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Weathering and Soils
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Regolith- The layer of weathered rock fragments beneath the soil and above the bedrock (solid rock). ← Soil ← Regolith ← Bedrock
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Soil = minerals, water, gases, organic mtl.
Soil Components Regolith is the basis for soil… Soil = minerals, water, gases, organic mtl.
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humus- dark, organic material made of decayed animal and plant remains
Found just beneath the vegetation Important part of soil- provides nutrients! ← Humus
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3 types of rock materials make up soil- classified by the size of the particles.
Sand (0.05 – 2 mm in dia.) Silt (0.002 to 0.05 mm) Clay (<0.002 mm in dia.) The amounts of each of these components depends on the parent rock!
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Soil Facts Lichens-die add organic nutrients to soil
Slowly renewable resource- 1cm=15 or more years Filters water-infiltrationleaching (diluting nutrient rich layers) into aquifers/surface runoff Decomposer Carbon Sink Biogeochemical Cycles!!! PROBLEM: Erosion
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Soil Triangle and Example
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Clay soils- high percentage of clay
Come from rocks with a lot of feldspar… Hold a lot of water Doesn’t drain well
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Silty soils Very fine particles, have a gritty feel Erodes easily
Often found on riverbanks
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Sandy soils- high percentage of sand
Come from weathered granite and rocks with a lot of quartz Doesn’t hold water, drains quickly
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Transported vs. Residual soil
Transported soil = moved from original location, will have a different composition than the bedrock below Residual soil = soil that rests on top of its parent rock
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Soil profile Cross-section of layers of soil and the bedrock beneath
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Horizons (Residual Soil)
A horizon – topsoil B horizon – subsoil (minerals, clay, humus) C horizon – partially weathered bedrock (regolith) O- Organic E- no organics R- bedrock Top 2 layers-bacteria, fungi, worms, insects
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Transported soils DO NOT have horizons, they are found in layers or unsorted depending on how they were transported!
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Soil and Climate Humid tropical climates: a lot of rain + high temps = chemical weathering Desert climates: minimal rain, high temps= minimal weathering Temperate climates: temperature range between cool and warm, rainfall varies = both types of weathering
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Tropical Soils Laterites – Thick but infertile soils produced in tropical climates Contains irons and other minerals that do not dissolve Topsoil often thin Organic matter constantly added
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Desert Soils Thin Made up of mostly rock fragments (evidence of mechanical weathering) Arctic soil similar
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Temperate Soils All three horizons can reach a thickness of several meters. 2 main types: 1. pedalfer- contains clay, quartz, and iron compounds, forms in places receiving 65cm + of rain per year (Ex. states east of Mississippi and Gulf Coast states)
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2. pedocal- contains large amounts of calcium carbonate, formed in places receiving less than 65 cm of rain per year.
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Soil types around the world correspond to climates…
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Topography and Soil Too flat = poor drainage
On slopes- soil is thick and fertile at the bottom and thin and nutrient-poor on the slope. Ideal soil conditions = fairly flat but with good drainage
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