北京市街道灰尘中重金属元素赋存状态及环境效应   总被引：5，自引：3，他引：2  

刘春华  岑况  于扬 《岩矿测试》2011,30(2):205-209

采用Tessier的五步提取法,对北京北西—南东剖面所采集的街道灰尘样品粒度≤100μm组分中As、Cd、Cr、Hg、Pb和Zn等6元素的5个形态(可交换态、碳酸盐结合态、铁锰氧化物结合态、有机物结合态、残渣态)的分布特征研究发现,在可交换态和碳酸盐结合态中Cd的含量比都为最高,Pb、Hg、Zn和As在有机物结合态中含量比相近,铁锰氧化物结合态中Pb所占比例最高,而As和Cr主要存在于残渣态中。6种街道灰尘污染元素的相对活动性和潜在生物利用度顺序为:Cd>Zn>Pb>Cr>Hg>As。  相似文献   

Chronostratigraphic basin framework for Palaeoproterozoic rocks (1730–1575 Ma) in northern Australia and implications for base‐metal mineralisation     

P. N. Southgate  B. E. Bradshaw  J. Domagala  M. J. Jackson  M. Idnurm  A. A. Krassay 《Australian Journal of Earth Sciences》2013,60(3):461-483

Sequence‐stratigraphic interpretations of outcrop, drillcore, wireline and seismic datasets are integrated with SHRIMP zircon and palaeomagnetic determinations to provide a detailed chrono‐stratigraphic basin framework for the base‐metal‐rich Palaeoproterozoic rocks of the southern McArthur, Lawn Hill and Mt Isa regions. The analysis forms a basis for future correlations across northern Australia. Nine second‐order unconformity‐bounded supersequences are identified. Supersequences have a duration of 10–20 million years; some hitherto‐unrecognised unconformity surfaces record up to 25 million years of missing rock record. The second‐order supersequences contain a series of nested third‐, fourth‐ and fifth‐order sequences many of which can be correlated across the Mt Isa, Lawn Hill and southern McArthur regions. The analysis relates accommodation history to major intraplate tectonic events evident on the apparent polar wander path for northern Australia. Major tectonic events at approximately 1735 Ma, 1700 Ma, 1670 Ma, 1650 Ma, 1640 Ma, 1615 Ma, 1600 Ma and 1575 Ma impacted on accommodation rates and basin shape in northern Australia. Sub‐basin depocentres, the hosts for major sulfide mineralisation, are attributed to reactivated faults that controlled local subsidence. Pb/Pb model ages of 1653 Ma, 1640 Ma and 1575 Ma for the Mt Isa, McArthur River and Century Pb–Zn–Ag deposits, suggest that changes to intraplate stresses at tectonic events of like age resulted in the migration of metal‐bearing fluids into the sub‐basins. A Pb/Pb model age of 1675 for the Broken Hill deposit suggests that intraplate stresses manifest in northern Australia also affected rocks of similar age further south. Magmatic events close to 1700 Ma (Weberra Granite) and 1675 Ma (Sybella Granite) coincide with times of regional incision and the formation of supersequence‐bounding unconformity surfaces.  相似文献   

Stable isotope,petrological, and fluid inclusion studies of minor mineral deposits from the McArthur Basin: Implications for the genesis of some sediment‐hosted base metal mineralization from the Northern Territory     

M. D. Muir  T. H. Donnelly  R. W. T. Wilkins  K. J. Armstrong 《Australian Journal of Earth Sciences》2013,60(3):239-260

The geology, stable isotopes and fluid inclusions from mineralized and unmineralized Middle Proterozoic sequences of the McArthur Basin, Northern Territory, have been studied at Eastern Creek, Bulman Mines, Beetle Springs, and other localities in the McArthur Basin where disseminated sulphides in unmineralized black shales were available from drill core. At Eastern Creek, galena and minor chalcopyrite (δ³⁴S+3.6 to +11.2%o) occur in an evaporitic sedimentary sequence. Barite (δ³⁴S+18.4 to +24.7%o) also occurs, and saline brines are trapped along healed fractures in the barite. Pressure‐corrected trapping temperatures in the barite (95–138°C), and in vein dolomite (158–168°C) agree with temperature estimates from the degree of maturation of the sedimentary organic matter. The δ¹⁸O and δ¹³C_Co2 values of the mineralizing fluid were calculated to be +3.5 to +4.5%o and ‐2.7%o, respectively. Sedimentary dolomite has restricted δ¹³C and δ¹⁸O ranges, within the reported ranges for non‐mineralized Middle Proterozoic dolomite. An ore formation model developed for Eastern Creek, in which a basinal fluid at about 200°C carrying base metals and sulphide was released from underlying sediments during local fault movement, may be applicable to a number of other deposits. The mineralization deposited from these fluids occurs only below the pre‐Roper Group unconformity, implying that it may be older than the basal Roper Group. The δ³⁴S values of iron sulphides in fine grained black dolostones (not associated with mineral deposits) from the McArthur Basin were assessed in the light of the values found for sulphides in modern organic‐rich sedimentary environments. The data so obtained suggest that the considerable concentration of iron sulphide in the mineral deposits formed, at least in part, from heated basinal waters and that disseminated iron sulphides remote from mineralization also formed from a similar source.  相似文献   

