[Dissolved Organic Matter Component and Source Characteristics of the Metropolitan Lakes and Reservoirs in a Typical Karst Region].

Q2 Environmental Science 环境科学 Pub Date : 2022-07-08 DOI:10.13227/j.hjkx.202110159
Mao-Fei Ni, Hui Zhou, Yong-Mei Ma, Yin Su, Xiao-Dan Wang, Zhi-Kang Wang
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引用次数: 1

Abstract

In order to explore dissolved organic matter (DOM) components and their origins in metropolitan lakes and reservoirs in the karst region, the typical Hongfeng Lake, Baihua Lake, Songbaishan Reservoir, and Aha Reservoir were investigated in Guiyang City. Surface water parameters, including dissolved organic carbon (DOC), chlorophyll a (Chla), and optical parameters (a254, a280, a350, E2:E3, S275-295, FI, β:α, BIX, and HIX) were analyzed. Fluorescence peaks (B, T, A, M, C, D, and N) and three-dimensional matrix fluorescence with parallel factor analysis (EEM-PARAFAC) were employed to explain distinct DOM abundances and proportions. Meanwhile, Spearman's correlation coefficients and principal component analysis (PCA) were used to decipher parameter types and primary environmental processes. The results showed that aquatic ρ(DOC) and ρ(Chla) ranged between 4.24-11.9 mg·L-1 and 0.32-19.7 μg·L-1, respectively. High humic-like (a254) and protein DOM (a280) were observed in the Songbaishan Reservoir, resulting in higher DOM molecular weight when compared to that in other lakes and reservoirs. Surface water DOM mainly contained visible-light humic-like (23.8%-46.9%) and terrestrial fulvic-like components (17.6%-28.4%). High FI, β:α, and BIX but low HIX values in this study suggested that endogenous inputs largely contributed to aquatic DOM. Aquatic DOM component and source characteristics were significantly correlated with each other. Furthermore, inputs of humic-like DOM and microbial metabolism, as well as coupled carbonate dissolution and photosynthesis, drove dynamic DOM behaviors in the karst lakes and reservoirs.

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[典型喀斯特地区都市湖泊和水库溶解有机质组分及物源特征]。
为探讨喀斯特地区大都市湖泊和水库中溶解有机质(DOM)组成及其成因,以贵阳市典型的红峰湖、白花湖、松白山水库和阿哈水库为研究对象。分析了表层水参数,包括溶解有机碳(DOC)、叶绿素a (Chla)和光学参数(a254、a280、a350、E2:E3、S275-295、FI、β:α、BIX和HIX)。利用荧光峰(B、T、A、M、C、D和N)和三维基质荧光平行因子分析(EEM-PARAFAC)来解释不同的DOM丰度和比例。同时,利用Spearman相关系数和主成分分析(PCA)来解析参数类型和主要环境过程。结果表明,水体ρ(DOC)和ρ(Chla)分别为4.24 ~ 11.9 mg·L-1和0.32 ~ 19.7 mg·L-1。松白山水库中存在高腐殖质样DOM (a254)和蛋白DOM (a280), DOM分子量高于其他湖泊和水库。地表水DOM主要含有可见光腐植酸类成分(23.8% ~ 46.9%)和陆生腐殖酸类成分(17.6% ~ 28.4%)。在本研究中,高FI、β:α和BIX值但低HIX值表明内源性输入对水生DOM有很大贡献。水生DOM成分与源特征呈显著相关。此外,腐殖质样DOM和微生物代谢的输入,以及碳酸盐溶解和光合作用的耦合作用,驱动了喀斯特湖泊和储层中DOM的动态行为。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
环境科学
环境科学 Environmental Science-Environmental Science (all)
CiteScore
4.40
自引率
0.00%
发文量
15329
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