酒西盆地侏罗-白垩系储油层特征及其影响因素分析     

顿铁军 《地球科学与环境学报》1988,(1)

本文以酒西盆地侏罗—白垩系储油层为例,对低渗透砂岩及孔隙—裂隙双重介质储集层的孔隙结构进行了较详尽的研究,并对其某些特征参数进行了计算,进而试图从其宏观和微观规律入手查明该储层的储集特征、分布规律及其影响因素,以达到指导油田今后勘探和开发的目的。  相似文献   

Smart anticorrosion coating based on stimuli-responsive micro/nanocontainer: a review     

Cai  Haoyuan  Wang  Peng  Zhang  Dun 《中国海洋湖沼学报》2020,38(4):1045-1063

Smart coating for corrosion protection of metal materials(steel,magnesium,aluminum and their alloys) has drawn great attention because of their capacity to prevent crack propagation in the protective coating by releasing functional molecules(healing agents or corrosion inhibitors) on demand from delivery vehicle,that is,micro/nanocontainer made up of a shell and core material or a coating layer,in a controllable manner.Herein,we summarize the recent achievements during the last 10 years in the field of the micro/nanocontainer with different types of stimuli-responsive properties,i.e.,pH,electrochemical potential,redox,aggressive corrosive ions,heat,light,magnetic field,and mechanical impact,for smart anticorrosion coating.The state-of-the-art design and fabrication of micro/nanocontainer are emphasized with detailed examples.  相似文献   

Bifunctional nanozyme activities of layered double hydroxide derived Co-Al-Ce mixed metal oxides for antibacterial application     

Chen  Chao  Wang  Yi  Zhang  Dun 《中国海洋湖沼学报》2020,38(4):1233-1245

Journal of Oceanology and Limnology - Marine biofouling is an expensive problem that needs evolved chemical or physical antifouling strategies. However, most of the current antifouling materials...  相似文献   

The Shanggong gold deposit, Eastern Qinling Orogen, China: Isotope geochemistry and implications for ore genesis   总被引：13，自引：0，他引：13  

Yan-Jing Chen  Franco Pirajno  Jin-Ping Qi 《Journal of Asian Earth Sciences》2008,33(3-4):252-266

The Shanggong Au deposit in the Xiong’er Terrane, East Qinling, China, has resources of about 30 ton Au, making it one of the largest orogenic-mesothermal Au deposits hosted in volcanic rocks of the Mesoproterozoic Xiong’er Group. Three stages of hydrothermal activity are recognized (early, middle and late), of which two (early and middle) were ore producing and characterized by quartz–pyrite and polymetallic sulfides, respectively. The third and late stage is represented by a carbonate–quartz assemblage. Hydrogen, oxygen and carbon isotope systematics of the Shanggong deposit from a previous work suggest that the early stage fluids were derived from magmatic and/or metamorphic devolatilization of sedimentary rocks at depth. This is supported by new C, S and published Sr and Pb isotopic data, presented in this paper. These new data, δ¹³C values ranging from 1.5 ‰ for early stage ankerite to −2.2 ‰ for late stage ankerite, negative δ³⁴S values for sulfides from the middle stage (–19.2 to –6.3 ‰), suggest a contribution from organic matter and that the ore fluid evolved from deeply sourced to shallowly sourced, with those of the middle stage representing a mixture of these two fluid systems. The comparison of the hydrogen–oxygen–carbon–sulfur–lead–strontium isotope systematics between the Shanggong deposit and the main lithologies in the Xiong’er Terrane, shows that neither these nor the underlying lower crust and mantle, or combinations thereof, could be considered as the source of ore fluids for the Shanggong Au deposit. A likely source was a carbonaceous carbonate, sandstone, shale, chert sequence in the underthrusted Guandaokou and Luanchuan Groups, exposed south of the Xiong’er Terrane.Ar–Ar and Rb–Sr isochron ages for mineral phases of the early, middle and late stages, together with geological field data, constrain the timing of the hydrothermal activity and Au metallogenesis at 242 ± 10, 167 ± 7 and 112 ± 7 Ma, respectively. This metallogenesis and associated granitic magmatism, can be related to the continental collision between the Yangtze and North China Cratons that resulted in the formation of the Qinling Orogen, led to the different hydrothermal systems that were responsible for the three stages that formed the Shanggong Au deposit, over a period of about 130 Myrs.  相似文献   

