Mytilus galloprovincialis and Parapenaeus longirostris as bioindicators of heavy metal and organochlorine pollution

The worth of the data obtained from Mytilus galloprovincialis and Parapenaeus longirostris for the purpose of assessing the extent to which the areas they come from are polluted by heavy metals (Fe, Zn, Cu, Pb, Mn, Ni, Cd, Cr, Co) and chlorinated hydrocarbons (PCBs, p,p'DDE, p,p' DDT, p,p'DDD, BHCs, heptachlor epoxide, dieldrin, endrin), was thoroughly investigated. The work embraced the accuracy of the determinations, the spot and area variability, the overall coefficient of variation, the effect of the season and the size, together with, in the case of P. longirostris, the differences observed in four sections of the Saronikos Gulf, in Greece, the degree of pollution, which was estimated independently by measuring the concentration in the water of nutrients (phosphate, ammonia, nitrite, nitrate, silicate) and dissolved oxygen. The study proved the feasibility of employing the organisms as bioindicators of pollution. It also established that the individual variability of response, the season and the size do not cause as much assessment error as the commonly huge temporal fluctuations and the frequent inadequacies of the analytical procedures. A scheme is described for the collection of a truly representative sample.     

鹫峰国家森林公园大气中VOCs的组成与特点

采用TCT-GC/MS方法对鹫峰国家森林公园大气中挥发性有机物(VOCs)的组成进行分析,共检测到175种挥发性有机化合物,主要成分包括烷烃类、芳香烃类、酯类、酸类、醛类、酮类和萜烯类等七类,平均相对含量分别为48.11%,15.67%,17.28%,3.13%,3.17%,1.36%和1.45%;活动区中检测到的挥发性有机化合物种类最多,缓冲区次之,非活动区最少,这与每个区中人类活动的频率相一致.同时分析了大气中的VOCs的时空分布特点.     

野生及养殖背角无齿蚌中元素的生物积累特征

作为建立渔业生态环境“淡水贝类观察”体系的基础研究之一,以宜兴养殖水域（N=7）和太湖三山岛自然水域（N=7）采集的背角无齿蚌（Anodonta woodiana）为对象,运用电感耦合等离子质谱仪测定了背角无齿蚌软组织中元素Na、K、Ca、Mg、Mn、Fe、Co、Ni、Se、Cu、Cr、Cd的质量分数范围,并对各种元素积累水平的差异进行比较研究。结果表明,两水域中背角无齿蚌对元素的积累高低顺序具有相似的趋势。其中Ca质量分数最高,Co、Cr的质量分数最低,其它元素界于其间。养殖蚌样中的常量元素Na、K、Ca、Mg和微量元素Mn、Co的积累质量分数高于或接近自然水域蚌样中的相应元素,但后者中的重金属元素Cr、Cu、Cd、Ni质量分数显著地高于前者。养殖水域蚌样中的Mg-K、Mg-Ca、Mg-Ni、Mg-Mn、K-Ca、K—Co、K．Mn、Ca—Co、Ca—Ni、Ca．Mn、Ni—Mn、Cr-Co、Cu-Cd以及自然水域蚌样中的Mg—K、Ca-Cr、Ca—Mn、Ca-Ni、Ca-Cd、Cr—Mn、Cr-Ni、Cr-Cd质量分数之间呈现显著的相关性。     

