14
Soil Conservation

Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Embed Size (px)

Citation preview

Page 1: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Soil Conservation

Page 2: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Erosion

• Two billion tons of U.S. soil lost annually

• Improved from Five billion tons in 1982

• Conservation programs and voluntary conservation tillage practices

• Tolerable losses (rule of thumb) at most –• One to five tons/acre annually• Missouri 4.1 tons/acre (2003 data)

Page 3: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Erosion

• Damage may be On-site or Off-site

• On-site damage includes:• Topsoil losses• O.M. and nutrients• Decreased root zone• Decreased Plant Available Water• Gullies - make equipment operation difficult

Page 4: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Erosion

• Off-site damage includes:

• Pollution of lakes and streams (nutrients and pesticides carried with eroded soil)

• Sediment filling in lakes and reservoirs

Page 5: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Erosion

• Cost of Erosion

• Two separate costs

» Costs to the farmer and consumer (production loss)

» Costs to the public (pollution and sedimentation)

Page 6: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

How Water Erosion Occurs

• Three steps:

• 1) raindrop impact shatters aggregates• Loosened particles seal soil voids limiting infiltration• Moving water also removes particles

• 2) detached grains move in flowing water

• 3) soil is deposited when water slows down

Page 7: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

How Water Erosion Occurs

• Erosion (a form of work) takes energy

• Energy comes from falling raindrops or moving water

• Energy relates to size of drop and velocity

• High energy can remove more and larger particles affecting amount carried off field

• Deposition occurs when energy of running water decreases

Page 8: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Four Erosion Factors

• Texture and Structure

• Slope

• Soil cover

• Roughness of soil surface

Page 9: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Four Erosion Factors

• Texture and Structure• Texture has two effects

– Influences infiltration rate– Particle size affects ease of detachment

» Silt particles are most easily detached

• Structure also influences infiltration– Granules reduce runoff– Strong peds resist impact of raindrops– O.M. content aids in good structure formation

Page 10: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Four Erosion Factors

• Slope:

• Two components• Length• Grade

• Long, gentle slopes can have the same erosive potential as short, steep slopes– see figure 18-6, p. 300

Page 11: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Four Erosion Factors

• Surface Roughness

– Rough surface slows velocity– Depends on tillage practices

• Conventional tillage – smooth• Chisel plowing - rough

Page 12: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Four Erosion Factors

• Soil cover– Reduces energy available to cause erosion

• Mulch• Cover of crop

– e.g. turf or hay reduces energy plus plant roots hold soil

• Row crops or nursery have varying effects depending on planting distances and stage of growth (canopy increases with growth)

Page 13: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Types of Water Erosion

Listing by Increasing Severity

• Splash erosion• Sheet erosion• Rill erosion• Ephemeral gullies• Gully erosion

• Severity limits workability; e.g. gullies can’t be crossed by equipment

Page 14: Soil Conservation. Erosion Two billion tons of U.S. soil lost annually Improved from Five billion tons in 1982 Conservation programs and voluntary conservation

Predicting Soil Loss:The USLE and RUSLE

• Universal Soil Loss Equation• Main tool for estimating erosion rates• Predicts only sheet and rill erosion