31.2: The Soil

31.2.1: Soil Composition

Learning Objective

Explain soil composition

Key Points

• The chemical composition of the soil, the topography, and the presence of living organisms determines the quality of soil.
• In general, soil contains 40-45% inorganic matter, 5% organic matter, 25% water, and 25% air.
• In order to sustain plant life, the proper mix of air, water, minerals, and organic material is required.
• Humus, the organic material in soil, is composed of microorganisms (dead and alive) and decaying plants.
• The inorganic material of soil is composed of rock, which is broken down into small particles of sand (0.1 to 2 mm), silt (0.002 to 0.1 mm) , and clay (less than 0.002 mm).
• Loam is a soil that is a mix sand, silt, and humus.

Key Terms

loam

soil with no dominant particle size that contains a mixture of sand, silt, and humus

humus

a large group of natural organic compounds found in the soil composed of decaying plants and dead and living microorganisms

Soil Composition

Plants obtain inorganic elements from the soil, which serves as a natural medium for land plants. Soil is the outer, loose layer that covers the surface of Earth. Soil quality, a major determinant, along with climate, of plant distribution and growth, depends not only on the chemical composition of the soil, but also the topography (regional surface features) and the presence of living organisms.

Soil consists of these major components :

Components of soil

The four major components of soil are shown: inorganic minerals, organic matter, water, and air.

• inorganic mineral matter, about 40 to 45 percent of the soil volume
• organic matter, about 5 percent of the soil volume
• water, about 25 percent of the soil volume
• air, about 25 percent of the soil volume

The amount of each of the four major components of soil depends on the quantity of vegetation, soil compaction, and water present in the soil. A good, healthy soil has sufficient air, water, minerals, and organic material to promote and sustain plant life.

The organic material of soil, called humus, is made up of microorganisms (dead and alive), and dead animals and plants in varying stages of decay. Humus improves soil structure, providing plants with water and minerals. The inorganic material of soil is composed of rock, slowly broken down into smaller particles that vary in size. Soil particles that are 0.1 to 2 mm in diameter are sand. Soil particles between 0.002 and 0.1 mm are called silt, and even smaller particles, less than 0.002 mm in diameter, are called clay. Some soils have no dominant particle size, containing a mixture of sand, silt, and humus; these soils are called loams.

31.2.2: Soil Formation

Learning Objective

Describe the five factors that account for soil formation

Key Points

• Parent material is the organic and inorganic material from which soil is formed.
• Climate factors, such as temperature and wind, affect soil formation and its characteristics; the presence of moisture and nutrients is also needed to form a quality soil.
• Topography, or regional surface features, affects water runoff, which strips away parent material and affects plant growth (the steeper the soil, the more erosion takes place).
• The presence of microorganisms in soil creates pores and crevices; plants promote the presence of microorganisms and contribute to soil formation.
• Soil formation takes place over long periods of time.

Key Terms

horizon

a soil layer with distinct physical and chemical properties that differ from those of other layers

bedrock

the solid rock that exists at some depth below the ground surface

rhizosphere

the soil region subject to the influence of plant roots and their associated microorganisms

Soil Formation

Soil formation is the consequence of a combination of biological, physical, and chemical processes. Soil should ideally contain 50 percent solid material and 50 percent pore space. About one-half of the pore space should contain water, while the other half should contain air. The organic component of soil serves as a cementing agent, returns nutrients to the plant, allows soil to store moisture, makes soil tillable for farming, and provides energy for soil microorganisms. Most soil microorganisms, bacteria, algae, or fungi, are dormant in dry soil, but become active once moisture is available.

Soil distribution is not homogenous because its formation results in the production of layers; the vertical section of the layers of soil is called the soil profile. Within the soil profile, soil scientists define zones called horizons: a soil layer with distinct physical and chemical properties that differ from those of other layers. Five factors account for soil formation: parent material, climate, topography, biological factors, and time.

Parent Material

The organic and inorganic material in which soils form is the parent material. Mineral soils form directly from the weathering of bedrock, the solid rock that lies beneath the soil; therefore, they have a similar composition to the original rock. Other soils form in materials that came from elsewhere, such as sand and glacial drift. Materials located in the depth of the soil are relatively unchanged compared with the deposited material. Sediments in rivers may have different characteristics, depending on whether the stream moves quickly or slowly . A fast-moving river could have sediments of rocks and sand, whereas a slow-moving river could have fine-textured material, such as clay.

Soft sediment deformation

Soil distribution is not the same at all depths. The vertical section of soil layers is called the soil profile. The soil profile contains defined zones called horizons whicht have distinct physical and chemical properties that differ from those of other layers. An example is shown here in the soft sediment deformation in the Navajo Sandstone.

Climate

Temperature, moisture, and wind cause different patterns of weathering, which affect soil characteristics. The presence of moisture and nutrients from weathering will also promote biological activity: a key component of a quality soil.

Topography

Regional surface features (familiarly called "the lay of the land") can have a major influence on the characteristics and fertility of a soil. Topography affects water runoff, which strips away parent material and affects plant growth. Steep soils are more prone to erosion and may be thinner than soils that are relatively flat or level.

