南京北郊冬季大气SO_2、NO_2和O_3的变化特征   总被引：4，自引：0，他引：4       下载免费PDF全文

张敏  朱彬  王东东  周毓荃   《大气科学学报》2009,32(5):695-702

利用差分吸收光谱仪DOAS(differential optical absorption spectroscopy),对2007年11月—2008年1月南京北郊大气SO2、NO2和O3进行了观测。结合Parsivel降水粒子谱仪和自动气象站的资料,对冬季大气污染气体的浓度变化规律及降水和风速风向对其的影响进行了分析。结果表明,南京北郊大气SO2浓度较高,呈明显双峰特征,分别在12时(北京时,下同)和00时达最大,受附近排放源的影响最大,东风及南风时比静风时SO2浓度更高。降水对SO2湿清除效果明显,清除系数平均为0.168 h-1。NO2气体呈明显单峰特征,在18时达最高值。南京北郊是NO2源区之一,主要受附近高速公路汽车尾气排放源的影响。静风时NO2浓度最高。O3浓度受NO2的影响较明显。O3日变化呈单峰特征,在15时达最大值,静风时O3浓度最低。降水对O3的间接影响较明显,在降水时,白天由于太阳辐射较弱,O3浓度降低;夜晚NO浓度较低,使得O3浓度升高。  相似文献   

Carbon and Noble Gas Isotopes in the Tengchong Volcanic Geothermal Area, Yunnan, Southwestern China   总被引：1，自引：0，他引：1  

Shun''ichi NAKAI  Hiroshi WAKITA 《《地质学报》英文版》2004,78(5):1122-1135

Carbon and noble gas isotope analyses are reported for bubbling gas samples from the Tengchong volcanic geothermal area near the Indo-Eurasian suture zone. All samples contain a resolvable component of mantle-derived 3He. Occurrence of mantle-derived 3He coincides with surface volcanism. However, 3He occurs over a larger geographic areathan do surface volcanics. δ13C values for CO2 and CH4 vary from -33.4‰ to 1.6 ‰ and from -52.8‰ to -2.8‰, respectively. He and C isotope systematics indicate that CO2 and CH4 in the CO2-rich gases originated predominantly from magmatic component mixed with crustal CO2 produced from carbonate. However, breakdown of organic matter and near-surface processes accounts for the CH4 and CO2 in N2-rich gases. 3He/4He ratio distribution pattern suggests that mantle-derived He and heat sources of high-temperature system in central Tengchong originate from a hidden magma reservoir at subsurface. CO2-rich gases with the highest 3He/4He ratio (5.2 Ra) may be representative of the  相似文献   

山东东营凹陷古近系碎屑岩储层特征及控制因素   总被引：25，自引：10，他引：15       下载免费PDF全文

张琴  朱筱敏  钟大康  宋刚 《古地理学报》2004,6(4):493-502

通过对大量储层物性数据的分析和整理,结合薄片观察和扫描电镜分析结果,研究了不同构造背景、不同沉积类型及不同埋深的储层物性特征及其控制因素。东营凹陷近系碎屑岩储层类型多样,大多形成在冲积扇-河流、扇三角洲、近岸水下扇、深水浊积扇、三角洲前缘滑塌浊积扇以及滨浅湖滩坝等多种沉积环境中。碎屑岩储层类型主要包括砾岩、含砾砂岩、中粗砂岩、细砂岩及粉砂岩。其中中砂岩和细砂岩是最好的储层。但是不同地区、不同类型储层物性存在较大的差异。物性最好的储层为河道、（扇）三角洲前缘水下分流河道及河口坝砂体。在相同深度条件下,中央隆起带的物性最好,北部和南部次之。另外,本区随埋藏深度增加,碎屑岩储层物性逐渐变差（剔除次生孔隙的影响）。根据碎屑岩储层物性差异性分析和储层成岩演化研究结果,其储层物性主要受压实作用、碳酸盐溶蚀与胶结作用及沉积条件四大因素控制,其中压实作用、溶蚀作用及胶结作用是主要控制因素,而沉积条件对物性的影响主要表现在控制原生孔隙的发育程度,并进一步控制溶蚀、胶结等成岩作用。  相似文献   

走滑断裂、"挤压性盆-山构造"与油气资源关系的探讨   总被引：25，自引：0，他引：25  

许志琴曾令森  杨经绥李海兵 姜枚金之钧  郑和荣郭齐军 《地球科学》2004,29(6):631-643

了解含油气盆地的形成及其演化的影响因素对于含油气盆地的勘探和开发是至关重要的．以美国西部的圣安德烈斯断裂带及伴生的南加州油气盆地作为参考,对中国青藏高原北部与阿尔金走滑断裂系相关的盆-山构造进行了剖析．探讨阿尔金走滑断裂系在其演化过程中,怎样控制区域应力场、变形构造及盆地的形成,进而制约油气的迁移和圈闭．分析结果表明与圣安德烈斯断裂带在美国南加州的盆-山构造体系所起的作用相比较,阿尔金走滑断裂系在青藏高原北部的盆-山构造体系的形成和演化中起相似的作用．青藏高原相对于塔里木盆地的斜向运动导致在阿尔金走滑断裂的东南形成走滑-挤压构造域．形成一系列的走滑和推覆构造,在地形上表现为包括柴达木盆地在内的有序的盆-山相间的构造体系,与南加州富含油气的盆地相似,阿尔金走滑断裂及相配套的走滑-逆冲推覆构造促使在这些盆地中形成富集油气的构造。  相似文献   

GIS Platform-based Multi-source Information System for Evaluation of Cu, W and Au Resources in the Northern Qilian, China     