武汉月湖水体主要元素与浮游植物的PCA与CCA分析

通过2007年1—12月对武汉月湖不同的取样点进行监测,并选择汉江琴台段水域作为研究对照,调查了月湖水体硅藻、蓝藻与水体主要元素的种类,采用PCA、CCA分析法探讨了月湖水体硅藻、蓝藻与水体元素种类的关系。结果表明:月湖水体中所含元素全年监测出28种;汉江琴台段水域中所含元素全年监测出27种。经PCA分析表明,月湖水体中累计贡献率较大为磷(P)、砷(As)、铁(Fe)、铜(Cu)、锰(Mn);汉江琴台段水域累计贡献率较大为硅(Si)、锑(Sb)、镉(Cd)、钒(V)、钡(Ba)、Ag(银)、钼(Mo)。月湖水体中蓝藻密度大于硅藻,汉江琴台段水域硅藻密度大于蓝藻。经CCA分析表明,月湖硅藻密度与硒(Se)、锶(Sr)、银(Ag)、Ba、铝(Al)呈正相关关系;月湖蓝藻密度与P、Cu、铬(Cr)呈正相关关系,月湖蓝藻密度与镁(Mg)、镍(Ni)、钙(Ca)、锌(Zn)、硫(S)呈负相关关系。CCA分析中,汉江琴台段硅藻密度与铅(Pb)、硼(B)、As、Cr、Zn、Al、Cu、Mn、Fe、P呈负相关关系,汉江琴台段硅藻密度与Mo、Ca、钴(Co)、V、Sr、Ag呈正相关关系;汉江琴台段蓝藻密度与钠(Na)、S、Mg、Ni、钾(K)呈负相关关系。月湖水体缺乏可溶硅(dissolved silicon,DSi),硅藻会提升对其他元素(Se、Sr、Ag、Ba、Al)的吸收能力,这些元素会起到缺乏元素(Si)近似的作用,替代性可能出现。水中各种元素的组态是导致月湖浮游植物群落发生演变的重要原因之一。     

Löwenzahn Taraxacum officinale Web. als (städtischer) Bioindikator

Investigations of the dandelion, Taraxacum officinale Web. in Poland, Romania and Germany showed that the species concentrates various elements dependent on the intensity of the pollutants. In this study, we followed up the question of whether T. officinale enriches pollutants by the atmospheric deposition on the leaves or via the soil. Therefore, samples from at least 10 plants and a soil sample at 57 sample sites were collected from a grid of 500 m × 500 m. In addition to the analysis of the total soil sample, the (mobile) ion pool of the soil (DIN V 19739) was analysed. The elements Al, As, Ba, Ca, Cd, Ce, Co, Cr, Cu, Fe, Ga, K, Mg, Mn, Mo, Na, Ni, Rb, Sr, Ti, Tl, V, and Zn were determined through the use of spectrometry with inductive coupled plasma (ICP-MS and ICP-OES). The results are compared with the element concentrations of washed and unwashed leaf samples in T. officinale. We could only find two direct correlations (Ti and Zn) between the element content, of the entire soil samples, but 14 correlations (As, Ba, Cd, Cu, Ga, K, Mn, Mo, Na, Ni, Rb, Ti, Tl und Zn) between the ion pool of the soil and the washed samples. The grid point data interpolation by ArcInfo showed a similar distribution pattern for the unwashed leaf elements Al, Ce, Fe, Ti and V (r≥0.75). The elements Al, Ce, Fe, Ti, and V are washed out at the same ratio. Thus, although the concentration of these elements were significantly reduced by the washing procedure, the correlations were not influenced. The admissibility of the grid point data interpolation for a distribution map of the town area was investigated, as well. It is shown that the element content varies with the land use (meadow, field, rural areas), the sampling point and the local pollutants. However, none of the discussed elements, Al, Ce, Fe, Ti, and V, is significantly influenced by the land use. The data allows one to make the conclusion that the elements of Al, Ce, Fe, Ti and V are dependent on the dry and wet deposition on the leaves of T. officinale. These elements are taken up not only by the roots, but also by the surface of the leaves. This is evident because there is no correlation between one of these elements in the leaves and the ion pool of the soil.     

