Explaining and mapping total phosphorus content in French topsoils

被引:29
作者
Delmas, M. [1 ]
Saby, N. [1 ]
Arrouays, D. [1 ]
Dupas, R. [2 ,3 ]
Lemercier, B. [2 ,3 ]
Pellerin, S. [4 ]
Gascuel-Odoux, C. [2 ,3 ]
机构
[1] INRA Infosol, Orleans, France
[2] INRA, UMR1069, Sol Agro & Hydrosyst Spatialisat, F-35000 Rennes, France
[3] Agrocampus Ouest, Sol Agro & Hydrosyst Spatialisat, UMR1069, F-35000 Rennes, France
[4] INRA, UMR1391, Atmosphere Plant Soil Interact, Bordeaux, France
关键词
Total phosphorus; mapping; spatial analysis; multiple linear regression model; controlling factors; SOIL-PHOSPHORUS; EUTROPHICATION; SEDIMENT; IMPACT; LEVEL; FLOWS; FORMS; MODEL; RISK;
D O I
10.1111/sum.12192
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Total phosphorus (TP) build-up in agricultural soils represents both a threat to aquatic ecosystems and a valuable resource for future crop production, given the context of increasing food demand combined with the rapid depletion of the world's phosphate reserves. Therefore, it is crucially important (i) to identify the main factors controlling topsoil TP and (ii) to develop methods for mapping its spatial distribution. Multiple linear regression models were used with two distinct approaches to calculate TP and covariates linked to the P cycle. Firstly, covariates were selected from the Reseau de Mesures de la Qualite des Sols database, the French soil monitoring network, which consists of soil samples collected from 2158 sites on a 16-km regular grid. Secondly, covariates were selected to map TP from spatially exhaustive datasets in France. The first approach explains 80% of variability in topsoil TP. The variables selected are linked to the autochthonous origin of P (parent material), to allochthonous origin (organic carbon and nitrogen contents) and to the retention capacity of soil (Al, Fe, Ca and clay contents). The predicted map obtained from the second approach provides a mean TP of 0.76g/kg. This study demonstrates that creating national scale maps of TP, based on detailed soil sampling and many variables, is feasible and can be used to model the P cycle and P transfer processes. Such maps can be used in P erosion and transfer models over river basins, and therefore to predict P exports to surface waters.
引用
收藏
页码:259 / 269
页数:11
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