Biological factors

The presence of living organisms greatly affects soil formation and structure. Animals and microorganisms can produce pores and crevices. Plant roots can penetrate into crevices to produce more fragmentation. Plant secretions promote the development of microorganisms around the root in an area known as the rhizosphere. Additionally, leaves and other material that fall from plants decompose and contribute to soil composition.

Time

Time is an important factor in soil formation because soils develop over long periods. Soil formation is a dynamic process. Materials are deposited over time, decompose, and transform into other materials that can be used by living organisms or deposited onto the surface of the soil.

31.2.3: Physical Properties of Soil

Learning Objective

Describe the physical properties or profile of soil

Key Points

• The O horizon, or topsoil, is made of decaying organisms and plant life; it is responsible for plant production.
• The A horizon is of a mixture of organic material and inorganic products of weathering; it is the beginning of true mineral soil.
• The B horizon, or subsoil, is a dense layer of mostly fine material that has been pushed down from the topsoil.
• The C horizon, or soil base, is located just above bedrock and is made of parent, organic, and inorganic material.

Key Terms

subsoil

dense layer of soil containing fine material that has moved downward; the layer of earth that is below the topsoil

topsoil

top layer of soil containing humus at its surface and decomposing vegetation at its base; the most fertile soil

Physical Properties of the Soil

Soils are named and classified based on their horizons . The soil profile has four distinct layers:

Soil profile

This soil profile shows the different soil layers (O horizon, A horizon, B horizon, and C horizon) found in typical soils.

1. The O horizon has freshly-decomposing organic matter, humus, at its surface, with decomposed vegetation at its base. Humus enriches the soil with nutrients, enhancing soil moisture retention. Topsoil, the top layer of soil, is usually two to three inches deep, but this depth can vary considerably. For instance, river deltas, such as the Mississippi River delta, have deep layers of topsoil. Topsoil is rich in organic material. Microbial processes occur there; it is responsible for plant production.
2. The A horizon consists of a mixture of organic material with inorganic products of weathering; it is the beginning of true mineral soil. This horizon is typically darkly colored because of the presence of organic matter. In this area, rainwater percolates through the soil and carries materials from the surface.
3. The B horizon, or subsoil, is an accumulation of mostly fine material that has moved downward, resulting in a dense layer in the soil. In some soils, the B horizon contains nodules or a layer of calcium carbonate.
4. The C horizon, or soil base, includes the parent material, plus the organic and inorganic material that is broken down to form soil. The parent material may be either created in its natural place or transported from elsewhere to its present location. Beneath the C horizon lies bedrock.

Some soils may have additional layers, or lack one of these layers. The thickness of the layers is also variable, depending on the factors that influence soil formation. In general, immature soils may have O, A, and C horizons, whereas mature soils may display all of these, plus additional layers .

Mature soil

The San Joaquin soil is a mature soil that has an O horizon, A horizon, B horizon, and C horizon.

Attributions

• Soil Composition
  • "OpenStax College, Biology. October 17, 2013." http://openstaxcollege.org/textbooks/biology. OpenStax CNX CC BY-SA 3.0.
  • "humus." http://en.wiktionary.org/wiki/humus. Wiktionary CC BY-SA 3.0.
  • "loam." http://en.wiktionary.org/wiki/loam. Wiktionary CC BY-SA 3.0.
  • "OpenStax College, Biology. November 21, 2013." http://cnx.org/content/m44715/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
  • "OpenStax College, Biology. October 17, 2013." http://cnx.org/content/m44715/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
  • "OpenStax College, The Soil. October 17, 2013." http://cnx.org/content/m44715/latest/Figure_31_02_01.png. OpenStax CNX CC BY 3.0.
• Soil Formation
  • "Boundless." http://www.boundless.com/. Boundless Learning CC BY-SA 3.0.
  • "bedrock." http://en.wiktionary.org/wiki/bedrock. Wiktionary CC BY-SA 3.0.
  • "rhizosphere." http://en.wiktionary.org/wiki/rhizosphere. Wiktionary CC BY-SA 3.0.
  • "OpenStax College, Biology. October 17, 2013." http://cnx.org/content/m44715/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
  • "Soft sediment deformation." http://commons.wikimedia.org/wiki/File:Soft_sediment_deformation.JPG. Wikimedia CC BY-SA.
• Physical Properties of Soil
  • "OpenStax College, Biology. October 17, 2013." http://openstaxcollege.org/textbooks/biology. OpenStax CNX CC BY-SA 3.0.
  • "subsoil." http://en.wiktionary.org/wiki/subsoil. Wiktionary CC BY-SA 3.0.
  • "topsoil." http://en.wiktionary.org/wiki/topsoil. Wiktionary CC BY-SA 3.0.
  • "OpenStax College, Biology. October 17, 2013." http://cnx.org/content/m44715/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
  • "OpenStax College, The Soil. October 17, 2013." http://cnx.org/content/m44715/latest/Figure_31_02_02.png. OpenStax CNX CC BY 3.0.
  • "OpenStax College, The Soil. October 17, 2013." http://cnx.org/content/m44715/latest/Figure_31_02_03.jpg. OpenStax CNX CC BY 3.0.