Soil Type Investigation

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Soil Type Investigation

The aim of the experiment is to establish what types of soil holds the

most water and to see if changing a certain variable such as the ph

value of the water has any effect on how much water each type of soil

will hold.

Background Information

Many factors might affect the absorbency of soil, some affecting only

certain types of soil in particular. For example the obvious

influences such as the amount of soil and the amount of water added to

it will certainly limit how much water the soil can hold and the

amount able to pass through. However, there are also other less

apparent aspects that might also have an effect on the limit of water

different soils can hold. For example the size of the soil particles

might have an influence because if the soil is in large chunks that

leaves gaps in between them then the water may just filter straight

through so little is absorbed by the soil. On the other hand, if the

soil is in a fine grained sand this might trap the water because there

is little space between the particles causing a lot to be absorbed.

Foreign bodies in the soil such as debris, small pieces of litter,

chunks of clay or rocks and even the amount of glass wool used may

also effect the absorbency by either blocking the funnel so that the

outlet is blocked causing the water to be trapped in the filter under

the soil with soil floating on top - though the water is not actually

absorbed, or, if the outlet is not blocked helping the water to drain

easily through the soil so that it hold less.

Another factor which may effect it is the temperature of the water,

according to particle theory, the water particles have more energy and

move faster if the temperature is higher causing more particles from

the surface to escape into the air as they evaporate, thus meaning

that less is held in the soil because it is constantly evaporating at

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