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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Small-scale temporal and spatial variability in the erosion threshold and properties of cohesive intertidal sediments
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Small-scale temporal and spatial variability in the erosion threshold and properties of cohesive intertidal sediments

机译:侵蚀阈值和粘性潮间带沉积物性质的小规模时空变化

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摘要

Intertidal mudflats can be highly patchy due to both biotic and abiotic variability. The problems caused by such patchiness for the measurement of the erosion threshold of sediments has only received limited attention, primarily because of the limitations of the devices used to measure erosion threshold. The cohesive strength meter (CSM) erosion device partly overcomes these problems because it can collect numerous Measurements in a short time. This paper assesses the effects of site selection, small-scale spatial patchiness in a diatom biofilm and small-scale temporal variability over a tidal emersion on file measurement of erosion thresholds of cohesive intertidal sediments. Measurements were made with three CSM devices over a complete tidal emersion and at the beginning of the next emersion in the Westerschelde estuary. the Netherlands, in April 2001. Three different criteria were used in site selection: random sampling, random sampling with a user-bias towards visible diatom biofilms and sampling of only visible diatom biofilm areas. This resulted in different patterns of the measured sediment erodability. Contact core samples were collected to measure bio-dependant properties of the sediment known to influence erosion characteristics (water content and carbohydrates). In addition, variations in algal biomass (F-0(15)) over time were measured at the sediment surface with a fluorescence monitoring system (FMS). Three different operational extractions of carbohydrates were analysed to assess the roles of different carbohydrates in stabilising the sediment (colloidal-S-, EDTA- extracted and ETOH-precipitated).
机译:由于生物和非生物变异性,潮间带滩涂可能高度斑驳。主要由于由于用于测量侵蚀阈值的装置的局限性,由这种用于沉积物的侵蚀阈值的测量的斑点引起的问题仅受到了有限的关注。内聚强度计(CSM)腐蚀装置部分地克服了这些问题,因为它可以在短时间内收集大量测量值。本文评估了位点选择,硅藻生物膜中的小规模空间斑块以及潮汐爆发中的小规模时间变化对粘性潮间带沉积物侵蚀阈值文件测量的影响。在整个潮汐爆发期间以及在韦斯特切尔德河口的下一次潮汐开始时,使用三个CSM设备进行了测量。于2001年4月在荷兰进行。地点选择使用了三种不同的标准:随机采样,对可见硅藻生物膜有偏见的用户抽样和仅对可见硅藻生物膜区域的采样。这导致测得的沉积物可蚀性的模式不同。收集接触岩心样品以测量已知影响侵蚀特征(水含量和碳水化合物)的沉积物的生物依赖性。此外,使用荧光监测系统(FMS)在沉积物表面测量了藻类生物量(F-0(15))随时间的变化。分析了三种不同的碳水化合物的操作性提取物,以评估不同碳水化合物在稳定沉积物中的作用(胶态S-,EDTA提取和ETOH沉淀)。

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