Pollutant metal removal and release via reactions with sedimentary pyrite in Galveston Bay
Date
1993
Authors
Morse, John W.
Journal Title
Journal ISSN
Volume Title
Publisher
Galveston Bay National Estuary Program
Abstract
The chemically reactive fraction of trace metals commonly undergoes diagenesis in sediments. Trace metals associated with metal oxides, organic matter, and other reactive components can be released to pore waters as these components are broken down by a variety of biologic and chemical processes. The trace metals may then be transported to overlying waters or be reprecipitated as discrete phases or as coprecipitates with other authigenic minerals.
Description
pgs. 125-126
Keywords
anoxic conditions, sediments, trace metals