论我国水生态的保护与修复:任务与对策

本文聚焦我国水生态保护与修复工作,结合长期实践,分析当前的形势和任务,指出了当前要着力解决的水生态问题主要是:在大坝上游,河流变湖库,生境变化导致生物物种变化;水库水流流速变缓,水体自净能力降低,导致富营养化及藻类水华。在大坝下游,清水下泄,冲刷下游河道导致局部河道河势变化较大;水库蓄水使坝下游春季水温下降、秋季水温升高,水温变化过程滞后;水库蓄水导致大坝下游的水文过程改变,水的流量、流速、流态发生变化。在河道(航道)整治工程中,裁弯取直,缩短水流在河道中的停留时间,河岸衬砌和硬化,减少水向沿河堤岸的渗透,在大降水和洪水时易造成涝灾和洪灾。在涉湖工程中,阻隔河湖,填湖造地。在明确存在问题和迫切需求的基础上,提出了切实可行的对策建议。当前水生态保护与修复要围绕一条主线,即"人要发展,鱼要生存"的"人鱼线",要采取"调、控、退、通、改、拆"的综合措施,即生态调度,控制水污染,退建还水、退田还湖,河湖连通,对已建涉水工程进行生态化改造,对在保护区、重点风景名胜区、特有鱼类栖息地修建的小型工程要采取坚决措施拆除,恢复原貌。     

Relationship between heavy metal concentrations of herbaceous plants and soils at four Pb-Zn mining sites in Yunnan, China

This paper studied the relationship between heavy metal concentrations of herbaceous plants and soils at four Pb-Zn mining sites in Yunnan, China. 50 herbaceous plant samples of 9 plant species from 4 families and 50 soil samples were collected and then ana1yzed for the tota1 concentrations of Pb, Cd, and Zn. The results showed that the average concentrations of Pb, Cd, and Zn in soil samples were 3772.83, 168.81, and 5385.65 mg/kg, respectively. The average concentrations of Pb, Cd, and Zn were 395.68, 28.14, and 1664.20 mg/kg in the shoots, and 924.12, 57.25, and 1778.75 mg/kg in the roots, respectively. Heterospecific plants at the same site and conspecific plants at various sites had different average levels of Pb, Cd, and Zn, both in the shoots and the roots. Enrichment coefficients of Pb, Cd, and Zn were greater than 1 in 2, 3, and 9 herbaceous plant samples, respectively. Translocation factors of Pb, Cd, and Zn were greater than 1 in 10, 17, and 25 herbaceous plant samples, respectively. In all 50 samples, the concentrations of Pb, Cd, and Zn between the shoots and the roots, the shoots, and the soils, and the roots and the soils had significant positive relationships.     

