| 高砷地下水中溶解性有机碳和无机碳稳定同位素特征 |
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| 引用本文： | 周殷竹,郭华明,逯海.高砷地下水中溶解性有机碳和无机碳稳定同位素特征[J].现代地质,2015,29(2):252-259. |
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| 作者姓名： | 周殷竹 郭华明 逯海 |
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| 作者单位： | (1.中国地质大学(北京)生物地质与环境地质国家重点实验室，北京100083；
2.中国地质大学(北京)水资源与环境学院，北京100083；
3.中国计量科学研究院，北京100013) |
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| 基金项目： | 国家自然科学基金项目(41222020,41172224);霍英东基金会第十三届高等院校青年教师基金基础性研究课题(131017);中央高校基本科研项目(2652013028) |
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| 摘 要： | 随着稳定同位素分析技术的逐步完善，碳稳定同位素被广泛应用于地球化学领域。高砷地下水砷的生物地球化学循环是目前环境化学研究热点之一。分析概括了碳稳定同位素应用于地下水领域的研究现状，介绍了地下水中有机碳和无机碳稳定同位素的前处理方法以及测试技术。在此基础上，选取了内蒙古河套平原具有代表性的高砷地下水进行氧化还原敏感组分、碳稳定同位素的测定与分析。结果表明，As分布极不均匀，其含量为1.24~387 μg/L。地下水溶解性有机碳(DOC)含量相对较高，与溶解性无机碳(DIC)浓度基本呈正相关。δ13CDIC相对δ13CDOC较富集13C；δ13CDIC-δ13CDOC与δ13CDIC之间具有显著的正相关关系；表明δ13CDIC值越贫化，δ13CDIC-δ13CDOC越小，地下水中来源于有机物氧化分解的无机碳越多，进一步说明有机碳的氧化分解在无机碳稳定同位素贫化过程中起主要作用。此外，δ13CDIC-δ13CDOC与As浓度呈一定的负相关关系；表明有机物的微生物降解对砷的富集具有明显的促进作用。微生物可利用的碳源增加，促进异养微生物的代谢，并消耗氧气，最终形成有利于地下水As富集的还原环境。
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| 关 键 词： | 溶解性有机碳 溶解性无机碳 稳定同位素 地下水 砷 |
Stable Isotope Characteristics of Dissolved Organic Carbon and Inorganic Carbon in High Arsenic Groundwater |
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| ZHOU Yin-zhu;GUO Hua-ming;LU Hai.Stable Isotope Characteristics of Dissolved Organic Carbon and Inorganic Carbon in High Arsenic Groundwater[J].Geoscience——Journal of Graduate School,China University of Geosciences,2015,29(2):252-259. |
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| Authors: | ZHOU Yin-zhu;GUO Hua-ming;LU Hai |
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| Institution: | (1.State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing100083, China;
2.School of Water Resources and Environment, China University of Geosciences, Beijing100083, China;
3.National Institute of Metrology, Beijing100013, China) |
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| Abstract: | With improved technology for stable isotope analysis, stable carbon isotope has extensively been used in the field of geochemical study. Biogeochemical cycle of groundwater arsenic is one of the hot topics in environmental studies. This paper summarizes research status of stable carbon isotope in groundwater, and introduces pretreating methods and measuring technology of organic and inorganic carbon isotope. Representative groundwater samples with high As concentrations were collected from the Hetao basin, Inner Mongolia, and analyzed for redox sensitive components, stable carbon isotope in dissolved organic carbon (DOC) and dissolved inorganic carbon (DIC). Results indicate that As distribution is patchy with concentrations between 1.24 and 387 μg/L, and that DOC concentration is relatively high and positively correlated with DIC. In comparison with DOC, DIC is enriched in 13C. There is a positive correlation between δ13CDIC-δ13CDOC and δ13CDIC. It indicates that groundwater with low δ13CDIC and low δ13CDIC-δ13CDOC values has high contribution of DOC to DIC, which suggests that degradation of organic carbon results in depletion of 13C in DIC of groundwater. In addition, there is a negative correlation between δ13CDIC-δ13CDOC and As. In groundwater with low δ13CDICand low δ13CDIC-δ13CDOC values, high As concentrations are observed. High As groundwater experiences intensive biodegradation of organic carbon, and microbial degradation of organic matters plays a significant role in promoting the enrichment of As in groundwater. The increase in bioavailable organic carbon promotes microbial dissimilation, consumes dissolved oxygen, and leads to formation of reducing conditions favorable for As enrichment in groundwater. |
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| Keywords: | dissolved organic carbon dissolved inorganic carbon stable carbon isotope groundwater arsenic |
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