Abstract
Elements such as Ca, Mg, and K, which are required for plant growth, are important components of the nutrient cycle in forested ecosystems, and by far the largest store of these elements in North American and European forests is within the minerals constituting the forest soil. Although external inputs from the atmosphere in both the dissolved and particulate load can provide a portion of these elements to a growing forest, the ultimate source of most inorganic elemental nutrients is provided through cation exchange and mineral weathering reactions that take place in the soil profile. Mineral inventories and determinations of the physical characteristics, mineralogy and chemistry of soil components, and mineral weathering reactions that occur in soils must be an integral part of any study that attempts to document the nutrient status of a forested ecosystem.
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April, R., Newton, R. (1992). Mineralogy and Mineral Weathering. In: Johnson, D.W., Lindberg, S.E. (eds) Atmospheric Deposition and Forest Nutrient Cycling. Ecological Studies, vol 91. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-2806-6_10
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DOI: https://doi.org/10.1007/978-1-4612-2806-6_10
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