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What is a soil catena?
The sequence of different soils down a slope, the soils usually derived from the same or similar parent materials but they vary with relief, drainage, and land use. Every disturbance affects all the ecosystems around it.
what are the effects of routine soil disturbance?
Short-term- Increase in porosity that allows water infiltration, facilitates seed germination, and establishment of seedling
Long-term
increase in bulk density and decrease in porosity
decrease organic matter content and reduce microbial diversity
Reduce ability to store water and nutrients
what are the effects of forest conversion on forest soil properties and erosion risk?
increase in bulk density and penetration resistance(compaction)
smaller aggregates(mean weight diameter)
decrease in infiltration
increased erosion risk because tree canopy is removed
How does forest conversion lead to water table rise and formation of saline soils?
Trees have deep roots that take up a lot of water and when they are replaced with shallow-rooted crops the water table rises. Salt content rises when the water table rises because the water and salt rise to the surface, the water dissolves and the salt stays.
What effects do grassland conversion have on soil properties?
decrease in organic matter content
Overgrazing can cause higher sand content
Animals hooves lead to compaction
smaller aggregates and lower infiltration rate
Why are wetland areas “attractive” for conversion to agricultural and commercial/residential uses?
they make good ag fields because of high organic matter content
wetlands in coastal areas are highly valued for residential development
What happens when the wetland is drained and converted to other uses?
increases the rate of organic matter decomposition, more co2 emissions,
soil subsidence
Changes in properties, destroys soil peds and decrease in water holding capacity
higher rate of nutrient mineralization. and release of complexed pollutants
What are the unique properties of urban soils?
disturbed in a portion of profile or whole thing
mixing, filling, and contamination creates a soil material that is unlike its natural counterpart
could be contaminated with pollutants
Basics about soil loss process
Erosion- wearing away of the land by water or wind
natural and accelerated erosion
detachment, transport, deposition
overgrazing, deforestation, mismanagement of cultivated lands
What are the leading causes of water-induced accelerated erosion?
overgrazing 35%
deforestation 30%
mismanagement of cultivated lands 28%
How do soil properties change because of erosion?
increase- crusting, compaction, sand content, salinity, acidity, water pollution, greenhouse gas(c02), eutrophication, organic matter decomposition
decrease- topsoil depth, structure, porosity, water infiltration, plant available water capacity, nutrient exchange, biomass production, organic matter
The wind erosion process. What are the different modes of wind-induced sediment transport?
wind moves 40% of soil tranported by erosion in us, problem in 75mil acres of land in us.
-saltation- short bounces along ground, 50-90%
-creep- rolling or sliding of larger particles, 5-25%
-suspension- fine sand is carried up into the air, 15%
What is agroforestry?
a land management system that combines trees and/or shrubs with agricultural crops and even liverstock production on the same piece of land. grows trees and crops, improves bulk density and water infiltration and yield, trees slow water erosion, give organic matter, buffer wind erosion, and can be additional income
Erosion control and rehabilitation of saline soils
cultural control- water(conservation tillage, cover cropping, mulching, proper timing of cultivation, addition of soil conditioners, contour cultivation, strip cropping or planting buffer strips/vegetation barriers) wind(maintain surface cover, conservation tillage, wind breaks, keep surface moist and rough)
engineering control- riprap, terracing, bioengineering, sediment traps, retention ponds
salinity- leaching soils by applying water or lower water table by drainage or by planting deeply rooted vegetation
conventional tillage
soil tillage such as plowing to produce a porous seedbed, and also the removal of the of the plant residue from the previous crop
conservation tillage
a system of soil cultivation that involves limited disturbance and leaves at least 30% of the soil surface covered with residues
types of conservation tillage
no till
strip till
ridge till
short term and long term effects of soil tillage
short term- increase in porosity that allows for water infiltration, facilitates seed germination, and establishment of seedling
long-term- increase in bulk density and decrease porosity, decrease in oraganic matter and reduces microbial diversity, reduce ability to store water and nutrients
mono-cropping
planting the same crop year after year, decreasing soil fertilty, quality of physical properties, and microbial diversity
crop rotation
growing a series of different crops in the same area, improves soil fertility, organic matter content, and microbial diversity
forest
a non-agricultural land with at least 10% tree cover. 30% of total terrestrial surface
functions of forest soils
foundation of forest ecosystems and productions of forest products
carbon sequestration
water storage
slash and burn agriculture/ fire fallow
trees are cut down and burned for cultivation, farmers move on once the soil becomes infertile after a few years
grasslands
area where vegetation is dominated by grasses, thin soil, sloping areas, shallow water table, bad weather. they have great amounts of organic matter
overgrazing
having too many animals grazing in an area of keeping animals in one spot for too long. increases sand content, decreases organic matter, aggregate stability, and infilitration rate
wetlands
occur in transition zones between well-drained uplands and true aquatic habitats. has hydric soils, certain vegetation, and hydrology
hydric soil
soils formed under consitions of saturation, flooding or ponding long enough during the growing seasonto develop anaerobic conditions in the upper part. have unique features that are a result of organic matter accumulation and or redox reactions involving iron and manganese
soil subsidence
a drop in elevation of the soil surface resulting from the combined effect of organic matter decomposition due to aerobic conditions and decrease in volume of organic soils due to loss of water
urban soil
soil material previously utilized for more natural uses that has a man-made surface layer >50cm think produced by mixing, filling or by comtamination of land in urban and suburban areas
general characteristics of urban soils
great vertical and spatial variablity
modified soil structure leading to compaction
presence of a surface crust on bare soil
restricted aeration and water drainage
presence of anthropic materials and other contaminants
natural v. accelerated erosion
natural happens under natural environmental conditions and accelerated is more rapid usually as a result of human activities
to control erosion what part of the erosion process needs to be prevented
detachment
on site effects of soil erosion
soil structural degradation and compaction
nutrient depletion
loss of soil organic matter
poor seedling emergence and reduced crop yields
off site effects of soil erosion
sedimentation and sedment pollution
alteration of landscape
runoff
that portion of precipitation or irrigation in an area that does not infiltrate, but instead moves out of the area by surface flow
splash erosion
the detachment and airborne movement of small soil particles caused by the impact of raindrops on soils
sheet erosion
the removal of a relatively uniform thin layer of soil from the land surface by rainfall or irrigation and surface runoff; soil particles are easily transported in a thin layer by water flowing on surface. #1 cause of erosion is ag lands!
rill erosion
process on sloping areas in which numerous and randomly occuring small channels of only a few inches in depth are formed, occirs mainly on recently opened or cultivated areas
gully erosion
process where water accumulates and often recurs in narrow channels and over short periods removes the soil from this narrow area to considerable depths. too deep to easily repair with regular tillage equipment
stream erosion
erosion that occurs along the banks of streams
what is the threshold velocity for wind erosion to occur
15mph
factors affecting wind erosion
wind velocity and turbulance (15mph)
surface roughness
soil properties (moisture content, aggregate stability, and size of erodible fractions)
how many years does it take 1in of soil to form and how long does it take to wash away
500, 1 rain event
how to deal with land use changes
prevention, minimize impact, rehabilitate
how far do wind breaks protect the soil
30x the height of the tree