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Variations in light absorption properties during a phytoplankton bloom in the Pearl River estuary

机译:珠江口浮游植物开花过程中光吸收特性的变化

摘要

From 15 to 28 August in 2007, a Chaetoceros socialis bloom was detected in the Pearl River Estuary water with chlorophyll a concentration (Chl a) up to 30 mg m(-3) and cell density up to 10(6) cells L-1. Time series of bio-optical measurements was obtained at a single site (114.29 degrees E, 22.06 degrees N) with the mooring of marine optical buoy. Light absorption properties of seawater experienced large variability throughout the algal bloom. Absorption by colored dissolved organic matter (CDOM) was one of the dominant optical components of the light absorption (30-70%) especially for pre- and post-bloom waters, and it tended to decrease with Chl a during the algal bloom. Absorption by phytoplankton was another dominant optical component (18-50%) and increased rapidly with Chl a. Phytoplankton and accompanying material played dominant roles in light absorption as indicated by the relationship between absorption coefficient and Chl a. At high pigment concentrations, water samples showed significantly lower specific phytoplankton absorption, compared with pre- and post-bloom conditions, with the specific phytoplankton concentration at 443 nm varied between 0.011 and 0.022 m(2) mg(-1) and that at 676 nm between 0.007 and 0.018 m(2) mg(-1); small values of blue-to-red ratio of phytoplankton were also observed. These lower values were associated with variations in phytoplankton size structure. Spectral variability of phytoplankton absorption and total absorption (not including the fixed background absorption by pure water itself) could be expressed as simple linear functions linking absorption at one wavelength to the absorption at the other wavelengths, with the slope of the relationship changing with wavelength. The absorption coefficients by non-algal particles and CDOM follow the general exponential functions with remarkably limited variability in the exponent with means of 0.0105 and 0.0166 nm(-1), respectively. These spectral dependencies of absorption coefficients provide useful information for retrieving inherent optical properties from reflectance data in a remote-sensing context. (C) 2010 Elsevier Ltd. All rights reserved.
机译:从2007年8月15日至28日,在珠江口水中检测到一个Chaetoceros socialis绽放,其叶绿素a浓度(Chl a)高达30 mg m(-3),细胞密度高达10(6)个L-1细胞。随着海洋光学浮标的系泊,在单个位置(东经114.29度,北经22.06度)获得了生物光学测量的时间序列。整个藻华期间,海水的光吸收特性经历了很大的变化。有色溶解有机物(CDOM)的吸收是吸光的主要光学成分之一(占30-70%),尤其是在开花前和开花后的水中,并且在藻华期间,随着Chla的增加,吸收率趋于下降。浮游植物的吸收是另一个主要的光学成分(18-50%),并且随着Chla迅速增加。如吸收系数与Chla的关系所示,浮游植物和伴生物质在光吸收中起主要作用。在高色素浓度下,水样显示出的水浮游生物吸收率与开花前后相比明显降低,在443 nm处的浮游生物比浓水浓度在0.011至0.022 m(2)mg(-1)和676之间变化nm在0.007至0.018 m(2)mg(-1)之间;浮游植物的蓝红比例也很小。这些较低的值与浮游植物大小结构的变化有关。浮游植物吸收和总吸收的光谱变异性(不包括纯水本身的固定背景吸收)可以表示为简单的线性函数,将一个波长的吸收与其他波长的吸收联系起来,关系的斜率随波长而变化。非藻类颗粒和CDOM的吸收系数遵循一般的指数函数,指数的可变性分别受到限制,分别为0.0105和0.0166 nm(-1)。吸收系数的这些光谱相关性为在遥感环境中从反射率数据中检索固有光学特性提供了有用的信息。 (C)2010 Elsevier Ltd.保留所有权利。

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