is funding a 2 year research project to assess and improve current management practices for PFW discharge.
Reinjection
Reinjection of water or gas down wells is sometimes used to increase the amount of oil recovered.  Reinjection of gas decreases the volume of gas that might be otherwise flared (reducing emissions of greenhouse gases).  Reinjection of gas or water is costly but where possible, is often a more environmentally sound option than discharge to the environment. 
Sewage
Increased nutrient content in the water column. May increase population numbers of some organisms. Quantities are small and treated before discharge. Dispersion rapidly dilutes any effect.
Greenhouse gas emissions
Negligible Contributes to global greenhouse concentrations. Exploration and production activities contribute less than 3% of Australia's total greenhouse gas emissions.  Minimised through careful management of sources, including power generating equipment, flaring and fugitive fuel emissions. APPEA member companies participate in voluntary cooperative action to minimise avoidable greenhouse gas emissions. 
Oil spills
May have toxic and/or smothering effects for some species on contact. Most offshore platforms are considerable distances from sensitive species.
A range of safety features such as automatic shut-down valves ensures that the risk of a significant oil spill is extremely small.
Possible impacts on the food chain, as a result of contamination or loss of food sources. However effects are transient. Hydrocarbons are organic compounds and are readily decomposed or used as food sources by some microorganisms.
Most Australian crude oils are light and evaporate readily (adding to the volume of atmospheric greenhouse concentrations), and greatly reduce the likelihood of impacts on sensitive coastal or marine organisms.
The proximity to sensitive species is dependent on the type of oil, currents, and wind. Oil spill risk cannot be eliminated but may be reduced to very low levels. The Australian industry has an excellent record of minimal spills and virtually no impacts over 25 years. APPEA is funding a 3 year research project on the impacts of oils spills on key mangrove species, to recommend improved procedures to protect and enhance recovery of affected mangroves. (NB the few instances of oil spills on mangroves are associated with port and onshore processing rather than exploration and production activities.)


Greenhouse

Exploration and production activities result in the release or emission of several greenhouse gases, notably carbon dioxide and methane. Small quantities of other gases such as the hydrocarbons propane and butane, and other products of fuel combustion are also released. The industry recognises the need to carefully manage and reduce the levels of emissions, and is participating in the Federal Government's Greenhouse Challenge program to voluntarily address the issue of emissions. Greenhouse gases are those gases suspected of contributing to global warming in the lower atmosphere (Table 2). The primary greenhouse gas emitted by human activities in Australia is carbon dioxide from energy use, including transport and industrial processes, land use change and forestry and energy production. The main sources of methane emissions in Australia are coal mining, agriculture, decomposing wastes and energy production.
Table 2: Greenhouse Gases
 


Greenhouse Gas Description
Carbon dioxide
(CO 2 ) 
CO 2 is the dominant greenhouse gas in Australia and effectively accounts for about 75% of all greenhouse gas emissions. 
Methane
(CH 4 ) 
CH 4 is a very effective greenhouse gas with a high global warming potential (GWP), and although present at much lower levels than CO 2 may have significant impact because of this higher GWP. The main source of CH 4 is from agriculture (mainly livestock). 
Nitrogen oxides
(NO x )
Nitrogen oxides consist of nitrogen oxide (NO) and nitrogen dioxide (NO 2 ). NO x is a small component of greenhouse emissions (<1%). 
Nitrous oxides
(N 2 O)
N 2 O is a gas produced both naturally and by combustion of fuels. The majority of N 2 O (80%) is produced from agriculture. They mostly come from burning fuel (cars and power stations). 
Volatile organic compounds
(VOC's)
Volatile organic compounds are hydrocarbons (excluding methane) which are capable of forming oxidants (particularly ozone) by reactions with nitrogen oxides in the presence of sunlight. Major sources of VOC's are vehicles, solvents and process industry emissions. 
Carbon monoxide
(CO)
CO is generated as a result of incomplete combustion(eg poorly maintained wood heaters and cars), and reacts preferentially with naturally occurring hydroxyl radicals in the lower atmosphere. This has the effect of increasing the lifetime of VOC's and so enhances the formation of photochemical smog (largely ozone). 
Hydrogen sulphide
(H 2 S)
H 2 S is a toxic gas occurring naturally during decomposition. Natural gas is normally treated to remove this H 2 S to form sulphur or it can be burned. H 2 S forms SO 2 during the combustion process or photochemically when released to the atmosphere. 
Sulphur dioxide
(SO 2 )
SO 2 results in dry acid deposition and in the formation of acid rain thereby increasing the acidity of soils. This is a major problem in the Northern hemisphere, but is not a significant pollutant in Australia except in a few instances. 

