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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Temporal and spatial distributions of moisture and organic contents across a macro-tidal mudflat
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Temporal and spatial distributions of moisture and organic contents across a macro-tidal mudflat

机译:潮间带滩涂中水分和有机物的时空分布

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The purpose of this study was to make comprehensive surface measurements of the changes in moisture and organic contents across the Skeffling mudflats (Humber Estuary, UK) and to examine the effects of exposure and location on the sediment properties. Sediment cores were collected using modified 50 mi syringes, and the data compared with measurements of chlorophyll a and colloidal carbohydrate concentrations. The temporal and spatial relationships between these surface sediment properties were quantified and related to the measured critical erosion shear stress. Moisture and organic contents correlate significantly with respect to morphology, both across the mudflat and with depth below the sediment surface, These variations affected the distributions of bulk density and sediment erodibility, although these two variables were not directly related. The relatively coarse vertical resolution of the cores prevented clear relationships being identified between critical erosion shear stress, moisture and organic contents, and the chlorophyll a and colloidal carbohydrate concentrations. Analysis of mean values removed some of the spatial variability and a reasonable exponential relationship was obtained between erosion shear stress and colloidal carbohydrate. This paper highlights the influence of the physical, morphological and biological characteristics of the surface sediment upon its erosion resistance. The implications for the development of the surface morphology and mudflat are considered. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 20]
机译:这项研究的目的是对Skeffling滩涂中水分和有机物含量的变化进行全面的表面测量,并研究暴露和位置对沉积物特性的影响。使用改良的50 mi注射器收集沉积物芯,并将数据与叶绿素a和胶体碳水化合物浓度的测量值进行比较。这些表面沉积物特性之间的时间和空间关系被量化并与测得的临界侵蚀剪切应力有关。在整个泥滩和沉积物表面以下的深度,水分和有机物含量均与形态显着相关。尽管这两个变量没有直接关系,但这些变化影响了堆积密度和沉积物易蚀性的分布。岩心的相对较粗的垂直分辨率阻止了在临界侵蚀剪切应力,水分和有机物含量以及叶绿素a和胶体碳水化合物浓度之间的明确关系。平均值分析消除了一些空间变异性,并且在侵蚀剪切应力和胶体碳水化合物之间获得了合理的指数关系。本文重点介绍了表面沉积物的物理,形态和生物学特性对其耐蚀性的影响。考虑了对表面形态和泥滩发展的影响。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:20]

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