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Geochemical characteristics and genesis of selenium in soil in northern Muchuan County, Sichuan Province |
HAN Wei1,2,3(), WANG Qiao-Lin1,2,3, SONG Yun-Tao1,2,3, PENG Min1,2,3, WANG Cheng-Wen1,2,3 |
1. Institute of Geophysical and Geochemical Exploration,CAGS,Langfang 065000,China 2. Research Center of Geochemical Survey and Assessment on Land Quality,CGS,Langfang 065000,China 3. Key Laboratory of Geochemical Cycling of Carbon and Mercury in the Earth's Critical Zone,CAGS,Langfang 065000,China |
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Abstract Based on geochemical investigation of land quality in northern Muchuan County of Sichuan Province, the authors identified the geochemical characteristics of Se element in the soil of the working area and carried out a study of its causes . The results show that the Se content of the soil in the working area ranges from 0.06×10-6 to 1.49×10-6, with an average value of 0.41×10-6. It is mainly dominated by selenium-enriched soil, which satisfies the conditions of selenium-enriched soil and possesses 60% of the whole working area. The content of Se in different parent rocks is quite different and tends to be enriched in the surface layer. The content of Se in soils with Xiangxi Group as the parent rock is higher but the content of heavy metals is lower; the content of Se is the highest in forest land in different land use types; the difference in content of Se in different soil types is relatively small. Correlation analysis shows that the Se content of the soil is significantly positively correlated with SOM, Pb, As, Cd, etc. Different parent rocks have a greater influence on the correlation between Se content and pH, indicating that the main factors of Se content in soil are parent rocks, SOM and heavy metal elements in the working area.
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Received: 13 May 2020
Published: 01 March 2021
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指标 | 分析方法 | 检出限 | 测定范围 | Se | AFS | 0.01 | 0.01~100 | As | AFS | 0.5 | 0.5~500 | Cd | ICP-MS | 0.03 | 0.02~4.0 | Cr | XRF | 2.5 | 2.5~3500 | Cu | XRF | 1 | 1~2000 | Hg | AFS | 0.0005 | 0.001~10 | Ni | XRF | 1.5 | 1~2000 | Pb | XRF | 2 | 2~2000 | Zn | XRF | 4 | 1~3000 | pH | ISE | 0.1 | 1.00~14.00 | 有机质 | VOL | 0.02 | 0.05~10 |
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The analysis method and detection limit of target elements
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指标 | 样品数 | 平均值 | 中位数 | 背景值 | 标准离差 | 变异系数 | 最大值 | 最小值 | Se | 1847 | 0.41 | 0.4 | 0.40 | 0.13 | 0.31 | 1.49 | 0.06 | As | 1847 | 11.5 | 10.1 | 11 | 5.31 | 0.46 | 38.3 | 2.24 | Cd | 1847 | 0.33 | 0.31 | 0.32 | 0.16 | 0.48 | 2.42 | 0.04 | Cr | 1847 | 94 | 83.1 | 80.4 | 53.6 | 0.57 | 515 | 32.3 | Cu | 1847 | 38.3 | 28.6 | 28.3 | 39 | 1.02 | 445 | 2.81 | Hg | 1847 | 0.11 | 0.1 | 0.1 | 0.15 | 1.44 | 4.76 | 0.02 | Ni | 1847 | 34.3 | 30.9 | 30.9 | 16.1 | 0.47 | 166 | 4.6 | Pb | 1847 | 36 | 35.4 | 35.4 | 8.82 | 0.25 | 244 | 13.1 | Zn | 1847 | 93.8 | 93.5 | 92.2 | 22.3 | 0.24 | 409 | 29.6 | pH | 1847 | 4.77 | 5.02 | 4.86 | 1.19 | 1.28 | 8.4 | 3.77 | 有机质 | 1847 | 29.2 | 26.8 | 28.2 | 11.4 | 0.39 | 212 | 7.1 |
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Geochemical parameters of target elements
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Geochemical evaluation grade of selenium in topsoil in research area P2β—Emeishan basalt;T1f+t—Tongjiezi and Feixianguan formation;T1j—Jialingjiang formation;T2-3l-k—Kuahongdong and Leikoupo formation;T3-J1x—Xiangxi group;J2s1—lower Shaximiao formation;J2z—Ziliujing formation