Atmospheric releases from oil and gas production activities are attracting increasing interest from both industry operators and regulatory authorities. Concerns focus on the contribution from industry sources to national emissions.
Growth in Australia's emissions in the past few years has principally been because of growth in the economy and population growth which have been higher in Australia than the rest of the developed countries. Australia's greenhouse gas emissions are about 1.5% of the annual global total, and the underlying rate of growth of emissions annually is little more than one per cent.
An inventory of greenhouse gas emissions from flaring, venting and fuel consumption in the Australian exploration and production industry reveals that approximately 50% of emissions are sourced from fuel consumed in the machinery and equipment used to produce petroleum.
Oil and gas explorers and producers are actively identifying where, and how much, greenhouse gas emissions are produced in their operations. Efforts are being made across the industry to reduce these emissions through measures that are technically and economically possible.
Natural gas is one of the cleanest fuels to use to produce heat and electricity and its use is growing in Australia, replacing other energy sources. This growth in gas use means that emission from gas explorers and producers are likely to increase. The net effect for Australia is positive, as switching to natural gas means less emissions overall.


Figure 1: Sources of Greenhouse Gas Emissions in Australia by Sector



Figure 2: Sources of Carbon Dioxide (CO 2 )
Emissions from the Australian Petroleum Industry (3% of Australian Emissions)



Figure 3: Sources of Methane (CH 4 )
Emissions from the Australian Petroleum Industry (3% of Australian Emissions)



Decommissioning

Decommissioning of offshore production facilities has recently become a topical issue. As a producing field reaches the end of its operational life, several options are available for the removal and disposal of redundant facilities. The extent to which offshore petroleum facilities must be removed is determined by the responsible Government authority on case by case basis. Although the responsibility for decommissioning lies with the operators, government departments have a role in ensuring the acceptability of any removal program. Under the guidelines developed by the International Maritime Organisation (IMO) there are specific requirements depending on the water depth, weight of structure and date of construction. Various options are recognised for the removal and disposal process: Complete removal requires that no debris remain above the mudline at the platform site and the sea bed is returned to its natural state.
Partial removal is restricted to structures on which the entire base may be left in place. The requirement under the IMO guidelines is to remove all components of the structure to a minimum depth of 55 metres below the surface to ensure safe navigation in the waters above.
In situ toppling is only feasible in deep water, where it does not pose a hazard for navigation and fishing. Hazardous material and equipment which can be reused is transported onshore. The platform is toppled using explosives, or by underwater cutting of the supports.
Alternative uses : several alternatives for decommissioning exist including:
  • Artificial reefs : the facility may be placed as artificial reefs in selected areas. Artificial reefs benefit the local ecology by creating additional habitats, which will support marine organisms which previously may not have been able to live there. Artificial reefs can be formed through placement of toppled and partially removed structures. A 'Rigs to reefs' program operates in the Gulf of Mexico, where some 100 platforms have been converted to artificial reefs.
  • Marine research centres : this is an alternative where the facility remains in place, and is used by universities and research institutions for on site studies of the marine environment.
The guidelines issued by the IMO, combined with the Geneva Convention of 1958, the Law of the Sea of 1982 and the London Convention of 1972 provide the major guidance when addressing decommissioning issues. The industry believes that decommissioning options must have regard for a wide range of relevant safety issues, environmental and cost considerations and the interests of other users of the ocean. Each decommissioning case therefore must be considered and decided on its own merits.
top...
It is neither sensible nor practical to rule out offshore disposal of installations until environmental impact and safety assessments have been conducted for the range of options available to individual proposals. In some instances the safest and most environmentally acceptable alternative may be offshore disposal, with decisions being based on objective and scientific evidence, and assessed on a case-by-case basis. Oil spills

The petroleum industry's safety record of handling oil and its products in Australia is excellent and has been maintained throughout the past two decades, with increasing volumes being produced and transported in Australian waters. Oil spills from offshore production have been insignificant, and while there have been some spills arising from shipping accidents, none have had lasting adverse effects on the marine environment. In over 25 years of operation in Commonwealth waters, the petroleum industry has produced nearly 4 billion barrels of oil and only 900 barrels of oil have been spilt (or about 0.00002%).




