Robert W. Nairn, R. S. Hedin, George R. Watzlaf
Abstract
The rate of 1 imestone dissolution and a1 kal inity generation in an anoxic 1 imestone drain is determined by many factors, including the qua1 i ty of the limestone used and the partial pressure of carbon dioxide within the system. Carbon dioxide concentrations greater than
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The rate of 1 imestone dissolution and a1 kal inity generation in an anoxic 1 imestone drain is determined by many factors, including the qua1 i ty of the limestone used and the partial pressure of carbon dioxide within the system. Carbon dioxide concentrations greater than
Key concepts: Alkalinity, Anoxic waters, Geology, Environmental science, Oceanography, Chemistry, Organic chemistry