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Why is a study of soil important?. 90% of the world’s food comes from land-based agriculture. Maintenance of soil is the cornerstone of sustainable civilizations. Simply stated, it is the “foundation” of terrestrial life. Global Trend: Where Did All the Farms Go?.
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Why is a study of soil important? • 90% of the world’s food comes from land-based agriculture. • Maintenance of soil is the cornerstone of sustainable civilizations. • Simply stated, it is the “foundation” of terrestrial life.
Global Trend: Where Did All the Farms Go? • 22% global land for crops grazing and forestry are degraded; reduced potential productivity. • Poor farming practices = loss of soils and farmland. • Erosion • Salinization • Development in United States = loss of 1.4 million acres of farmland per year.
Soil Profile Not all soil under your feet is the same. Soil becomes more mineral and rocky with depth as organic input is at the surface and weathering of bedrock (parent material) at depth. Nutrient content often decreases with depth
Soil Texture • Soil texture refers to the percentage of each type of particle found in the soil. • Loam soil is approximately 40% sand, 40% silt, and 20% clay. Sand (large) 2 - 0.02 mm Silt (small) 0.02 – 0.002 mm Clay (smaller) < 0.002 mm
Soil Texture Classification Feel Your Soil Assignment #7 • Draw three lines as follows: • From %clay value run line parallel to %sand. • From %silt value run line parallel to %clay. • From %sand value run line parallel to %silt E.g. Sandy Clay Loam: 25% clay 15% silt 60% sand
Soil Classes • Mollisols: fertile soils with deep A horizon; best agriculture soils • Oxisols: iron and aluminum oxides in B horizon; little O horizon; Poor agriculture soils • Alfisols: well-developed O, A, E, and B horizons; suitable for agriculture if supplemented • Aridisols: little vertical structure; thin and unsuitable for sustainable agriculture
Plant-soil-water Relationships Plants need water for photosynthesis, cell function, and turgor pressure so not to wilt. Water return to the atmosphere is slower by transpiration than direct evaporation from bare mineral soil.
Productive Soil • Good supply of nutrients and nutrient-holding capacity • Infiltration, good water-holding capacity, resists evaporative water loss • Porous structure for aeration • Near-neutral pH • Low salt content • Moderate organic content • Active Detritus Food Web