LI Chunxi  FU Shuixing  ZHANG Shoulin Beijing Institute of Geology for Mineral Resources  Beijing 《《地质学报》英文版》2004,78(2):558-561

Based on the information of geology, geochemistry, geophysics and remote sensing, the GIS of multi-source information is used to evaluate Cu, W and Au mineral resources in Northern Qilian, China. As the GIS evaluation system works out in the thinking of geological prospecting, its functions include file management, graph edition, database maintenance, information inquiry and comprehensive spatial analysis as well as prospecting target prognosis. Accordingly, the GIS evaluation system can be used directly and conveniently for inquiry and analysis of visual graphs or images.  相似文献   

Massive Sulphide Deposits Related to the Volcano-Passive Continental Margin in the Altay Region   总被引：3，自引：0，他引：3  

WANG Jingbin  DENG Jiniu  ZHANG Jinhong  QIN KezhangBeijing Institute of Geology for Mineral Resources  State Bureauof Nonferrous Metal Industry  Andingmenwai  Beijing Zhu Xiling 《《地质学报》英文版》1999,73(3):253-263

The Devonian volcano-passive continental margin in southern Altay is a significant volcanogenic massive sulphide metallogenic belt. Acidic volcanism has been dominant on the inner side of the volcano-passive continental margin, i.e., near the old land, resulting in a Pb-Zn metallogenic sub-belt, in which the ore deposits are hosted by sedimentary rocks in volcanic series, as represented by the large Koktal Pb-Zn deposits. In the central part of the margin far away from the old land, bimodal volcanic formations are well developed, forming volcanics-hosted Cu-Zn metallogenic sub-belts, e.g., the large-scale Ashele Cu-Zn deposit. The Qiaoxiahala sub-belt on the outer side of the margin near the ocean ridge is located at the spreading central trough, where ophiolite suites are developed. This type of deposits is rich in gold and copper, similar to the Cyprus-type Fe-Cu-Au metallogenic sub-belt in metallogenic environment (represented by the Qiaoxiahala medium-scale Fe-Cu-Au deposit). From the old land to th  相似文献   

实散组合桩承载原理及应用   总被引：4，自引：1，他引：3  

王长科  戴志祥  柯文开 《工程地质学报》1999,7(4):327-331

本文提出了实散组合桩概念,即一根桩由上下两段组成,上段是实体桩,下段是散体桩。这样就克服了散体桩通常桩头承载能力低的缺陷。本文对实散组合桩的受力概念进行了分析研究,给出了其承载力、沉降、临界桩长等计算方法和公式。最后介绍了首次工程实例。  相似文献   

日本1999年到2002年测地学与地球物理学活动报告     

郝清源  孙振凯 《国际地震动态》2005,(3):33-36

日本是测地学与地球物理学国际联合会(IUG)最开始的9个成员国之一。IUGG成立于919年,现在有66个成员国。日本测地学与地球物理学国家委员会是作为日本科学委员会180个联络委员会的一个成员而成立的,其作用是为了商讨地学的重要性,为了执行在测地学和地球物理学方面的科学研究的国际合作和协调方面的决定。  相似文献   

Petrogenesis of Volcanic Rocks in the Khabr-Marvast Tectonized Ophiolite:Evidence for Subduction Processes in the South-Western Margin of Central Iranian Microcontinent   总被引：1，自引：1，他引：0  

Azam SOLTANMOHAMMADI  Mohammad RAHGOSHAY  Morteza KHALATBARI-JAFARI 《《地质学报》英文版》2009,83(5):884-892

Abstract: The Late Cretaceous Khabr–Marvast tectonized ophiolite is located in the middle part of the Nain–Baft ophiolite belt, at the south-western edge of the central Iranian microcontinent. Although all the volcanic rocks in the study area indicate subduction-related magmatism (e.g. high LILE (large ion lithophile elements) / HFSE (high field strenght elements) ratios and negative anomalies in Nb and Ta), geological and geochemical data clearly distinguish two distinct groups of volcanic rocks in the tectonized association: (1) group 1 is comprised of hyaloclastic breccias, basaltic pillow lavas, and andesite sheet flows. These rocks represent the Nain–Baft oceanic crust; and (2) group 2 is alkaline lavas from the top section of the ophiolite suite. These lavas show shoshonite affinity, but do not support the propensity of ophiolite.  相似文献   

Lithostratigraphy, Sedimentology, and Provenance of the Balfour Formation (Beaufort Group) in the Fort Beaufort–Alice Area, Eastern Cape Province, South Africa   总被引：1，自引：1，他引：0  

David KATEMAUNZANGA  and Cornelis Janse GUNTER 《《地质学报》英文版》2009,83(5):902-916

Abstract: The Balfour Formation has a pronounced lithological variation that is characterized by alternating sandstone- and mudstone-dominated members. The sandstone-dominated Oudeberg and Barberskrans Members are composed of lithofacies that range from intraformational conglomerates to fine-grained sediments, whereas the mudstone-dominated members (Daggaboersnek, Elandsberg, and Palingkloof) are dominated by the facies Fm and Fl. Petrography, geochemistry, and a paleocurrent analysis indicated that the source rock of the Balfour Formation was to south east and the rocks had a transitional/dissected magmatic arc signature. The sandstones-rich members were deposited by seasonal and ephemeral high-energy, low-sinuous streams, and the fine-grained-rich members were formed by ephemeral meandering streams. The paleoclimates have been equated to present temperate climates; they were semiarid becoming arid towards the top of the Balfour Formation. This has been determined by reconstructing the paleolatitude of the Karoo Basin, geochemistry, paleontology, sedimentary structures, and other rock properties, like color.  相似文献