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Fig.1) ">
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Geochemical map of selenium in topsoil in research area(the legend description is the same as Fig.1)
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地层 | 样品数 | 均值/10-6 | 中位数/10-6 | 标准离差 | 变异系数/% | 最大值/10-6 | 最小值/10-6 | 香溪群 | 1163 | 0.43 | 0.42 | 0.11 | 0.25 | 1.14 | 0.1 | 峨眉山玄武岩 | 57 | 0.47 | 0.46 | 0.2 | 0.43 | 1.28 | 0.08 | 垮洪洞组—雷口坡组 | 146 | 0.47 | 0.44 | 0.17 | 0.36 | 1.49 | 0.19 | 嘉陵江组 | 219 | 0.4 | 0.39 | 0.09 | 0.23 | 0.72 | 0.17 | 铜街子组—飞仙关组 | 85 | 0.29 | 0.29 | 0.1 | 0.36 | 0.6 | 0.08 | 沙溪庙组下段 | 82 | 0.25 | 0.25 | 0.07 | 0.28 | 0.46 | 0.06 | 自流井组 | 94 | 0.29 | 0.29 | 0.08 | 0.27 | 0.5 | 0.08 |
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Geochemical parameters of Se in soils from different parent rocks
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The distribution of Se in different soil profiles
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The mean histogram of Se in soils of different types of land use
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土壤类型 | 样品数 | 均值/10-6 | 中位数/10-6 | 标准离差 | 变异系数/% | 最大值/10-6 | 最小值/10-6 | 水稻土 | 814 | 0.4 | 0.4 | 0.11 | 0.28 | 1.06 | 0.08 | 紫色土 | 371 | 0.39 | 0.39 | 0.13 | 0.33 | 1.15 | 0.06 | 黄壤 | 515 | 0.43 | 0.42 | 0.14 | 0.32 | 1.49 | 0.14 | 石灰岩土 | 115 | 0.43 | 0.41 | 0.12 | 0.28 | 0.94 | 0.15 | 潮土 | 21 | 0.38 | 0.37 | 0.08 | 0.2 | 0.5 | 0.21 |
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Geochemical parameters of Se in soils from different types
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变量 | As | Cd | Cr | Cu | Hg | Ni | Pb | Zn | 有机质 | pH | 全区 | 相关性 | 0.392** | 0.384** | -0.202** | -0.017 | 0.133** | -0.113** | 0.538** | 0.253** | 0.682** | -0.027 | | p | 0.000 | 0.000 | 0.000 | 0.458 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.238 | 香溪群 | 相关性 | 0.312** | 0.387** | 0.335** | 0.376** | 0.052 | 0.350** | 0.638** | 0.432** | 0.709** | -0.042 | | p | 0.000 | 0.000 | 0.000 | 0.000 | 0.077 | 0.000 | 0.000 | 0.000 | 0.000 | 0.150 | 玄武岩 | 相关性 | 0.632** | 0.485** | -0.2 | -0.022 | 0.781** | -0.164 | 0.860** | 0.452** | 0.571** | -0.129 | | p | 0.000 | 0.000 | 0.137 | 0.870 | 0.000 | 0.224 | 0.000 | 0.000 | 0.000 | 0.339 | 垮洪洞及雷口坡组 | 相关性 | 0.430** | 0.793** | 0.128 | 0.095 | 0.342** | 0.244** | 0.583** | 0.478** | 0.850** | 0.280** | | p | 0.000 | 0.000 | 0.125 | 0.252 | 0.000 | 0.003 | 0.000 | 0.000 | 0.000 | 0.001 | 嘉陵江组 | 相关性 | 0.646** | 0.510** | -0.504** | -0.440** | 0.209** | -0.474** | 0.450** | 0.131 | 0.525** | 0.226** | | p | 0.000 | 0.000 | 0.000 | 0.000 | 0.002 | 0.000 | 0.000 | 0.054 | 0.000 | 0.001 | 铜街子及飞仙关组 | 相关性 | 0.697** | 0.412** | -0.654** | 0.265* | 0.676** | -0.332** | 0.693** | 0.307** | 0.384** | -0.055 | | p | 0.000 | 0.000 | 0.000 | 0.014 | 0.000 | 0.002 | 0.000 | 0.004 | 0.000 | 0.619 | 沙溪庙组下段 | 相关性 | 0.621** | 0.279* | 0.057 | -0.174 | 0.533** | -0.256* | 0.543** | -0.063 | 0.530** | -0.296** | | p | 0.000 | 0.011 | 0.612 | 0.117 | 0.000 | 0.020 | 0.000 | 0.575 | 0.000 | 0.007 | 自流井组 | 相关性 | 0.481** | 0.067 | -0.078 | -0.121 | 0.578** | -0.457** | 0.389** | -0.182 | 0.653** | -0.657** | | p | 0.000 | 0.523 | 0.455 | 0.244 | 0.000 | 0.000 | 0.000 | 0.079 | 0.000 | 0.000 |
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The Correlation between Se contents and other elements contents in top soils
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The scatter plots of soil selenium content and SOM content in soils from different parent rocks
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[1] |
涂光炽, 高振敏, 胡瑞忠, 等. 分散元素地球化学及成矿机制[M]. 北京: 地质出版社, 2004.
