Article ID Journal Published Year Pages File Type
5752666 Applied Geochemistry 2017 21 Pages PDF
Abstract
Temporal and spatial changes in SIcalc and IRcalc values in surface waters were mainly attributed to an increase in the intensity of bioactivity, which is in turn connected with an increase in water temperature.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Authors
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