吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (1): 181-192.doi: 10.13278/j.cnki.jjuese.20160080

• 地质与资源 • 上一篇    下一篇

广西北部湾地区表层土壤As分布特征及其影响因素

郑国东1, 覃建勋1, 付伟2, 杨志强1, 赵辛金1, 卢炳科1   

  1. 1. 广西地质调查院, 南宁 530023;
    2. 桂林理工大学地球科学学院, 广西 桂林 541004
  • 收稿日期:2016-11-21 出版日期:2018-01-26 发布日期:2018-01-26
  • 通讯作者: 杨志强(1963),男,教授级高级工程师,主要从事勘查地球化学方面的研究,E-mail:zyyangzq@163.com E-mail:zyyangzq@163.com
  • 作者简介:郑国东(1983),男,硕士研究生,工程师,主要从事环境地球化学方面的研究,E-mail:156001601@qq.com
  • 基金资助:
    国家自然科学基金项目(41462005);中国地质调查局国家专项(GZTR20060115,GZTR20070107,GZTR20080110);广西自然科学基金项目(2014GXNSFAA118304)

Influencing Factors on Distribution and Accumulation of Arsenic in Topsoil in Beibu Gulf of Guangxi

Zheng Guodong1, Qin Jianxun1, Fu Wei2, Yang Zhiqiang1, Zhao Xinjin1, Lu Bingke1   

  1. 1. Guangxi Institute of Geological Survey, Nanning 530023, China;
    2. College of Earth Sciences, Guilin University of Technology, Guilin 541004, Guangxi, China
  • Received:2016-11-21 Online:2018-01-26 Published:2018-01-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41462005),National Special Project of China Geological Survey (GZTR20060115, GZTR20070107, GZTR20080110) and Natural Science Foundation of Guangxi Province (2014GXNSFAA118304)

摘要: 选取广西北部湾地区表层土壤中As元素为研究对象,采集了7 327个土壤样品,400个岩石样品,分析As、K2O、Na2O、CaO、MgO、SiO2、Al2O3、TFe2O3、Mn、Ti、pH和有机碳(SOC)等指标,探讨了土壤成土母岩、成土作用、土壤组成、pH和有机质等对表层土壤As元素的影响。结果表明:As元素平均质量分数为7.96×10-6,为中国土壤背景值0.80倍;风化作用对于As元素的次生富集起到极为重要的作用,明显强于成土母岩As元素背景的影响。Pearson相关分析和主成分分析表明:在土壤组成和土壤性质等因素中,含Al矿物(Al2O3)、含Fe矿物(TFe2O3)、含Si矿物(SiO2)和SOC,对土壤As的富集起到主导作用;pH 和含 Ca矿物(CaO)的作用较弱;而含K矿物(K2O)、含Na矿物(Na2O)和含Mg矿物(MgO)对As的次生富集作用可以忽略不计。

关键词: As, 分布特征, 影响因素, 北部湾, 表层土壤

Abstract: A total of 7 327 topsoil and 400 rock samples were collected in Beibu Gulf of Guangxi, and the concentration of the arsenic (As) and other elements or soil properties, such as K2O, Na2O, CaO, MgO, SiO2, Al2O3, TFe2O3, Mn, Ti, soil organic matter (SOC) and pH, were analyzed to discuss the relationship between the As and parent rock, weathering process, main elements, and soil properties. Moreover, we attempted to delineate the primary and secondary relationships between these factors. The results of this study show that the concentration of As is 7.96×10-6, lower than the background value of China soil. Weathering play a role in As accumulation more important than parent rocks. The results of Pearson and principal analyses indicate that Al-bearing, Fe-bearing minerals and SOC play a primary role in As accumulation, the influence of pH and Ca-bearing mineral is weak, and the role of K-bearing, Na-bearing and Mg-bearing minerals in As accumulation is negligible.

