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1. Soil pH is an important property influenced by parent material, precipitation, land management, organic input, and organism activity. 2. Soil pH is maintained through a balance of hydrogen ion production and consumption, with buffering provided by exchangeable cations/anions, organic matter, aluminum hydrolysis, and carbonate dissolution/precipitation. 3. Salt accumulation in soils is caused by processes like evaporation exceeding precipitation, terminal lake effects, saline seepage, and altered hydrol

Author

Josue A. Sespene Jr.

Language

EN