Occurrence, Origin and Transformation Processes of Geogenic Chromium in Soils and Sediments

• Published in: Current pollution reports 2016-12, Vol.2 (4), p.224-235
• Main Authors: Chrysochoou, Maria, Theologou, Elina, Bompoti, Nefeli, Dermatas, Dimitris, Panagiotakis, Iraklis
• Format: Article
• Language: English
• Subjects: Aquatic Pollution; Aquifers; Atmospheric Protection/Air Quality Control/Air Pollution; Chromic hydroxide; Chromium; Drinking water; Earth and Environmental Science; Environment; Environmental Law/Policy/Ecojustice; Geochemistry; Groundwater; Hexavalent chromium; Hydrogen peroxide; Industrial Pollution Prevention; Metamorphic rocks; Mineralogy; Monitoring/Environmental Analysis; Organic matter; Organic soils; Oxidation; Pollution; Public health; Rocks; Section Editors; Sediment and Other Pollutions (R Datta and P Zhang; Sediments; Serpentine; Serpentine soils; Soil mineralogy; Soils; Surface water; Topical Collection on Sediment and Other Pollutions; Trivalent chromium; Ultramafic materials; Waste Water Technology; Water Management; Water Pollution Control; Weathering
• ISSN: 2198-6592; 2198-6592
• DOI: 10.1007/s40726-016-0044-2

Weathering of ultramafic rocks has been linked to the occurrence of elevated concentrations of hexavalent chromium (Cr(VI)) in soils, sediments, and groundwater. Ultramafic rocks and the derived serpentine soils and sediments are encountered in populated areas around the world and present high Cr concentrations, with an average of 2200 and 2650 mg/kg for rocks and soils, respectively. Groundwater concentrations between 0.2 and 180 μg/L have been reported for Cr(VI) in ultramafic areas, exceeding occasionally the most prevalent drinking water limit of 50 μg/L Cr tot , the 5 μg/L Cr(VI) limit established in Italy, and the 10 μg/L Cr(VI) limit proposed in California. Cr release in groundwater occurs through the dissolution of trivalent chromium (Cr(III)) from its mineral hosts, followed by sorption of Cr(III) onto high-valence Mn oxides and oxidation to Cr(VI), which desorbs and is mobile at alkaline pH. Recent findings indicate that hydrogen peroxide and birnessite produced on the surface of Cr(OH) 3 by heterogeneous oxidation are two additional potential mechanisms. Thus, groundwater concentrations are controlled by a variety of geoenvironmental factors, including climate, soil mineralogy, pH, organic matter, and others. To provide a basis for the evaluation of Cr mobility in ultramafic environments, this paper presents an overview of the mineralogy and geochemistry of Cr-rich rocks, sediments, and soils, along with the weathering and geochemical processes that control the fate and transport in the subsurface.