用户名: 密码: 验证码:
新疆博斯腾湖表层沉积物金属元素地球化学特征研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
湖泊是陆地水圈的重要组成部分,并与大气、生物、土壤等多种环境密切联系。随着城镇化与工业化的加速,以及农业生产活动的影响,湖泊水体污染和富营养化也逐渐成为最为突出的水环境问题之一。湖泊是大陆内部流域的尾端,流域内人类活动产生的污染物随水体带入湖泊中,并在湖泊沉积物中聚集。对金属元素在不同流域的迁移特征的了解,可以加深对元素的迁移、富集的认识,对湖泊环境的污染监测和控制有重要的意义。
     博斯腾湖是中国内陆最大的淡水湖。它不仅对该流域起着重要的生态调节作用,也直接影响着该地区的经济社会环境的可持续发展。但是随着人们对该地区的工农业生产,以及对局部地区河流的人工调节,近几十年来,博斯腾湖正在受到高矿化度农田排水和工业污水的污染,湖水水质正在不断恶化,严重影响了该地区的生态平衡,对人类的生存环境产生了极大的破坏。本文以干旱区湖泊博斯腾湖为研究对象,通过分析博斯腾湖表层沉积物中常、微量元素的含量和空间变化特征,研究了沉积物中元素之间的相关性,探讨了常、微量元素空间分布的控制因素,同时对研究区域沉积物中重金属进行了污染评价。
     本文对博斯腾湖的47个水样以及29个沉积物样品进行分析,主要得到以下结论:
     (1)博斯腾湖为半封闭湖泊,出入水口位于湖泊西端相距较近,全湖区水动力差,水体滞留时间长。博斯腾湖的主要污染源分布于黄水湾区域。湖区的水化学环境存在区域性差异,水样的电导率等值线和pH等值线反映开都河口水体污染程度低,黄水湾处最大,而湖中心区则介于两者之间。
     (2)通过对沉积物常量元素的分析可知,表层沉积物中以CaO、AI2O3、SiO2的含量为主.沉积物中Fe2O3、AI2O3、SiO2、K20、MgO的分布趋势相同,即在开都河入湖处含量较高,在黄水湾附近含量较低;CaO则与这几种常量组分的分布趋势相反,即在黄水湾附近含量最高,在开都河入湖处含量最低。微量元素Co、Cr、Cu、Ni、Pb、Zn的分布趋势相同,在开都河河口处含量较高,从西北黄水湾入湖处含量较小,湖中心区值变化稳定位于两者之间。As含量的分布规律不明显。元素Sr与CaO的分布趋势基本相同,Sr与CaO二者的含量都受生物碳酸盐介壳影响。
     (3)对元素进行相关性分析及因子分析探讨了其地球化学意义,结果如下:
     ①Ti与Fe2O3、SiO2、A12O3、MgO、K2O显著正相关;主要代表了陆源碎屑和黏土组分来源。CaO与Ti、MgO、K2O、SiO2、A12O3、Fe2O3显著负相关,CaO的富集不同于以上几种元素,代表了生物碎屑组分来源。As与CaO呈弱的负相关性,与其他元素有弱的正相关关系,表明As除了经陆源输入外还有其他来源。Co, Ni、Pb、Cr、Zn、Cu与Ti等常量元素显著正相关,表明这些元素分布受陆源影响。Sr与Ti、SiO2、A12O3等常量组分显著负相关。
     ②对常微量元素进行因子分析,可提取4个主因子:F1代表陆源与生源沉积,正载荷A12O3、Fe2O3、SiO2、MgO、K2O、Ti、Cu、As、Ni、Pb等元素组合,Sr和CaO表现为负载荷。F2可能反映研究区受到湖水对湖底沉积物的影响,主要元素组合为Na2O。F3代表与人类活动相关的污染源的输入有关,主要元素为As。F4代表了陆源碎屑和湖泊自生的混合沉积,主要元素为P。
     (4)用富集因子法对沉积物中重金属Ni、Co、Cr、Zn、Pb、Cu进行污染评价,富集程度为Ni>Co>Cr>Zn>Pb>Cu。结果表明Ni、Co、Cr、Zn处于中度污染水平,Pb是处于轻微污染水平,Cu处于无污染水平。
The lakes are an important part of the terrestrial hydrosphere, and close contact with the atmosphere, biology, soil environment.. With the acceleration of urbanization and industrialization, and the influence of agricultural production activities, pollution and eutrophication of the lake water is becoming one of the most prominent water environmental problems. The lake is within the mainland end of the basin, pollutants produced by human activities within the basin with water into the lake, and gathered in lake sediments.Understanding of the migration characteristics of the metallic elements in the different basins to understand element migration and enrichment, this has important implications for pollution monitoring and control of the lake environment.