Geochemical Characters of Water Coproduced with Coalbed Gas and Shallow Groundwater in Liulin Coalfield of China     

YANG Mei  JU Yiwen  LIU Guijian  TONG Li  KANG Yu  HOU Quanlin 《《地质学报》英文版》2013,87(6):1690-1700

To reveal the geochemical characters of water coproduced with coalbed gas and shallow groundwater,water samples were collected from 12 wells of coalbed methane and 7 wells of shallow groundwater.The pH,CODMn,fCO2,total dissolved solids （TDS）,total hardness,and concentrations of metasilicic acid,sodium and kalium,calcium ion,magnesium ion,ammonium iron,bicarbonate ion,carbonate,chloride,sulfate ion,nitrate ion,fluoride,lithium,zinc,nickel,manganese,iron,boron,barium,etc.of the samples were measured.Research results showed the following：（1） Concentrations of TDS,chloride,fluoride,sodium and kalium,ammonium,iron,and barium in the water coproduced with coalbed gas exceeded the national standards of China; however,physical,chemical,and biological properties of shallow groundwater could meet the national standard.（2） The water produced from coalbed contained mainly Na-Cl·HCO3,with average TDS of 4588.5 ppm,whereas shallow groundwater contained a mixture of chemicals including Na.Mg.Ca-HCO3·SO4 and Na.Mg-HCO3·SO4,with average TDS of 663.8 ppm.（3） In general,it was observed that bicarbonate and sodium accumulated in a reducing environment and deeper system,while depletion of hydrogen ions and dissolution of sulfate,calcium,and magnesium occurred in a redox environment and shallow system.（4） Sodium and kalium,ammonium,chloride,and bicarbonate ions were the main ions found in the study area.  相似文献   

甘肃省张掖-永昌地区土壤重金属元素地球化学特征     

刘文辉 《物探与化探》2013,(5):883-888

通过对甘肃省张掖一永昌地区土壤重金属元素富集与分布规律的研究表明,研究区土壤以Cd、As、Cr、Ni污染为主,工业废水、厂矿企业、人类活动及大气降尘是研究区土壤的主要污染源。从土壤污染程度综合评价图来看,全区土壤一级质量区占总面积的1．87％,二级质量区占总面积的87．13％,三级质量区占9．92％,四级质量区占1．09％。从土壤污染现状来看,重金属土壤以一、二级为主,说明研究区土壤总体质量较好。从土壤Cd、As、Cr、Ni相态分析结果看,各元素多以残渣态为主,但cd的离子结合态和水溶态占总量的5％左右,是极其危险的,需要引起重视。  相似文献   

新型磁力打捞器的研制及其应用     

梁贵和  郭道强  姜焕忠 《探矿工程》2013,40(9):26-28,40

通过对钻探过程中孔底形成金属落物的原因及事故征兆分析,研制出了一种能高效打捞孔底金属落物的新型磁力打捞器,在现场应用中取得了良好的效果。介绍了该新型磁力打捞器的设计思路、结构原理、操作技术以现场应用效果等。  相似文献   

河南省石门沟钼矿床地质特征及成因探讨     

王长永  王瑞良  汤清龙 《上海国土资源》2013,(3)

