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首页> 外文期刊>Aquatic Sciences >Spatial models as a tool to identify spatial patterns of surficial sediment composition and their contributing factors in the littoral zone of Lake Constance (Germany)
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Spatial models as a tool to identify spatial patterns of surficial sediment composition and their contributing factors in the littoral zone of Lake Constance (Germany)

机译:空间模型作为识别博登湖沿岸带表层沉积物组成的空间格局及其影响因素的工具(德国)

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摘要

For a lake-wide investigation of littoral surface sediments, we collected approximately 800 samples from Lake Constance along 235 parallel transects of 1 km distance along the shore at water depths of 1, 2, 4 and 8 m. Sediment samples were analyzed for the presence of spatial patterns in mineralogical and granulometric composition and contents of carbon and sulphur, with the purpose of identifying general and lake specific processes that contribute to the observed patterns. In particular, we wanted to test if the general factors known for contributing to littoral sediment composition could be revealed by spatial modeling of a dataset based on a systematic sampling scheme. Explanatory variables for a regression model were derived from GIS-analyses of the dataset, and also from other available data on Lake Constance. Highest levels of variance explained by the model (30-40%) were reached for the parameters calcite, clay minerals, sulphur and inorganic carbon content. Regional patterns in sediment composition, described by the proportion of explained between-transect variance (VE_t) in the model, are explained by up to 70%. The observed east-west gradient of mineralogical sediment composition is ascribed to the respective regional patterns of allogenic and endogenic sources. Allogenic minerals such as clay, dolomite and quartz dominate the littoral surface sediments of the eastern part of the lake and the areas near river mouths. Endogenic minerals like calcite dominate the littoral sediments of the western parts of the lake, reflecting internal process of biogenic carbonate precipitation that corresponds to the distribution patterns of submersed macrophytes (particularly Charophytes). This study confirms the major factors contributing to littoral sediment composition found in previous studies. However, their explanatory power for spatial patterns of a specific lake will be weak if respective spatial patterns of influence are neglected. The present study provides a guide to future sampling schemes and corresponding spatial statistics for lake specific application of general models. It also provides a basis to support engineering decisions for specific lake development.
机译:为了在全湖范围内调查沿海地表沉积物,我们在沿水深分别为1、2、4和8 m的沿岸1公里的235个平行样点中,从康斯坦茨湖收集了大约800个样本。分析了沉积物样品的矿物学和粒度组成以及碳和硫含量的空间格局,目的是确定有助于观测格局的一般和湖泊特定过程。特别是,我们想测试是否可以通过基于系统采样方案的数据集空间建模来揭示有助于沿海沉积物成分的一般因素。回归模型的解释变量来自数据集的GIS分析,也来自康斯坦茨湖上的其他可用数据。方解石,粘土矿物,硫和无机碳含量的参数达到了模型所解释的最高变化水平(30-40%)。用模型中解释的横断面间方差(VE_t)的比例描述的沉积物组成的区域模式最多可以解释70%。观察到的矿物沉积物组成的东西向梯度被归因于异源和内源的各自区域格局。诸如粘土,白云石和石英之类的同质矿物主导着湖东部和河口附近地区的沿海地表沉积物。方解石等内生矿物在该湖西部沿海沉积物中占主导地位,反映出生物碳酸盐沉淀的内部过程,这与沉没大型植物(尤其是Charophytes)的分布模式相对应。这项研究证实了先前研究中发现造成沿海沉积物成分的主要因素。但是,如果忽略各自影响的空间格局,那么它们对特定湖泊空间格局的解释力将很弱。本研究为一般模型在特定湖中的应用提供了未来采样方案和相应空间统计的指南。它还为支持特定湖泊开发的工程决策提供了基础。

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