电子废物不当处置的重金属污染及其环境风险评价 Ⅳ. 电子废物不当回收地区流域水体沉积物的重金属污染

为了解电子废物不当处置活动对小流域内水体沉积物金属污染的影响,采集了位于广东省清远市龙塘镇和石角镇的电子废物焚烧和酸解活动核心区内水塘和水库的0～40cm沉积物以及附近河流大燕河表层(0～5cm)沉积物样本,分析了样本中的金属(水塘、水库:Zn、Cu、Pb、Cd、Cr;大燕河:Zn、Cu、Pb、Cd、Cr、Ni、Mg、Mn)含量.作为对照,对珠江口伶仃洋沉积物中的5种重金属(Zn、Cu、Pb、Cd、Cr)含量也进行了分析.结果表明,1)在核心区内,5种重金属的平均含量在接近酸解作坊的水塘沉积物中呈Cu(766.16mg·kg-1)>Zn(181.12mg·kg-1)>Pb(129.56mg·kg-1)>Cr(1.89mg·kg-1)≈Cd(1.12mg·kg-1),在其下游的水库沉积物中呈现相同的规律,但水塘沉积物的Cu、Zn、Pb含量均高于水库.水塘、水库沉积物重金属含量分布规律明显不同于伶仃洋沉积物,与伶仃洋沉积物相比,核心区水体沉积物Cu含量特别高,是伶仃洋沉积物的7～17倍,Pb和Cd则分别是伶仃洋的2.3～3.0倍和1.9～2.4倍,Zn、Cr含量与伶仃洋沉积物相近.2)Zn含量在核心区水体沉积物中均呈现出在20.0～30.0cm深度最高的趋势,Cu、Pb含量在水库沉积物中也有类似的表现,说明该深度的沉积物可能是电子废物回收处置活动最频繁的时期形成的,近年来随着政府取缔工作的加强,电子废物非法处置活动的减少,Zn、Cu、Pb含量有明显的下降.3)大燕河沉积物中6种重金属(Zn、Cu、Pb、Cr、Cd、Ni)的总含量表现为中游下段(1261.3mg·kg-1)>中游中段(1049.2mg·kg-1)>中游上段(401.8mg·kg-1)>上游(364.6mg·kg-1)>下游(215.4mg·kg-1).Cu、Zn、Pb和Cr含量均在中游下段的沉积物中出现最大值,次大值出现在中游中段,Ni、Cd在中游中段出现最大值,次大值出现在中游下段.中游中、下段沉积物中金属含量最大值和其上游(或中游上段)河段含量最低值的比值呈现Cu(10.1)>Cr(7.8)>Zn(3.8)>Cd(2.0)>Pb(1.9)>Ni(1.8),显示这些重金属主要从中游中、下段进入大燕河沉积物,其中Cu污染最为严重,而Cr污染可能与水土流失或当地其他活动释放的Cr有关.4)比较流域内土壤和各种沉积物以及伶仃洋沉积物中重金属的构成比例发现,核心区土壤和沉积物以及大燕河沉积物中的重金属具有明显的同源性.随着离源区距离的增加,重金属的构成比例中最明显的变化是Cu的比例下降以及Zn的比例上升。     

云南元谋干热河谷区土壤侵蚀对土壤肥力的影响

探讨了云南元谋干热河谷区土壤侵蚀对土壤肥力性质的影响．研究表明，土壤侵蚀使土壤中全氮、全磷、全钾以及碱解氮、速效磷、速效钾等养分淋失；同时，有机质含量减少，土壤有机无机复合量降低，松结态腐殖质减少．Ａ／Ｃ值下降；土壤中的过氧化氢酶、蔗糖酶、脲酶等活性也因侵蚀而降低．土壤侵蚀越强烈，土壤肥力退化愈严重．     

草地枯落物分解研究进展及展望

草地枯落物是草地生态系统中生物组分枯死后所有有机物质的总称,是草地生态系统重要的组成部分,是除冠层外,大气与矿质土壤层、植物根系层进行物质与能量交换的另一介质,在生态学中起着不可替代的作用。随着西部大开发战略和退耕还林还草工程的实施,大型家畜等草食性动物退出草地生态系统后,枯落物成为草地生态系统物质和能量循环的重要调节枢纽。近年来,随着全球应对气候变化、节能减排和低碳经济所面临的压力,作为全球碳循环的重要组成部分,草地枯落物的研究被越来越多的学者所重视。文章在综述国内外大量文献的基础上,对草地枯落物的概念进行了比较分析,对其进行了准确定义;归纳出了尼龙网袋法、室内分解培养法、现量估算法和同位素法等多种草地枯落物分解方法,并就枯落物分解过程中经常采用的分解率概算模型、时间衰减模型、影响因子关系模型等进行了比较分析,总结出枯落物的分解是由淋溶、自然粉碎和代谢等3个主要作用,碎屑食物链、腐食食物链等2种不同的食物链共同组成的复杂过程。开展长期定位监测、形成统一的研究方法,探索枯落物分解过程中碳循环微观机理,以及影响因子之间的交互作用是未来草地枯落物研究工作的重点。     

《生药学》CAI软件的应用研究

探索了《生药学》辅助教学软件的制作,阐述了该软件制作方法,进行资料收集与整理制作,软件编制,描述了其应用特点,操作主界面简洁,按照《生药学》教学特点,编制了笔划、药用部位、科名、拉丁药名四种查询方法,不但在课堂教学中应用效果佳,而且还用于实验教学.进行CAI系统设计,动态组织教学内容,调整教学方法,加强了老师和学生之间的交互能力,实现了以学生为主体课程网络教学辅助方式.图2,参5.     