石门沟钼矿辉钼矿（化）特征为燕山晚期由基性岩浆底侵作用而形成的二长花岗岩体和地表出露的的厚大石英脉体全岩含矿。分析了河南西峡县石门沟钼矿成因机理与成矿模式。认为石门沟辉钼矿化二长花岗岩是下地壳物质部分熔融作用形成的富含Mo元素的花岗质岩浆,由基性向酸性正向演化,后经岩浆结晶分异、同化混染作用,钼（钨）等金属矿物以熔离状态分布在岩浆矿房中;岩浆热液沿构造薄弱带上升到地壳浅部后,富水热流体分离,进入气成热液阶段,形成高中温纵横交错含钼脉体或含钼花岗岩体。石门沟钼矿成因类型为岩浆型、热液充填石英脉型辉钼矿床,与斑岩型有明显区别。  相似文献   

海南文昌沿岸海草床的现状及其退化因素分析          下载免费PDF全文

徐步欣  张剑  郎尚昆  陈石泉  吴钟解  王道儒 《应用海洋学学报》2022,41(4):614-624

通过对比2012、2018、2020年海南文昌沿岸海草床的调查数据,对文昌海草床的现状、退化状况以及退化因素进行分析。结果表明,2020年文昌海域海草有2科6属6种,分别为泰来草（Thalassia hemprichii）、圆叶丝粉草（Cymodocea rotunda）、单脉二药草（Halodule uninervis）、海菖蒲（Enhalus acoroides）、卵叶喜盐草（Halophila ovalis）及针叶草（Syringodium isoetifolium）。文昌海草床的分布呈明显退化的趋势,海草床面积由2012年的31.8 km2减少到2018年的24.2 km2,2020年进一步降低至18.8 km2。分析数据显示, Cu、Cd、Cr等重金属离子与调查区海草床的盖度显著负相关,表明在低营养负载时文昌周边虾塘养殖废水排放带来的重金属污染也会导致文昌海草床的退化。  相似文献   

厦门湾常见海洋经济生物重金属污染特征及风险评价          下载免费PDF全文

吴昊  张乐蒙  黄智伟  林君卓  刘四光 《应用海洋学学报》2022,41(3):395-406

了解厦门湾海域海洋经济生物重金属污染现状及食用风险,于2019年8月至2020年4月分4个季节,在厦门湾海域捕获了常见的13种海洋经济生物,以ICP MS为检测手段分析其肌肉组织中7种重金属（Cr、Ni、Cu、Zn、As、Cd和Pb）的含量,并采用不同评价模型对人类及中华白海豚的健康风险进行评价。结果表明,①鱼类和头足类海洋经济生物体内Zn、As和Cu的含量比较高,而Pb和Cd的含量比较低。②鱼类体内大多数重金属残留量,夏季显著高于其他季节,这可能是由于夏季饵料丰富,生物体代谢旺盛所导致。③单因子污染指数（single factor index, SFI）法和目标危害系数评价（target hazard quotient, THQ）法的评价结果显示,厦门湾常见海洋经济生物样品中As的残留量不仅超出了国家食品安全限量标准,还会对人类的健康造成潜在的风险。厦门湾海洋经济生物As的污染应引起人们的高度关注,后续研究应深入调查厦门湾生物体内As的主要存在形态,进一步提高健康风险评价的准确性,为当地监管部门的监管工作以及相关政策的制定提供数据支撑。因中华白海豚进食方式的不同,相关评价结果仅供参考。  相似文献   

Response Surface Modeling of Cu(II) Removal from Electroplating Waste by Adsorption: Application of Box–Behnken Experimental Design     

Nurdan Gamze Turan  Başak Mesci  Okan Ozgonenel 《洁净——土壤、空气、水》2013,41(3):304-312

The use of kaolinite‐based clay minerals as a low‐cost natural adsorbent for the removal of Cu(II) from electroplating waste leachate was studied. Batch experiments were conducted to determine the effects of varying adsorbent loading, initial pH, adsorbent dosage, and contact time. Box–Behnken design with three variables like initial pH, adsorbent dosage, and contact time at three different levels was studied to identify a significant correlation between the effects of these variables to the amount of Cu(II) adsorbed. The methodology identifies the principal experimental variables, which have the greatest effect on the adsorption process. After optimizing the input variables by using Simplex algorithm, the adsorption of Cu(II) was maximal (99.9% with a maximum (positive) standard deviation of 9.4) at pH 6.24, adsorbent dosage of 0.83 g L^?1, and contact time of 97 min, respectively. Furthermore, the experimental values are in good agreement with predicted values, the correlation coefficient and adjusted correlation coefficients were found to be 0.96 and 0.87, respectively.  相似文献