     Bosten Lake is the largest inland rfreshwater lkae in China. It plays an important role in regulating ecological environment and maintaining sustainable development of local economy, society and environment of the area. However due to The regulation of this area industrial,agricultural production and local area river in recent decades,there are more and more sewage drained into Boston lake,which cause its water-quality deterioration. The ecological balance of the region severely affected.The survival of the human environment has been greatly damaged.In this paper,taking Bosten Lake, an arid areas lake, as the study object,a series of samples collected during the survey on the surface sedimentof the Bosten Lake was analyzed to reveal the content and spatial distribution of major and trace elements, study the correlation of the elements in sediments, discusses the control factors of the element, space distribution.Moreover, Pollution assessment of heavy metals was done in study area.
     In this paper47water and29sediment samples of the Boston Lake are analyzed,the main conclusions can besummed up as follows:
     (1)Bosten Lake is a semi-enclosed lakes, and the inlet and outlet at the western end of the of the lake and are in close proximity.The Lakes hydrodynamic conditions is poor, water residence time is long. And Bosten Lake pollution sources are mainly located Huangshui bay area.The conductivity contour and pH contour reflect the degree of pollution is low in Kaidu River estuary, a high degree in Huangshui region, while the center of the lake is between between them.
     (2) Major elements analyzing results show that the CaO、SiO、2and Al2O3are the most dominant components at the surface sediments. In sediments,Al2O3、Fe2O3、SiO2、K2O、MgO, distributed tendency is the same, namely the content is higher in Kaidu River estuary, lower in Huangshui region.The distribution tendency of CaO is the opposite,that is, the content of CaO is lower in Kaidu River estuary, higher in Huangshui region,. The distribution of trace elements:Co、 Cr、Cu、Ni、Pb、Zn contents is is the same, higher in Kaidu River estuary, lower in Huangshui region, middle and steady in lake center. The distribution of As is not evident. The distribution of elements:Sr、CaO contents is similar, the content of Sr and CaO are both subject to biological materials.
     (3)The significance of geochemistry was discussed by using the correlation analysis and factor analysis of elements. The results are as follows:
     ①Ti with Fe2O3、SiO2、A12O3、MgO and K2O was a significant positive correlation, they represents the source of terrestrial clastic and clay minerals.CaO with Ti、Fe2O3、SiO2、Al2O3、 and other major element was a significant negative correlation, suggesting the enrichment of CaO is different from the above elements, it represents the source of the bioclastic component..As exist a weak negative correlation with CaO,among Fe2O3、SiO2、Al2O3、MgO、K2O exist a weak positive correlation, suggesting that these elements not only came from terrestrial source, also have some other sources.Co、 Ni、Pb、Cr、Zn、Cu with Tk、SiO2、Al2O3and other major element was a significant positive correlation, suggesting the distribution of these elements affected by terrigenous material.Sr with Tk、 SiO2、A12O3、and other major element was a significant negative correlation.
     ②Major elements analyzing results show that:A12O3、Fe2O3、SiO2、MgO、K2O、Ti、Cu、 As、Ni、Pb and the other major element was a significant negative correlation, but the negative correlation with Sr and CaO.These factors came mostly from continental source and biological source(F1). F2showed that the main factors in this research area was lake chemistry, the main element component was Na2O.F3showed that the Pollution by human activity, the main elements was As.F4represents a mixed deposition of biogenic and autogenetic deposits, which the main elements component was P.
     (4)The heavy metals of surface sediments, such as Ni、Co、Cr、Zn、P、Cu were analyzed by using the method of Enrichment Factor.The accumulation degree of these heavy metals is as: Ni>Co>Cr>Zn>Pb>Cu.The result showed that Ni、Co、Cr and Zn were in a moderate level of pollution,Pb was in slightly heavy metal pollution level,Cu was in a pollution-free level.
引文
[1]Blaser P,Zimmermann S,Luster J,et al.Critical Examination of Trace Element Enrichments and Depletions in Soils:As,Cr,Cu,Ni,Pb and Zn in Swiss Forest Soils[J].The Science of the Total Environment,2000,249:257-280.
    [2]Daskalakis K,O'Conner T.Normalization and Elemental Sediment Contamination in the Coastal United States[J].Environmental Science and Technology,1995,29:470-477.
