CSEM 240 Lecture Notes - Lecture 20: Aluminium Sulfate, Soil Management, Total Dissolved Solids

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To ventilation of the soil, the ability of gases to move in and out. Respiration rate o2 consumption by soil organisms. *relative concentrations of co2 levels and o2 levels in the soil versus the atmosphere. *soil aeration and how it relates to microbial activity and decay of organic matter. Well-aerated higher levels of microbial activity, which speeds up decay of organic matter. *soil aeration as it changes with soil depth. Less well-aerated with increasing depth: water content increases, total pore space decreases. *oxidation and reduction potential of well aerated and poorly aerated soils. *the redox potentials of aerobic versus anaerobic soil. *aeration effects on microbial activity, organic matter, nutrient availability, soil color, root growth, availability of toxic compounds. Nutrient availability: humid areas: oxidized forms desired, arid areas: reduced forms desired. Soil color mainly due to oxidation status of fe and mn. Increased in well-aerated: nutrient uptake higher in well-aerated. Toxic compounds tend to be more available in anaerobic conditions.

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