- To learn more about soil, and why it is important
- To use this knowledge to understand human's policies and actions that may have an impact on soil health
We often just think of soil as dirt, and many of us no longer even touch it on a daily basis. We take it for granted. But without soil, humans would not exist.
The soil is the great connector of our lives, the source and destination of all.
(Wendell Berry, 1977)
What is soil?
Soil is the sum of its abiotic and biotic parts -
- mineral particles of different sizes and compositions derived from underlying rock
- mineral particles brought in from outside influences e.g. wind, moving water, animals
- gases and moisture adhering to the other components
- decaying organic matter (humus) - sometimes shortened to OM
- animals, plant roots, microbes and fungi that live among the minerals and humus
Soil particles are aggregated into clumps of varying sizes. These are often called peds. The spaces between them are filled with water and air.
A "standard" composition of soil is shown in the accompanying diagram.
Soil develops over long periods of time. Fundamentally, soil is derived from a so-called parent material, which consists of rocks and minerals that occur within a metre or so of the surface.
Five main interacting factors affect the formation of soil:
- parent material—minerals forming the basis of soil
- living organisms—influencing soil formation by their actions
- climate—affecting the rate of weathering and organic decomposition
- topography—grade of slope affecting drainage, erosion and deposition
- time—influencing soil depth Under temperate conditions, it can take about 20,000 years to create one metre
of soil. (What does this mean in terms of renewability?)
Interactions between these factors produce an infinite variety of soils across the earth’s surface.
What does soil do?
Soil serves several purposes
- a medium to anchor land plants in place
- a source of necessary nutrients for land plant growth
- a home for many species of organisms
- a recycling service for organic matter
- storage of forms of carbon, nitrogen and other elements
- water storage and filtration
The abiotic components
The solid mineral particles in soil (roughly 45%) are classified on the basis of size as sand, silt and clay.
|Particle Size in mm
|0.1 - 1.0
The relative proportions of these particles determines the texture of the soils. The soil texture table is used to relate the % of each particle size grouping to the designated texture.
Most (but not all) crop plants thrive in a loam soil because it retains moisture without getting too soggy and it has adequate mineral nutrition available.
Other properties of soil
Colour is determined by the nature of minerals present. Officially the colour of soil is determined by comparison to colour swatches in a special book called a Munsell chart.
Density is the measured by dividing the weight of a given amount of soil by its volume.
Pore space is that part of the bulk volume that is not occupied by solid matter. It is open space occupied by air and/or water. This air space is needed to supply oxygen to organisms decomposing organic matter, humus, and plant roots. Pore space also allows the movement and storage of water and dissolved nutrients.
Consistency is the ability of soil to stick together and resist fragmentation and deformation. It is of use in predicting cultivation problems and also the engineering of foundations of built structures. The consistency of dry soil ranges from loose to hard, whereas that of wet soil ranges from non-sticky to sticky.
The pH scale is a measure of the acidity or alkalinity. It ranges from 0 most acidic to 14 most alkaline. 7 is regarded as neutral, neither acidic nor alkaline.
Most soils range between 3.5 to 9.5.
Soil salinity is a measure of the salt content of soil. Most commonly, it references table salt (NaCl) but may also refer to other salts.
Soil temperature is an important property that influences soil processes and reactions such as
- water and nutrient uptakes
- microbial activities
- nutrient cycling
- root growth