Key words: arsenic, distribution, influence factors, Beibu Gulf, topsoil

中图分类号: 

  • P59
[1] 管东升, 陈玉娟, 阮国标.广州城市及近郊土壤重金属含量特征及人类活动的影响[J]. 中山大学学报(自然科学版), 2001, 40(4): 93-97. Guan Dongsheng, Chen Yujuan, Ruan Guobiao. Study on Heavy Metal Concentrations and the Impact of Human Activity on Them in Urban and Suburb Soils of Guangzhou[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2001, 40(4): 93-97.
[2] Staglini W M, Doelman P, Salomons W, et al. Che-mical Time Bombs: Predicting the Unpredictable Environment[J]. Environment Science and Policy for Sustainable Development, 1991, 33(4): 4-30.
[3] Salomons W, Konsten C J M, Meulen-Smidt G R B T, et al. Summary of the Workshop on Delayed Effects of Chemicals in Soils and Sediments (Chemical Time Bombs), with Emphasis on the Scandinavian Region[J]. Applied Geochemistry, 1993, 8(9): 295-299.
[4] Chen T B, Wong J W C, Zhou H Y, et al. Asse-ssment of Trace Metal Distribution and Contamination in Surface Soils of HongKong[J]. Environmental Pollution, 1997, 96(1): 61-68.
[5] Alloway B J. Heavy Metals in Soils[M]. London: Environmental Pollution, 1995:1318-1324.
[6] Siegel F R. Environmental Geochemistry of Potentially Toxic Metals[M]. Berlin: Springer Science & Business Media, 2002: 45-59.
[7] Hardy M, Cornu S. Location of Natural Trace Elements in Silty Soils Using Particle-Size Fractionation[J]. Geoderma, 2006, 133(3): 295-308.
[8] Acosta J A, Martínez-Martínez S, Faz A, et al. Accumulations of Major and Trace Elements in Particle Size Fractions of Soils on Eight Different Parent Materials[J]. Geoderma, 2011, 161: 30-42.
[9] Klassen R A. Geological Factors Affecting the Distri-bution of Trace Metals in Glacial Sediments of Central New Foundland[J]. Environmental Geology, 1998, 33(2): 154-169.
[10] Salminen R, Tarvainen T. The Problem of Defining Geochemical Baselines: A Case Study of Selected Elements and Geological Materials in Finland[J]. Journal of Geochemical Exploration, 1997, 60(1): 91-98.
[11] Tack F M G, Verloo M G, Vanmechelen L, et al. Baseline Concentrations Levels of Trace Elements as a Function of Clay and Organic Carbon Contents in Soils in Flanders (Belgium)[J]. Science of Total Environment, 1997, 201(2):113-123.
[12] Martinez C E, Motto H L. Solubility of Lead, Zinc and Copper Added to Mineral Soils[J]. Environmental Pollution, 2000, 107(1): 153-158.
[13] Ramos-Miras J J, Roca-Perez L,Guzmán-Palomino M, et al. Background Levels and Baseline Values of Available Heavy Metals in Mediterranean Greenhouse Soils (Spain)[J]. Journal of Geochemical Exploration, 2011,110(2): 186-192.
[14] 王世杰, 季宏兵, 欧阳自远,等. 碳酸盐岩风化成土作用的初步研究[J]. 中国科学:D辑, 1999, 29(5): 441-449. Wang Shijie, Ji Hongbing, Ouyang Ziyuan, et al. Study on Weathering Pedogenesis of Carbonate Rock[J]. Science in China: Series D, 1999, 29(5): 441-449.
[15] 杨元根, 刘丛强, 袁可能,等. 南方红土形成过程及其稀土元素地球化学[J]. 第四纪研究, 2000, 20(5): 469-480. Yang Yuangen, Liu Congqiang, Yuan Keneng, et al. Laterite Formation Process in Southern China and Its Rare Earth Element(REE) Geochemistry[J]. Quaternary Sciences, 2000, 20(5): 469-480.
