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APES 1/3 Take out your soil lab (on notebook paper) and Chapter 10 Reading Guide Get a computer
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Odds and Ends Missing many Plate Tectonics notes and Ch. 8 RG (p.3)
Chapter 10 RG is due today Chapter 7 Open-Note Test (12/14) No retakes, as it was open-note Biggest takeaways: learn the formulas, stick the landing on the FRQ
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Major Categories of Land Use
Forestry Grazing Crops Special Use (wilderness areas, military) Urban/suburban Mining- mixed into special use, grazing, forests
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Visualizing Land Use
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Learning Sequence Soils and mining for resources (Ch. 8)
Land-use principles (Ch. 10)- grazing, forests, special use areas, urban planning Croplands (Ch. 9)
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Soil Formation and Properties
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Soil Formation
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Soil Profile O Eluviation/Zone of Leaching – water percolates down the soil, transporting materials. Happens in Horizons A & E A E Illuviation/Zone of Accumulation – where transported materials are deposited. Happens in Horizon B. B C
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Soil Lab Components Soil Texture (set up last time; do today)
Soil porosity (done last time) Soil permeability (do today) Soil pH (do today) Answer all questions asked for on the lab handout. Write your answers on notebook paper.
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Gone last time? Intro: Summarize the three soil types and their relative ability to create a healthy environment. Test 2: Soil Porosity (percent pore space) Read the background and answer: - What is porosity and why is it important? - What is a rock type with high porosity? Low porosity?
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Soil Texture- follow the direction of the outer lines!
Find 40% Sand 45% Silt 15% Clay Loam Mixture of all 3 Really only need to find 2 of the 3 points. 3rd point acts as a clarifier Sandy loam would be a mixture of all 3, that has a significantly higher percentage of sand
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Soil Properties Notes
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Texture/Particle Size
Biggest Smallest Sand, Silt, Clay Fine particles have higher cohesion; that’s why water can’t get through clay as well
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Other Physical Properties
You should know porosity and permeability using the lab as the teaching tool. Porosity = how much water soil holds; permeability = how fast water flows through
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Chemical Properties 1. pH
2. Cation Exchange Capacity = ability of soil to absorb/release pos. charged ions (cations) Plants need Na+, K+, Mg2+, Ca2+ Clay has a high CEC (b/c of neg. particles) BUT if there’s too much clay, it absorbs water and drowns plant roots FYI, humus also has high CEC
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Chemical Properties 3. Base Saturation = ratio of base: acid in soil
Bases are acceptors of extra H+; high ratio means lots of bases present to take in extra H+ from acids that might harm plant roots We have lots of limestone in NW soil to counteract acids (high base saturation)
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Soil and Mining We know that good soil provides vital ecosystem services Unfortunately, we also know that the bedrock under it can hold very valuable ores…
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Minerals and Ores Earth’s crust is 88% iron, silicon, aluminum, and oxygen Valuable, rarer elements are found in uneven clusters because of variable distribution of rock types Mineral = naturally occurring, crystalline solid Ore = valuable, concentrated accumulation of minerals in rocks
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Important Ores Metallic minerals- valuable for ability to conduct electricity, structural purposes, etc. (i.e, copper, gold, lead, rare earth metals for batteries) Salt, sand Fossil fuels (carbon-based)
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MANGANESE COAL IRON MICA
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What do we mine for? Energy Metallic Non-metallic Ferrous Non-ferrous
Limestone Coal Iron Gold Nitrate Petroleum Manganese Silver Potash Natural Gas Chromite Copper Dolomite Pyrite Lead Mica Tungsten Bauxite Gypsum Nickel Tin Cobalt Magnesium
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Mining Homework Copper Mine Virtual Tour Assignment (Google classroom)
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