1996
DOI: 10.1007/bf00192057
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Self-organization of recent rhythmic iron-manganese precipitations in underground mines in the Harz mountains

Abstract: A recent early diagenetic banded iron-manganese mud has been forming underground in a closed lead-zinc mine for approximately 40 years. The processes leading to the banded structure of the precipitate were studied during a period of 2 years. Therefore, 19 physical and chemical parameters were measured regularly in short intervals. The resulting time series were analysed with respect to the data sets of the monthly chemical analyses of the descendent mine water, the daily rainfall and the mineral content. The r… Show more

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“…A third group of papers investigated the incorporation of Al (Cismasu et al, 2012), Ga (Xu et al, 2007), Ge (Liang et al, 2008), In (Chou et al, 2009), Nd (Nagano et al, 1999) and Nb (Oliveira et al, 2009) in the (crystal) structure of ferrihydrite, goethite, hematite (a-Fe 2 O 3 ), or amorphous iron hydroxides. A fourth process is co-precipitation of separate phases like beryllium hydroxide (Be(OH) 2 ) (Burguera et al, 2000) and birnessite (MnO 2 $ H 2 O) (Dietrich and Jacob, 1996) together with ferrihydrite and/or other iron hydroxides.…”
Section: Introductionmentioning
confidence: 99%
“…A third group of papers investigated the incorporation of Al (Cismasu et al, 2012), Ga (Xu et al, 2007), Ge (Liang et al, 2008), In (Chou et al, 2009), Nd (Nagano et al, 1999) and Nb (Oliveira et al, 2009) in the (crystal) structure of ferrihydrite, goethite, hematite (a-Fe 2 O 3 ), or amorphous iron hydroxides. A fourth process is co-precipitation of separate phases like beryllium hydroxide (Be(OH) 2 ) (Burguera et al, 2000) and birnessite (MnO 2 $ H 2 O) (Dietrich and Jacob, 1996) together with ferrihydrite and/or other iron hydroxides.…”
Section: Introductionmentioning
confidence: 99%