Removal of magnesium from interstitial waters in reducing environments--the problem reconsidered

Details Removal of magnesium from interstitial waters in reducing environments--the problem reconsidered Removal of magnesium from interstitial waters in reducing environments--the problem reconsidered

Dec 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978gecoa..42.1907h&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 42, Issue 12, pp.1907-1909

Physics

5

Scientific paper

Iron-containing smectites are not affected significantly by Mg-containing dilute sulphide solutions. Concentrated solutions reduce most of the Fe in montmorillonites; Fe is partially extracted from nontronite with concomitant disintegration of the structure. It is concluded that direct Mg Fe exchange in clays seems improbable, but that depletion of Mg in interstitial waters of anoxic sediments may be due to reaction of Mg-containing solutions with partially disintegrated clay.

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