Define what constitutes soil
Understand the biological significance of soil
Learn how soil forms from parent materials
Explore the importance of soil for plant growth
Assess the impact of intensive agriculture and deforestation on soil health
Processes: Volcanic activity, erosion, weathering, transport
Rocks:
Igneous: e.g., basalt (fine crystalline), granite (coarse crystalline)
Sedimentary: e.g., sandstone, limestone
Metamorphic: e.g., marble, slate
Cycles: Uplift, melting, metamorphism, deposition
Parent Material: Source from which soils develop
A-Horizon (Topsoil):
Organic matter decomposes, key for plant growth
Worms and microbes enrich the soil
B-Horizon (Subsoil):
Accumulates minerals leached from upper layers
C-Horizon:
Weathered parent material
Transition Zones:
Areas where different horizons meet
Water Interaction: Rain influences soil layers
Soil Character: Affected by climate, rainfall, and vegetation
Distinct composition and texture in different horizons
Importance of organic matter and minerals
Role of weathering in nutrient release
Strategies: Reduced fertilizer use, improved CO2 capture, enhanced soil health through bacteria
Influence on soil types in regions like New England
Features formed: Ground moraine, kettle lakes, outwash plains
Bedrock: Solid rock beneath soils
Types: Clay, silty clay, sandy, loam
Health Indicators: Combination of soil structure, chemistry, organic content, biology, permeability
Interdependence: Water, plants, and soil interactions
Processes: Transpiration, absorption, runoff
Eutrophication: Resulting from excess nitrogen and phosphorus
Soil Degradation: Consequences on agriculture and natural ecosystems
Key Terms:
Eutrophication
Soil health
Soil minerals
Parent material
Weathering
Glaciation
Moraine