Final Flashcards
(115 cards)
U.S. Dust Bowl of 1930s
- plowing the short-grass prairie of Am Modwest and drought causes the U.S. Dust Bowl during the 1930s
- John Steinbeck wrote an Am realist novel on the Joads, a poor family of tenant farmers driven from Oklahoma
- Dust Bowl Refugee (Woody Guthrie)
Soil degradation
- occurs when key soil attributes required for plant growth or other ecosystem services deteriorate
- when humans cut forests, graze livestock, or plant crops, the soil is managed or mismanaged
Soil
- solid material of geological and biological origin (not just dirt)
- chemical, biological, and physical processes change soil
- soils are 100s of yrs old and change very slowly
Soil characteristics
Soil is classified by profile, structure, and texture
- soil texture: proportions of sand, silt, and clay
- –parent material: mineral material of the soil (soil has its origin in the geological history of an area)
weathering
gradual physical and chemical breakdown of parent material
Soil texture
three texture classes:
- sand: particles from 2.0 to 0.063 mm (feels gritty) (largest)
- silt: particles range from 0.063 mm to 0.004 mm (feels smooth)
- clay: anything finer than 0.004 mm (feels gooey/sticky) (smallest)
sand, silt, and clay constitute the mineral part of soil - if one particle predominates, the soil is sandy, silty, or clayey
Loam: a soil with 40% sand, 40% silt, and 20% clay
Determine a soils texture by:
- feel-ribboning soil btwn thumb and index finger
- float soil in water and measure when settles (sand settles first)
- scientists classify with triangle
Soil properties and use
Soil properties are influenced by its texture
- large particles have larger spaces separating them
- small particles have surfaces that collect nutrient ions and water molecules
workability or arability (to plow) - the ease with which soil can be cultivated
Soil profiles
Horizons - horizontal layers of soil from soil formation (distinct)
soil profile - a vertical slice through the soil horizons (reveals the interacting factors in soil formation
Humus - decomposed dark material at the bottom of the O horizon
O horizon - topmost layer of soil
- dead organic matter (detritus) deposited by plants
- high in organic content
- primary source of energy for the soil community
Subsurface layers
OAEBC
O Horizon - humus
-organic horizon - contains detritus feeders and decomposers
A Horizon - topsoil (mixture of soil and humus, permeated by fine roots)
-if there is no O in the soil profile than it is A
E Horizon - zone of leaching (less humus, minerals resistant to leaching)
B Horizon - subsoil (contains minerals leached from A, permeated by fine roots, high in iron, aluminum, calcium, clay, reddish/yellow bc oxidized metals)
C Horizon - weathered parent material (partly broken down minerals, weathered rock, glacial deposits, volcanic ash, not affected by bio or chem processes)
O INTERACTS W/ LIVING THINGS/ORGANIC THINGS THE MOST
-least likely is C
Soil classification
Infinite variety of structures and textures but soils are classified by order (the most inclusive group)
Four major soil orders most important for agriculture, animal husbandry and forestry:
- Mollisols (prairie soils)
- Oxisols (tropical forest)
- Alfisols (high-nutrient)
- Aridisols (desert)
Mollisols
fertile, dark soils of temperate grasslands
- PRAIRIES
- most productive soils
- worlds best agricultural soils
- midwest U.S., Ukraine, Mongolia, Argentina
- Deep A horizon - rich in humus and minerals
Oxisols
soils of tropical and subtropical rain forests
- B horizon has a layer of iron and aluminum oxides
- little O horizon: rapid decomposition of vegetation
- limited agriculture: minerals are in living plant matter
- nutrient poor
- such high rainfall they get leached
Alfisols
widespread, moderately weathered forest soils
- well developed O, A, B horizons
- typical of moist, temperate forests
- suitable for agriculture if they are fertilized
Aridisols
soils of drylands and deserts
- unstructured bc lack of vegetation and precipitation
- thin, lightly colored
- some areas may support rangeland animal husbandry
- irrigation leads to salinization
Soil fertility
the soil’s ability to support plant growth
-initially become available through rock weathering (process much too slow to support normal plant growth - breakdown and release (Recycling) of detritus provides most nutrients)
leaching - nutrients are washed from the soil by water
- decreases soil fertility
- contributes to water pollution
Farming practice that prevents nutrient leeching and creates more sustainable soil: crop rotation, no til agriculture, and eliminate irrigation and water use
Fertilizer
agriculture removes nutrients from the soil - fertilizer (nutrients added to replace those that are lost)
- organic fertilizer: plant or animal wastes (manure, compost, leguminous fallow crops - alfalfa, clover) WHAT WE USE
- inorganic fertilizer: chemical formulations of nutrients (much more prone to leaching, Haber process)
Soil-water terms
infiltration - water soaks into the soil
water-holding capacity - soil’s ability to hold water after it infiltrates
transpiration - water is absorbed by roots and exits as water vapor through pores (stomata) in the leaves
soil aeration - allows diffusion of oxygen into, and carbon dioxide out of the soil
Erosion
the process of soil being picked up and carried away by water and wind (occurs any time soil is bared and exposed)
-vegetative cover prevents wind and water erosion (Reducing the energy of raindrops and allowing infiltration)
ONE OF THE BIG PROBLEMS WITH SOIL ENVIRONMENTALLY - nutrient loss
Splash, sheet, and gully erosion
-sequence of erosion from rainfall = splash, sheet, gully
Splash erosion - begins the process of erosion
- raindrops break up the clumpy structure of topsoil or what soil is left
- dislodged particles wash btwn other aggregates
- decreases infiltration and aeration
Sheet - the result of decreased infiltration
-more water runs off, carrying away fine particles
Gully - water converges into rivulets and streams
-water’s greater volume, velocity, energy remove soil
Once started erosion is a vicious cycle (less vegetation exposes soil to more erosion)
Reducing soil erosion
Contour strip cropping - plowing and cultivating at right angles to contour slopes
-shelterbelts: protective belts of trees and shrubs planted along plowed fields
The U.S. Natural resource conservation service (NRCS)
- established in response to the Dust Bowl
- regional offices provide info to farmers and others regarding soil and water conservation practices
overcultivation
general loss of fertility
- if detritus is lost, soil organisms starve
- humus decomposes, breaking down the clumpy aggregate structure of glued soil particles
- -water and nutrient holding capacities, infiltration, and aeration decline
- –all that remains are the minerals (sand, silt, clay)
- –there are no more nutrients for plants to grow
Importance of humus to topsoil
Loss of humus - topsoil mineralization and loss of water-holding capacity, nutrient-holding capacity, water infiltration, aeration
gain of humus - topsoil formation and gain in ^^^
Solution: no or low-till planting
No-till agriculture: a tech allowing continuous cropping while minimizing erosion (practiced in U.S.)
- after spraying a field with herbicide to kill weeds
- planting apparatus cuts a furrow through the mulch - rope seeds and fertilizer - closes the furrow
- the wast from the previous crop becomes detritus (so the soil is never exposed)
CAFOS
In the developed world, animals are raised in confined (compartment) animal feeding operations (CAFOs)
- CAFOs hurt the env. and ppl
- manure overwhelms treatments systems and enters water (fish kills, algal growth, and pathogens)
- crowded animals allow diseases to spread
- –humans (avian flu), salmonella causes $2.5 billion lost/yr in U.S.