5 Soil Formation Factors: Weathering Rocks Into Dirt
For humans, soil formation is vital for food production and plant growth.
Weathering is the long process that breaks rock down into soils. Without it, soil wouldn’t exist.
On top of that, climate, relief, organisms, parent material and time are all factors of soil formation.
So how do soils form? What are the soil formation factors? And most importantly, what is soil?
Soil is loose minerals and organic material
Soils are about half minerals, half-open space – all within the top few centimeters of the surface. It’s often mixed with organic material, sometimes called humus.
Soil texture describes particle size. For soil, it consists of sand, silt and clay. Sand is the largest in particle size. Silt is just sand, but smaller. Finally, clay has even smaller particles than silt.
Because clay is so small, it clump together easily. But sand has larger particles so it doesn’t tend to clump up as much. A loam is a mix of about 40% sand, 40% silt and 20% clay.
Humus is all the organic stuff. Basically, it’s an accumulation of decayed matter such as plants and animals. If you have ever made compost, you are making humus.
There’s different benefits for each type of soil. For example, high organic matter is good for crop production. But soils without humus is good for construction sites.
How weathering drives soil formation
If you start with a big boulder in the ground and leave it there for a long, long time. Over thousands of years, it will break down because of weathering.
Both mechanical and chemical weathering play an important role in soil formation. These processes will transform that boulder into particles of sands, silt and clays.
Soil formation is a function of the following 5 factors:
- Parent material
Soil formation is due to the percolation of water and weathering. This water seepage is what dissolves rocks into soil. As water seeps downwards, it breaks down material.
Eventually, you get a set of “soil layers”. These soil layers are dependent on how far down water seeps into the ground and the amount of weathering.
1 Climate impacts weathering rates
Climate, temperature and water affect how fast chemical weathering occurs. Moist regions experience more chemical weathering because water affects the abundance of chemical reactions.
In addition, both temperature and its rate of change are critical in weathering. Again chemical reactions tend to occur more rapidly when temperatures are higher, especially in moist areas.
2 Organisms decay material into organic matter
As plants die, small organisms break down and decay material into organic matter. During this process, bacteria and plants produce a type of acid. This acid is a big contributor to the breakdown of soil particles.
Next, soil with organic material is most important for humans because it supports plant biomass and agricultural crops. This is the topsoil which takes hundreds of thousands of years to form.
3 Soil inherits its traits from parent material
Soils are derived from its parent material. For example, feldspars go through a chemical process which convert it into clay. But if you have granite with feldspar, it could develop into clay and sand.
As mentioned above, soils can develop from bedrock in one place. But they can also be transported. For example, glaciers, water and wind can move and erode material.
4 Terrain relief affects water availability
The aspect that a hill faces influences the amount of sunlight it receives. If there’s more sunlight, it changes the amount of available water.
At the base of a landform, thicker, hummocky soils tend to form. Gravity moves water downward which is where water accumulates.
5 Weathering duration impacts particle size
Finally, all these factors take a long, long period of time to make a noticeable difference. Soils take thousands of years to form. In general, the longer rocks have the chance to weather, it will result in finer particle sizes.
But the reality is that our environment is constantly in flux. Soil formation factors such as water, organisms and relief is never a constant.