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Variability in the light absorption coefficients of phytoplankton, nonalgal particles, and colored dissolved organic matter in a subtropical bay (Brazil)

机译:亚热带海湾(巴西)中浮游植物,非藻类颗粒和有色溶解有机物的光吸收系数的变化

摘要

This study characterized the variability in magnitudes and spectral shapes of the absorption coefficients of phytoplankton, detritus, and colored dissolved organic matter (CDOM) in a dynamic bay (Santos Bay) in southeastern Brazil in response to the contributions of the main estuarine channel and large tide variations, therefore in different time scales. Two strategies were adopted: (1) monthly year-round sampling in the estuarine channel and Santos Bay and (2) sampling in Santos Bay during spring/neap tides and cold/warm months. Chlorophyll-a concentration and CDOM absorption were higher during warm (wet) months, while the relative contribution of organic and inorganic particles was driven by neap/spring tide cycles. Salinity partially accounted for changes in optical variables, especially for CDOM absorption and total suspended matter (TSM) during cold months and neap tides, respectively. The spectral shapes of detritus and CDOM absorption showed relatively little variability for the entire dataset and were not considered feasible for monitoring purposes. The spectral shape of phytoplankton absorption (index of cell size) varied broadly, with no remarkable dependence on the sampling conditions. Comparison of absorption coefficients measured by the Quantitative Filter Technique (QFT) and Transmittance Reflectance (TR) method showed higher phytoplankton coefficients toward longer visible wavelengths (flatter spectra) and shallower slopes of detritus absorption yielded by the TR method. Our results also suggest that measurements at the near red spectral region result from not only scattering signals but also non-algal particle absorption.
机译:这项研究描述了巴西东南部一个动态海湾(桑托斯湾)中浮游植物,碎屑和有色溶解有机物(CDOM)的吸收系数的大小和频谱形状的变化,以响应主要河道和大型河道的贡献。潮汐变化,因此在不同的时间范围内。采取了两种策略:(1)在春季/潮汐潮和寒冷/温暖的月份在河口海峡和桑托斯湾进行年度全年采样,(2)在桑托斯湾进行采样。在温暖(潮湿)的月份中,叶绿素a的浓度和CDOM的吸收较高,而有机和无机颗粒的相对贡献是由潮汐/潮汐周期驱动的。盐度部分地解释了光学变量的变化,尤其是寒冷季节和潮汐潮汐时期CDOM吸收和总悬浮物(TSM)的变化。碎屑的光谱形状和CDOM吸收对于整个数据集显示出相对较小的变化,并且被认为对于监测目的不可行。浮游植物吸收的光谱形状(细胞大小的指数)变化很大,与采样条件没有显着相关性。通过定量滤光片技术(QFT)和透射率反射(TR)方法测量的吸收系数的比较显示,浮游植物系数越高,可见波长越长(光谱越平坦),TR方法产生的碎屑吸收斜率越浅。我们的结果还表明,在近红色光谱区域的测量不仅来自散射信号,而且还来自非藻类颗粒吸收。

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