Statistics show that historically the petroleum industry is directly responsible for a very small proportion of marine oil spills however, the industry does not take the risk or consequences of spills lightly. There are strict regulations and management arrangements governing all aspects of exploration and production activities through to the delivery of refined petroleum products. In addition to the introduction of more rigorous inspections, standards, practices and safeguards on all installations and tanker fleets, the industry has established one of the best equipped marine oil spill response and training centres in the world. If an oil spill does occur off Australia's coastline, the oil industry, in association with government agencies, is well prepared to minimise possible impacts on the environment.
Marine protected areas

A Marine and Estuarine Protected Area (MEPA) is a defined area identified as environmentally significant and is designated by legislation for protection. There are many objectives for which MEPA's may be established, for example, protection of specific endangered species, breeding grounds for migratory species or for the sustainable use of resources. The industry supports the establishment of MEPA's for clearly defined objectives that have been determined on scientific evidence. Protected areas must be actively managed to be effective and achieve the objectives for which they were established. A range of activities, such as oil and gas exploration and production, fishing and tourism, may be permitted in some of the protected areas subject to strict conditions that ensure the management objectives of the MEPA can be achieved. This approach, often called multiple use, represents an important pathway to ecologically sustainable development. The petroleum industry is well aware of its responsibility to protect and preserve the environment in which it operates, wherever this may be - inside or outside a marine protected area. The industry works closely with environmental agencies to ensure that all interests are accommodated and protected.
The offshore continental shelf has the greatest potential for future discoveries of oil and gas. Continuing access to the offshore region for petroleum exploration and production is essential to maintain Australia's energy reserves. Energy supply and the petroleum industry are critical to the future performance of Australia's economy. The industry has significant expertise, and an excellent record, in operating in the marine environment and believes its activities are compatible with the objectives of marine conservation and management, permitting economic development that is sustainable in its environmental impacts.

Groundwater

 http://earthsci.org/education/teacher/basicgeol/groundwa/groundwa.html#WaterQualityandGroundwaterContamination
adapted to HTML from lecture notes of Prof. Stephen A. Nelson Tulane University

 
Groundwater is water that exists in the pore spaces and fractures in rock and sediment beneath the Earth's surface. It originates as rainfall or snow, and then moves through the soil into the groundwater system, where it eventually makes its way back to surface streams, lakes, or oceans.



  • Groundwater makes up about 1% of the water on Earth (most water is in oceans).



  •  


  • But, groundwater makes up about 35 times the amount of water in lakes and streams.






  • Groundwater occurs everywhere beneath the Earth's surface, but is usually restricted to depths less that about 750 meters.





  • The volume of groundwater is a equivalent to a 55 meter thick layer spread out over the entire surface of the Earth.





  • The surface below which all rocks are saturated with groundwater is the water table.





  • The Water Table

    wattab.gif

    Rain that falls on the surface seeps down through the soil and into a zone called the zone of aeration or unsaturated zone where most of the pore spaces are filled with air. As it penetrates deeper it eventually enters a zone where all pore spaces and fractures are filled with water. This zone is called the saturated zone. The surface below which all openings in the rock are filled with water (the top of the saturated zone) is called the water table
    The water table occurs everywhere beneath the Earth's surface. In desert regions it is always present, but rarely intersects the surface.
     
    chwattab.gif
    In more humid regions it reaches the surface at streams and lakes, and generally tends to follow surface topography. The depth to the water table may change, however, as the amount of water flowing into and out of the saturated zone changes. During dry seasons, the depth to the water table increases. During wet seasons, the depth to the water table decreases.
     
     
     

    Movement of Groundwater
    Groundwater is in constant motion, although the rate at which it moves is generally slower than it would move in a stream because it must pass through the intricate passageways between free space in the rock. First the groundwater moves downward due to the pull of gravity. But it can also move upward because it will flow from higher pressure areas to lower pressure areas, as can be seen by a simple experiment illustrated below. Imagine that we have a "U"-shaped tube, filled with water. If we put pressure on one side of the tube, the water level on the other side rises, thus the water moves from high pressure zones to low pressure zones.


    utube.gif

    movement.gif

    The same thing happens beneath the surface of the Earth, where pressure is higher beneath the hills and lower beneath the valleys
       The rate of groundwater flow is controlled by two properties of the rock: porosity and permeability.


    Porosity is the percentage of the volume of the rock that is open space (pore space). This determines the amount of water that a rock can contain.