[16] 孙承兴, 王世杰, 刘秀明,等. 碳酸盐岩风化壳岩-土界面地球化学特征及其形成过程:以贵州花溪灰岩风化壳剖面为例[J]. 矿物学报, 2002, 22(2): 126-132. Sun Chengxing, Wang Shijie, Liu Xiuming,et al. Geochemical Characteristics and Formation Mechanism of Rock:Soil Interface in Limestone Weathering Crust at Huaxi, Guizhou Province[J].Acta Mineralogica Sinica, 2002, 22(2): 126-132.
[17] 刘秀明, 王世杰, 孙承兴,等. 石灰土物质来源的判别:以黔北、黔中几个剖面为例[J].土壤, 2004, 36(1): 30-36. Liu Xiuming, Wang Shijie, Sun Chengxing, et al. Identification of Origin of Limestone Soil:A Case Study of Profiles in Central and North Guizhou[J]. Soils, 2004, 36(1): 30-36.
[18] 周德全, 王世杰, 刘秀明. 石灰土(碳酸盐岩风化壳)形成地球化学过程研究[J].地球与环境, 2005, 33(2): 31-38. Zhou Dequan, Wang Shijie, Liu Xiuming, et al. Study on Geochemical Processes in Limestone Soil Profiles[J]. Earth and Environment, 2005, 33(2): 31-38.
[19] 周长松, 邹胜章, 李录娟, 等. 岩溶区典型石灰土Cd形态指示意义及风险评价:以桂林毛村为例[J]. 吉林大学学报(地球科学版), 2016, 46(2): 552-562. Zhou Changsong, Zou Shengzhang, Li Lujuan, et al. Implications of Cadmium form and Risk Assessment of Calcareous Soil in Karst Area: A Case Study of Maocun in Guilin, China[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(2): 552-562.
[20] Yu W C, Wang R H, Zhang Q L, et al. Minera-logical and Geochemical Evolution of the Fusui Bauxite Deposit in Guangxi, South China: From the Original Permian Orebody to a Quarternary Salento-Type Deposit[J]. Journal of Geochemical Exploration, 2004, 146:75-88.
[21] Wei X, Ji H B, Li D J, et al. Material Source Analysis and Element Geochemical Research About Two Types of Representative Bauxite Deposits and Terra Rossa in Western Guangxi, Southern China[J]. Journal of Geochemical Exploration, 2013, 133: 68-87.
[22] Liu W J, Liu C Q, Zhao Z Q, et al. Elemental and Strontium Isotopic Geochemistry of the Soil Profiles Developed on Limestone and Sandstone in Karstic Terrain on Yunnan-Guizhou Plateau, China: Lmplications for Chemical Weathering and Parent Materials[J]. Journal of Asian Earth Sciences, 2013, 67(7):138-152.
[23] 多目标区域地球化学调查规范DD2005-1[S]. 北京: 中国标准出版社, 2005. Specification for Multi-Purpose Regional Geochemical Survey DD2005-1[S]. Beijing: Standards Press of China, 2005.
[24] 数据的统计处理和解释正态性检验GB/T4882-2001[S]. 北京: 中国标准出版社, 2001. Statistica Interpretation of Data-Normality Test GB /T4882-2001[S]. Beijing: Standards Press of China, 2001.
[25] 鄢明才, 迟清华, 顾铁新, 等. 中国东部地壳元素丰度与岩石平均化学组成研究[J]. 物探与化探, 1997(6): 451-459. Yan Mingcai, Chi Qinghua, Gu Tiexin, et al. Chemical Compositions of Continental Crust and Rocks in Eastern China[J]. Geophysical and Geochemical Exploration, 1997(6): 451-459.
[26] 鄢明才, 顾铁新, 迟清华, 等. 中国土壤化学元素风度与表生地球化学特征[J]. 物探与化探, 1997,21(3):161-167. Yan Mingcai, Gu Tiexin, Chi Qinghua et al. Abundance of Chemical Elements of Soils in China and Supergenesis Geochemistry Characteristics[J]. Geophysical and Geochemical Exploration, 1997, 21(3):161-167.
[27] Fichter J, Turpault M P, Dambrine E, et al. Loca-lization of Base Cations in Particle Size Fractions of Acid Forest Soils (Volges Mountains, N-E France)[J]. Geoderma, 1998, 82(4): 295-314.
