吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (2): 548-558.doi: 10.13278/j.cnki.jjuese.20170224
严克涛, 郭清海, 刘明亮
Yan Ketao, Guo Qinghai, Liu Mingliang
摘要: 西藏搭格架高温热泉是我国大陆少有的大型间歇性喷泉,砷元素作为对人类威胁极大的环境问题普遍存在于热泉之中,搭格架高温热泉中砷元素质量浓度最高已达到了9.75 mg/L,其对地表水和浅层地下水的污染不容忽视。硫代砷是富含硫化物热泉中砷的存在形态之一,鉴于国内相关研究较少,本文对西藏搭格架地热区的热泉样品进行了水化学分析,并利用水文地球化学模拟软件PHREEQC开展了对热泉中砷元素存在形态的地球化学模拟。结果表明:西藏搭格架热泉中砷元素的存在形态有亚砷酸盐、砷酸盐和硫代砷,其中亚砷酸盐与砷酸盐是砷的主要存在形态,且在pH影响下两者之间存在相互转化关系;各种硫代砷按质量浓度由高至低依次为一硫代砷酸盐、三硫代砷酸盐、二硫代砷酸盐、一硫代亚砷酸盐、四硫代砷酸盐;硫代砷形态占总砷浓度比例主要受热泉中硫化物质量浓度、Eh(氧化还原电位)和pH等因素的控制,在硫化物质量浓度总体偏低的情况下,硫化物质量浓度的上升可促进其他形态的砷向硫代砷形态转化,强还原性环境有利于硫代砷形态的存在;此外,在中性环境下,硫代砷占总砷浓度比例随pH上升亦有上升趋势。
中图分类号:
| [1] 孙贵范.我国地方性砷中毒研究进展[J].环境与健康杂志,2009,26(12):1035-1036. Sun Guifan. Research Progress of Endemic Arsenism in China[J]. Journal of Environment and Health,2009,26(12):1035-1036. [2] Craigmile P F,Calder C A,Li H,et al.Hierarchical Model Building,Fitting,and Checking:A Behind-the-Scenes Look at a Bayesian Analysis of Arsenic Exposure Pathways[J]. Bayesian Analysis,2009,4(1):1-35. [3] Figueira R,Sérgio C,Lopes J L,et al.Detection of Exposition Risk to Arsenic in Portugal Assessed by Air Deposition in Biomonitors and Water Contamination[J]. Int J Hyg Environ Health,2007,210(3/4):393-397. [4] Whanger P D,Weswig P H,Stoner J C.Arsenic Levels in Oregon Waters[J]. Environ Health Perspect,1977,19:139-143. [5] Subramanian K S,Kosnett M J.Human Exposures to Arsenic from Consumption of Well Water in West Bengal,India[J]. Int J Occup Environ Health,1998,4(4):217-230. [6] Anawar H M.Arsenic Poisoning in Groundwater:Health Risk and Geochemical Sources in Bangladesh[J].Environment International,2002,27(7):597-604. [7] Das D,Chatterjee A,Mandal B K,et al.Arsenic in Ground Water in Six Districts of West Bengal,India:The Biggest Arsenic Calamity in The World:Part 2:Arsenic Concentration in Drinking Water,Hair,Nails,Urine,Skin-Scale and Liver Tissue (Biopsy) of the Affected People[J].Analyst,1995,120(3):917-24. [8] 金银龙,梁超轲,何公理,等.中国地方性砷中毒分布调查:总报告[J].卫生研究,2003,32(6):519-540. Jin Yinlong,Liang Chaoke,He Gongli,et al. Study on Distribution of Endemic Arsenism in China[J]. Journal of Hygiene Research,2003,32(6):519-540. [9] 卞建民,查恩爽,汤洁,等.吉林西部砷中毒区高砷地下水反向地球化学模拟[J].吉林大学学报(地球科学版),2010,40(5):1098-1103. Bian Jianmin,Cha Enshuang,Tang Jie,et al.Inverse Geochemical Modeling of Arsenic Groundwater at Arseniasis Area in the Western of Jilin Province[J].Journal of Jilin University (Earth Science Edition),2010,40(5):1098-1103. [10] 赵娟,李育松,卞建民,等.吉林西部地区高砷地下水砷的阈值分析及风险评价[J].吉林大学学报(地球科学版),2013,43(1):251-258. Zhao Juan,Li Yusong,Bian Jianmin,et al. Threshold Analysis and Health Risk Assessment of Arsenic in Groundwater in Western Jilin Province[J]. Journal of Jilin University (Earth Science Edition),2013,43(1):251-258. [11] Cortecci G,Boschetti T,Mussi M,et al.New Chemical and Original Isotopic Data on Waters from El Tatio Geothermal Field,Northern Chile[J].Geochemical Journal,2015,39(6):547-571. [12] Khorasanipour M,Esmaeilzadeh E.Geogenic Arsenic Contamination in the Kerman Cenozoic Magmatic Arc,Kerman,Iran:Implications for the Source Identification and Regional Analysis[J].Applied Geochemistry,2015,63:610-622. [13] Birkle P,Bundschuh J,Sracek O,et al. Mechanisms of Arsenic Enrichment in Geothermal and Petroleum Reservoirs Fluids in Mexico[J].Water Research,2010,44(19):5605-5617. [14] Arnold Y P,Cabassi J,Tassi F,et al.Fluid Geochemistry of a Deep-Seated Geothermal Resource in The Puna Plateau (Jujuy Province,Argentina)[J].Journal of Volcanology & Geothermal Research,2017,338:121-134. [15] Kaasalainen H,Stefánsson A. The Chemistry of Trace Elements in Surface Geothermal Waters and Steam,Iceland[J]. Chemical Geology,2012,330/331:60-85. [16] Smedley P L,Kinniburgh D G.A Review of the Source,Behaviour and Distribution of Arsenic in Natural Waters[J].Applied Geochemistry,2002,17(5):517-568. [17] 丁爱中,杨双喜,张宏达.