Influence of Drilling Fluid Components on Shear Strength at Cement-aquifuge Interface in Coalbed Methane Wells     

GU Jun  WANG Shuai  MA Chao  GAN Pin  TANG Naiqian 《《地质学报》英文版》2017,91(4):1511-1512

<正>Objective The hydraulic fracturing is still an effective technology for the exploitation of coalbed methane(CBM).However,after the hydraulic fracturing operation,the high water cut or sudden water flooding of CBM well usually occurs due to upward migration of bottom water,which is called water channeling(water inrush).This problem has been severely limiting the hydraulic fracturing effect of CBM wells.Some studies show that the aquifuge and cement  相似文献   

塔里木盆地塔东2井奥陶系笔石化石层     

杜品德  詹士高  黄智斌  李猛  赵治信 《地层学杂志》2004,28(1):56-58

塔里木盆地东部塔东 2井岩心中新发现了一些奥陶系笔石化石 ,这些笔石标本呈炭质薄膜状 ,保存在该井4 5 5 0 .2 m至 4 5 5 5 .3m的灰黑色泥岩之中。经研究 ,笔石动物群的时代属于玉山晚期至达瑞威尔早期 ,含笔石化石层顶部层位可与塔里木盆地东北缘却尔却克山剖面中奥陶统却尔却克组底部 Pseudamplexograptus confertus笔石带相对比  相似文献   

CHARACTERISTICS OF MULTI-SCALE GRAVITY FIELD VARIATION AND SEISMOGENIC MECHANISM ANALYSIS IN THE SOUTHEASTERN TIBETAN PLATEAU          下载免费PDF全文

CHEN Zhao-hui  MENG Xiao-hong  ZHANG Shuang-xi  LIU Jin-zhao  WANG Tong-qing  ZHANG Pin  WEI Shao-gang 《地震地质》2019,41(3):690-703

As the most basic geophysical field, the earth gravity field has achieved wide attention, and its spatial anomaly characteristics and dynamic variation can provide important scientific basis for studying the internal structure and dynamics of the Earth. Based on the mobile gravity observation data of the southeastern Tibetan plateau from 2013 to 2016, the dynamic variation tendency and anomaly characteristics of the regional gravity field in different temporal resolutions are obtained before and after the Ludian and Jinggu earthquakes in the study area respectively. The method of wavelet multi-scale decomposition is used to analyze the relationships of gravity field variation with the earth movement, material density change, and strong earthquake preparation. The deep material variation, dynamic process and the mechanism of earthquake inoculation in the southeastern Tibetan plateau are further discussed. Results indicate that the gravity field variation in the source region before the Ludian and Jinggu earthquake respectively is characterized by obvious positive and negative anomalous transition zone and gradient zone that are consistent with the direction of fault tectonics, suggesting the strong crustal movement and mass migration during the earthquake incubation period. The result of wavelet multi-scale decomposition of the gravity field during the period from September 2013 to April 2014 shows that the gravity field variation at different depth and space scale in the crust and upper mantle of the southeastern Tibetan plateau is significantly correlated with seismic distribution and the location of active fault zone. This indicates that the earthquake inoculation in the study area is closely related to the fault movement and the distribution of material density in the crust and upper mantle, which may be affected by the complex deep dynamic process of the material migration in the crust and mantle. The characteristic that strong earthquakes always occur near positive and negative anomaly transition zones and gradient zones of gravity field change is preliminarily explained, based on the dynamic process of material migration in the crust and upper mantle of the southeastern Tibetan plateau. The research results of this paper have some reference value to the study on the earth movement and seismogenic mechanism.  相似文献   

Detection of thermal pollution from power plants on China’s eastern coast using remote sensing data     

Pin?Ma  Xiaoyan?DaiEmail author  Zhongyang?Guo  Chao?Wei  Weichun?Ma 《Stochastic Environmental Research and Risk Assessment (SERRA)》2017,31(8):1957-1975