|
[1] |
Tu G Z, Gao Z M, Hu R Z, et al. The geochemistry and deposit-forming mechanism of disperse element [M]. Beijing: Geological Publishing House, 2004.
|
[2] |
Rayman M P. The importance of selenium to human health[J]. The Lancet, 2000,356:233-241.
|
[3] |
谭见安. 环境生命元素与克山病:生态化学地理研究[M]. 北京: 中国医药科技出版社, 1996.
|
[3] |
Tan J A. Environmental life elements and Keshan disease:A study on ecological chemicogeography[M]. Beijing: China Medical Science Press, 1996.
|
[4] |
秦俊法. 中国硒研究历史回顾(上)[J]. 广东微量元素科学, 2014,21(11):44-57.
|
[4] |
Qin J F. Historical review on the research of selenium in China[J]. Guangdong Trace Elements Science, 2014,21(11):44-57.
|
[5] |
杨艳, 杨忠芳, 侯青叶, 等. 四川省盐亭县食管癌高发与环境地球化学关系[J]. 现代地质, 2008,22(6):1015-1021.
|
[5] |
Yang Y, Yang Z F, Hou Q Y, et al. Relationship between esophageal cancer and environmental geochemistry in Yanting County, Sichuan Province[J]. Geoscience, 2008,22(6):1015-1021.
|
[6] |
刘才泽, 王永华, 曾琴琴, 等. 成渝典型地区土壤硒地球化学特征及其成因分析[J]. 物探与化探, 2018,42(6):1289-1295.
|
[6] |
Liu C Z, Wang Y H, Zeng Q Q, et al. The distribution and source of soil selenium in typical areas of Chengdu-Chongqing region[J]. Geophysical and Geochemical Exploration, 2018,42(6):1289-1295.
|
[7] |
杨良策, 李明龙, 杨廷安, 等. 湖北省恩施市表层土壤硒含量分布特征及其影响因素研究[J]. 资源环境与工程, 2015,29(6):825-829.
|
[7] |
Yang L C, Li M L, Yang T A, et al. Study on distribution characteristics of selenium content of surface soil and its influencing factors in Enshi City, Hubei Province[J]. Resources Environment & Engineering, 2015,29(6):825-829.
|
[8] |
Chang C Y, Yin R S, Wang X, et al. Selenium translocation in the soil-rice system in the Enshi seleniferous area, central China[J]. Science of the Total Environment, 2019,669:83-90.
|
[9] |
朱建明, 秦海波, 李璐, 等. 湖北恩施渔塘坝高硒土壤中硒的结合态[J]. 环境科学学报, 2008,28(4):772-777.
|
[9] |
Zhu J M, Qin H B, Li L, et al. Fractionation of selenium in high-Se soils from Yutangba, Enshi, Hubei[J]. Acta Scientiae Circumstantiae, 2008,28(4):772-777.
|
[10] |
Zhu J M, Zheng B S. Distribution of selenium in a mini-landscape of Yutangba, Enshi, Hubei Province, China[J]. Applied Geochemistry, 2001,16(11-12):1333-1344.
|
[11] |
王芳, 鲁力, 康健, 等. 恩施渔塘坝硒矿床中硒的赋存状态研究[J]. 资源环境与工程, 2016,30(2):244-247.
|
[11] |
Wang F, Lu L, Kang J, et al. Study on the occurrence of Selenium in Yutangba of Enshi[J]. Resources Environment & Engineering, 2016,30(2):244-247.
