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Let’s Get Down and Dirty!. I . APES. Soil is a mixture of eroded rock, mineral nutrients, decaying organic matter, water, air, and living organisms. 5 Soil Forming Factors. Parent material Climate Living organisms Topography Time.
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Let’s Get Down and Dirty! I APES
Soil is a mixture of eroded rock, mineral nutrients, decaying organic matter, water, air, and living organisms
5 Soil Forming Factors • Parent material • Climate • Living organisms • Topography • Time
Soil texture is an important soil characteristic that drives crop production and field management. The textural class of a soil is determined by the percentage of sand, silt, and clay. Silty clay – rolls into a ball; dark in color Soil texture determines the rate at which water drains through a saturated soil; water moves more freely through sandy soils than it does through clayey soils.
Mature soils are arranged in a series of zones called soil horizons Most mature soils have at least three of the possible horizons
In forests you will find the O Horizon (surface litter layer) Topsoil layer (humus) Subsoil layer (inorganic matter) Parent material (inorganic matter)
The A and O Horizons is where the interaction with bacteria, fungi, earthworms, and small worms take place
Fertile soil that produces high crop yields has a thick topsoil layer with lots of humus
Dark brown or black topsoil is nitrogen rich and high in organic matter
Gray, bright yellow, or red topsoil is low in organic matter and needs Nitrogen enrichment
Soil permeability is a measurement of the rate water moves through soil. Soil permeability is governed by the makeup of the soil. Sandy and rocky soils have a high rate of soil permeability, while clay types of soils have a low rate. The rate of soil permeability can affect engineering and planning for structures such as sewer systems and earthen dams. It also is used to determine footings in buildings to prevent settling.
Porosity is the open space between soil grains. Soil scientists use porosity measurements to determine how effectively air and water move through the subsurface. Large pore spaces within a soil column help promote infiltration allowing the water to uptake into the root system of plants without mounding and becoming boggy.
There are three ways that wetland soils may filter contaminants from water: • Physical filtration occurs when moving water containing suspended • sediments floods a wetland. Often, the water’s movement is slowed, • perhaps even to a stand still. Sediments then settle out of the water. • Biological filtration occurs with nitrates. In the case of NO3-, anaerobic • bacteria use the nitrate molecule as their final electron acceptor, • reducing it to N2 gas or various nitrogen oxides (also gases). This • process is especially important when agricultural fields are adjacent to • waterways. • Chemical filtration occurs because wetland soils are often high in CEC • (cationexchange capacity). Positively charged particles are selectively • removed from the water.
Soil Problems • Acidic soil – decrease uptake of nutrients • add lime and organic fertilizer • Alkaline soil -western and southwestern United States • Add sulfur – converted by bacteria to sulfuric acid • Soil erosion • Sheet erosion • Rill erosion • Gully erosion
Soil removed in uniform layer; slowest moving water at top of hill
Flowing water coalesces into small channels; tiny gullies form
Gully Erosion Channels coalesce into larger channels; water increases velocity and volume; erodes into larger gully
Harmful Effects of Soil Erosion • Loss of soil fertility • Loss of ability to hold water • Pollutes water, kills fish and shellfish • Clogs irrigation ditches, boat channels • Fills lakes and reservoirs with silt
Providence Canyon resulted from poor farming practices – Lumpkin, GA
Global Soil Erosion • Topsoil is eroding faster than it forms on about one third of the world’s croplands • 15% of land scattered across the globe are too eroded to grow crops because • Overgrazing (35%) • Deforestation (30%) • Unsustainable farming (28%)
Global Soil Erosion • About 40% of world’s land used for agriculture is seriously degraded by • Erosion • Salinization • Waterlogging • Soil degradation has reduced food production on about 16% of world’s cropland
Practices That Leave Soil Vulnerable to Desertification • Overgrazing on fragile arid and semi-arid land • Deforestation without reforestation • Surface mining without reclamation • Irrigation techniques that lead to increase erosion • Salt buildup from irrigation • Farming on land with unsuitable terrain or soils • Soil compaction by farm machinery and cattle
Symptoms of Desertification • Loss of native habitat • Increased erosion • Salinization • Lowering of water table • Reduced surface water supply
Consequences of Desertification • Worsening drought • Famine • Declining health standards • Environmental refugees
Which of the following ecosystems best characterizes a thick O horizon? Chaparral Desert Grassland Semi-desert Taiga
Which of the following ecosystems best characterizes a thick O horizon? Chaparral Desert Grassland Semi-desert Taiga
How does soil compaction affect the use of the land? Compacted soils have negligible effects on land use. Compacted soils help reduce the threat of invasive species taking over. Although compacted soils reduce the flow of water through the soil, there is an increase in the availability of oxygen. Soil compaction helps to keep the topsoil from eroding. Compaction reduces space between soil particles, obstructing the flow of gases, nutrients, and water through the soil.
How does soil compaction affect the use of the land? Compacted soils have negligible effects on land use. Compacted soils help reduce the threat of invasive species taking over. Although compacted soils reduce the flow of water through the soil, there is an increase in the availability of oxygen. Soil compaction helps to keep the topsoil from eroding. Compaction reduces space between soil particles, obstructing the flow of gases, nutrients, and water through the soil.
Deforestation, overgrazing, and the overworking of soil for crop production can lead to which of the following> Salinization Monoculture Desertification Increased crop rotation Depletion of aquifers
Deforestation, overgrazing, and the overworking of soil for crop production can lead to which of the following? Salinization Monoculture Desertification Increased crop rotation Depletion of aquifers
Soil Conservation • Conservation tillage farming (no till) • Terracing • Contour farming • Strip cropping • Alley cropping • Gully reclamation • Windbreaks or shelterbreaks • Land classification
Strip Cropping – a row of crop such as corn alternates in strips with another crop, such as grass-legume mixture, that completely covers the soil
Alley cropping or agroforestry – several crops are planted together in strip or alleys between shrubs and trees
Windbreaks or shelterbreaks – reduce wind erosion (retain soil moisture, fuelwood, and provide a habitat
Restoring Soil Fertility Organic Fertilizers
Restoring Soil Fertility Commercial Inorganic Fertilizer
Green Manure – plowing into soil plants currently growing Composting Restoring Soil Fertility
Restoring Soil Fertility Crop Rotation – plant areas or strips with nutrient-depleting crops (tobacco, corn, and cotton deplete soil of nitrogen) one year and the next year they plant the same areas with legumes
Which of the following factors did NOT contribute to the Dust Bowl in the United States? No-till agriculture Removal of vegetative cover Soil erosion Desertification Drought
Which of the following factors did NOT contribute to the Dust Bowl in the United States? No-till agriculture Removal of vegetative cover Soil erosion Desertification Drought
If you were to practice crop rotation which of the following crops would be best for you rotate with corn? Tobacco Cotton Maize Soybeans Sugarcane
If you were to practice crop rotation which of the following crops would be best for you rotate with corn? Tobacco Cotton Maize Soybeans Sugarcane