    [3]Murray R W,Knowlton C,Leinen M,et al. Export production and terrigenous matter in the Central Equatorial Pacific Ocean during interglacial oxygen isotope stage 11 [J]. Glob.Planet. Change,2000,24:59-78.
    [4]Siegel F R.Enviromental geochemistry of potentially toxicemtals[M].springer,2002.
    [5]Steinnes E,Allen RO,Petersen H M,etal.Evidence of Large Scale Heavy Metal Contamination of Natural Surface Soils in Norway from Long2Range Atmospheric Transport [J].The Science of the Total Environment,1997,205:255-266.
    [6]Sutherland R A.Bed Sediment-Associated Trace Metals in an Urban Stream, Oahu, Hawaii[J]. Environ.Geol.,2000,39:611-627.
    [7]Tam N F Y,Yao M W Y.Normalisation and Heavy Metal Contamination in Mangrove Sediments[J].The Science of the Total Environment,1998,216:33-39.
    [8]Tania L,Micaela P,Malcolm C.Heavy Metal Distribution and Controlling Factors within CoastalPIainSediments,BellsCreekCatchment,SoutheastQueensland,Australia[J].Environment International,2003,29:935-948.
    [9]Vieente Clavero,joseA. Fernandez & F.xavier, Bioturbation by Nereissp.And its effects on the phosphate flux across the sesediment-water interface in the Palmones River estuary,Hydrobiologia,1992,235/236:387-392.
    [10]Wei G J,Liu Y,Li X H,et al. High resolution elemental records from the South ChinaSea and their paleoproductivity im-plications[J]. Paleoceanography,2003b,18(2):1054-1065.
    [11]Zhang, J., Huang, W.W., Liu, S.M., Liu, M.G., Yu, Q. (1992). Transport of particulate heavy metals towards the China Sea:a preliminary study and comparison.Marine Chemistry 40(3-4):161-178.
    [12]Zoller W H,Gladney E S,Duce R A.Atmospheric Concentrations and Sources of Trace Metals at the South Pole[J].Science,1974,183:199-201.
    [13]曹建廷,王苏民等.近千年来内蒙古岱海气候环境演变的湖泊沉积记录[J].地理科学,2000,20(5):391-396.
    [14]陈道华,蒋少涌,刘坚.西沙海槽表层沉积物地球化学特征及其地质意义[J].海洋地质与第四纪地质,2005,25(2):37-43.
    [15]陈弘,刘坚,王宏斌.琼东南海域表层沉积物常量元素地球化学及其地质意义[J].海洋地质与第四纪地质,2007,27(6):39-45.
    [16]陈静生,王飞越等.中国东部河流沉积物中重金属含量与沉积物主要性质的关系[J].环境化学,1996,15(1):8-14.
    [17]陈静生等.中国东部河流沉积物中重金属含量与沉积物主要性质的关系[J].环境化学,1996,15(1):8-14.
    [18]程凤鸣.南四湖水环境污染特征及其重金属离子去除机理研究[D].山东大学,2010.
    [19]程其畴.博斯腾湖水质矿化度演变及展望[J].大自然探索,1994,13(2):70-76.
    [20]楚蓓.珠江口滨海湿地沉积物重金属环境行为研究[D].暨南大学,2006.
    [21]丁海燕等.乐清湾近代沉积物元素地球化学特征及环境意义[J].海洋湖沼通报2010,(01):139-144.
    [22]丁淑萍.博斯腾湖水环境现状分析[J].中国西部科技,2008,07(14):23-24
    [23]董晓丹,周琪.我国河流湖泊污染的防治技术及发展趋势[J].地质与资源,2004,13(1):26-29.
    [24]高丽等.湖泊沉积物中磷释放的研究进展[J].土壤,2004,36(1):12-15.
    [25]庚莉萍.湖泊污染向人类敲响警钟[N].珠江水运,2006-5.
    [26]官宝聪等.泉州湾表层沉积物元素特征及其地球化学意义[J].台湾海峡,2010,29(1):59-64.
    [27]郭海全,郝俊杰,李天刚.河北平原土壤重金属人为污染的富集因子分析[J].生态环境学报,2010,19(4):786-791.
    [28]韩龙喜,张防修等.博斯腾湖湖流及矿化度分布研究[J].水利学报,2004,(10):100-105.
    [29]韩美等.近30年来我国湖泊沉积研究的进展[J].山东师范大学学报(自然科学版),2003,18(3):52-55.
    [30]贺志鹏.南黄海重金属的演变特征及控制因素[D].中国科学院海洋研究所.2008.
    [31]胡汝骥,姜逢清,王亚俊等.亚洲中部干旱区的湖泊[J].干旱区研究,2005,22(2):424-429.
