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基于悬浮物浓度模型化的旧金山湾微量元素浓度和分配。

Modeled trace element concentrations and partitioning in the San Francisco estuary, based on suspended solids concentration.

机构信息

Department of Ocean Sciences, University of California, Santa Cruz, California 95064, USA.

出版信息

Environ Sci Technol. 2010 Aug 1;44(15):5956-63. doi: 10.1021/es1001874.

Abstract

Although trace element (Ag, As, Cd, Co, Cr, Cu, Fe, Hg, Mn, Ni, Pb, Se, and Zn) and methylmercury (MeHg) concentrations have been systematically sampled 1-3 times per year throughout the San Francisco Bay estuary for more than two decades, those collections do not capture episodic events that may govern the biogeochemical cycles of these elements in the Bay and adjacent Pacific coastal waters. Analyses of the partitioning of in situ elemental concentrations between particulate and total dissolved (<0.45 microm) phases coupled with optically based measurements of suspended solids concentration (SSC) showed highly significant (p<0.001) associations between all elemental concentrations and SSC in the Bay. Predictive models were developed to estimate the distribution ratio (D), or partition coefficient (Kd), and total concentration of each element in the water column based solely on SSC measurements. Modeled predictions of total element concentrations and distribution ratios were then coupled with measured SSC to predict the concentrations of dissolved trace elements in the water column. These predicted total and dissolved concentrations of trace elements can provide both better diagnostics of biogeochemical cycling within the estuary and better estimates of fluxes to adjacent coastal waters, overcoming the limitations of the long-running but limited direct measurements of trace elements from existing sampling programs.

摘要

尽管在过去的二十多年里,旧金山湾流域已经系统地每年采集 1-3 次痕量元素(Ag、As、Cd、Co、Cr、Cu、Fe、Hg、Mn、Ni、Pb、Se 和 Zn)和甲基汞(MeHg)的浓度,但这些采集并不能捕捉到可能控制这些元素在海湾和相邻太平洋沿海水域生物地球化学循环的偶发事件。原位元素浓度在颗粒相与总溶解(<0.45 微米)相之间分配的分析,以及基于悬浮物浓度(SSC)的光学测量表明,所有元素浓度与海湾中的 SSC 之间存在高度显著的关联(p<0.001)。开发了预测模型,仅根据 SSC 测量值来估计水柱中各元素的分配比(D)或分配系数(Kd)和总浓度。然后,将模型预测的总元素浓度和分配比与实测的 SSC 相结合,以预测水柱中痕量元素的溶解浓度。这些预测的痕量元素总浓度和溶解浓度不仅可以更好地诊断河口内的生物地球化学循环,还可以更好地估计向相邻沿海水域的通量,克服了现有采样计划中痕量元素长期但有限的直接测量的局限性。

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