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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Australasia
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Australia
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Western Australia
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Kalgoorlie Australia (1)
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Canada
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Eastern Canada
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Ontario
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Cochrane District Ontario
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Kidd Creek Mine (1)
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Europe
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Southern Europe
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Iberian Peninsula
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Spain
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Andalusia Spain
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Huelva Spain
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Rio Tinto Spain (1)
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Seville Spain
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Aznalcollar Spain (1)
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South America
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Bolivia (1)
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elements, isotopes
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isotopes
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radioactive isotopes
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U-235 (1)
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U-238 (1)
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stable isotopes
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Pb-206 (1)
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Pb-207 (1)
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Pb-208 (1)
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metals
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actinides
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uranium
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U-235 (1)
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U-238 (1)
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aluminum (1)
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antimony (1)
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arsenic (1)
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chromium (1)
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copper (1)
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iron
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ferric iron (1)
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lead
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Pb-206 (1)
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Pb-207 (1)
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Pb-208 (1)
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vanadium (1)
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minerals
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arsenates
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beudantite (1)
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scorodite (1)
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minerals (1)
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oxides
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goethite (1)
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lepidocrocite (1)
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maghemite (1)
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sulfates
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alunite (3)
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beudantite (1)
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jarosite (4)
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rozenite (1)
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Primary terms
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Australasia
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Australia
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Western Australia
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Kalgoorlie Australia (1)
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-
-
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Canada
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Eastern Canada
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Ontario
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Cochrane District Ontario
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Kidd Creek Mine (1)
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-
-
-
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crystal chemistry (2)
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crystal structure (3)
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crystallography (1)
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Europe
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Southern Europe
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Iberian Peninsula
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Spain
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Andalusia Spain
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Huelva Spain
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Rio Tinto Spain (1)
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-
Seville Spain
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Aznalcollar Spain (1)
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-
-
-
-
-
-
isotopes
-
radioactive isotopes
-
U-235 (1)
-
U-238 (1)
-
-
stable isotopes
-
Pb-206 (1)
-
Pb-207 (1)
-
Pb-208 (1)
-
-
-
metals
-
actinides
-
uranium
-
U-235 (1)
-
U-238 (1)
-
-
-
aluminum (1)
-
antimony (1)
-
arsenic (1)
-
chromium (1)
-
copper (1)
-
iron
-
ferric iron (1)
-
-
lead
-
Pb-206 (1)
-
Pb-207 (1)
-
Pb-208 (1)
-
-
vanadium (1)
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minerals (1)
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pollution (3)
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South America
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Bolivia (1)
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symposia (1)
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Low-temperature crystallography and vibrational properties of rozenite (FeSO 4 ·4H 2 O), a candidate mineral component of the polyhydrated sulfate deposits on Mars
Uptake and release of arsenic and antimony in alunite-jarosite and beudantite group minerals
Abstract Minerals are naturally occurring inorganic solids that make up the solid part of most solar terrestrial planets. Redox-active elements such as iron, manganese, titanium and sulfur, in these minerals allow them to engage in a wide range of electron-transfer reactions including those mediated by biota or processes involved in palaeo-weathering and biogeochemical cycling. The importance of redox-reactive minerals in many natural and industrial processes has been demonstrated by a plethora of scientific publications and industrial applications in recent decades. In this book, the influence of redox-reactive minerals on key biogeochemical processes and opportunities for their application in environmental technologies are outlined and illustrated in 14 comprehensive chapters. The book will be a key reference for Earth science students, geologists, geochemists and engineers and other researchers and practitioners in this rapidly growing interdisciplinary field.
Abstract Mining, oil and gas and other extractive industries are vital and irreplaceable constituents of the modern global economy. The overall demand for the products of these industries rises inexorably with economic growth and developing prosperity. However, these industries produce vast quantities of potentially harmful waste. Many of the elemental, and hence mineralogical, components of the waste stream are redox active. This review focuses on redox-reactive minerals sourced from this waste stream in reuse and remediation schemes. Copper-, manganese- and iron-bearing mine wastes are used as pigments, in fertilizers, sorbents of toxic compounds in water treatment systems, and for the production of SO 2 and H 2 SO 4 . Some solid mine wastes can be remediated by phytostabilization, where plants are used to induce the precipitation of secondary redox reactive minerals that sequester contaminants. Liquid wastes are remediated using a variety of abiotic and biotically-assisted schemes such as anoxic limestone drainages and permeable reactive barriers. These schemes use phases such as zero-valent iron and Fe-oxyhydroxides, and produce mineralogical by-products such as sulfides, green rust and oxyhydroxides. Further research is needed to optimize the reuse and remediation schemes in mine wastes and to develop new and innovative systems employing redox active minerals.