    [32]霍坎松L,杨松M..湖泊沉积学原理[M].北京:北京科学出版社.1992
    [33]蒋富清等.冲绳海槽南部表层沉积物地球化学特征及其物源和环境指示意义[J].沉积学报,2002,20(4):680-685.
    [34]金相灿,章宗涉等.中国湖泊环境(第二册)[M].北京:海洋出版社.1995.
    [35]金相灿等.沉积物污染化学[M].北京:中国环境科学出版社,1992,66-67.
    [36]康跃惠,麦碧娴.珠江三角洲河口及邻近海区沉积物中含氯有机污染物的分布特征[J].中国环境科学,2000,20(3):245-249.
    [37]兰文辉,刘建平.博斯腾湖水质变化分析与对策研究.重庆环境科学[J],2000,24(4):86-88.
    [38]蓝先洪,申顺喜.南海中部沉积岩心的地球化学特征[J].海洋地质与第四纪地质,2000,20(2):33-38.
    [39]蓝先洪.中国主要河口沉积物的重金属地球化学研究[J].海洋地质动态,2004,20(12):1-4.
    [40]蓝先洪等.珠江三角洲第四纪沉积Ti02/A1203值及地质意义[J].台湾海峡,1992,11(3):227-232.
    [41]李传顺,冲绳海槽西南端全新世以来的沉积特征及其物源与环境意义[D].中国科学院海洋研究所,2009.
    [42]李世杰,窦鸿身等.我国湖泊水环境问题与水生态系统修复的探讨[J].中国水利,2006,13:14-17.
    [43]李益敏等.滇池污染特征及治理对策[J].云南地理环境研究,2003,4(15):33-37.
    [44]李玉,俞志明,宋秀贤.运用主成分分析(PCA)评价海洋沉积物中重金属污染来源[J].环境科学,2006,27(1):137-141.
    [45]李玉等.重金属在胶州湾表层沉积物中的分布与富集[J].海洋与湖沼,2005,36(6):580-586.
    [46]林炳煌等.九龙江河口表层沉积物元素特征及地球化学意义[J].厦门大学学报(自然科学版)2002,20(4):681-686.
    [47]刘恩峰,沈吉.太湖表层沉积物重金属元素的来源分析[J].湖泊科学,2004,16(2):113-119.
    [48]刘广虎,李军,陈道华,等.台西南海域表层沉积物元素地球化学特征及其物源指示意义[J].海洋地质与第四纪地质,2006,26(5):61-68.
    [49]刘卫国,安尼瓦尔·木扎提,吕光辉.博斯腾湖流域风险评价[J].干旱区资源与环境, 2008,22(8):33-37.
    [50]刘月杰.博斯腾湖芦苇湿地生态恢复研究[D].北京化工大学,2004.
    [51]马英军,万国江.湖泊沉积物-水界面微量重金属扩散作用及其水质影响研究[J].环境科学,1999,20(3):7-11.
    [52]孟伟,翟圣佳,秦延文等.渤海湾潮间带(大沽口)柱状沉积物中的重金属来源判别[J].海洋通报,2006,25(1):62-69.
    [53]孟翊等.长江口沉积物重金属元素地球化学特征及其底质环境评价[J].海洋地质与第四纪地质,2003,23(3):37-43.
    [54]牟保磊等.元素地球化学[M].北京:北京大学出版社.1999.
    [55]欧文佳.正构烷烃分布特征及稳定同位素组成在湖泊污染监测中的应用——以新疆博为例[D].兰州大学,2010.
    [56]沈吉,王苏民,羊向东.湖泊沉积物中有机碳稳定同位素测定及其古气候环境意义[J].海洋与湖沼,1996,27(4):400-403.
    [57]沈吉等,湖泊沉积与环境演化[M].北京:科学出版社,2010.
    [58]孙千里,周杰,肖举乐.岱海沉积物粒度特征及其古环境意义[J].海洋地质与第四纪质,2001,21(1):93-95.
    [59]孙占东,王润,黄群等.近20年博斯腾湖与岱海水位变化比较分析[J].干旱区资源与环境,2006,20(5):56-60.
    [60]唐兵,安瓦尔等.新疆博斯腾湖水污染现状评价[J].伊犁师范学院学报(自然科学版)[J],2011,4:35-39
    [61]田文成等.博湖县志[M].乌鲁木齐:新疆大学出版社.1993.
    [62]王博等.兰州市城区河道表层沉积物地球化学元素分布特征[J].中国沙漠,2012,32(1):168-174.
