(A consideration of the natural processes leading to soil formation. The importance of limestone products is considered
Note that sections related to rates of reaction are not included this year) by Mr. Lorimer.
Soil is formed when rocks are weathered into small particles. These particles come together to form soil.
Types of Weathering:
Rocks are weathered into soil, by physical, biological, or chemical weathering. (Exfoliation is another type of weathering but I don't think you don't have to know this one in science, only in geography)
Physical
Physical weathering is when a rock is broken into fragments, but not chemically changed. An example of physical weathering is "freeze-thaw" weathering. When temperature changes, water that goes into cracks in the rock freezes and because water expands when it freezes, it makes the cracks widen. This causes the rock to weaken physically and start to erode.
Chemical
Chemical weathering, is when a rock is broken down because its chemical composition is changed. A common example of this is when rocks are eroded by acid rain (carbonic acid).
Biological Weathering
Biological weathering is when roots of of plants, like trees, grows through large rocks and break them into pieces. You know when you walk down the street, you sometimes see a part of the pavement being pushed up and has cracks all over them because of the roots growing under the concrete right? Thats an example of biological weathering. Usually biological weathering starts when a seed gets into the crack of a rock and starts growing. The seed may get into the rock because of the wind carring the seed, animals carrying them and ejesting them, or a tree near the rock can start growing into the rock. 
Types of Rocks
Rocks are classified into three classes, igneous, metamorphic, and sedimentary rock.
Sedimentary Rocks
Sedimentary rocks are rocks that from when sediment is packed together under ground, over the course of millions of years. An example of a sedimentary rock is limestone, which comes from the bodies of ancient dead sea animals, which have been churned into limestone.
Igneous Rocks
Igneous rock is formed from magma (molten rock) that then cools and recrystallizes again. The most common example of igneous rock, is granite. It forms in the hot soft layer of rock below the lithosphere, which is the outer part of the world.
Metamorphic Rocks
Metamorphic rock is made from a combination of the processes that make igneous and sedimentary rock. It is formed when grains of different rocks are pushed together, circulating water speeds up the reaction, and the pieces of rock melt and recrystalize. Then pressure forces the rocks together to make larger grains, or if pressure mainly omes from two sides, the rocks becomes layered. Some common examples of a metamorphic rock are marble, and shale.
How limestone is formed:
Creatures from the sea often have shells and skeletons made up of calcium carbonate. Over millions of year pressure turns layers of shell and bones fragments into limestone rock. After other millions of years powerful forces raise the seabed and forms montains. This is why limestone is found inland.
Uses:
Crushed limestone is used for:
- extracting iron from iron ore
- making sodium carbonate
- making materials for road building
- making concrete
When limestone is heated it forms quicklime;
Quicklime is used for:
- making steel from iron
- neutralizing acidity in the soil
- industrial drying agent (taking humidity out of chemicals)
When limestone is heated with clay it forms cement.
Cement is:
When crushed limestone is grinded it becomes powdered limestone.
Powdered limestone:
- neutralize acidity in soil
- neutralize acidity in water
- neutralize sulphur dioxide in flue gases from power stations
- making glass
When water is added to quicklime it forms Slaked lime.
Slaked lime produces/makes/does:
- neutralizes acidity in soil in lakes affected by acid rain.
- purifying water
- making mortar
- pottery
- chemicals
- dyes
- solvents
- paints
- medicine
Comments (4)
Julie G. said
at 10:21 am on May 9, 2008
that is not what freeze-thaw is
water goes into holes in the rock and freezes
this causes the water to expand and make the rock crack (so there is a bigger hole)
then more water goes in, freezes, etc. until the rock breaks in half or even more parts
writing this in bullet points would make it easier to reader and less "boring"
(you could list the freeze-thaw thing by steps)
Eric and Antonia said
at 10:25 am on May 9, 2008
adding on to julie's comment you could put this picture in to explain freeze thaw more clearly.
http://www.gly.uga.edu/railsback/1121WeatheringIIIa.jpeg
Simon Lorimer said
at 12:24 pm on May 9, 2008
Good stuff. Could someone add some detail about limestone and it's uses here.
max said
at 3:32 pm on May 17, 2008
good job with the bullet points
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