Soil

Surface-water-gley developed in glacial "till", Northern Ireland.

Loess field in Germany (loess is wind-blown dust that is mostly silt)

A, B, and C represent the soil profile; A is the topsoil; B is a loose soil; C is weathered rock; the bottom-most layer is the bedrock.

Soil is loose stuff which lies on top of the land. It has many things in it, like tiny bits of rock, minerals, water and air. Soil also has living things and dead things, called organic matter.

Soil is important for life on Earth because soil holds water and nutrients. It is a very good place for plants to grow. Soil holds the roots, and lets plants stand above the ground to collect the light they need to live. Almost as important are the fungi. There are fungi which grow into plant roots, a symbiosis known as mycorrhiza. This helps trees grow. There are many other fungi that live by breaking down dead organic material: the remains of other living things. The broken down material is a main source of plant nutrients. The soil also has many microorganisms living in it. Many of them eat the organic material in the soil. They use oxygen and release carbon dioxide. They also release mineral nutrients into the soil.

Many animals dig into the soil and make the soil their home. The large animals use soil to make dens for sleeping and giving birth. The small animals live most of their life in the soil. Earthworms are famous for improving soil. This is because the holes they make let air go into the soil. The holes also let water go through.

Soil is different in different places on Earth. This is because the climate and rocks in the Earth are different in different places on Earth. Soils are usually thicker in places where ice sheets covered the land during the Pleistocene ice ages. This is because the ice sheets ground the rock into powder as they slowly moved over the surface.

What is soil

Soil is made of four things.

1. Rock pieces and the rocks are made of minerals,
2. dead and living things (organic matter, humus),
3. water (soil moisture),
4. air.

Components of a loam soil by percent volume      Water (25%)     Gases (25%)     Sand (18%)     Silt (18%)     Clay (9%)     Organic matter (5%)

Soil has rock pieces made small by wind and rain and sun and snow. The rocks are made of minerals and some of the minerals dissolve in water. Some of the minerals dissolved in water can be used as food by plants. Soil also has dead and living things (organic matter) in it. When a plant dies, it is eaten by animals including bacteria in the soil. When the bacteria are done eating, what is left behind is called humus. When the bacteria die the plant food (minerals) goes back into the soil. A food for plants is called a "plant nutrient". There are many kinds of plant nutrients.

Water can enter the gaps in the soil. Half of the soil is gaps filled with water and air. Water in soil is called soil moisture. Plants drink the water and the minerals in the water. Plant roots need air to live. If plant roots do not have air, the roots will die. If the plant roots die, the plant will die. A plant that dies is eaten by bacteria and becomes plant nutrients again.

There are many kinds of soil. Each kind of soil has big and small rocks in it and some humus. If rocks in a soil are as big as your fingers, we call those rocks "gravel". Smaller rocks are called sand. Very small rocks are called silt. Very, very small rocks are called clay. You can see sand with your eye. Sand feels rough between your toes. Silt rock is very small and you must use a lens to see silt. Silt rock is smooth between your toes. Clay rock is too small to see with a lens. To see the smallest things you must use a big microscope. You must use a big microscope to see clay too. Clay rock feels slippery between your toes. Most soils contain all kinds of small rocks. The three best rocks for making soil are sand, silt, and clay.

Soil texture

Every soil has different amounts of sand and silt and clay. The mix of sand and silt and clay is the "texture" of the soil. We can also say the mix has a "soil texture". A soil with a lot of sand is called a "sandy soil texture". A soil with a lot of silt is called a "silt soil texture". A soil with a lot of clay is called a "clay soil texture". Farmers like to grow food in the best soil. The best soil is half sand and some silt and a little clay. The organic matter found in the soil is not counted in the soil texture. Only the rocks are counted when we discover the soil texture. Soil texture is very important.

Clay and humus are special parts of the soil. They help keep water and plant food (plant nutrients) in the soil. Water and plant nutrients stick to clay and humus. Water sticks to all of the rock in the soil. But, water sticks best to clay. Water is taken into (absorbed) into humus like a sponge absorbs water. Humus holds a lot of water and plant nutrients. Clay and humus keep water and plant nutrients in the soil. Sand will hold only a little water in the soil. If the soil has too much sand, the water will flow down into the earth. The water that flows down takes plant nutrients down too. The plant roots can not get at water and plant nutrients if they go too deep. It is best for soil to have a little bit of clay and humus in it for growing plants.

