Magnesium in continental runoff

Details Magnesium in continental runoff Magnesium in continental runoff

Sep 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978gecoa..42.1459b&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 42, Issue 9, pp.1459-1462

Physics

Scientific paper

A mass balance for Mg in continental runoff has been constructed. The sources of runoff Mg in this model are cyclic salts, carbonate rock and silicate rock weathering. The calculations indicate that the Mg concentration reported for average continental runoff is anomalously high. The anomaly may be due to recent disturbances in the weathering regimes of calcite, dolomite and silicates, or to unreliable Mg concentrations reported in older analyses.

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