DDT对池塘模型生态系统的影响

运用微宇宙实验方法研究了浓度为0.2、2.0、20.0和200.0μg·L-1的DDT对池塘模型生态系统结构和功能的影响.结果表明,整个实验过程(4周)中对照组和浓度为0.2、2.0、20.0和200.0μg·L-1的DDT暴露组水体pH均值分别比实验前下降了0.28、0.19、0.15、0.38和0.37,电导率均值分别下降了6.3%、3.1%、4.7%、6.6%和8.6%;对照组和0.2、2.0、20.0μg·L-1组水体溶解氧(DO值)分别上升了27.3%、28.1%、26.4%和14.4%,而200.0μg·L-1组的DO值下降了7.2%.各组中总磷浓度在实验中后期即下降到较低的水平,总氮的浓度也大幅度下降.和对照组相比,200.0μg·L-1的DDT对大型水生植物优势种类浮萍(Lemna minor)的生长繁殖具有抑制作用,而其它浓度的DDT具有促进作用;DDT对菹草(Potamogeton crispus)的生长影响不明显.DDT可使浮游动物种类减少.2.0μg·L-1的DDT对方形网纹溞(Ceriodaphnia quadrangula)、枝角类和桡足类密度均具有促进作用,20.0和200.0μg·L-1的DDT使轮虫和介形亚纲动物数量在实验后期上升,除此以外,随时间的推移,各浓度的DDT使各类浮游动物密度下降的幅度均大于对照组.与实验前相比,对照组以及浓度为0.2、2.0和20.0μg·L-1的暴露组中凸旋螺(Cyraulus convexiusculus)重量分别增加了12.8%、5.3%、102.2%和219.9%,而200.0μg·L-1组中凸旋螺重量下降了33.8%.随着DDT浓度的升高,微宇宙中的细菌总数总体呈现出下降的趋势.整个实验过程中,对照组的群落总生产量/群落呼吸量(P/R比值)的平均值接近于1,表明生态系统成熟稳定;而各暴露组P/R比值均大于1.1,这可能与DDT对浮游动物具有较强的毒性作用,而对水生植物没有明显影响有关.     

多种盐分离子作用下苋菜对重金属的吸收累积特征

模拟不同淋洗脱盐阶段滩涂土壤孔隙水中盐分和重金属含量,通过苋菜水培试验,研究多种盐分离子（SO42-、Cl-、NO3-、CO32-、Na＋、Ca2＋、K＋和Mg2＋等）的共同作用下,苋菜对Zn、Cu、Ni、Cr、Pb和Cd 6种重金属的吸收、累积和转运的变化。结果表明,与对照相比,在不同盐分离子浓度影响下,苋菜茎叶中Cd的累积增幅为69.2%～146.2%,而茎叶中其他重金属的含量无显著变化,苋菜根系中Cd、Pb、Cr、Ni和Cu含量的最大增幅分别为187.8%、197.7%、305.7%、228.1%和58.2%,但根系中Zn含量未受到显著影响。在相对较高的盐分离子浓度（〉1 312.4 mg.L-1）范围内,不同盐分离子浓度处理间苋菜茎叶和根系中6种重金属含量差异均不显著。盐分处理显著降低了苋菜对Pb、Cr、Ni和Cu的转移系数,但未显著影响苋菜对Cd和Zn的转移系数。     

