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Biogeochemical origins of particles obtained from the inversion of the volume scattering function and spectral absorption in coastal waters

机译:沿海水域中体积散射函数和光谱吸收反演获得的颗粒的生物地球化学起源

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In the aquatic environment, particles can be broadly separated into phytoplankton (PHY), non-algal particle (NAP) and dissolved (or very small particle, VSP) fractions. Typically, absorption spectra are inverted to quantify these fractions, but volume scattering functions (VSFs) can also be used. Both absorption spectra and VSFs were used to estimate particle fractions for an experiment in the Chesapeake Bay. A complete set of water inherent optical properties was measured using a suite of commercial instruments and a prototype Multispectral Volume Scattering Meter (MVSM); the chlorophyll concentration, [Chl] was determined using the HPLC method. The total scattering coefficient measured by an ac-s and the VSF at a few backward angles measured by a HydroScat-6 and an ECO-VSF agreed with the LISST and MVSM data within 5%, thus indicating inter-instrument consistency. The size distribution and scattering parameters for PHY, NAP and VSP were inverted from measured VSFs. For the absorption inversion, the "dissolved" absorption spectra were measured for filtrate passing through a 0.2 μm filter, whereas [Chl] and NAP absorption spectra were inverted from the particulate fraction. Even though the total scattering coefficient showed no correlation with [Chl], estimates of [Chl] from the VSF-inversion agreed well with the HPLC measurements (r Combining double low line 0.68, mean relative errors Combining double low line-20%). The scattering associated with NAP and VSP both correlated well with the NAP and "dissolved" absorption coefficients, respectively. While NAP dominated forward, and hence total, scattering, our results also suggest that the scattering by VSP was far from negligible and dominated backscattering. Since the sizes of VSP range from 0.02 to 0.2 μm, covering (a portion of) the operationally defined "dissolved" matter, the typical assumption that colored dissolved organic matter (i.e., CDOM) does not scatter may not hold, particularly in a coastal or estuarine environment.
机译:在水生环境中,颗粒可以大致分为浮游植物(PHY),非藻类颗粒(NAP)和溶解的(或非常小的颗粒,VSP)级分。通常,将吸收光谱倒置以量化这些分数,但也可以使用体积散射函数(VSF)。切萨皮克湾的实验中,吸收光谱和VSF均用于估算颗粒分数。使用一套商业仪器和一个原型多光谱体积散射仪(MVSM)测量了一套完整的水固有光学特性。用HPLC法测定叶绿素浓度[Chl]。由ac-s和VSF在HydroScat-6和ECO-VSF测得的几个向后角处测得的总散射系数与LISST和MVSM数据在5%之内相吻合,从而表明了仪器间的一致性。 PHY,NAP和VSP的尺寸分布和散射参数与测量的VSF颠倒了。对于吸收反转,测量了通过0.2μm过滤器的滤液的“溶解”吸收光谱,而[Chl]和NAP吸收光谱则是从颗粒级分反转的。即使总散射系数与[Chl]没有相关性,来自VSF反演的[Chl]估计值也与HPLC测量非常吻合(r合并双低线0.68,平均相对误差合并双低线20%)。与NAP和VSP相关的散射分别与NAP和“溶解”吸收系数相关。尽管NAP主导了向前的散射,因此总体上还是散射,但我们的结果也表明,VSP的散射远不能忽略,而且主导的反向散射也很远。由于VSP的大小范围为0.02至0.2μm,覆盖了操作中定义的“溶解”物质(的一部分),因此有色溶解有机物质(即CDOM)不扩散的典型假设可能无法成立,特别是在沿海地区或河口环境。

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