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Soil as a Dynamic Ecosystem
Soil is a dynamic ecosystem with inputs, outputs, storages, and flows.
Importance of Soil
Soil is crucial for plant growth, water storage, filtration, nutrient cycling, habitat for organisms, and providing raw materials.
Soil Composition
Soil consists of mineral particles (45%), organic material (5%), water (25%), air (25%), nutrients (N, K, P), and living organisms.
Soil Profile Horizons
The soil profile consists of distinct layers: Horizon O (organic matter), Horizon A (mineral soil), Horizon B (accumulation layer), Horizon C (large rocks), Horizon R (parent rock).
Inequities in Food Systems
Food availability is unevenly distributed between MEDCs and LEDCs, leading to malnutrition and food security issues.
Food Security
Having access to sufficient, safe, and nutritious food to remain healthy.
Malnutrition
Insufficiency in one or more nutritional elements necessary for health.
The Green Revolution
A period (1960-1970) that increased crop yields through new agricultural techniques but led to biodiversity loss.
Types of Soil Degradation
Includes erosion, biological degradation, physical degradation, and chemical degradation.
Conservation Measures
Strategies to combat soil degradation, such as planting trees, using cover crops, and improving irrigation practices.
Soil Degradation
The widespread issue of soil degradation where 75% of soil has some degree of degradation due to human causes.
Types of Soil Degradation
Includes erosion (transfer of soil particles), biological degradation (loss of humus/microorganisms), physical degradation (loss of structure/permeability), and chemical degradation (acidification, decreased fertility).
Erosion
The transfer of soil particles primarily caused by water and wind.
Biological Degradation
The loss of humus and microorganisms in the soil.
Physical Degradation
The loss of soil structure and changes in permeability.
Chemical Degradation
Includes issues like acidification, decreased fertility, pH changes, and salinity.
Overgrazing
Damages vegetation, compacts soil, and increases erosion; excessive livestock feed on all vegetation.
Deforestation
Removes tree cover and increases water erosion.
Inappropriate Agricultural Practices
Includes overuse of pesticides, removal of crops at harvest, row cropping, plowing on slopes, and monocultures.
Urbanization
Paving over soil, which increases runoff and contributes to degradation.
Desertification
The gradual conversion of productive land into desert, affecting fragile ecosystems.
Consequences of Degradation
Includes desertification, erosion (sheet, gullies, wind) and overall loss of soil fertility.
Conservation Measures
Strategies such as wind reduction, soil conditioners, better cultivation techniques, improved irrigation, and not plowing unproductive soils.
Ecological Succession
Fertile soils require time to develop through succession, emphasizing the long-term process of soil formation.
Climate Change and Soil Degradation
Human activities that reduce soil fertility and increase soil erosion contribute to a negative feedback loop in climate change.
Soil as a System
Examine the soil as a dynamic ecosystem with inputs, outputs, storages, and flows.
Terrestrial Food Production Systems
Compare and contrast commercial and subsistence agricultural systems, considering socio-cultural factors.
Soil Degradation and Conservation
Investigate the causes and consequences of soil degradation and explore potential conservation techniques.
Case Study: Commercial vs. Subsistence Farming
Compare the inputs, outputs, and environmental impacts of commercial farming in the US and subsistence farming in Sub-Saharan Africa.
Deforestation and Soil Erosion
Analyze the relationship between deforestation in the Amazon Rainforest and the resulting soil erosion.
The Green Revolution in India
Evaluate the positive and negative impacts of the Green Revolution on food production and soil health.
Terraces in Asian Agriculture
Evaluate how terraces help to harness water that runs down slopes.
No-Till vs. Conventional Agriculture
Analyze the differences in soil health and water retention between no-till farming and conventional plowing.
Methodology for Case Studies
Use literature reviews, data analysis, and field studies to gather insights for case studies.
Key Questions for Soil Case Studies
Consider how soil texture affects water retention, implications of nutrient leaching, and contributions of living organisms.
Soil Texture
Soil texture refers to the proportion of sand, silt, and clay particles.
Sand
Sand particles range from 0.05 mm to 2 mm, characterized by fast-draining properties and low water retention.
Silt
Silt particles range from 0.002 mm to 0.05 mm, providing medium water retention.
Clay
Clay particles are smaller than 0.002 mm, known for being sticky, having high water retention, but low permeability.
Impact of Soil Texture on Soil Structure
Soil structure is determined by texture, affecting aeration, water retention, drainage, and root penetration.
Factors Affecting Primary Productivity
Primary productivity depends on mineral content, drainage, water retention, air spaces, biota, and the potential for retaining organic matter.
Mineral Content of Clay Soil
Clay soil can be rich in minerals but is often less fertile due to its low permeability.
Horizon O
Organic matter.
Horizon A
Mineral soil with organic matter accumulation and soil life.
Horizon B
Accumulation of Fe, clay, Al, and organic compounds.
Horizon C
Layer of large unbroken rocks that can accumulate soluble compounds.
Horizon R
Partially weathered parent rock.