Laboratoire des Sciences et de l'Environnement, UMR 8212 (CEA/CNRS/UVSQ), Université Paris-Saclay, Domaine du CNRS, Avenue de la Terrasse, 91198 Gif-sur-Yvette Cedex, France.
E.A 6293, Laboratoire GéoHydrosystèmes Continentaux (GéHCO), Université F. Rabelais de Tours, Faculté des Sciences et Techniques, Parc de Grandmont, 37200 Tours, France.
Sci Total Environ. 2016 Oct 1;566-567:968-980. doi: 10.1016/j.scitotenv.2016.05.093. Epub 2016 Jun 11.
Soil erosion often supplies high sediment loads to rivers, degrading water quality and contributing to the siltation of reservoirs and lowland river channels. These impacts are exacerbated in agricultural catchments where modifications in land management and agricultural practices were shown to accelerate sediment supply. In this study, sediment sources were identified with a novel tracing approach combining cesium ((137)Cs) and strontium isotopes ((87)Sr/(86)Sr) in the Louroux pond, at the outlet of a lowland cultivated catchment (24km(2), Loire River basin, France) representative of drained agricultural areas of Northwestern Europe. Surface soil (n=36) and subsurface channel bank (n=17) samples were collected to characterize potential sources. Deposited sediment (n=41) was sampled across the entire surface of the pond to examine spatial variation in sediment deposits. In addition, a 1.10m sediment core was sampled in the middle of the pond to reconstruct source variations throughout time. (137)Cs was used to discriminate between surface and subsurface sources, whereas (87)Sr/(86)Sr ratios discriminated between lithological sources. A distribution modeling approach quantified the relative contribution of these sources to the sampled sediment. Results indicate that surface sources contributed to the majority of pond (μ 82%, σ 1%) and core (μ 88%, σ 2%) sediment with elevated subsurface contributions modeled near specific sites close to the banks of the Louroux pond. Contributions of the lithological sources were well mixed in surface sediment across the pond (i.e., carbonate sediment contribution, μ 48%, σ 1% and non-carbonate sediment contribution, μ 52%, σ 3%) although there were significant variations of these source contributions modeled for the sediment core between 1955 and 2013. These fluctuations reflect both the progressive implementation of land consolidation schemes in the catchment and the eutrophication of the pond. This original sediment fingerprinting study demonstrates the potential of combining radionuclide and strontium isotopic geochemistry measurements to quantify sediment sources in cultivated catchments.
土壤侵蚀常常为河流输送高含沙量水流,从而降低水质,并导致水库淤积和低地河流航道淤塞。在农业流域,土地管理和农业实践的改变被证明会加速泥沙供应,这些影响更为严重。在本研究中,通过一种新的示踪方法,结合铯(137Cs)和锶同位素(87Sr/86Sr),在卢瓦尔河流域低地耕作流域(法国,24km2)的 Louroux 池塘出口处确定了泥沙来源,该流域代表了西北欧排水农业区。采集了表层土壤(n=36)和地下河道岸坡(n=17)样本,以表征潜在来源。在整个池塘表面采集了沉积泥沙(n=41)样本,以检验沉积物的空间变化。此外,在池塘中部采集了 1.10m 的沉积物岩芯,以重建随时间变化的源变化。137Cs 用于区分表层和地下源,而 87Sr/86Sr 比值则用于区分岩性源。分布模型方法量化了这些源对采集到的泥沙的相对贡献。结果表明,表层源对池塘(μ 82%,σ 1%)和岩芯(μ 88%,σ 2%)沉积物的贡献最大,在 Louroux 池塘岸边附近的特定位置模拟出较高的地下贡献。在整个池塘的表层沉积物中,岩性源的贡献很好地混合在一起(即,碳酸盐沉积物的贡献,μ 48%,σ 1%和非碳酸盐沉积物的贡献,μ 52%,σ 3%),尽管在 1955 年至 2013 年期间,对岩芯沉积物的这些源贡献的模拟存在显著变化。这些波动反映了流域土地整治计划的逐步实施以及池塘的富营养化。这项原始的泥沙示踪研究表明,结合放射性核素和锶同位素地球化学测量,有潜力量化耕作流域的泥沙来源。