Hydrogen (protium)-deuterium exchange in clays

Details Hydrogen (protium)-deuterium exchange in clays Hydrogen (protium)-deuterium exchange in clays

Sep 1958

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1958gecoa..14..250m&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 14, Issue 3, pp.250-252

Physics

1

Scientific paper

The mobility of the hydrogen in clay minerals has been examined by exchange reactions with deuterium dioxide. It was found that the hydrogen of the clay minerals was present in three distinct states, each with its particular rate of exchange. The adsorbed water is exchanged in a matter of seconds or minutes; the H 3 O + water m a matter of weeks, and the OH - water in a matter of years or even centuries.

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