农田土壤重金属污染状况及修复技术研究

重金属污染因具有毒性、易通过食物链在植物,动物和人体内累积,对生态环境和人体健康构成严重威胁。随着工业快速发展、农药及化肥的广泛使用,农田土壤重金属污染越来越严重,研究农田土壤重金属污染现状及修复技术对农产品安全具有重要意义。综合国内外农田土壤重金属污染状况,农田土壤重金属污染主要来源于固体废弃物堆放及处置、工业废物大气沉降、污水农灌和农用物质的不合理施用。该文综述了国内外有关农田重金属污染土壤修复技术（物理修复、化学修复、生物修复、农业生态和联合修复）的研究进展,并针对各种修复方法,阐述了其原理、修复条件、应用实例及其优缺点,重点论述了植物修复的机理和应用,提出了草本与木本联合修复可有效提高农田土壤重金属复合污染的修复效率,为农田土壤土壤重金属复合污染修复提出了新的途径。最后在对已有研究分析的基础上,提出了联合修复技术（如生物联合技术、物理化学联合技术和物理化学-生物联合技术）可以在一定程度上克服使用单一修复手段存在的缺点,可提高复合污染的修复效率、降低修复成本,未来应深入探索联合修复技术间的相互作用机理,以期为农田土壤重金属综合治理与污染修复提供科学依据。     

The spatial relationship between human activities and C,N, P,S in soil based on landscape geochemical interpretation

The development and formation of chemical elements in soil are affected not only by parent material, climate, biology, and topology factors, but also by human activities. As the main elements supporting life on earth system, the C, N, P, S cycles in soil have been altered by human activity through land-use change, agricultural intensification, and use of fossil fuels. The present study attempts to analyze whether and how a connection can be made between macroscopical control and microcosmic analysis, to estimate the impacts of human activities on C, N, P, S elements in soil, and to determine a way to describe the spatial relationship between C, N, P, S in soil and human activities, by means of landscape geochemical theories and methods. In addition, the disturbances of human activities on C, N, P, S are explored through the analysis of the spatial relationship between human disturbed landscapes and element anomalies, thereby determining the diversified rules of the effects. The study results show that the rules of different landscapes influencing C, N, P, S elements are diversified, and that the C element is closely related to city landscapes; furthermore, the elements N, P, and S are shown to be closely related to river landscapes; the relationships between mine landscapes and the elements C, N, P, S are apparent; the relationships between the elements C, N, P, S and road landscapes are quite close, which shows that road landscapes have significant effects on these elements. Therefore, the conclusion is drawn that the response mechanism analysis of human disturbance and soil chemical element aggregation is feasible, based on the landscape geochemical theories and methods. The spatial information techniques, such as remote sensing and geographic information systems, are effective for research on soil element migration.     

植物挥发性气体与人类的健康安全

植物挥发性气体产生的原因主要是由于植物与自然的协同进化而产生的。一方面，植物挥发性气体的产生受昆虫、微生物、人类的干扰的影响；另一方面，植物的挥发性气体能对昆虫、微生物起到抑制作用，减少自身受伤害。目前国内外对植物挥发性气体的研究多从植物与昆虫、微生物的关系来进行，并形成了以化感作用研究为核心的化学生态学；而植物挥发性气体对人类的负面影响，特别是对人体健康安全的研究很少。文章结合作者的初步研究结果，综述植物的挥发性物质的产生原因、主要成份和对环境与生物的影响，特别是对人体健康安全的负面效应，为进一步研究植物挥发性气体和评价它们对人体健康安全的效应提供依据。     

Geochemistry of the barkinite liptobiolith (Late Permian) from the Jinshan Mine,Anhui Province,China

