File:Jarosite, KFe3-3(OH)6(SO4)2 - geograph.org.uk - 460813.jpg

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English: Jarosite, KFe3+3(OH)6(SO4)2 Jarosite is a straw-yellow basic sulphate that forms on the oxidation of iron sulphides (FeS2) in soils and sediments. This soil sample was removed from the subsoil of a trial pit at the Arthur Rickwood Experimental Husbandry Farm, Mepal Fen, Cambs. Oxidation has been brought about by drainage of the land for agriculture and associated features are strong acidity (pH less than 4) caused by the release of sulphuric acid, orange-coloured deposits of ochre in drainage pipes and drains, and aluminium toxicity causing a stunted, deformed root system. Soils with strong acidity formed by this process are known as 'acid sulphate soils'; they are common in the perimarine zone of the Fenland of Eastern England where the original sulphides were supplied by a series of marine transgressions. Jarosite is a prominent feature of mineral sediments such as the Fen Clay but is absent from fen peat which also experiences strong acidification in these areas.
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Source From geograph.org.uk
Author Rodney Burton
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Rodney Burton / Jarosite, KFe3+3(OH)6(SO4)2 / 
Rodney Burton / Jarosite, KFe3+3(OH)6(SO4)2
Camera location52° 25′ 23.1″ N, 0° 06′ 25″ E Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location52° 25′ 23.1″ N, 0° 06′ 25″ E Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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Attribution: Rodney Burton
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9 June 2007

52°25'23.12"N, 0°6'25.20"E

52°25'23.12"N, 0°6'25.20"E

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current18:58, 4 February 2011Thumbnail for version as of 18:58, 4 February 2011480 × 640 (429 KB)GeographBot== {{int:filedesc}} == {{Information |description={{en|1=Jarosite, KFe3+3(OH)6(SO4)2 Jarosite is a straw-yellow basic sulphate that forms on the oxidation of iron sulphides (FeS2) in soils and sediments. This soil sample was removed from the subsoil of
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