首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Bio-physical characterization of sediment stability in mudflats using remote sensing: A laboratory experiment
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Bio-physical characterization of sediment stability in mudflats using remote sensing: A laboratory experiment

机译:利用遥感对滩涂沉积物稳定性进行生物物理表征:实验室实验

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Mudflats are important for coastal zone ecosystems by providing wildlife habitat and by acting as natural sea defenses that serve to dissipate tidal and wave energy. Geomorphological models of these intertidal flats and estuaries require site-specific bio-physicochemical sediment parameters as input. Hyperspectral remote sensing can be used as a tool providing synoptic maps of these properties. However, the interpretation of hyperspectral remotely sensed images over mudflats is only possible if the appropriate bio-geophysical or empirical models for information extraction are available. Therefore, the objective of this paper was to model the effects of varying sediment properties on the reflectance in laboratory conditions. The methodology consisted of (i) hyperspectral measurements of sediment mixtures with varying physical and biological characteristics in laboratory conditions, (ii) determination and quantification of specific absorption features and (iii) regression between the absorption features and physical parameters. In laboratory conditions, quantification of clay in dry sediment, moisture in unsaturated sediment and chlorophyll a in sediment mixtures was achieved with coefficients of determination (r~2) of 0.98, 0.90 and of 0.96 using the scaled band area of absorption features at 2204, 1450 and 673 nm, respectively. Additionally, the water absorption at 1190 nm was identified as suitable to predict moisture content in very wet sediment and preliminary results showed the potential of hyperspectral signals to assess the effect of bioturbation on sediment properties. Future work will consider the applicability of this methodology in field situations to relate bio-physical sediment parameters to the hyperspectral signal.
机译:滩涂对沿海地区的生态系统很重要,它可以为野生生物提供栖息地,并起到消散潮汐和波浪能的天然海洋防御作用。这些潮间带和河口的地貌模型需要特定地点的生物物理化学沉积参数作为输入。高光谱遥感可以用作提供这些属性概要图的工具。但是,只有在有合适的信息提取生物地球物理或经验模型可用的情况下,才有可能对泥滩上的高光谱遥感图像进行解释。因此,本文的目的是模拟实验室条件下不同沉积物特性对反射率的影响。该方法包括:(i)在实验室条件下对具有不同物理和生物学特征的沉积物混合物进行高光谱测量,(ii)确定和量化特定吸收特征,以及(iii)吸收特征与物理参数之间的回归。在实验室条件下,使用在2204处吸收特征的标定能带面积,可以对干沉积物中的粘土,不饱和沉积物中的水分和沉积物混合物中的叶绿素a进行定量,测定系数(r〜2)为0.98、0.90和0.96。分别为1450和673 nm。此外,已确定在1190 nm处的吸水率适合预测非常潮湿的沉积物中的水分含量,初步结果表明,高光谱信号可能会评估生物扰动对沉积物性质的影响。未来的工作将考虑该方法在现场情况下的适用性,以将生物物理沉积物参数与高光谱信号相关联。

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