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贺兰山中段奥陶系米钵山组砂岩地球化学及构造背景分析 总被引:2,自引:0,他引:2
本文利用奥陶系米钵山组砂岩地球化学分析,结合区域地质研究,探讨贺兰山中、晚奥陶世的构造环境。贺兰山中段奥陶系米钵山组砂岩的地球化学研究表明,砂岩的SiO2平均含量为81.3%;Al2O3/SiO2值0.07~0.11,平均值为0.08;K2O/Na2O值变化较大,最大60.7,一般介于4.79~7.81;Fe2O3+MgO含量较低,介于2.1%~2.81%。砂岩微量元素Nb丰度及V/(V+Ni)与Ce/La、Sr/Ba值均较高,说明砂岩沉积于湿热、还原、低盐度环境,具有大陆型沉积特征。砂岩稀土元素富集,含量在116×10-6~195×10-6之间,平均值为158×10-6;δEu为0.52~0.58,具显著的负铕异常。这些数据指示了米钵山组具有重力流快速堆积的特征和大量陆源补给,浊流沉积作用是重力流携带陆源物质的主要途径。通过多种构造环境判别图解分析,显示物源区地质构造具有被动大陆边缘性质。 相似文献
224.
Geochemical index of trace metals in the surficial sediments from the western continental shelf of India, Arabian Sea 总被引:1,自引:0,他引:1
The present study focuses on the determination and abundance of trace metals (viz. Cu, Ni, Zn, Cr, Co, Cd, Mn and Fe) in the
surficial sediments of west coast of Arabian Sea along the Indian subcontinent. Sediment samples were collected from three
transects along the western continental shelf of Arabian Sea. The enrichment of Fe and Mn in coastal oxic-sediments indicates
the precipitation of these redox sensitive elements as Fe- and Mn-hydroxides and oxides, whereas the low Fe and Mn concentrations
in the oxygen deficient sediments of deeper stations reflects the dissolution of their hydroxides and oxides. Concentrations
of fairly redox insensitive trace metals like Cu, Ni, Zn, Cr and Cd (with the exceptions of Cr) showed higher values at nearshore
sediments, then it decreased towards seaward and again showed a slight increase at oxygen minimum stations in all the three
transects. This geochemical variability in their distributional characteristics is mainly associated with the extent to which
the precipitation or dissolution of Fe- and Mn-oxides/hydroxides occur since the scavenging or releasing effects of Fe- and
Mn-oxides/hydroxides act as significant ‘sinks’ or ‘sources’ of heavy metals. The change in wind pattern, coastal upwelling
and increased productivity are also the reported factors which influence the biogeochemical cycling of trace metals in the
surface sediments of west coast of India. Enrichment factor generally showed a high gradient accumulation from nearshore to
shelf. 相似文献
225.
Heavy Metal Contamination and Distribution in the Urban Environment of Guangzhou, SE China 总被引:6,自引:0,他引:6
Duzgoren-Aydin NS Wong CS Aydin A Song Z You M Li XD 《Environmental geochemistry and health》2006,28(4):375-391
Ever-increasing heavy metal accumulation in the urban environment of Guangzhou, the largest light industrial production base and one of the most rapidly developing cities in China, poses a serious threat to environment as well as to human health in the region. As a sink or source, urban deposits are good indicators of the level and extent of heavy metal accumulation in the surface environment. The aim of this preliminary study was to examine the distribution of heavy metal contamination in the urban environment of Guangzhou. It was based on a systematic sampling of road dusts and corresponding gully sediments along major roads running mainly through commercial and residential to industrial districts of the city. In addition to road dusts and gully sediments, ceiling dusts from the Pearl River Tunnel were also collected to characterize anthropogenic emissions dominated by traffic-related activities. In general, the level of Cd, Cu, Pb and Zn contaminations were more severe on the industrialized side of Guangzhou than on the western side where heavy traffic and industrial activities were limited. The primary determinants of the level of heavy metal contamination and the distribution of this contamination in the urban environment of Guangzhou were the site-specific conditions of its urban setting, particularly the types of industries, the nature of the traffic flow, sample residence times and variations in grain size of the particulate contaminants. This study highlights the complexity of the urban system and indicates that in just such a system individual urban components should be interlinked to assess the long-term environmental and health effects of heavy metal contamination. Among the heavy metals tested – Cd, Cu, Pb and Zn – the level of Zn contamination was the most severe and widespread, and thus requires immediate attention. 相似文献
226.
