U.S. Department of Agriculture: Agricultural Research Service, Lincoln, Nebraska

 

Document Type

Article

Date of this Version

1996

Comments

Published in of Soil Analysis. Part 3. Chemical Methods--SSSA Book Series no. 5. Chapter 15, 1272, 437-474

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.

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