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K-State Agronomy eUpdates

Department of Agronomy

Kansas State University

1712 Claflin Rd.

2004 Throckmorton PSC

Manhatan, KS 66506

785-532-6101

agronomy@ksu.edu

Extension Agronomy

Gypsum vs. lime: Facts about minerals

Evaporite minerals commonly occur in Kansas as geologic depositions. As the name would imply, these form by the evaporation of sea water millions of years ago.

Gypsum and limestone are two evaporate minerals found in Kansas and used for agricultural amendments. Some facts:

  • Lime is CaCO3.  The chemical name is calcium carbonate.
  • Gypsum is CaSO4.H2O. It can occur in many forms. Selenite is the crystal form shown in the photo below. The powdery form mined for sheetrock is called alabaster.
  • Lime and gypsum can both be used to supply calcium as a fertilizer.
  • Since gypsum contains sulfur (S), it is a good source of that element.
  • Lime is used to increase soil pH.
  • Gypsum does not affect soil pH. Elemental S is the correct form to use to reduce pH.
  • Gypsum is ≈200 times more soluble than lime.
  • Gypsum is usually only found naturally in the soil profiles of the more arid parts of the state. .
  • Lime occurs as nodules of calcium carbonate deep in the soil profile in most of eastern Kansas. In western Kansas, it can occur very near the surface.

Figure 1. Gypsum outcropping in Hodgeman County. Photo by DeAnn Presley, K-State Research and Extension.

For more information, see a 2011 Extension publication titled “Gypsum as an agricultural amendment” by L. Chen and W.A. Dick, Ohio State University, at: http://ohioline.osu.edu/b945/b945.pdf 

DeAnn Presley, Soil Management Specialist
deann@ksu.edu