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改进原位荧光测量法估算河口和沿海湿地溶解有机碳(DOC)浓度。

Improving Estimates of Dissolved Organic Carbon (DOC) Concentration from In Situ Fluorescence Measurements across Estuaries and Coastal Wetlands.

机构信息

Department of Earth and Environment, Boston University, Boston, Massachusetts 02215, United States.

Department of Marine and Coastal Environmental Science, Texas A&M University, Galveston Campus, Galveston, Texas 77553, United States.

出版信息

Environ Sci Technol. 2024 May 28;58(21):9213-9226. doi: 10.1021/acs.est.3c10850. Epub 2024 May 15.

DOI:10.1021/acs.est.3c10850
PMID:38748643
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11138529/
Abstract

The use of optical proxies is essential to the sustained monitoring of dissolved organic carbon (DOC) in estuaries and coastal wetlands, where dynamics occur on subhour time scales. In situ dissolved organic matter (DOM) fluorescence, or FDOM, is now routinely measured along with ancillary water-quality indicators by commercial sondes. However, its reliability as an optical proxy of DOC concentration is often limited by uncertainties caused by in situ interferences and by variability in DOM composition and water matrix (ionic strength, pH) that are typical at the land-ocean interface. Although corrections for in situ interferences already exist, validated strategies to account for changes in the DOM composition and water matrix in these systems are still lacking. The transferability of methods across systems is also poorly known. Here, we used a comprehensive data set of laboratory-based excitation-emission matrix fluorescence and DOC concentration matched to in situ sonde measurements to develop and compare approaches that leverage ancillary water-quality indicators to improve estimates of DOC concentration from FDOM. Our analyses demonstrated the validity of in situ interference correction schemes, the importance of ancillary water-quality indicators to account for DOM composition and water matrix change, and the good transferability of the proposed methods.

摘要

在河口和沿海湿地中,由于动态变化发生在亚小时时间尺度上,因此使用光学代理对于持续监测溶解有机碳(DOC)至关重要。原位溶解有机物(DOM)荧光或 FDOM 现在通常与商业探测器一起测量辅助水质指标。然而,其作为 DOC 浓度的光学代理的可靠性通常受到原位干扰和 DOM 组成和水基质(离子强度、pH 值)变化引起的不确定性的限制,这些变化在陆海界面很常见。尽管已经存在针对原位干扰的校正方法,但在这些系统中仍然缺乏针对 DOM 组成和水基质变化的验证策略。方法在不同系统之间的可转移性也知之甚少。在这里,我们使用了一个基于实验室的激发-发射矩阵荧光和与原位探测器测量相匹配的 DOC 浓度的综合数据集,开发并比较了利用辅助水质指标来提高 FDOM 估算 DOC 浓度的方法。我们的分析证明了原位干扰校正方案的有效性、辅助水质指标对于解释 DOM 组成和水基质变化的重要性,以及所提出方法的良好可转移性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/28ed52bb5a71/es3c10850_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/bf1d7d5b6f22/es3c10850_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/f8f2a47a9937/es3c10850_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/911e09049811/es3c10850_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/3665b09ecff6/es3c10850_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/43c10e9a24a6/es3c10850_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/28ed52bb5a71/es3c10850_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/bf1d7d5b6f22/es3c10850_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/f8f2a47a9937/es3c10850_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/911e09049811/es3c10850_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/3665b09ecff6/es3c10850_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/43c10e9a24a6/es3c10850_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8b18/11138529/28ed52bb5a71/es3c10850_0006.jpg

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本文引用的文献

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加拿大安大略省南部和不列颠哥伦比亚省河流流域中的叶绿素-a、溶解有机碳、浊度和其他具有生态重要性的变量。
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