区域地震地质灾害损失分析系统的开发     

李恒  魏贵春  特木其勒  王墩 《大地测量与地球动力学》2007,27(Z1):64-66

介绍基于地理信息系统（GIS）的区域地震地质灾害损失分析系统的开发。顾及不同用户的需求，资料搜集精度可调以适应不同经济水平，设计一组可以模拟减灾效果的功能模块，发展了基于反应谱的建筑物破坏模型，并考虑了场地条件对地震动的影响。  相似文献   

电离层闪烁对全球导航卫星系统（GNSS）的定位影响分析   总被引：1，自引：1，他引：1  

刘钝  冯健  邓忠新  甄卫民 《全球定位系统》2009,34(6):1-8

电离层闪烁是影响卫星导航系统定位性能的重要因素之一，中国南方区域是全球电离层闪烁多发区之一，开展电离层闪烁对卫星导航系统性能的影响研究具有重要意义。利用中国区域的电离层闪烁数据和GPS测量数据，对电离层闪烁情况下的用户定位性能进行了比较分析，发现电离层闪烁将引起用户定位误差的普遍增大，严重时可能出现定位异常，电离层闪烁对不同的定位应用方式具有不同程度的影响，电离层闪烁对卫星导航系统的多种影响是卫星导航系统的重要威胁之一。  相似文献   

基于图像法的多孔介质双分子反应溶质运移模拟     

刘咏  张琪  钱家忠  吴盾  张文永 《地学前缘》2022,29(3):248-255

采用图像分析法确定溶质浓度,以硫酸铜和EDTA二钠作为双分子反应物,在多孔介质模型中开展了不同粒径(1.52.0,2.53.0,3.54.0 mm)和流量(1.0,1.5,2.0 mL/s)下反应性溶质运移实验,探讨了应用不完全混合的对流弥散模型(IM-ADRE)对双分子反应溶质运移的模拟和预测,并进行了参数敏感性分析。结果表明:图像分析法可准确获取多孔介质中显色反应性溶质的浓度,灰度值与浓度的决定系数R²大于0.96;用IM-ADRE模型能够准确预测双分子反应性溶质硫酸铜和EDTA二钠在3种不同多孔介质中的运移过程,误差低于3.71%;实验条件的改变对IM-ADRE模型参数D、m和β₀的影响显著,说明模型参数依赖于环境条件,其变化规律需要根据实际环境条件进一步率定,便于IM-ADRE模型的进一步推广应用。  相似文献   

一种基于GIS的气象要素空间插值方法     

除多  珠海英  任秀珍  巴顿 《四川气象》2010,(1):41-44

根据气候学方程建立的多元回归方法,在地理信息系统空间分析功能的支持下,实现了西藏拉萨地区气温、降水等气象要素的空间网格化。得出,上述方法对拉萨地区等山地地区气象要素的空间网格化方面是有效的手段,该方法对气温的空间插值精度优于降水。  相似文献   

中国区域电离层相关结构对卫星增强系统的影响     

刘钝  冯健  邓忠新  余侯方 《全球定位系统》2009,34(4):14-19

利用GPS测量数据对中国低纬区域的电离层相关结构特性进行了分析研究，并进一步和美国区域的数据处理结果进行了比较。结果表明：中国低纬地区存在的电离层异常是影响卫星增强系统中电离层延迟误差修正及完好性实现的重要因素，并且即使在低年，电离层异常的这种影响也存在。  相似文献   

九江-瑞昌地震序列的构造背景与发震构造探讨   总被引：7，自引：0，他引：7  

王墩  肖和平  姚运生  宋琛  李恒 《大地测量与地球动力学》2007,27(Z1):15-20

通过遥感、余震分布、现场考察等各种手段证实瑞昌北部存在一组至少切穿上地壳的北北西向断裂--武山隐伏断裂,并认为九江-瑞昌地震是北东向瑞昌-武宁断裂与武山隐伏断裂共同作用的结果.更具体地说,主震由瑞昌-武宁断裂控制,余震受武山隐伏断裂控制.  相似文献