Soil structure (clumps)

The smallest parts of soil are sand and silt and clay. Those small parts join to make larger parts we call "clumps" or "aggregates". The clumps are made when sand and silt and clay stick together. The humus and clay and minerals in the soil are like glue. The glue sticks the sand and silt and clay together and makes clumps. The clumps make shapes by themselves. Some soils have small round clumps. Other soils have large, hard and flat clumps. The soil with small round clumps is best because it lets in air and water. A little glue is best. If the soil has only a little glue there will be space for water and air and the soil will be soft. If the soil has too much glue the soil will be hard. If the soil has no glue, there will be no space in the soil for air and water. A soil with no spaces is not healthy. Worms in the soil make a slippery glue. When worms make holes in the soil they leave some glue in the soil. Plant roots also make spaces in the soil. When the roots die they leave holes in the soil.

Soil horizons (layers)

Soil horizons are caused by combined biological, chemical and physical effects

A soil has a "soil texture" (sand and silt and clay) and it has organic matter mixed in it. But weather changes the soil. It is cold on the Earth near the north and south poles. It is hot near the equator of the Earth. Some places on Earth get a lot of rain and some places get no rain. Hot and wet weather make one kind of soil. Cold and dry weather make another kind of soil. Rain water makes small things in the soil move down with the water. When the things in the water get stuck in the soil those things make a layer in the soil. If you dig down into the soil you may find many layers in the soil. The layers may have different colors. The layers may have different "soil textures". The top part of the soil may have a lot of humus and sand. Below that layer there may be a layer of silt. Below that layer there may be a layer of clay.

The sand stays on the top because it is large. The silt goes down a little with the water and makes a layer because it is small. The silt is smaller than some of the spaces in the soil. The clay can go down even lower with the water because it is the smallest. The sand will make one layer, the silt will make another layer and the clay will make another layer. The humus can move down with the water and make a layer too. The silt and clay and humus can move down because of the spaces in the soil. But, the silt, clay, and humus will fill the spaces in the soil. When the spaces in the soil are closed, it makes it hard for air to go into the soil. Plant roots do not go where there is no air. When we dig down we find layers in the soil.

We call those layers "soil horizons". The top horizon may be an inch (25mm) thick. We call that layer the "O" horizon or sometimes "topsoil". The next layer (horizon) is the "B" horizon. The next lower layer of soil is the "C" horizon. The bottom layer has many rocks and may be called the bedrock or "R" horizon for "rock". Deep down, there is always bedrock. But you may have to dig down a mile (a km) or more. When the soil dries, the soil may shrink and cracks will form in the soil. The soil in the top layer may fall down into the cracks. This causes the layers of soil to be changed because they are mixed. There may be many types soil where you live or only one type of soil. Different rocks make different soil textures. Different weather makes the different soil textures different. And so, there are different soils all over the world.

Soil carbon

People want to keep carbon in the soil, because when it is in the air (in carbon dioxide or methane) it makes the world hotter. If people dig or plow too much then carbon can escape from the soil into the air.

Soil Media

• 

  Soil measuring and surveying device

• 

  A soil texture triangle plot is a visual representation of the proportions of sand, silt, and clay in a soil sample.

• 

  Soil erosion, Southfield Days of dry warm south westerly winds and bare fields provide the ideal conditions for windblown soil erosion. The fine particles of sandy soil become airborne and get into everything. Here by Southfield a plantation of young trees is being sand blasted. *Where this soil became airborne 367915

• 

  "Valuable information on conservation buffers is still flowing from Bear Creek in Story County, Iowa. A riparian buffer first established in 1990 on the Ron Risdal farm has been studied extensively for ten years; ten major findings have been gleaned from the research at the site."

Related pages

• Agronomy
• Soil fertility

Other websites

• Short video about soil from The Guardian newspaper