Ian B. Paton Christine S. Dayton David M. Jubenville Eugene R. Weiner Martha W. Hyder 《Journal of the American Water Resources Association》2004,40(2):359-369
ABSTRACT: Migration of plutonium, americium, and uranium (actinides) in the environment at the Rocky Flats Environmental Technology Site (RFETS) is the subject of ongoing studies to develop effective strategies for cleanup and regulatory closure of the Department of Energy facility. The Actinide Migration Evaluation pathway analysis quantified actinide transport processes to validate a qualitative conceptual model of environmental actinide transport. Major actinide transport mechanisms evaluated include surface water, ground water, airborne, and biological pathways. Relative quantities of actinide movement via different pathways were compared in terms of actinide loads delivered off the RFETS, using a combination of monitoring data, predictive transport models and results from historic RFETS studies. Results indicate air and surface water constitute the dominant transport mechanisms for plutonium and americium. In ground water, shallow alluvial flow is a limited pathway for plutonium and americium because of the low aqueous solubility of these actinides and their tendency to sorb to soil. However, localized flow in shallow alluvium is a more significant pathway for uranium movement, because of the relatively higher solubility of uranium (VI) species, though isotopic ratios indicate much of the uranium is from natural sources. Biological transport of actinides by mammals, birds, fish, and arthropods is small compared to the other pathways. 相似文献
227.
本文提出一种研究区域环境地球化学解决宏观环境问题的新思路,按照环境—地球化学—地质构造三对应的原则提出“八五”后期、“九五”和2000年后区域环境地球化学分阶段发展的设想。除了为国家提供保护治理环境的决策依据外,区域环境地球化学在理论上需要建立起地质地球化学—生态系统物质大循环模型,进行典型环境元素全球对比研究。 相似文献
228.
为摸清土壤氟异常对生态环境的影响,利用贵州省多目标区域地球化学调查(1:250 000)项目成果,对贵阳中心区土壤氟的地球化学特征进行了深入研究,并采用全氟指数法对土壤环境质量及其生态环境效应进行初步评价.结果表明:①贵阳中心区土壤氟含量较高,表层、深层土壤氟含量平均值分别为1 143、1 438 mg/kg,且空间分布变化较大;氟含量随土层深度的增加而升高. ②不同类型土壤中氟含量变化较大,其中紫色土中含量(1 306 mg/kg)最高,水稻土次之,石灰土、粗骨土、黄壤等差别较小,其含量范围在1 099~1 167 mg/kg之间. ③土壤氟含量与其母岩呈显著正相关性,且土壤中氟含量较母岩更高,表明风化成土过程中存在一定富集,土壤氟与成土母岩之间具有一定继承性. ④土壤氟环境质量评价结果表明,研究区土壤存在局部氟污染(异常),污染区、警戒区、安全区和清洁区所占比例分别为13.6%、62.2%、19.2%和5.0%. ⑤生态环境效应初步调查结果显示,局部土壤受氟污染区的油菜和稻谷样品中氟含量范围分别为1.86~2.68和10.40~13.50 mg/kg,同时地下水也受到一定程度的氟污染.因此,贵阳中心区土壤氟含量较高,局部土壤已受到氟污染,可能会对农产品质量、饮水安全及人体健康产生一定影响,建议政府部门及科研工作者予以高度重视. 相似文献
229.
通过对目前全世界元古宙———寒武纪地层中的浮游植物 (疑源类 )的统计 ,发现在新元古代晚期和早、中寒武世相对较短的时间间隔内发生了一系列的微体植物 (疑源类 )辐射和绝灭事件。而这些辐射和绝灭事件又与早期后生生物的辐射、绝灭都有密切的镜像关系。通过对古海洋的δ13 C、87Sr/ 86Sr研究 ,发现元古宙—寒武纪浮游植物 (疑源类 )的辐射演化、绝灭作用与古海洋环境变化有着密切的关系 ,即生物辐射时期 ,δ13 C、 87Sr/ 86Sr呈现高异常 ;生物绝灭时期 ,δ13 C、87Sr/ 86Sr呈现低异常 ;冰期δ13 C呈现明显的负异常。 相似文献
230.