The acceleration of the industrialization process in China has increased the demand for electricity and triggered a power-plant building boom, especially along China’s eastern coast, where the economy gets off early and enjoys a fast development. The thermal plumes, residual chlorine, nuclides and other pollutions produced by the thermal and nuclear power plants have exerted an impact on the coastal eco-environment. To monitor the thermal pollution from the power plants at Yueqing Bay on the eastern coast, in this research, the distribution of sea surface temperature (SST) surrounding the power plants is obtained by using the SST retrieval methods developed for Landsat Enhanced Thematic Mapper Plus (ETM+), HJ-1B infrared sensor (IRS) and Terra moderate resolution imaging spectroradiometer (MODIS) data. The comparison of the SST retrieval results before and after the operation of power plants indicates that the total area of sea waters that is impacted by the thermal discharge from the two power plants at Yueqing Bay is approximately 17.95 km², with the highest SST rise of 4.5 °C appearing over the waters around the outlet of the Huaneng Yuhuan power plant on the eastern shore, whereas the highest SST rise around the Zheneng Yueqing power plant on the western shore reaches 3.8 °C. The intensity and scope of influence of the thermal discharge mainly depend on the installed capacity of power plants, coastal terrain, and tide. Although the area where the SST rise is more than 3 °C is not large, thermal discharge still has an impact on bay ecosystems due to the relatively closed nature of the bay environment. Due to the influence of rising water temperatures on the reproduction and individual evolution of fish, shrimp, crabs, shellfish and other aquatic creatures, in the long term, the thermal pollution from coastal power plants will affect the volume of natural fishery and biological resources throughout the waters. The quantitative retrieval results also suggest that relative to MODIS data, Landsat ETM+ and HJ-1B IRS data with a high spatial resolution are more applicable to the estimation of small-scale SST, and IRS data with a high temporal resolution are more helpful in the study of spatio-temporal variability of thermal plumes from coastal power plants.  相似文献   

滇西南发现石英面状变形构造          下载免费PDF全文

刘海龄  Adrian Jones  施小斌  阎贫  丘学林  刘迎春  Roger Mason 《地质科学》2006,41(3):518-522

采自云南省西南部澜沧江中游临景大桥以东约2km、勐戛河下游北岸的岩石样品的薄片中发现了非常清晰的石英面状变形构造(PDFs)。根据伦敦大学矿物岩石与冰物理实验室费氏台(universalstage)测量分析结果、样品所在地地层时代特征和航卫遥感图像特征的综合分析,认为该PDFs属陨击成因,其陨击事件大约发生在白垩/第三纪边界(距今65Ma),所引起的冲击变质作用已接近最高级阶段的高压二氧化硅相,样品位置接近陨击坑的中心。  相似文献   

德国能源转型进程及对中国的启示     

李品  谢晓敏  黄震 《气候变化研究进展》2023,19(1):116-126

总结发达国家能源转型过程中的经验和教训,对中国推动能源转型和实现“双碳”目标具有重要意义。文中回顾了中国和德国电力结构的演变进程,阐述了中国和德国能源转型的机制,并以2022年3月19日为例,分析了德国电力系统灵活性调节的经验。研究表明,健全的法律体系为德国能源转型提供了重要保障,“煤炭委员会”和相关财政支持有效解决了煤电转型过程中的问题,电力市场化是发展可再生主体新型电力系统的重要前提,风力和光伏发电精准预测与管理是可再生能源消纳的关键,煤电和互联互通的欧洲电网是当前德国电力供给的重要保障,过于激进的退煤去核战略是造成2022年德国能源危机的重要原因。最后,从法律保障、市场改革和可再生能源预测与管理等方面提出了中国能源转型的政策建议。  相似文献   

南海北部潮汕坳陷海区海底地震仪调查实验   总被引：6，自引：2，他引：4  

罗文造  阎贫  温宁  王嘹亮 《热带海洋学报》2009,28(4):59-65

潮汕坳陷被认为是一个具有良好油气前景的中生代残留沉积坳陷，其中生代地层也被新近的钻井证实。为研究其盆地深部构造，“十五”863课题跨越该区进行了深地质调查。调查采用5台国产海底地震仪记录深部地震资料。处理结果显示本次调查清楚地记录到了来自地壳内部和Moho面的震相，这是国产海底地震仪在南海地区的首次成功实践。海底地震仪记录揭示沿测线的地壳在南海形成过程中减薄程度较低，中生代地层速度较高，代表致密的岩石，这些因素可能不利于油气的储集，需要在勘探中避开。  相似文献   

