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Application of a chemical leach technique for estimating labile particulate aluminum, iron, and manganese in the Columbia River plume and coastal waters off Oregon and Washington

机译:化学浸出技术在俄勒冈州和华盛顿的哥伦比亚河羽流岩石羽状岩,铁和锰的应用

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摘要

In order to determine the total concentration of bioavailable trace metals in seawater, measurement of both the dissolved and labile particulate fractions is necessary. Comparison of labile particulate metal concentrations from various researchers is limited because of differing definitions of the fraction that is potentially available to phytoplankton on a time frame of generations. A comparison experiment was conducted on coastal and riverine suspended particulate matter to determine the difference between several commonly used techniques that operationally define the labile particulate trace metal fraction. Furthermore, we compared two leach techniques for surface transect samples from within the Columbia River plume and water offshore of Oregon and Washington, United States. The particulate trace metal concentration in the leachate was determined by high-resolution inductively coupled plasma–mass spectrometry. From this comparison, one chemical leach was chosen to best define the labile particulate fraction of Al, Fe, and Mn: a weak acid leach (25% acetic acid at pH 2) with a mild reducing agent (0.02 M hydroxylamine hydrochloride) and a short heating step (10 min 90–95°C). This leach was applied to three surface transects within the Columbia River plume. These coastal waters were found to be rich in labile particulate trace metals that are directly delivered from the Columbia River and indirectly supplied via resuspension from upwelling over a broad continental shelf.
机译:为了确定海水中生物可利用的痕量金属的总浓度,需要溶解和不稳定颗粒馏分的测量。各种研究人员的不稳定颗粒金属浓度的比较是有限的,因为级分的不同定义可能在几代人的时间框架上可获得浮游植物。对沿海和河流悬浮颗粒物进行的比较实验,以确定在操作上定义不稳定颗粒痕量金属馏分的几种常用技术之间的差异。此外,我们将两种浸出技术与来自俄勒冈州和华盛顿华盛顿的哥伦比亚河羽流和水海上的表面横渗样品进行了两种浸出技术。通过高分辨率电感耦合等离子体质谱法测定渗滤液中的颗粒状痕量金属浓度。从这种比较中,选择一种化学浸出以最佳地定义Al,Fe和Mn的不稳定颗粒部分:弱酸浸出(pH 2下的25%乙酸),用轻度还原剂(0.02M羟胺)和a短加热步骤(10分钟90-95°C)。这种浸出在哥伦比亚河羽流内的三个表面横断面。这些沿海水域被发现富含不稳定的微粒痕量金属,这些痕量金属直接从哥伦比亚河送出,并通过重新悬浮,从升高到广阔的大陆架上。

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