Evaluating the effect of grain size and salts on liquid water content in frozen soils of Antarctica by combining NMR, chemical equilibrium modeling, and scattered diffraction analysis

Author:

Vugmeyster Liliya,Hagedorn Birgit,Clark Matthew A.,Sletten R.S.

Funder

CU

National Science Foundation Cooperative

State of Florida

U.S. Department of Energy

Publisher

Elsevier BV

Subject

Soil Science

Reference67 articles.

1. Geomorphology: The Mechanics and Chemistry of Landscapes;Anderson,2010

2. Physics, chemistry, and mechanics of frozen ground: a review permafrost;Anderson,1973

3. The unfrozen water and the apparent specific heat capacity of frozen soils;Anderson,1973

4. Evolution of the adsorbed water layer structure on silicon oxide at room temperature;Asay;J. Phys. Chem. B,2005

5. Quantifying sulfate components and their variations in soils of the McMurdo Dry Valleys, Antarctica;Bao;J. Geophys. Res.,2006

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