2009
DOI: 10.1016/j.apgeochem.2008.11.006
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Mobility of major-, minor- and trace elements in solutions of a planosolic soil: Distribution and controlling factors

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Cited by 6 publications
(9 citation statements)
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“…3). In the upper horizon, the thermodynamic calculations suggest the same, which is not in line with the monitoring results (no binary correlation was recorded in the upper horizon, in contrast to the concretion-rich horizon [Pelfrêne et al, 2009]). In this horizon, the soil matrix may have a greater impact.…”
Section: Coppersupporting
confidence: 47%
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“…3). In the upper horizon, the thermodynamic calculations suggest the same, which is not in line with the monitoring results (no binary correlation was recorded in the upper horizon, in contrast to the concretion-rich horizon [Pelfrêne et al, 2009]). In this horizon, the soil matrix may have a greater impact.…”
Section: Coppersupporting
confidence: 47%
“…The chemical characteristics of soil solutions recorded in the three sites differ due to rate of weathering and water circulation [Pelfrêne et al, 2009]. The speciation distribution observed between the two horizons could also be linked to horizon matrix composition, and to the water residence time and chemical reactivity of the circulating solution.…”
Section: Modelling Of Trace Metal Speciationmentioning
confidence: 95%
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“…The bioavailability of trace elements in the soil is decisive for agriculture purposes. The speciation of trace metals ultimately determines their bioavailability and their mobility in the soil (Pelfrêne et al, 2009). A number of trace elements (Cu, Zn, Pb, Fe, Cr, Co, Cd and Ni) are contributed through the weathering of igneous and sedimentary rocks in the study area.…”
Section: Trace Elementsmentioning
confidence: 99%