    In sediments or sedimentary rocks the porosity depends on grain size, the shapes of the grains, and the degree of sorting, and the degree of cementation.

    pores.gif
    Well-rounded coarse-grained sediments usually have higher porosity than fine-grained sediments, because the grains do not fit together well.

    poorsort.gif
    Poorly sorted sediments usually have lower porosity because the fine-grained fragments tend to fill in the open space.

    cemented.gif
    Since cements tend to fill in the pore space, highly cemented sedimentary rocks have lower porosity.
     

    igmettext.gif
    In igneous and metamorphic rocks porosity is usually low because the minerals tend to be intergrown, leaving little free space. Highly fractured igneous and metamorphic rocks, however, could have high porosity


    Permeability is a measure of the degree to which the pore spaces are interconnected, and the size of the interconnections. Low porosity usually results in low permeability, but high porosity does not necessarily imply high permeability. It is possible to have a highly porous rock with little or no interconnections between pores. A good example of a rock with high porosity and low permeability is a vesicular volcanic rock, where the bubbles that once contained gas give the rock a high porosity, but since these holes are not connected to one another the rock has low permeability.
    molecattr.gif
    A thin layer of water will always be attracted to mineral grains due to the unsatisfied ionic charge on the surface. This is called the force of molecular attraction. If the size of interconnections is not as large as the zone of molecular attraction, the water can't move. Thus, coarse-grained rocks are usually more permeable than fine-grained rocks, and sands are more permeable than clays.


    Movement in the Zone of Aeration
    Rainwater soaks into the soil where some of it is evaporated, some of it adheres to grains in the soil by molecular attraction, some is absorbed by plant roots, and some seeps down into the saturated zone. During long periods without rain the zone of aeration may remain dry.

    Movement in the Saturated Zone
    In the saturated zone (below the water table) water percolates through the interconnected pore spaces, moving downward by the force of gravity, and upward toward zones of lower pressure. Where the water table intersects the surface, such as at a surface stream, lake, or swamp, the groundwater returns to the surface.
    recharea.gif

    Recharge Areas and Discharge Areas
    The Earth's surface can be divided into areas where some of the water falling on the surface seeps into the saturated zone and other areas where water flows out of the saturated zone onto the surface. Areas where water enters the saturated zone are called recharge areas, because the saturated zone is recharged with groundwater beneath these areas. Areas where groundwater reaches the surface (lakes, streams, swamps, & springs) are called discharge areas, because the water is discharged from the saturated zone. Generally, recharge areas are greater than discharge areas.


    Discharge and Velocity

    hydgrad.gif
    The rate at which groundwater moves through the saturated zone depends on the permeability of the rock and the hydraulic gradient. The hydraulic gradient is defined as the difference in elevation divided by the distance between two points on the water table. Velocity, V, is then:


    V = K(h2 - h1)/L where K is the coefficient of permeability.
    If we multiply this expression by the area, A, through which the water is moving, then we get the discharge, Q.

    Q = AK(h2 - h1)/L,  which is Darcy's Law.
    Springs and Wells
    A spring is an area on the surface of the Earth where the water table intersects the surface and water flows out of the ground. Springs occur when an impermeable rock (called an aquiclude) intersects an permeable rock that contains groundwater (an aquifer). Such juxtaposition between permeable and impermeable rock can occur along geological contacts (surfaces separating two bodies of rock), and fault zones.



    springs.gif

    A well is human-made hole that is dug or drilled deep enough to intersect the water table. Wells are usually used as a source for groundwater. If the well is dug beneath the water table, water will fill the open space to the level of the water table, and can be drawn out by a bucket or by pumping. Fracture systems and perched water bodies can often make it difficult to locate the best site for a well.


    wells.gif

    Aquifers An aquifer is a large body of permeable material where groundwater is present in the saturated zone. Good aquifers are those with high permeability such as poorly cemented sands, gravels, and sandstones or highly fractured rock. Large aquifers can be excellent sources of water for human usage such as the High Plains Aquifer (in sands and gravels) or the Floridian Aquifer (in porous limestones) as outlined in your text. Aquifers can be of two types:


  • Unconfined Aquifers - the most common type of aquifer, where the water table is exposed to the Earth's atmosphere through the zone of aeration. Most of the aquifers depicted in the drawings so far have been unconfined aquifers.







  • Confined Aquifers - these are less common, but occur when an aquifer is confined between layers of impermeable strata. A special kind of confined aquifer is an artesian system, shown below. Artesian systems are desirable because they result in free flowing artesian springs and artesian wells.








  • artesian.gif


    Changes in the Groundwater System When discharge of groundwater exceeds recharge of the system, several adverse effects can occur. Most common is lowering of the water table, resulting in springs drying up and wells having to be dug to deeper levels. If water is pumped out of an aquifer, pore pressure can be reduced in the aquifer that could result in compaction of the now dry aquifer and result in land subsidence. In some cases withdrawal of groundwater exceeds recharge by natural processes, and thus groundwater should be considered a non-renewable natural resource.

