2005
DOI: 10.3133/ofr20051178
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Sediment chemistry of the Colorado River delta of Lake Powell, Utah, 2001

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Cited by 7 publications
(1 citation statement)
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“…In a bottom sediment core from Lake Powell, Utah (Fig. 10 in Hart et al 2005), the B concentration peak at the boundary of ferrous Fe oxidation (indicated by the typical colour shift) is clearly seen, most probably as the result of B coprecipitation via sorption onto ferric Fe compounds. Thus, B mobility can indirectly be affected by sediment redox processes.…”
Section: Bottom Sedimentsmentioning
confidence: 99%
“…In a bottom sediment core from Lake Powell, Utah (Fig. 10 in Hart et al 2005), the B concentration peak at the boundary of ferrous Fe oxidation (indicated by the typical colour shift) is clearly seen, most probably as the result of B coprecipitation via sorption onto ferric Fe compounds. Thus, B mobility can indirectly be affected by sediment redox processes.…”
Section: Bottom Sedimentsmentioning
confidence: 99%