explain different types of soil water
Answers
Explanation:
Soil water is the term for water found in naturally occurring soil. Soil water is also called rhizic water.
There are three main types of soil water - gravitational water, capillary water, and hygroscopic water -
and these terms are defined based on the function of the water in the soil.
Gravitational Water
Gravitational water is free water moving through soil by the force of gravity. It is largely found in the macropores of soil and very little gravitational water is available to plants as it drains rapidly down the water table in all except the most compact of soils.
Capillary Water
Capillary water is water held in the micropores of the soil, and is the water that composes the soil solution. Capillary water is held in the soil because the surface tension properties (cohesion and adhesion) of the soil micropores are stronger than the force of gravity. However, as the soil dries out, the pore size increases and gravity starts to turn capillary water into gravitational water and it moves down.
Capillary water is the main water that is available to plants as it is trapped in the soil solution right next to the roots if the plant.
Hygroscopic Water
Hygroscopic water forms as a very thin film surrounding soil particles and is generally not available to the plant. This type of soil water is bound so tightly to the soil by adhesion properties that very little of it can be taken up by plant roots. Since hygroscopic water is found on the soil particles and not in the pores, certain types of soils with few pores (clays for example) will contain a higher percentage of it.
Explanation:
Soil Types
Soil is a natural resource that can be categorised into different soil types, each with distinct characteristics that provide growing benefits and limitations.
Identifying the type of soil you require for a project is paramount to support the healthy growth of plant life.
Soil can be categorised into sand, clay, silt, peat, chalk and loam types of soil based on the dominating size of the particles within a soil.
Here is a break down of the common traits for each soil type:
Sandy Soil
Sandy soil
Sandy Soil is light, warm, dry and tend to be acidic and low in nutrients. Sandy soils are often known as light soils due to their high proportion of sand and little clay (clay weighs more than sand).
These soils have quick water drainage and are easy to work with. They are quicker to warm up in spring than clay soils but tend to dry out in summer and suffer from low nutrients that are washed away by rain.
The addition of organic matter can help give plants an additional boost of nutrients by improving the nutrient and water holding capacity of the soil.
Clay Soil
Clay Soil
Clay Soil is a heavy soil type that benefits from high nutrients. Clay soils remain wet and cold in winter and dry out in summer.
These soils are made of over 25 percent clay, and because of the spaces found between clay particles, clay soils hold a high amount of water.
Because these soils drain slowly and take longer to warm up in summer, combined with drying out and cracking in summer, they can often test gardeners.
Silt Soil
Silt Soil
Silt Soil is a light and moisture retentive soil type with a high fertility rating.
As silt soils compromise of medium sized particles they are well drained and hold moisture well.
As the particles are fine, they can be easily compacted and are prone to washing away with rain.
By adding organic matter, the silt particles can be bound into more stable clumps.
Peat Soil
Peat Soil
Peat soil is high in organic matter and retains a large amount of moisture.
This type of soil is very rarely found in a garden and often imported into a garden to provide an optimum soil base for planting.
Chalk Soil
Chalk Soil
Chalk soil can be either light or heavy but always highly alkaline due to the calcium carbonate or lime within its structure.
As these soils are alkaline they will not support the growth of ericaceous plants that require acidic soils to grow.
If a chalky soil shows signs of visible white lumps then they can’t be acidified and gardeners should be resigned to only choose plants that prefer an alkaline soil.
Loam Soil
Loam Soil
Loam soil is a mixture of sand, silt and clay that are combined to avoid the negative effects of each type.
These soils are fertile, easy to work with and provide good drainage. Depending on their predominant composition they can be either sandy or clay loam.
As the soils are a perfect balance of soil particles, they are considered to be a gardeners best friend, but still benefit from topping up with additional organic matter