|
[12] |
李忠惠, 金立新, 徐洲, 等. 四川省盐亭县癌症高发区与地球化学环境关系研究[J]. 地球科学进展, 2012(S1):381-391.
|
[12] |
Li Z H, Jin L X, Xu Z, et al. Impact of the geochemical environment on the cancer incidence in the Yanting area, Sichuan province[J]. Advances in Earth Sciences, 2012(S1):381-391.
|
[13] |
黄春雷, 宋明义, 魏迎春, 等. 浙中典型富硒土壤区土壤硒含量的影响因素探讨[J]. 环境科学, 2013,34(11):4405-4410.
|
[13] |
Huang C L, Song M Y, Wei Y C, et al. Study on selenium contents of typical selenium-rich soil in the middle area of Zhejiang and its influencing factors[J]. Environmental Science, 2013,34(11):4405-4410.
|
[14] |
周墨, 陈国光, 张明, 等. 赣南地区土壤硒元素地球化学特征及其影响因素研究:以青塘—梅窖地区为例[J]. 现代地质, 2018,32(6):1292-1301.
|
[14] |
Zhou M, Chen G G, Zhang M, et al. Geochemical characteristics and influencing factors of selenium in soils of south Jiangxi province: A typical area of Qingtang-Meijiao[J]. Geoscience, 2018,32(6):1292-1301.
|
[15] |
肖高强, 宗庆霞, 向龙洲, 等. 云南省盈江县旧城—姐冒地区土壤和农产品硒地球化学特征及影响因素[J]. 物探与化探, 2020,44(2):412-418.
|
[15] |
Xiao G Q, Zong Q X, Xiang L Z, et al. Geochemical characteristics and influencing factors of Selenium in soils and agricultural products in the Jiucheng-Jiemao area, Yingjiang County, Yunnan Province[J]. Geophysical and Geochemical Exploration, 2020,44(2):412-418.
|
[16] |
吴俊. 福建省寿宁县富硒土壤地球化学特征[J]. 物探与化探, 2018,42(2):386-391.
|
[16] |
Wu J. Geochemical characteristics of selenium-rich soil in Shouning County of Fujian Province[J]. Geophysical and Geochemical Exploration, 2018,42(2):386-391.
|
[17] |
中国环境监测总站. 中国土壤元素背景值[M]. 北京: 中国环境科学出版社, 1990.
|
[17] |
China National Environmental Monitoring Centre. Chinese soil element background value [M]. Beijing: China Environmental Science Press, 1990.
|
[18] |
李家熙, 张光弟, 葛晓立, 等. 人体硒缺乏与过剩的地球化学环境特征及其预测[M]. 北京: 地质出版社, 2000.
|
[18] |
Li J X, Zhang G D, Ge X L, et al. Prediction and geochemical environmental character of human selenium imbalances[M]. Beijing: Geological Publishing House, 2000.
|
[19] |
冯彩霞, 刘燊, 胡瑞忠, 等. 遵义下寒武统富硒黑色岩系地球化学:成因和硒富集机理[J]. 地球科学:中国地质大学学报, 2010,35(6):947-958.
|
[19] |
Feng C X, Liu S, Hu R Z, et al. Geochemistry of lower Cambrian Se-rich black rock series in Zunyi, Guizhou Province,southwest China: The petrogenesis and enrichment mechanism of selenium[J]. Earth Science Journal of China University of Geosciences, 2010,35(6):947-958.
|
[20] |
朱建明, 梁小兵, 凌宏文, 等. 环境中硒存在形式的研究现状[J]. 矿物岩石地球化学通报, 2003,22(1):75-81.
|
[20] |
Zhu J M, Liang X B, Ling H W, et al. Advances in studying occurrence modes of selenium in environment[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2003,22(1):75-81.
|
[21] |
Swaine D J, Goodarzi F. Environmental aspects of trace elements in coal[M]. Netherlands: Kluwer Academic Publisers, 1995.
|
[22] |
Elrashidi M A, Adriano D C, Workman S M, et al. Chemical equilibria of selenium in soil: A theoretical development[J]. Soil Science, 1987,144(2):141-151.
|
[23] |
Jayaweera G R, Biggar J W. Role of redox potential in chemical transformations of selenium in soils[J]. Soil Science Society of America Journal, 1996,60:1056-1063.
|
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