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Stable Carbon and Sulfur Isotope Characteristics of Stream Water in a Typical Karst Small Catchment, Southwest China
Water ( IF 3.0 ) Pub Date : 2021-02-18 , DOI: 10.3390/w13040523
Yang Tang , Ruiyin Han

Surface water samples from the Maolan National Natural Reserved Park (MNNRP) were analyzed from Sept. 2013 to June 2014, for major ion concentrations (K+, Na+, Ca2+, Mg2+, Cl, SO42−, HCO3), δ13C-DIC and δ34S-SO42− to quantify the sources of solutes and chemical weathering. The results show that HCO3 and SO42− are the main anions in Banzhai watershed, which account for 86.2 and 10.4% of the total anion equivalent, respectively. While Ca2+ and Mg2+ account for 76.9 and 20.5%, respectively. Considerable Mg2+ in stream water indicates that it may be affected by dolomite weathering. stream water samples present the δ13C-DIC values in the range of −16.9‰~−10.8‰ (mean value was −13.9‰), which were lower than that of the groundwater. The δ34S-SO42− values ranged from −15.2‰ to 1.7‰ (mean value was −4.4‰). There was a negative correlation between HCO3 content and δ13C value, implying the result of the interaction of temperature and precipitation intensity in different seasons. The significant positive correlation between SO42− content and δ13C-DIC indicates that H2SO4 may be involved in the weathering process of carbonate rocks in small watershed scale. The content of SO42− in a school sample site was much higher than that of other sample sites for the interference from human sources. The δ34S values show that the average δ34S-SO42− in most sites is close to the δ34S isotopic values of Guizhou coal and rain, indicating that they may be affected by local coal.

中文翻译:

典型西南喀斯特小流域溪流水的碳和硫同位素稳定特征

从茂兰国家自然保留公园(MNNRP)地表水样品进行分析,从2013年9月到2014年6月,为主要的离子浓度(K +,钠+,钙2+,镁2+,氯-,SO 4 2-, HCO 3 - ),δ 13 C-DIC和δ 34 S-SO 4 2-以量化溶质和化学风化的来源。结果表明,HCO 3 -和SO 4 2-在Banzhai主阴离子分水岭,分别占86.2和阴离子等效总的10.4%。而Ca 2+和Mg2+分别占76.9和20.5%。溪流水中大量的Mg 2+表明它可能会受到白云石风化的影响。流的水样呈现δ 13 C-DIC值-16.9‰〜-10.8‰范围内(平均值为-13.9‰),其明显低于地下水的下部。的δ 34 S-SO 4倍2-的值从-15.2‰至1.7‰范围(平均值为-4.4‰)。有HCO之间呈负相关3 -含量和δ 13 C值,这意味着温度和降水强度在不同的季节的相互作用的结果。SO 4 2−含量与δ之间呈显着的正相关13 C-DIC表明H 2 SO 4可能参与了小流域碳酸盐岩的风化过程。由于人为干扰,学校采样点的SO 4 2-含量远高于其他采样点。的δ 34价值观表明平均δ 34 S-SO 4 2-在大多数网站接近δ 34贵州煤和雨的同位素值,这表明它们可以通过本地煤的影响。
更新日期:2021-02-18
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