地下水砷污染分析[J].吉林大学学报(地球科学版),2007,37(2):319-325. Ding Aizhong,Yang Shuangxi,Zhang Hongda.Analysis of Groundwater Arsenic Pollution[J]. Journal of Jilin University (Earth Science Edition),2007,37(2):319-325. [18] Bostick B C,Fendorf S,Brown G E. In Situ Analysis of Thioarsenite Complexes in Neutral to Alkaline Arsenic Sulphide Solutions[J].Mineralogical Magazine,2005,69(5):781-795. [19] Helz G R,Tossell J A.Thermodynamic Model for Arsenic Speciation in Sulfidic Waters:A Novel Use of Ab Initio,Computations[J].Geochimica Et Cosmochimica Acta,2008,72(18):4457-4468. [20] Parkhurst D L.User's guide to PHREEQC:Version 2:A Computer Program for Speciation,Batch-Reaction,One-Dimensional Transport,and Inverse Geochemical Calculations[R].Water Resources Investigations Report,1999:99-4259. [21] Zakaznova-Herzog V P,Seward T M.A Spectrophotometric Study of the Formation and Deprotonation of Thioarsenite Species in Aqueous Solution at 22℃[J].Geochimica Et Cosmochimica Acta,2012,83(1):48-60. [22] Thilo E,Hertzog K,Winkler A.Vber Vorgänge bei der Bildung des Arsen(V)-Sulfids Beim Ansäuern von Tetrathioarsenatlösungen[J].Zeitschrift Für Anorganische Und Allgemeine Chemie,1970,373(2):111-121. [23] Guo Q,Planer-Friedrich B,Liu M,et al.Arsenic and Thioarsenic Species in the Hot Springs of the Rehai Magmatic Geothermal System,Tengchong Volcanic Region,China[J]. Chemical Geology,2017,453:12-20. [24] 郭清海,刘明亮,李洁祥.腾冲热海地热田高温热泉中的硫代砷化物及其地球化学成因[J].地球科学,2017,42(2):286-297. Guo Qinghai,Liu Mingliang,Li Jiexiang.Thioarsenic Species in the High-Temperature Hot Springs from the Rehai Geothermal Field (Tengchong) and Their Geochemical Geneses[J]. Earth Science,2017,42(2):286-297. [25] 庄亚芹,郭清海,刘明亮,等.高温富硫化物热泉中硫代砷化物存在形态的地球化学模拟:以云南腾冲热海水热区为例[J].地球科学,2016,41(9):1499-1510. Zhuang Yaqin,Guo Qinghai,Liu Mingliang,et al.Geochemical Simulation of Thioarsenic Speciation in Hgh-Temperature,Sulfide-Rich Hot Springs:A Case Study in the Rehai Hydrothermal Area,Tengchong,Yunnan[J]. Earth Science,2016,41(9):1499-1510. [26] 朱弟成,莫宣学,赵志丹,等.西藏南部二叠纪和早白垩世构造岩浆作用与特提斯演化:新观点[J].地学前缘,2009,16(2):1-20. Zhu Dicheng,Mo Xuanxue,Zhao Zhidan,et al.Permian and Early Cretaceousc Tectonomagmatism in Southern Tibet and Tethjy and Evolution:New Perspective[J]. Earth Science Frontier,2009,16(2):1-20. [27] 郑绵平,王秋霞,多吉.水热成矿新类型西藏铯硅华矿床[M].北京:地质出版,1995. Zheng Mianping,Wang Qiuxia,Duo Ji. New Types of Hydrothermal Mineralization,Tibet Cesium Silicate Deposit[M].Beijing:Geological Publishing House,1995. [28] 赵元艺,聂凤军,侯增谦,等.西藏搭格架热泉型铯矿床地质特征及形成时代[J].矿床地质,2006,25(3):281-291. Zhao Yuanyi,Nie Fengjun,Hou Zengqian,et al.Geological Characteristics and Formation Age of Hot Spring Cesium Deposit Area,Tibet[J].Mineral Deposits,2006,25(3):281-291. [29] 赵元艺,聂凤军,侯增谦,等.西藏搭格架热泉型铯矿床地球化学[J].矿床地质,2007,26(2):163-174. Zhao Yuanyi,Nie Fengjun,Hou Zengqian,et al.Geochemistry of Targejia Hot Spring Type Cesium Deposit in Tibet[J]. Mineral Deposits,2007,26(2):163-174. [30] 沈立成,伍坤宇,肖琼,等.西藏地热异常区CO2脱气研究:以朗久和搭格架地热区为例[J].科学通报,2011,56(26):2198-2208. Shen Licheng,Wu Kunyu,Xiao Qiong,et al.Carbon Dioxide Degassing Flux from Two Geothermal Fields in Tibet,China[J].Chinese Science Bulletin,2011,56(26):2198-2208. |
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