    Water Quality and Groundwater Contamination
     Water quality refers to such things as the temperature of the water, the amount of dissolved solids, and lack of toxic and biological pollutants. Water that contains a high amount of dissolved material through the action of chemical weathering can have a bitter taste, and is commonly referred to as hard water. Hot water can occur if water comes from a deep source or encounters a cooling magma body on its traverse through the groundwater system. Such hot water may desirable for bath houses or geothermal energy, but is not usually desirable for human consumption or agricultural purposes. Most pollution of groundwater is the result of biological activity, much of it human. Among the sources of contamination are:


  • Sewers and septic tanks






  • Waste dumps (both industrial and residential)






  • Gasoline Tanks (like occur beneath all service stations)





  • Biological waste products - Biological contaminants can be removed from the groundwater by natural processes if the aquifer has interconnections between pores that are smaller than the microbes. For example a sandy aquifer may act as a filter for biological contaminants.





  • Agricultural pollutants such as fertilizers and pesticides.





  • Salt water contamination - results from excessive discharge of fresh groundwater in coastal areas.








  • saltwater.jpg


    Geologic Activity of Groundwater


  • Dissolution - Recall that water is the main agent of chemical weathering. Groundwater is an active weathering agent and can leach ions from rock, and, in the case of carbonate rocks like limestone, can completely dissolve the rock.







  • Chemical Cementation and Replacement - Water is also the main agent acting during diagenesis. It carries in dissolved ions which can precipitate to form chemical cements that hold sedimentary rocks together. Groundwater can also replace other molecules in matter on a molecule by molecule basis, often preserving the original structure such as in fossilization or petrified wood







  • caveformation.gif

    Caves and Caverns - If large areas of limestone underground are dissolved by the action of groundwater these cavities can become caves or caverns (caves with many interconnected chambers) once the water table is lowered. Once a cave forms, it is open to the atmosphere and water percolating in can precipitate new material such as the common cave decorations like stalagtites (hang from the ceiling), stalagmites (grow from the floor upward), and dripstones, and flowstones.
     
     
    sinkhole2.gif
    Sinkholes - If the roof of a cave or cavern collapses, this results in a sinkhole. Sinkholes, likes caves, are common in areas underlain by limestones. For example, in Florida, which is underlain by limestones, a new sinkhole forms about once each year, gobbling up cars and houses in process.
    Karst Topography - In an area where the main type of weathering is dissolution (like in limestone terrains), the formation of caves and sinkholes, and their collapse and coalescence may result in a highly irregular topography called karst topography
     
    Factories and underground storage tanks are a source of groundwater pollutants. If a tank with a water soluble liquid leaks the liquid travels down to the water table. It then dissolves in the groundwater.  These pollutants flow as a plume along with the groundwater. They can pollute wells and surface water fed by the groundwater along the plume path.
    If the liquid that leaks is less dense than water, it floats on top of the groundwater table. Some of the liquid will evaporate, traveling upwards to the surface in the form of vapor fumes. Some of the liquid will dissolve and travel as a plume in the groundwater.
    If the chemical is not very soluble in water the major part of the liquid will float on the groundwater and flow along with the groundwater.
    Liquids that are denser than water sink through the groundwater until they reach an aquitard. They then move along the top of the aquitard along with the groundwater.
    Cemeteries are another source of pollution for groundwater. They are often located at the top of  hills, and are thus upgradient from the local groundwater flow. Decomposing bodies within the cemetery release bacteria, breakdown products from decay and chemicals used for embalming into the local groundwater supply.
            Areas surrounded by the saltwater, need to be concerned about contamination by sea water. Since the specific gravity of fresh water is less than that of salt water (1.0 vs. 1.025), fresh water floats on top of sea water, forming a fresh water lens.


      For every foot of fresh water above the sea level, there are 40 feet of freshwater below sea level. Below the fresh water salt water saturates the aquifer. When you pump out fresh water rapidly, you lower the height of the freshwater in the aquifer forming a cone of depression. The salt water rises 40 feet for ever 1 foot of freshwater depression and forms a cone of ascension. Seawater may eventually enter a well that was once pumping fresh water, making it unusable.



    Contour Exercise
    Where is the Groundwater divide?


