U.S. Department of Agriculture: Agricultural Research Service, Lincoln, Nebraska
Date of this Version
1996
Abstract
The carbonate minerals and gypsum exert a dominating influence on soils in
which they are present because of their relatively high solubility, and in the case
of the carbonates, their alkalinity and pH buffering properties. In this chapter,
procedures for the determination of quantity, reactivity and equilibrium relations
of these minerals will be discussed.
Comments
Published in of Soil Analysis. Part 3. Chemical Methods--SSSA Book Series no. 5. Chapter 15, 1272, 437-474