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Importance & Formation of Soil
Importance of Soil
• Much of the United States’ success is due to the productive capacity of the soil– U. S. produces enough food and fiber for its own use
and exports these commodities to other countries
Importance of Soil
• Habitat for soil organisms• Engineering medium• System for water supply and purification • Original source of most nutrients for plant and
animal life– Provides nutrients for plant growth– Animals get nutrients from plants or from animals
that eat plants
Soil Acts as a Recycling System
Soil Permanence
• Soils appear permanent and unchanging• Actually very dynamic, constantly changing• Changes must balance to maintain
productivity
Soil Formation
• Based on weathering of rocks and minerals• Physical and chemical decomposition break down
rocks and minerals into the mineral matter component of soil
• On average, it takes about 100 years to develop one inch of topsoil
Factors Affecting Soil Formation
• Climate• Living organisms• Parent soil material• Topography• Time
Different combinations of these factors lead to the formation of different soils
Climate
• Refers to the average course of weather at a particular place as exhibited by temperature, wind velocity, and precipitation
• Temperature and precipitation greatly affect the rate of weathering
• Increased temperature causes an increased rate of chemical reaction and increased growth of fungi, soil bacteria and plants
Climate
• Adequate moisture causes an increased rate of chemical reaction and increased growth of fungi, soil bacteria and plants
• Excess moisture retards microbe growth• Water carries minerals and organic matter
downward, forming horizons• High rainfall areas generally have leached,
acidic soils
Average Annual PrecipitationUnited States
Climate
• Low humidity and high winds tend to dry out soils, reducing chemical reaction and microbe growth
Photo courtesy of USDA NRCS
• High winds can cause cause significant erosion on some unprotected soils
Living Organisms
• Bacteria and fungi – break down organic materials
• Insects, “insect-like” creatures, and animals – break down and mix soil materials
• Plants– roots break up mineral matter
• Humans– land clearing and cultivation remove vegetation
and disturb soil structure
Parent Material
• Influences texture, structure,color, and fertility• Clay soils generally form from easily
weathered materials• Sandy soils form from more resistant materials
Topography
• On sloping land, loose material is moved downward by runoff and gravity– breaks up soil materials and deposits them at
lower levels– exposes subsoil materials on upper slopes
• Influences percolation and drainage– sloping land has more runoff and less percolation– low-lying soil may tend to be saturated, leading
to less biologic and chemical activity
Time
• Soils form by chemical and physical weathering of parent material over time– chemical weathering results from chemical
reactions upon soil materials– physical weathering results from mechanical
forces such as freezing and thawing, erosion, and gravitational movements
• Soils age and mature over time
Soil Maturity
• Initially, nutrients are released quickly, plant growth increases, and organic matter accumulates
• Eventually, soluble nutrients are lost through leaching, plant growth decreases, and organic matter is lost
• Fine clay particles move downward from surface• Mature soils gradually decline to lower levels of
production
Variety in Soils
Climate, living organisms, parent material, topography, and time impact soil formation and changes in soil composition.Variations in these factors have resulted in the wide variety of soils that are present today.
ALL RIGHTS RESERVED Reproduction or redistribution of all, or
part, of this presentation without written permission is prohibited.
Instructional Materials ServiceTexas A&M University
2588 TAMUSCollege Station, Texas 77843-2588
http://www-ims.tamu.edu 2006