    Saturday, March 12, 2011

    Green Architecture

    Arsitektur yang memperhatikan potensi lingkungan

    (artikel koran Sindo by Probo Hindarto)

    http://astudioarchitect.wordpress.com/

    Permulaan tahun baru 2010 ini, saya diberi pertanyaan dari mas Herman dari Koran Sindo tentang tren arsitektur khususnya rumah tinggal pada tahun 2010 ini. Saya berpendapat bahwa tren tahun ini tentunya didasari oleh tren arsitektur yang berkembang pada tahun 2009 akhir. Uniknya, apa yang berkembang saat ini tidak seharusnya hanya berdasarkan tren semata, karena justru dari sini bisa kita lihat masyarakat makin menyadari pentingnya arsitektur yang ramah lingkungan. Karya arsitektur rumah tinggal yang banyak diminati adalah yang memperhatikan potensi lingkungan, menunjukkan kesadaran arsitek dan masyarakat tentang desain hijau yang mutakhir.

    Dalam Koran Sindo: Arsitektur Tropis Cenderung Ramah Lingkungan

    TREN desain rumah selalu didasari pergerakan pasar karena tren memang sering kali diusung untuk menjawab kebutuhan pasar. Seperti fashion,tren desain arsitektur selalu berganti-ganti dan tidak tetap, meskipun sebenarnya tidak selalu dibutuhkan. Itu karena memang merupakan faktor tambahan dalam desain arsitektur yang sesungguhnya. Banyak orang menyukai tren arsitektur karena dipandang bisa meningkatkan citra bangunan, terutama rumah tinggal. Beruntung bahwa tren yang sedang berjalan saat ini menuju pada pergerakan positif pada upaya pelestarian, pemanfaatan secara efektif dan pemeliharaan lingkungan.
    Hal ini didasari keadaan dan kondisi bumi yang makin terpengaruh pemanasan global yang banyak memicu kesadaran arsitek untuk menciptakan desain arsitektur yang ramah lingkungan. Arsitek dari astudioarchitect Probo Hindarto menjelaskan, kesadaran akan lingkungan dalam rumah yang baik sudah makin dimiliki masyarakat.Konsep arsitektur tropis yang ramah lingkungan dan sesuai untuk orang Indonesia mulai diminati kembali dengan sentuhan lebih modern.

    Dalam hal ini, tetap stylish dengan gaya modern, tapi juga hijau. Arsitektur yang tren sesaat seperti Spanyol, Mediterania atau minimalis dipandang bukan lagi tren arsitektur rumah yang esensial karena hanya merupakan tren tampilan rumah saja,tapi belum menyentuh konsep ruang yang merupakan esensi arsitektur terpenting. Desain arsitektur tropis menjadi tren karena didasari kesadaran dalam dunia desain,terutama oleh para arsitek,ilmuwan dan pencinta lingkungan hidup untuk menggunakan desain yang ramah lingkungan, hijau, dan berkelanjutan.
    Konsep ini lebih didasari oleh kesadaran, karena itu dengan adanya kesadaran untuk arsitektur yang lebih hijau dan berwawasan lingkungan.” Hal ini berarti kesadaran masyarakat dan para praktisi arsitek pada umumnya sudah meningkat daripada sekedar membuat desain bangunan yang tidak berwawasan lingkungan,” jelas dia saat dihubungi Seputar Indonesia. Ciri khas desain arsitektur tropis ini adalah memanfaatkan sumber daya alam yang ada dengan baik.Sehingga meminimalkan kerusakan lingkungan akibat desain arsitektur.

    Beberapa contoh aplikasi desain yang ‘hijau’.Misalkan saja sinar atau cahaya matahari untuk mengurangi atau menghilangkan pemakaian listrik untuk penerangan buatan. Berbagai trik desain seperti atap yang tinggi,ventilasi yang baik, unsur tanaman dan perkerasan di sekitar rumah menjadi pendukung untuk konsep ini. Selain itu, penghawaan alami yang didukung oleh desain yang tidak memerlukan AC atau penghawaan buatan,karena sudah terasa dingin dan sejuk,didukung oleh pelestarian tanah dengan menanam banyak pohon untuk penghijauan.
    ”Lahan yang makin sempit dan mahal harus didesain dengan seksama sehingga tetap memiliki taman yang menyegarkan area rumah,menjadi area peresapan air sehingga mengurangi banjir,” terangnya. Pembangunan yang cenderung vertikal, sehingga makin banyak lahan tersisa untuk penghijauan dan peresapan air tanah.Meskipun tidak memiliki taman di atas tanah, bisa juga menggunakan taman di atas atap dak beton,hal ini juga mulai menjadi tren, sehingga tetap ada area untuk bersantai bagi keluarga menikmati alam.

