topic 5 part 1 soil. what is soil and why do we care about it? complex mixture: weathered mineral...
TRANSCRIPT
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Topic 5 Part 1Topic 5 Part 1
soilsoil
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What is soil and why do we care about it?
What is soil and why do we care about it?
complex mixture: weathered mineral
materials from rocks partially decomposed
organic molecules Ecosystem services
complex mixture: weathered mineral
materials from rocks partially decomposed
organic molecules Ecosystem services
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Soil formationSoil formation Many factors contribute to this LONG process
ClORPT Help determine soil type
Many factors contribute to this LONG process ClORPT
Help determine soil type
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Temperature and Moisture influence the speed of chemical reactions, which in turn, control how fast rocks weather and dead organisms decompose.
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Soils develop fastest in warm, moist climates, and slowest in cold and arid ones.
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The shape of the land and the direction in faces makes a difference in how much sunlight the soil gets, and how much water it keeps.
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Deeper soils form at the bottom of a hill than at the top because gravity and water move soil particles down the slope.
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Just like you inherited some characteristics from your parents, every soil inherits traits from the material from which it formed.
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Soils that form in limestone bedrock are rich in calcium, Soils that formed from materials at the bottom of lakes are high in clay.
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Time
Older soils differ from younger soils because they have had longer to develop
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EXAMPLE: In the Northern U.S., soils tend to be younger, because glaciers covered the surface during the last ice age, which kept soils from forming. In the southern U.S., there were no glaciers. There, the soils have been exposed for a longer time, so they are more weathered.
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Soil Texture Soil Texture Ratio of soil particle size determines some soil
properties Ratio of soil particle size determines some soil
properties
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Determining soil typeDetermining soil type
% I
ncre
asin
g C
lay
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Soil Properties: Porosity Soil Properties: Porosity Affects water infiltration, water holding capacity,
aeration, workability Affects water infiltration, water holding capacity,
aeration, workability
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Soil Properties: Chemical Soil Properties: Chemical Cation exchange capacity (aka nutrient holding
capacity) Cation exchange capacity (aka nutrient holding
capacity)
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SOIL ProfileSOIL Profile
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Weak humus-mineral mixture
Mosaicof closelypackedpebbles,boulders
Dry, brown toreddish-brown, with variable accumulationsof clay, calciumcarbonate, andsoluble salts
Desert Soil(hot, dry climate)
Grassland Soil(semiarid climate)
Alkaline,dark,and richin humus
Clay,calciumcompounds
Soil Profiles in Different BiomesSoil Profiles in Different Biomes
aridisolsmollisols
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Acidiclight-coloredhumus
Iron andaluminumcompoundsmixed withclay
Forest litterleaf mold
Humus-mineralmixture
Light, grayish-brown, silt loam
Dark brownfirm clay
Tropical Rain Forest Soil(humid, tropical climate)
Deciduous Forest Soil(humid, mild climate)
Soil Profiles in Different BiomesSoil Profiles in Different Biomes
oxisols alfisols
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Soil Properties: BioticSoil Properties: Biotic
surface = algae top few cm of soil =
bacteria & fungi roundworms, segmented
worms, mites, insects farther down: burrowing
animals--gophers, moles, insect larvae, worms
even farther: some plant roots
surface = algae top few cm of soil =
bacteria & fungi roundworms, segmented
worms, mites, insects farther down: burrowing
animals--gophers, moles, insect larvae, worms
even farther: some plant roots
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Soil CommunitySoil Community
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Soil Community -- MycorrhizaeSoil Community -- Mycorrhizae
Redwood seedlings with (right) and without (left) mycorrhizae.
Pine seedling showing how mycorrhizal roots from one tree spread to inoculate other tree roots.
mycorrhizal symbiosis - mutualism between plant roots & fungi