Articles | Volume 17, issue 10
Hydrol. Earth Syst. Sci., 17, 4269–4281, 2013
https://doi.org/10.5194/hess-17-4269-2013
Hydrol. Earth Syst. Sci., 17, 4269–4281, 2013
https://doi.org/10.5194/hess-17-4269-2013

Research article 30 Oct 2013

Research article | 30 Oct 2013

Spatiotemporal characterization of dissolved carbon for inland waters in semi-humid/semi-arid region, China

K. S. Song2,1, S. Y. Zang3, Y. Zhao1, L. Li2, J. Du1, N. N. Zhang3, X. D. Wang3, T. T. Shao1, Y. Guan3, and L. Liu3 K. S. Song et al.
  • 1Northeast Institute of Geography and Agroecology, CAS, Changchun, China
  • 2Department of Earth Sciences, Indiana University – Purdue University, Indianapolis, IN, USA
  • 3College of Geographical Science, Harbin Normal University, Harbin, China

Abstract. Spatiotemporal variations of dissolved organic carbon (DOC) and inorganic carbon (DIC) in 26 waters across the semi-humid/semi-arid Songnen Plain, China, were examined with data collected during 2008–2011. Fresh (n = 14) and brackish (n = 12) waters were grouped according to electrical conductivity (threshold = 1000 μS cm−1) Significant differences in the average DOC and DIC concentrations were observed between the fresh (5.63 mg L−1, 37.39 mg L−1) and the brackish waters (15.33 mg L−1, 142.93 mg L−1). Colored dissolved organic matter (CDOM) and DOC concentrations were mainly controlled by climatic–hydrologic conditions. The investigation indicated that the outflow conditions in the semi-arid region had condensed effects on the dissolved carbon, resulting in close relationships between salinity vs. DOC (R2 = 0.66), and salinity vs. DIC (R2 = 0.94). An independent data set collected in May 2012 also confirmed this finding (DOC: R2 = 0.79, DIC: R2 = 0.91), highlighting the potential of quantifying DOC and DIC via salinity measurements for waters dispersed in the plain. Indices based on the CDOM absorption spectra (e.g., the DOC-specific CDOM absorption (SUVA254), absorption ratio a250 : a365 (E250 : E365) and the spectral slope ratio (Sr, S275−295/S350−400) were applied to characterize CDOM composition and quality. Our results indicate that high molecular weight CDOM fractions are more abundant in the fresh waters than the brackish waters.

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