SOIL FORMATION

CLORPT - for short!

Soils differ from one part of the world to another, even from one part of a backyard to another. They differ because of where and how they formed. Climate, organisms, relief (landscape), parent material and time are five major factors of interaction creating different types of soils.

Climate: Temperature and moisture influence the speed of chemical reactions, which in turn help control how fast rocks weather and dead organisms decompose. Soils develop faster in warm, moist climates and slowest in cold or arid ones.

Rainfall is one of the most important climate factors in soil formation.

Organisms: Plants root, animals burrow, and bacteria eat – these and other organisms speed up the breakdown of large soil particles into smaller ones. For instance, roots produce carbon dioxide that mixes with water and forms an acid that wears away rock. Learn more on our Soil Biology page!

Termites can generate mounds in the soil that are three stories tall!!!

Relief (landscape): The shape of the land and the direction it faces make a difference in how much sunlight the soils gets and how much water it keeps. Deeper soils form at the bottom of a hill because gravity and water move soil particles down the slope.

Soils are different depending on the location in the slope that they are located.

Parent material: Every soil “inherits” traits from the parent material from which it formed. For example, soils that form from limestone are rich in calcium and soils that form from materials at the bottom of lakes are high in clay. Every soil formed from parent material deposited at the Earth's surface. The material could have been bedrock that weathered in place or smaller materials carried by flooding rivers, moving glaciers, or blowing winds. Parent material is changed through biological, chemical and environmental processes, such as weathering and erosion.

These are soils forming in real time from the side of the volcano. They form into rock first, then weather into fertile soil.

Time: All of these factors work together over time. Older soils differ from younger soils because they have had longer to develop. As soil ages, it starts to look different from its parent material. That is because soil is dynamic. Its components—minerals, water, air, organic matter, and organisms—constantly change. Components are added and lost. Some move from place to place within the soil. And some components are totally changed, or transformed.

Who studies about soil and how it forms?

Evaluating a soil profile can tell a lot of stories how soils form, and what they can be used for.

Soil pedologists and morphologists study how different soils form. How do soils form? How is this important for soil management? What impact do humans have on the evolution and formation of soils?

Soil Mapping

Did you know that the soil under your feet has a name (there's an app for that)? Soils, like species, can be identified through a process of taxonomy. Taxonomy groups soils with similar features into the same category. There are over 25,000 different named soils in the US. People who map soils generate digital copies of the world beneath our feet, and draw lines to estimate boundaries between soil with different names. 

This is an example of a soils map over a small area in Wisconsin. The little letter are different soil series

Disturbed Soils

When humans build buildings and roads they change soils, often removing the surface soil and drastically changing the areas. When this change happens, soil formation starts to change. People who study disturbed soils map how these soils respond to human manipulation.

WEATHERING

Weathering is a natural process in the rock cycle that contributes to soil formation. There are two types of weathering; physical and chemical. Physical weathering involves breaking things into smaller pieces; rocks, minerals, and soil particles into smaller particles. No other property of the particle changes. Chemical weathering may change the size of the particle, but also changes one mineral into another, which changes other properties, like color, hardness, and density. The rate of weathering is affected by the type of mineral, climate factors (especially temperature and precipitation) and biological activity.