    Sementara pada unsur tampilan, desain rumah pada 2010 cenderung akan mengadopsi gaya arsitektur modern dan tropis yang banyak menggunakan unsur material ekspos seperti batuan ekspos dan lapisan kayu. Ini membuat tampilannya menjadi makin segar. Sayangnya belum banyak pengembang yang membangun rumah dengan desain seperti itu. Ini karena orientasi pengembang saat ini barangkali masih 90% berorientasi pada keuntungan ekonomis dari penjualan rumah-rumah atau apartemen. Karena itu tren yang ditawarkan perumahan pengembang pada umumnya masih kalah maju selangkah daripada karya arsitek yang sudah memiliki kesadaran itu.
    Hal ini karena arsitek ‘perumahan’ berbeda dengan arsitek independen, dimana arsitek yang independen lebih bisa mengimplementasikan berbagai konsep arsitektur tropis dan hijau tanpa terpengaruh oleh faktor keuntungan. Apabila ada pengembang yang berani menawarkan konsep arsitektur ‘hijau’ yang tidak terpengaruh unsur ekonomis bangunan,maka pengembang ini sudah mengikuti tren dunia yang berkembang saat ini.

    Arsitek dari PT Buanareksa Binaperkasa,Andry Hermawan menjelaskan, tren desain rumah pada 2010 lebih kepada sustainable environment dan ecological issue. Efisiensi biaya dan energi menjadi suatu keniscayaan. Di Indonesia sendiri masih akan menganut minimalis dan tropical design,namun tidak tertutup kemungkinan berkembangnya arsitektur organik. ”Arsitektur vernakular bergaya Sunda dan Bali modern pun semakin dilirik,”ucapnya. (hermansah)
    ________________________________________________


    Rumah bambu bertenaga surya

    Universitas Tonji Shanghai membuat rumah bambu bertenaga surya. Panel surya pada atap dan dinding rumah tersebut menghasilkan daya listrik sebesar 9 kW. Rumah dengan satu kamar tidur dan satu ruang tamu tersebut dirancang dengan menggabungkan arsitektur bangunan khas Cina dan teknologi terkini. Ia memiliki sistem kendali suhu dan kelembaban, sistem isolasi panas, dan taman berdinding bambu.
    [ENGLISH] from Sun-Powered Bambu House Sprouts at Solar Decathlon Europe [Inhabitat]
    solar powered home, renewable energy, off the grid, solar power your home, solar decathalon europe, BAMBU HOUSE, Tonji University Shanghai, bamboo house, sustainable building competition
    Tonji University Shanghai’s Bambu House at the European Solar Decathlon is a beautiful sun-powered abode inspired by nature. It has two elegant sloping roofs and is almost entirely constructed from bamboo. Its impressive solar array generates 9 kilowatts of electricity which powers its one bedroom, one living room layout. We love how the house combines traditional Chinese architecture with state of the art technology — it has temperature and humidity control systems, high-level thermal insulation systems, and a bamboo enclosed garden.


    solar powered home, renewable energy, off the grid, solar power your home, solar decathalon europe, BAMBU HOUSE, Tonji University Shanghai, bamboo house, sustainable building competition
    Tonji University’s team has 20 members and is composed of doctors, postgraduates, and undergraduate students who range across many disciplines — from architecture and urban planning to energy development. They hope that their solar-powered house can help promote their forward-thinking ideas about renewable energy use in residential urban areas. The team has spent six months designing and constructing the house from scratch and they are hoping their hard work will pay off. Structurally, the house is strongly influenced by traditional Chinese architecture but with a tinge of the efficient look of contemporary architecture.
    The Solar Decathlon Europe kicked off with a bang today and Inhabitat is on the scene to provide a first peek at the amazing sun-powered architecture on display. The European Solar Decathlon is the sister of the US Solar Decthalon — which we covered in Washington DC this past October — and was organized in a partnership between Government of Spain’s Ministry of Housing and the United States Government. The decathlon is taking place all through next week in Madrid, so stay tuned to Inhabitat as we bring you a front seat view of all the action!

    Links:
    + Tonji University Shanghai
    + Solar Decathlon Coverage on Inhabitat

    Perubahan Iklim

    Pengertian Iklim dan Perubahan Iklim
    Pada umumnya orang sering menyatakan kondisi iklim sama saja dengan kondisi cuaca, padahal kedua istilah tersebut adalah suatu kondisi yang tidak sama.

    Beberapa definisi cuaca adalah :
    • Keadaan atmosfer secara keseluruhan pada suatu saat termasuk perubahan, perkembangan dan menghilangnya suatu fenomena (World Climate Conference, 1979). 
    • Keadaan variable atmosfer secara keseluruhan disuatu tempat dalam selang waktu yang pendek (Glen T. Trewartha, 1980). 
    • Keadaan atmosfer yang dinyatakan dengan nilai berbagai parameter, antara lain suhu, tekanan, angin, kelembaban dan berbagai fenomena hujan, disuatu tempat atau wilayah selama kurun waktu yang pendek (menit, jam, hari, bulan, musim, tahun) (Gibbs, 1987).
    Ilmu yang mempelajari seluk beluk tentang cuaca disebut meteorologi.

