4.7 Article

Dynamic changes in size-fractionated dissolved organic matter composition in a seasonally ice-covered Arctic River

期刊

LIMNOLOGY AND OCEANOGRAPHY
卷 66, 期 8, 页码 3085-3099

出版社

WILEY
DOI: 10.1002/lno.11862

关键词

-

资金

  1. National Science Foundation [EAR-0554781]
  2. University of Wisconsin-Milwaukee [DIG-101X405]
  3. Freshwater Collaborative of Wisconsin
  4. UWM's Distinguished Dissertation Fellowship

向作者/读者索取更多资源

Arctic rivers are sensitive to climate and environmental change, but the biogeochemical response is poorly understood. Through the analysis of monthly size-fractionated dissolved organic matter samples using various spectroscopy techniques, insights were gained into the seasonal variation in DOM composition for different size-fractions and the dynamics of source waters.
Arctic rivers are sensitive to climate and environmental change, but the biogeochemical response remains poorly understood. Monthly size-fractionated dissolved organic matter (DOM) samples from the lower Yukon River were characterized using UV-visible, fluorescence, and Fourier transform-infrared (FT-IR) spectroscopy techniques. The EEM-PARAFAC analysis revealed three major fluorescent DOM components, including two humic-like components (C-480 and C-400) and one protein-like component (C-310), with their relative importance following the order of C-480 >= C-400 > C-310 in the high-molecular-weight DOM (1 kDa-0.4 mu m) and C-400 > C-480 > C-310 in the low-molecular-weight DOM pool (< 1 kDa). Transformation in DOM and change in sources were manifested in major fluorescent components and optical properties, including biological index (BIX), humification index (HIX), spectral slope (S275-295) and specific UV absorbance at 254 nm (SUVA(254)). These changes occurred within different DOM size-fractions and among ice-covered, spring freshet, and open seasons. Joint analysis of EEM and FT-IR spectra using a data fusion technique showed that humic-like DOM is mostly associated with CH, CC, and CO bonds, while protein-like DOM is correlated more with CN and NH related structures. DOM aromaticity and the ratios of HIX to BIX and protein-like to humic-like components may be used as a compelling proxy to measure change in source waters and to infer permafrost dynamics. Our results provide insight into the seasonal variation in DOM composition for different size-fractions in the lower Yukon River, and a baseline dataset against which future changes can be understood in the context of arctic basin biogeochemical cycling.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据