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• W2767201487 startingPage "768" @default.
• W2767201487 abstract "Abstract The distribution of phosphorus (P) along a loess–limestone soil transect were investigated to delineate the spatial variation of the nutrient vertically in the soil profiles and laterally in the landscape. We hypothesized that spatial P patterns result from translocation caused by P mobilization, although P fixation would be expected along the slope. To depict this, three P fractions clearly differing in solubility were determined. Soil samples were treated with 0.1 M hydrochloric acid (HCl), with 12.1 M HCl, and with aqua regia (AR). In the profiles the spatial P distribution slightly corresponds to the occurrence of different bedrocks and substrata. Thus, a native “P loading” might not primarily explain the spatial P patterns. Especially the strong enrichment of the toeslope with easily soluble P indicates P translocation and prior mobilization. The enrichment is detectable throughout the profiles. Thus, superficial translocation ( e.g ., erosion) cannot sufficiently explain that pattern. Instead, underground processes must be the cause for this. They cause relatively high vertical and lateral variation in the spatial P distribution, e.g ., within soil horizons and substratum layers. Hence, mixed sampling of soil sections might not produce data accurate enough for some kinds of P research and for P management. Also, the lateral P distribution should be detected more precisely prior to fertilization of agricultural land." @default.
• W2767201487 created "2017-11-10" @default.
• W2767201487 creator A5034058515 @default.
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• W2767201487 date "2017-10-23" @default.
• W2767201487 modified "2023-10-03" @default.
• W2767201487 title "Soil phosphorus dynamics along a loess–limestone transect in Mihla, Thuringia (Germany)" @default.
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• W2767201487 doi "https://doi.org/10.1002/jpln.201700324" @default.
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