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This deck focuses on Soil Formation And Erosion, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Study Soil Formation And Erosion in AP Environmental Science with focused flashcards that help you recognize the idea, recall the key rule, and apply it in practice-style prompts.
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Which soil property affects water retention and permeability?
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Texture. Particle size distribution affects how water and nutrients move through soil.
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This deck focuses on Soil Formation And Erosion, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Work through these flashcards in short sessions. Try to answer each prompt before flipping the card, then revisit any cards you miss until the explanation feels automatic.
Answer: Texture. Particle size distribution affects how water and nutrients move through soil.
Answer: Clay. Clay particles are less than 0.002 mm in diameter.
Answer: Soil profile. Distinct layers form as soil develops from surface to bedrock.
Answer: Crop rotation. Rotating crops prevents nutrient depletion and breaks pest cycles.
Answer: Improves air and water flow. Pore spaces allow oxygen to reach roots and water to infiltrate.
Answer: Sand. Large particles create pore spaces but cannot hold nutrients effectively.
Answer: Weathering. Physical and chemical processes break down rock into smaller particles over time.
Answer: Minerals, organic matter, air, and water. These four components combine in varying proportions to form soil.
Answer: Lime. Calcium carbonate neutralizes soil acidity and increases pH levels.
Answer: Improves structure. Organic matter creates aggregation and increases water-holding capacity.
Answer: Clay. Clay particles bind together and create stable soil aggregates.
Answer: Reforestation. Plant roots physically hold soil particles in place against erosion.
Answer: Disintegration. Physical breakdown of bedrock creates the mineral component of soil.
Answer: B horizon. Located below the A horizon where nutrients accumulate from above.
Answer: Clay. Clay particles are less than 0.002 mm in diameter.
Answer: Humus. Decomposed organic matter forms a dark, nutrient-rich layer at the surface.
Answer: Loam. Equal parts sand, silt, and clay create ideal drainage and fertility.
Answer: Water. Water dissolves minerals and causes chemical reactions that decompose rock.
Answer: Percolation. Gravity pulls water and dissolved materials downward through soil layers.
Answer: Sand. Large particles create pore spaces but cannot hold nutrients effectively.
Answer: Break down organic matter. Bacteria and fungi decompose dead plants and animals into soil nutrients.
Answer: Soil fertility. Nutrient content and water-holding capacity determine plant growth potential.
Answer: Strip cropping. Alternating strips reduce wind speed and trap eroded soil particles.
Answer: Mechanical weathering. Physical forces like freeze-thaw cycles fracture rocks without chemical changes.
Answer: 6 to 7.5. This range provides optimal nutrient availability for most crop plants.
Answer: Tillage. Repeated plowing and cultivation compress soil particles together.
Answer: Improves structure. Organic matter creates aggregation and increases water-holding capacity.
Answer: Irrigation. Adding water with dissolved salts increases soil salt concentration over time.
Answer: Climate. Temperature and precipitation patterns determine weathering rates and soil development.
Answer: Erosion. Moving water and wind carry away soil particles from their original location.
Answer: Water. Water dissolves minerals and causes chemical reactions that decompose rock.
Answer: Decomposition. Microorganisms break down dead organic material into simpler compounds.
Answer: Irrigation. Adding water with dissolved salts increases soil salt concentration over time.
Answer: Strip cropping. Alternating strips reduce wind speed and trap eroded soil particles.
Answer: Cover cropping. Continuous plant cover protects soil from wind and water erosion.
Answer: Leaching. Downward water movement carries dissolved nutrients away from plant roots.
Answer: Weathering. Physical and chemical processes break down rock into smaller particles over time.
Answer: Climate. Temperature and precipitation patterns determine weathering rates and soil development.
Answer: Reduces availability. Low pH makes essential nutrients less available to plant roots.
Answer: Leaching. Downward water movement carries dissolved nutrients away from plant roots.
Answer: Soil profile. Distinct layers form as soil develops from surface to bedrock.
Answer: Organic matter. Dark organic matter gives soil its characteristic brown or black color.
Answer: Texture. Particle size distribution affects how water and nutrients move through soil.
Answer: O horizon. The surface organic layer contains fresh and partially decomposed plant matter.
Answer: Fertility. Nutrient content determines how well plants can grow in the soil.
Answer: Pedogenesis. The scientific term for soil development from weathered rock material.
Answer: O horizon. The surface organic layer contains fresh and partially decomposed plant matter.
Answer: Terracing. Creating stepped platforms reduces slope angle and water runoff velocity.
Answer: Crop rotation. Rotating crops prevents nutrient depletion and breaks pest cycles.
Answer: Organic matter. Dark organic matter gives soil its characteristic brown or black color.
Answer: A horizon. The surface layer contains the most organic matter and biological activity.
Answer: B horizon. Located below the A horizon where nutrients accumulate from above.
Answer: 6 to 7.5. This range provides optimal nutrient availability for most crop plants.
Answer: Pedogenesis. The scientific term for soil development from weathered rock material.
Answer: Soil fertility. Nutrient content and water-holding capacity determine plant growth potential.
Answer: A horizon. The surface layer contains the most organic matter and biological activity.
Answer: Decomposition. Microorganisms break down dead organic material into simpler compounds.
Answer: Mechanical weathering. Physical forces like freeze-thaw cycles fracture rocks without chemical changes.
Answer: Tillage. Repeated plowing and cultivation compress soil particles together.
Answer: C horizon. This layer sits above bedrock and shows early stages of soil development.
Answer: Improves air and water flow. Pore spaces allow oxygen to reach roots and water to infiltrate.
Answer: Clay. Clay particles bind together and create stable soil aggregates.
Answer: Cover cropping. Continuous plant cover protects soil from wind and water erosion.
Answer: Percolation. Gravity pulls water and dissolved materials downward through soil layers.
Answer: Erosion. Moving water and wind carry away soil particles from their original location.
Answer: Reforestation. Plant roots physically hold soil particles in place against erosion.
Answer: Break down organic matter. Bacteria and fungi decompose dead plants and animals into soil nutrients.
Answer: Minerals, organic matter, air, and water. These four components combine in varying proportions to form soil.