    [63]王静雅.成都市湖塘沉积物重金属元素环境地球化学研究及城市污染史初析[D].成都理工大学,2005.
    [64]王军广,海南岛北部红树林地区沉积物元素地球化学特征研究[D].海南师范大学,2011.
    [65]王君波,朱立平.藏南沉错沉积物的粒度特征及其古环境意义[J].地理科学进展,2002,21(5):459-467.
    [66]王开勇,杨乐,庞玮.博斯腾湖入湖水质分析与评价[J].石河子大学学报(自然科学版).2008.26(4):423-426.
    [67]王苏民,窦鸿身.中国湖泊志.北京:科学出版社.1998.
    [68]王亚俊,李宇安,谭芫.新疆博斯腾湖生态环境变迁分析[J].干旱区资源与环境,2004,18(2):61-64.
    [69]王亚俊,李宇安等.20世纪50年代以来博斯腾湖水盐变化及趋势[J].干旱区研究,2005.22(3):357-359.
    [70]夏军,左其亭,邵民诚.博斯腾湖水资源可持续利用——理论·方法·实践[M].北京:科学出版社.2003.
    [71]夏鹏等.连云港近岸海域表层沉积物中重金属的地球化学特征及其源解析[J].海洋环境科学,2011,30(4):520-524.
    [72]谢贵娟,张建平等.博斯腾湖水质现状(2010-2011年)及近50年来演变趋势[J].湖泊科学2011,23(6):837-846.
    [73]徐海量,陈亚宁,李卫红.博斯腾湖湖水污染现状分析.干旱区资源与环境[J],2003,17(3):95-97.
    [74]杨彬,解启来等.博斯腾湖沉积物中有机氯农药的分布特征及生态风险评价[J].湖泊科学,201123(1):29-34.
    [75]杨守业等.中韩河流沉积物微量元素地球化学研究[J].海洋地质与第四纪地质,2003,23(2):21-24.
    [76]殷福才等.巢湖富营养化研究进展[J].湖泊科学,2003,15(4):377-384.
    [77]袁峡,杨佃华.博斯腾湖水污染控制与治理技术路线分析[J].环境工程,2009,27(z):16-19.
    [78]曾前东,朱明华等.苏州河底质中有机污染物对河水影响的估价和预测[J].中国环境科学,1993,13(2):112-115.
    [79]张成君等.博斯腾湖碳酸盐和同位素组成的全新世古环境演变高分辨记录及与冰川活动的响应.地质学报[J].2007,81(12):1658-1671.
    [80]张虎才等.元素表生地球化学特征及理论基础[M].兰州:兰州大学出版社.1997.
    [81]张建平等.博斯腾湖流域生态环境现状及治理对策浅析[J].环境科技,2010,23(2):76-79.
    [82]张经.中国河口地球化学的一些研究进展[J].海洋与湖沼,1994,25(4):438-445.
    [83]张俊,周成虎等.新疆焉奢盆地近40年土地利用与土地覆被演化[J].资源科学,2004,26(6):30-37.
    [84]张秀芝,鲍征宇,唐俊红.富集因子在环境地球化学重金属污染评价中的应用[J].地质科技情报,2006,25(1):65-72.
    [85]张永三,吴丰昌等.新疆博斯腾湖重金属污染的沉积记录[J],地球与环境,2009,37(1):50-55.
    [86]张远辉,杜俊民.南海表层沉积物中主要污染物的环境背景值[J].海洋学报,2005,27(4):161·166.
    [87]张振克,吴瑞金.岱海湖泊沉积物频率磁化率对历史时期环境变化的反映[J].地理研究,1998,17(3):297-302.
    [88]赵龙,单秀琴,达伟等.新疆博斯腾湖水量的演变[J].河南水利与南水北调,2009,152(2):15-16.
    [89]赵伦山,张本仁.地球化学[M].北京:地质出版社.1987.
    [90]赵青芳等.南海神狐表层沉积物常量元素地球化学特征及其物源分析[J].海洋地质动态,2009,25(5):10-14.
    [91]赵万苍,何江等.达里诺尔湖表层沉积物中腐殖质的分布特征[J].农业环境科学学报,2011,30(2):341-346.
    [92]赵雪力.博斯腾湖生态告急[N].亚洲中心时报(汉),2008-8-19(001).
    [93]赵一阳,鄢明才,中国浅海沉积物地球化学[M].北京:科学出版社,1994.
    [94]朱程等.湘西河流表层沉积物重金属污染特征及其潜在生态毒性风险[J].生态学报,2010,30(15):3982-3993.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700