[28] 广西土壤肥料工作站. 广西土壤[M]. 南宁: 广西科学技术出版社, 1994: 300-301. Guangxi Soil and Fertilizer Station. Soil in Guangxi[M]. Nanning: Guangxi Science and Technology Press, 1994: 300-301.
[29] Zhang X P, Deng W, Yang X M. The Background Concentrations of 13 Soil Trace Elements and Their Relationships to Parent Materials and Vegetation in Xizang (Tibet), China[J]. Journal of Asian Earth Sciences, 2002, 21(2): 167-174.
[30] Chen M, Ma L Q, Harris W G. Baseline Concen-trations of 15 Trace Elements in Florida Surface Soils[J]. Journal of Environmental Quality, 1999, 28(4): 1173-1181.
[31] Tack F M G, Vanhaesebroeck T, Verloo M G, et al. Mercury Baseline Levels in Flemish Soils (Belgium)[J]. Environmental Pollution, 2005, 134(1): 173-179.
[32] Huang P M. Feldspars, Olivines, Pyroxenes, and Amphiboles[C]//Dixon J B, Weed S B. Minerals in Soil Environments. Madison: Soil Science Society of America Journal, 1989: 975-1050.
[33] Monger H C, Kelly E F. Silica Minerals[C]//Dixon J B, Schulze D G. Soil Mineralogy with Environmental Applications. Madison: Soil Science Society of America Journal, 2002: 611-636.
[34] Bigham J M, Fitzpatrick R W, Schulze D G, et al. Iron Oxides[C]//Dixon J B, Schulze D G. Madison: Soil Mineralogy with Environmental Applications. Madison: Soil Science Society of America Journal, 2002: 323-367.
[35] Nachtegaal M, Sparks D L. Effect of Iron Oxide Coatings on Zinc Sorption Mechanism at the Clay-Mineral/Water Interface[J]. Journal of Colloid and Interface Science, 2004, 276(1): 13-23.
[36] Sterckeman T, Douay F, Baize D, et al. Factors Affecting Trace Element Concentrations in Soils Developed on Recent Marine Deposits from Northern France[J]. Applied Geochemistry, 2004, 19(1): 89-103.
[37] Sipos P, Németh T, Kis V K, et al. Association of Individual Soil Mineral Constituents and Heavy Metals as Studied by Sorption Experiments and Analytical Electron Microscopy Analyses[J]. Journal of Hazardous Materials, 2009, 168(2/3): 1512-1520.
[38] Obrist D, Johnson D W, Lindberg S E, et al. Mercury Distribution Across 14 US Forests:Part I: Spatial Patterns of Concentrations in Biomass, Litter, and Soils[J]. Environmental Science and Technology, 2011, 45(9): 3974-3981.
[1] 于影, 陈俊杰, 林耿煨, 李青松. 多孔结构CuFe2O4-P材料制备及其催化过一硫酸盐降解咖啡因[J]. 吉林大学学报(地球科学版), 2026, 56(3): 1002-1012.
[2] 王健, 张媛瑗, 吴楠, 徐清海, 崔子岳, 刘显凤, 付清萌. 鄂尔多斯盆地志靖—安塞地区长7段夹层型页岩油储层特征及分类评价[J]. 吉林大学学报(地球科学版), 2026, 56(2): 453-468.
[3] 王振军. 油气储层裂缝预测进展[J]. 吉林大学学报(地球科学版), 2026, 56(2): 469-482.
[4] 徐骏, 高阳, 刘军, 王晓彤, . 大兴安岭北段三矿沟铁铜矿床成因——来自石榴子石U-Pb定年及元素地球化学证据[J]. 吉林大学学报(地球科学版), 2026, 56(2): 540-556.
[5] 张文, 王骏城, 陈俊淇, 崔洪海, 孔祥礼, 郭涛, 王明, 王佳, 张书睿, 孙琦, 张涵, . 长白山山脉基本地质概况与火成岩崩滑灾变类型及机制[J]. 吉林大学学报(地球科学版), 2026, 56(2): 568-583.
[6] 束龙仓, 位书静, 澈丽木格, 温中琦, 刘波. 西辽河平原生态输水的地下水响应及不确定性量化[J]. 吉林大学学报(地球科学版), 2026, 56(2): 647-660.
[7] 范晓鹏, 李晨熠, 初东方, 李冰, 宫达, 李亚洲, 杨一凡, 刘西牧, 张楠, Pavel Talalay. 冰下湖可回收式热融探测器钻孔倾斜影响因素[J]. 吉林大学学报(地球科学版), 2026, 56(2): 713-723.
[8] 刘涛, 刘宗堡, 张可佳, 张岩, 张瑞雪, 刘晓文, 徐翠云.