This paper discusses the geochemistry and mineralogy of the barkinite liptobiolith of the Late Permian age from the Jinshan Mine, Guangde County, Anhui Province, China. Samples were examined using inductively coupled plasma-mass spectroscopy, X-ray fluorescence, cold-vapor atomic absorption spectrometry, ion-selective electrode, sequential chemical extraction, scanning electron microscopy equipped with energy-dispersive X-ray, and optical microscopy. The coal is a medium-ash and high-sulfur resource. Minerals in the coal are composed of kaolinite, pyrite, calcite, and quartz. Pyrite and calcite are derived from seawater during peat accumulation. Quartz in the coal is of authigenic origin. Part of the kaolinite is from a land-source region, and part occurs as cell-fillings and is of authigenic origin. The results also indicate that the barkinite liptobiolith contains some toxic elements in high concentrations. Elements including Li, Be, Si, Sc, Ti, V, Cr, Fe, Ga, Se, Y, Zr, Mo, the rare earth elements (REEs), W, Hg, Tl, Pb, Th, and U in the coals are enriched in the barkinite liptobiolith. Results of sequential chemical extraction showed that Li, Sc, Ti, Cr, Y, Zr, REEs, and Th in the coal mainly occur as silicates, while Be and W are related to organic matter. Pyrite is the dominant source of S, Mo, Hg, Tl, and Pb. Gallium only occurs in silicate, and U and V occur both in organic and silicate associations.     

实现传统经济向生态经济的转变

认为生态环境危机的出现，归根结蒂，在于人类社会的价值观存在着重大的错误以及由此而采取的经济发展模式存在着重大的错误；要缓解生态环境危机，人类社会必须改变价值观，改变经济发展模式，实现传统经济向生态经济的转变，走可持续发展的道路；为了实现这种转变，人类在经济活动中，必须遵循生态经济规律，建立企业生态经济管理模式，合理利用资源，优化产业结构，重视经济效益、社会效益和生态效益的协调和统一。文章还认为，为了实现这种转变，从联合国到个人，各国政府、各种组织、各行各业，都必须行动起来，参与生态经济建设。最后提出和讨论了生态经济学今后应该加强研究的几个问题。     

Trace element geochemistry of the Keana brines field,middle Benue trough,Nigeria

A trace elements study of various samples from the Keana brines field, middle Benue Trough was carried-out to determine the extent to which Pb–Zn–S and BaSO₄ mineralisations have affected the quality of the brines and the waters in the area. Different sample media such as well-water, pond water, brine spring pool water, stream water, stream sediments etc. were analysed. Geochemical results show that Cu, Zn, Pb, As and S are concentrated in the waters (0.3, 0.36, 0.05, 0.07 and 1 1.5 ppm respectively). These elements are more concentrated in both the spring and pond waters, suggesting that the spring water could have acted as the transport medium for these elements released from deep-seated sources. Transitions elements (Ti, V, Cr, Fe, Co, Ni and Sr) are concentrated in the waters. Compared to the World Health Organization (WHO) admissible limits, the well waters present very high concentrations in Cd (0.56 ppm) and Sb (0.40 ppm) (200× and 70× WHO admissible values respectively). There is a preferential concentration of transition elements (Ti, V, Fe, Co and Ni) in the sediments (41.38, 362, 52.21, 269 and 54 ppm respectively) than in the waters (0.70, 0.05, 5.6, 0.04 and 0.02 ppm respectively). Similarly, Cu, Zn, Pb and As are concentrated in the sediments (44, 72, 41 and 14 ppm respectively). The concentrations of transition elements (Ti, V, Cr, Fe, Co and Ni) in the refined salt were highly elevated (784, 363, 283, 105, 59.2 and 42.6 ppm respectively) (7000–10,000× well water). Similarly, the concentrations of As, Pb, Br and Sr in the refined salt were also alarming (11.6, 16.4, 16.4 and 122 ppm respectively), (1000, 700, 3000 and 20,000× well water values respectively). S on the other hand is absent. One of the striking features is the absence of I, Cd, Sb and Se in the refined salt crystals which were detected in the waters and the brines. Compared to WHO admissible values, the refined salt crystal concentrations for Ni (426 ppm) and Cr (283 ppm) were also very high (2000× WHO values respectively) and to a lesser extent Cu (26.9 ppm) and Zn (21.7 ppm) (12 and 7× WHO values respectively).     

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