Soil chemistry. Orlov, D. S. 1992.
Soil chemistry. [link]Paper  abstract   bibtex   
Carbonates are arguably the most important dissolved component of soil solutions and in alkaline soils this statement is even less disputable. Implicit in this statement is the relationship among dissolved carbonate species whether or not they are in equilibrium with solid phase metal carbonates. The simplest example of carbonates is the control which dissolved carbon dioxide has on water pH and buffering. In this section of the course we will consider the effect of carbon dioxide on water pH, the influence of solid phase calcium carbonate on solution composition and the implications of these reactions. Several systems including carbon dioxide, solution and solid phase.
@book{ orlov_soil_1992,
  title = {Soil chemistry.},
  shorttitle = {Soil chemistry.},
  url = {http://www.cabdirect.org/abstracts/19931973534.html},
  abstract = {Carbonates are arguably the most important dissolved component of soil solutions and in alkaline soils this statement is even less disputable. Implicit in this statement is the relationship among dissolved carbonate species whether or not they are in equilibrium with solid phase metal carbonates. The simplest example of carbonates is the control which dissolved carbon dioxide has on water {pH} and buffering. In this section of the course we will consider the effect of carbon dioxide on water {pH}, the influence of solid phase calcium carbonate on solution composition and the implications of these reactions. Several systems including carbon dioxide, solution and solid phase.},
  author = {Orlov, D. S.},
  year = {1992}
}

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