基于深度学习的致密砂岩储层薄片图像生成与识别方法 [J]. 吉林大学学报(地球科学版), 2026, 56(2): 724-738.

[9] 尹志刚, 姜琦, 李萌萌, 吴子杰, 陈军典, 张凯强, 郭浩, 马岩. 辽东本溪地区新太古代晚期刘家堡子岩体成因及地质意义[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1549-1563.
[10] 周柳湘, 余思琴, 陈俊华, 刘城, 陈义, 张鑫鑫, . 潜孔锤与冲击钻机联合钻进工艺成孔碎岩过程数值模拟[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1608-1618.
[11] 闫纲丽, 冯屾, 刘睿男, 黄冠星. 地下水背景值评估研究进展[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1655-1670.
[12] 马玮瞳, 纪雪, 朴东范, 王明常, 刘子维, 刘星男. 基于博弈论-物元可拓模型的多时空森林健康评价——以中朝俄跨境区域为例[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1742-1756.
[13] 苏杨鑫, 李军辉, 付秀丽, 张新荣, 郑强, 吴丽芳, 霍元勃, 孙琦. 内蒙古新发水库现代堰塞湖沉积底泥色度与气候参数耦合关系[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1445-1461.
[14] 王志勇, 刘国昌, 王梓旭, 郭严粮, 秦晨.

基于振幅一致性残差卷积编码-解码器的不规则缺失数据重建 [J]. 吉林大学学报(地球科学版), 2025, 55(4): 1336-1350.

[15] 孙敬雯, 吕子强, 孔庆翰, 唐泽豪, 邱俊辉, 刘珈君. 基于背景噪声成像的沂沭断裂带及邻区波速变化[J]. 吉林大学学报(地球科学版), 2025, 55(4): 1361-1371.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 吴远坤, 刘成林, 于春勇. 松辽盆地双城断陷深层原油成藏模式[J]. 吉林大学学报(地球科学版), 2024, 54(5): 1443 -1456 .
[2] 马荣,石建省,刘继朝. 人工内分泌网络模型在水文地质参数研究中的应用[J]. 吉林大学学报(地球科学版), 2013, 43(3): 914 -921 .
[3] 李宁, 王成文. 东北及邻区晚古生代地层接触关系与佳-蒙地块的形成和演化[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1331 -1340 .
[4] 胡大千,初凤友,姚 杰. 中太平洋YJA海山富钴结壳矿物组成与元素地球化学[J]. J4, 2006, 36(01): 32 -0037 .
[5] 姜 雪, 程日辉,于民凤. 裂谷地层的气候和构造控制:Zscape模型分析与在松辽盆地北安断陷的应用[J]. J4, 2006, 36(01): 54 -0059 .
[6] 李春柏,张新涛,刘 立,任延广,孟 鹏. 布达特群热流体活动及其对火山碎屑岩的改造作用--以海拉尔盆地贝尔凹陷为例[J]. J4, 2006, 36(02): 221 -0226 .
[7] 孟宪纲,薄万举,刘志广,刘勇,畅柳,李朝柱,王子平. 芦山7.0级地震与巴颜喀拉块体中东段的活动性[J]. 吉林大学学报(地球科学版), 2014, 44(5): 1705 -1711 .
[8] 陈欢庆, 梁淑贤, 舒治睿, 邓晓娟, 彭寿昌. 冲积扇砾岩储层构型特征及其对储层开发的控制作用——以准噶尔盆地西北缘某区克下组冲积扇储层为例[J]. 吉林大学学报(地球科学版), 2015, 45(1): 13 -24 .
[9] 贾大成,邢立新, 潘 军, M. J. van Bergen, H. van Roermund. 伊通上地幔剪切带捕虏体中富铝尖晶石的地球化学特征[J]. J4, 2006, 36(04): 497 -502 .
[10] 谢忠雷,杨佰玲,包国章,董德明. 茶园土壤不同形态镍的含量及其影响因素[J]. J4, 2006, 36(04): 599 -604 .