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首页> 外文期刊>Journal of environmental monitoring: JEM >Identification of dredged sediment-derived soils in the alluvial plains of the Leie and the Upper and Sea Scheldt rivers (Belgium) based on physico-chemical soil properties
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Identification of dredged sediment-derived soils in the alluvial plains of the Leie and the Upper and Sea Scheldt rivers (Belgium) based on physico-chemical soil properties

机译:根据理化土壤特性,识别莱伊河冲积平原和Scheldt河上游和比利时的疏of沉积物土壤

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摘要

An approach was developed to identify surface soils affected by historical dredged sediment disposal in the alluvial plains of the Upper Scheldt, the Sea Scheldt and the Leie river. Dredged sediment-derived soils were identified based on field observations, comparative granulometric analyses and chemical analyses. Criteria developed were based on a comparison between reference data from 102 aerobic soil samples of areas known to e affected by dredged sediment disposal and 104 samples from undisturbed alluvial soils along the studied rivers. A comparative grain size analysis with optical laser diffractometry between the A and C horizon proved useful for the identification of levelled-up sites. The chemical soil characteristics that were most useful in identifying dredged sediment-derived soils were CaCO_3, sulfur (S), organic carbon (OC) and phosphorus (P) contents, electrical conductivity (EC), and the C/P and C/S ratios. Criteria for concluding the origin of an investigated soil were specific for the studied area, but the approach presented may provide useful guidelines for developing criteria valid for different regions.
机译:开发了一种方法来识别受历史疏sediment的沉积物影响的表土,这些沉积物是在上谢尔德,海谢尔德和莱伊河冲积平原上进行的。根据现场观察,比较粒度分析和化学分析,确定了疏sediment的沉积物来源的土壤。制定标准的依据是,对被研究疏sediment的沉积物影响的102个好氧土壤样品的参考数据与研究河流沿岸未冲积的土壤104个样品的参考数据进行比较。在A和C层之间使用光学激光衍射法对晶粒度进行比较分析,可用于鉴定平整部位。在识别疏sediment的沉积物来源的土壤中最有用的化学土壤特征是CaCO_3,硫(S),有机碳(OC)和磷(P)含量,电导率(EC)以及C / P和C / S比率。确定被调查土壤起源的标准是针对所研究区域的特定标准,但是提出的方法可能为制定适用于不同地区的标准提供有用的指导。

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