    Sedangkan iklim didefinisikan sebagai berikut : 
    • Sintesis kejadian cuaca selama kurun waktu yang panjang, yang secara statistik cukup dapat dipakai untuk menunjukkan nilai statistik yang berbeda dengan keadaan pada setiap saatnya (World Climate Conference, 1979). 
    • Konsep abstrak yang menyatakan kebiasaan cuaca dan unsur-unsur atmosfer disuatu daerah selama kurun waktu yang panjang (Glenn T. Trewartha, 1980). 
    • Peluang statistik berbagai keadaan atmosfer, antara lain suhu, tekanan, angin kelembaban, yang terjadi disuatu daerah selama kurun waktu yang panjang (Gibbs,1987).
    Ilmu yang mempelajari seluk beluk tentang iklim disebut klimatologi.
    Adapun definisi perubahan iklim adalah berubahnya kondisi fisik atmosfer bumi antara lain suhu dan distribusi curah hujan yang membawa dampak luas terhadap berbagai sektor kehidupan manusia (Kementerian Lingkungan Hidup, 2001). Perubahan fisik ini tidak terjadi hanya sesaat tetapi dalam kurun waktu yang panjang. LAPAN (2002) mendefinisikan perubahan iklim adalah perubahan rata-rata salah satu atau lebih elemen cuaca pada suatu daerah tertentu. Sedangkan istilah perubahan iklim skala global adalah perubahan iklim dengan acuan wilayah bumi secara keseluruhan. IPCC (2001) menyatakan bahwa perubahan iklim merujuk pada variasi rata-rata kondisi iklim suatu tempat atau pada variabilitasnya yang nyata secara statistik untuk jangka waktu yang panjang (biasanya dekade atau lebih). Selain itu juga diperjelas bahwa perubahan iklim mungkin karena proses alam internal maupun ada kekuatan eksternal, atau ulah manusia yang terus menerus merubah komposisi atmosfer dan tata guna lahan.

    Istilah perubahan iklim sering digunakan secara tertukar dengan istilah ’pemanasan global’, padahal fenomena pemanasan global hanya merupakan bagian dari perubahan iklim, karena parameter iklim tidak hanya temperatur saja, melainkan ada parameter lain yang terkait seperti presipitasi, kondisi awan, angin, maupun radiasi matahari. Pemanasan global merupakan peningkatan rata-rata temperatur atmosfer yang dekat dengan permukaan bumi dan di troposfer, yang dapat berkontribusi pada perubahan pola iklim global. Pemanasan global terjadi sebagai akibat meningkatnya jumlah emisi Gas Rumah Kaca (GRK) di atmosfer. Naiknya intensitas efek rumah kaca yang terjadi karena adanya gas dalam atmosfer yang menyerap sinar panas yaitu sinar infra merah yang dipancarkan oleh bumi menjadikan perubahan iklim global (Budianto, 2000).

    Meskipun pemanasan global hanya merupakan 1 bagian dalam fenomena perubahan iklim, namun pemanasan global menjadi hal yang penting untuk dikaji. Hal tersebut karena perubahan temperatur akan memperikan dampak yang signifikan terhadap aktivitas manusia. Perubahan temperatur bumi dapat mengubah kondisi lingkungan yang pada tahap selanjutkan akan berdampak pada tempat dimana kita dapat hidup, apa tumbuhan yang kita makan dapat tumbuh, bagaimana dan dimana kita dapat menanam bahan makanan, dan organisme apa yang dapat mengancam. Ini artinya bahwa pemanasan global akan mengancam kehidupan manusia secara menyeluruh.

    Studi perubahan iklim melibatkan analisis iklim masa lalu, kondisi iklim saat ini, dan estimasi kemungkinan iklim di masa yang akan datang (beberapa dekade atau abad ke depan). Hal ini tidak terlepas juga dari interaksi dinamis antara sejumlah komponen sistem iklim seperti atmosfer, hidrofer (terutama lautan dan sungai), kriosfer, terestrial dan biosfer, dan pedosfer. Dengan demikian, dalam studi-studi mengenai perubahan iklim dibutuhkan penilaian yang terintegrasi terhadap sistem iklim atau sistem bumi.

    sistem-iklim
    Gambar 1 : Sistem iklim

    Sumber : http://www.ncdc.noaa.gov/paleo/ctl/about1a.html