山东微山稀土矿床成矿预测分析          下载免费PDF全文

张旭  张照荷  何平 《山东国土资源》2019,35(10)

微山稀土矿是鲁西地区已查明的一处中型稀土矿床,研究表明,目前的开采深度还处于岩体顶部的脉状矿体,成矿流体温度剖面初步揭示了高温区域随深度增加有明显收窄的趋势,经勘查工程验证,稀土矿脉深部厚度增大,数量增多,总体矿化强度增强。该文总结了微山稀土矿成矿要素和找矿标志,在成矿要素划分的基础上,增加放射性异常特征,建立了10个要素组成的预测要素表。依据地质成果,叠加放射性异常,编制了预测模型图,圈定出3个最小预测成矿靶区,编号分别为1~#,2~#,3~#。其中,1~#成矿预测区内有石英脉出露,推测为地下岩浆热液填充裂隙形成石英脉,存在伴生矿脉的可能;2~#成矿预测区包含2个放射性异常,南东侧为(12)号含稀土石英重晶石矿脉,推断该预测区浅部可能存在NW向延伸的隐伏矿脉;3~#成矿预测区包含4个放射异常区,异常区周边发育(15)(16)号含稀土矿脉,是最为有利的稀土矿找矿地段。验证已发现多个新矿脉,厚度在2.35～8.90m,稀土氧化物品位(TRE_2O_3)2.35%～6.40%,显示成矿预测区具有较好的稀土矿找矿潜力。  相似文献   

研究海水温盐结构的反射地震方法   总被引：2，自引：1，他引：1  

郑红波  阎贫  王彦林  张辉  吕修亚  邢玉清 《热带海洋学报》2009,28(1)

在物理海洋学的研究中,利用CTD(Conductivity, Temperature and Depth sensors)测量方法研究海水温盐结构存在着获取数据时间长、数据横向精度低的缺点,而利用反射地震记录可以获得剖面上连续的水体温盐结构,弥补了传统方法的不足.反射地震方法研究海水温盐结构是个新的交叉学科方法,称为"地震海洋学".由于海水水体的物性变化比地层物性变化小得多,造成海水水体的反射地震资料信噪比很低,各类干扰强烈,因而海水水体的反射地震资料处理也和常规地震资料处理方法有所不同.它处理的重点是振幅补偿,叠前去噪以及叠后处理.笔者通过对"十五"973项目在南海东北部采集的一条高分辨率多道反射地震测线的海水水体部分的地震数据进行处理,压制了强线性干扰波,获得了水体反射图像.地震叠加速度分析获取的3个CDP (Common Depth Point)的垂向速度从1540 m·s-1单调减小到1478 m·s-1,与CTD测量得到的速度变化趋势一致.  相似文献   

Modelling the hydrologic effects of dynamic land‐use change using a distributed hydrologic model and a spatial land‐use allocation model     

Hone‐Jay Chu  Yu‐Pin Lin  Chun‐Wei Huang  Cheng‐Yu Hsu  Horng‐Yng Chen 《水文研究》2010,24(18):2538-2554

This study develops a novel approach for modelling and examining the impacts of time–space land‐use changes on hydrological components. The approach uses an empirical land‐use change allocation model (CLUE‐s) and a distributed hydrological model (DHSVM) to examine various land‐use change scenarios in the Wu‐Tu watershed in northern Taiwan. The study also uses a generalized likelihood uncertainty estimation approach to quantify the parameter uncertainty of the distributed hydrological model. The results indicate that various land‐use policies—such as no change, dynamic change and simultaneous change—have different levels of impact on simulating the spatial distributions of hydrological components in the watershed study. Peak flow rates under simultaneous and dynamic land‐use changes are 5·71% and 2·77%, respectively, greater than the rate under the no land‐use change scenario. Using dynamic land‐use changes to assess the effect of land‐use changes on hydrological components is more practical and feasible than using simultaneous land‐use change and no land‐use change scenarios. Furthermore, land‐use change is a spatial dynamic process that can lead to significant changes in the distributions of ground water and soil moisture. The spatial distributions of land‐use changes influence hydrological processes, such as the ground water level of whole areas, particularly in the downstream watershed. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献