乌南油田滨浅湖砂体储层构型及其油气意义          下载免费PDF全文

石金华  韩登林  于炳松  李仕远  王宝  陈景华 《地质科学》2016,(4):1310-1323

基于Miall储层构型研究思想,结合岩心、测井、测试等资料,对乌南油田砂坝砂体储层构型界面特征进行了研究,确定了储层构型界面识别标志;在此基础上,将砂坝内部构型分为坝主体和坝侧缘,同时通过动、静态结合,明确砂坝外部构型存在孤立、视连通、左侧向叠置和右侧向叠置4种模式;纵向上发育湖退（进积）和湖进（退积）两种砂体发育模式。坝主体是主力储层,具有良好油气显示;坝主体分布面积大、出现频率高为油气有利区域。  相似文献   

页岩孔隙系统研究实验方法     

张天付  鲍征宇  李东  唐俊红  周闻达 《地质科技情报》2016,(4):192-198

基于页岩孔隙系统的特殊性,讨论了FESEM-QEMSCAN、FIB-FESEM、NANO-CT、氮气吸附法、小角中子散射等几种页岩孔隙系统研究方法的特点和适用范围。指出场发射扫描电镜以及与之结合的能谱和矿物定量评价系统(FESEM-QEMSCAN)是研究页岩纳米级孔隙类型、大小、形态以及矿物分布的基础手段;聚焦离子束扫描电镜、微纳米CT可刻画页岩孔隙系统在三维空间的展布特征,利用获得的三维数据体进行数值模拟,可进一步计算孔隙度、渗透率等物性参数;氮气吸附法可对小于100nm的极微孔隙的孔径、形态进行求算;小角中子散射则可利用孔隙中存在的气体分子,获得孔隙系统连通性等重要参数。最后从页岩岩石组构的角度,探讨了页岩孔隙控制因素,指出有机质含量与成熟度,黏土矿物类型、含量,碎屑颗粒的含量以及成岩强度是影响页岩孔隙系统的主要因素。  相似文献   

Comparative Analysis of International Energy Consumption Characteristics and China's Countermeasures     

Yang Zhanhong  Lü  Lianhong  Cao Bao  Wang Xiao  Luo Hong 《地球科学进展》2016,31(1):94-102

With the rise of low carbon economy and the deterioration of the international energy situation, most countries in the world pay more attention to energy issues. In this paper, based on a comparison with several countries of large energy consumption, we used long sequence statistics to analyze the energy consumption characteristics from the world and the history, including energy consumption, energy consumption structure and energy efficiency, and then summed up the characteristics of energy consumption in developed countries, analyzed China's energy consumption process and the current stage, and found out the main problems of energy consumption in China. At last, countermeasures for the healthy development of China's energy were proposed, including actively promoting scientific and technological progress, upgrading energy structure, developing low carbon economy, rationalizing energy prices, improving the proportion of clean energy consumption and emphasizing synergistic effect on environment protection.  相似文献   

小黄鱼(Pseudosciaena polyactis)形态性状与体质量的相关性及通径分析   总被引：4，自引：0，他引：4  

刘峰  陈琳  楼宝  詹炜  陈睿毅  徐冬冬  王立改  徐麒翔  马涛  毛国民 《海洋与湖沼》2016,47(3):655-662

为了研究野生小黄鱼(Pseudosciaena polyactis)繁殖后代的形态性状对体质量的影响作用,以随机采集的729尾4.5月龄小黄鱼为研究对象,对每尾个体的体质量(g)和8个形态性状(cm):全长(X1)、体长(X2)、头长(X3)、躯干长(X4)、尾部长(X5)、尾柄长(X6)、尾柄高(X7)和体高(X8)进行准确测定,运用相关分析、多元回归分析和通径分析方法,分别计算性状间的相关系数、构建形态性状与体质量的多元回归方程,获得了通径系数和决定系数,进行了养殖小黄鱼的形态性状对体质量的影响研究。结果显示,8个形态性状与体质量的相关系数均达到极显著水平(P0.01);通径分析中,4个形态性状对体质量的通径系数达到极显著水平(P0.01),它们是影响体质量的重要指标,其中体长(通径系数:0.589)对体质量的直接影响最大。应用逐步多元回归分析建立了以体质量为因变量(Y),体长(X2)、躯干长(X4)、尾柄高(X7)和体高(X8)为自变量的回归方程:Y=–32.377+3.064X2–1.511X4+14.285X7+4.438X8。模型等式中形态性状与体质量的相关指数R2=0.927,说明所选性状是影响体质量的主要形态性状。以上分析结果为小黄鱼的选育测量指标的确定提供了理论依据。  相似文献   

近60年来长江河口河势变化及其对水动力和盐水入侵的影响I.河势变化   总被引：4，自引：4，他引：0  

朱建荣  鲍道阳 《海洋学报》2016,38(12):11-22

河势是影响河口水动力和盐水入侵基本因子。本文利用20世纪50和70年代长江河口海图,数值化岸线和水深,结合2012年长江河口实测水深资料,分析长江河口自50年代以来的河势变化。长江河口为分汊河口,50年代仅为二级分汊,至70年代才形成三级分汊,四口入海的河势格局。70年代相比于50年代,北支淤浅严重,其上、中、下段容积变化分别为-64.13×106、-306.60×106和-639.27×106 m3,对应的变化率分别为-16.30%、-22.74%和-25.69%,均显著减小;南支的上、中、下段容积变化分别为-28.61×106、-35.69×106和126.43×106 m3,相应的变化率分别为-1.30%、-2.12%和4.36%;北港由于崇明浅滩和横沙浅滩的淤浅,下段容积明显减小,其上段和下段容积变化分别为109.21×106和-797.14×106 m3,对应的变化率分别为5.01%和-15.25%;南港上段由于河道淤浅容积减小,下段北由于铜沙浅滩被冲开形成北槽,导致水深变深、容积增加,其上段、下段北和下段南容积变化分别为-238.95×106、203.58×106和153.34×106 m3,对应的变化率分别为-8.96%、6.85%和3.26%。2012年相比于70年代,北支由于大量淤浅和围垦容积大幅减小,其上、中、下段容积变化分别为-199.06×106、-504.61×106和-654.12×106 m3,对应的变化率分别为-60.45%、-48.44%和-35.38%;南支的上、中、下段容积变化分别为92.34×106、193.01×106和-163.62×106 m3,相应的变化率分别为4.24%、11.73%和-5.40%;北港上段青草沙水库的围垦和下段横沙东滩的围垦造成面积和容积减小,其上段和下段容积变化分别为-154.64×106和-511.79×106 m3,对应的变化率分别为-6.75%和-11.55%;南港由于上段河道刷深而下段九段沙以及南汇边滩淤浅、围垦,导致其容积上段增加,下段减小,上段、下段北和下段南容积变化分别为136.39×106、-658.28×106和-1266.11×106 m3,对应的变化率分别为5.62%、-20.73%和-26.06%。  相似文献   

Anthropogenic,detritic and atmospheric soil-derived sources of lead in an alpine poor fen in northeast China     

Kun-shan Bao  Ji Shen  Guo-ping Wang  Shurkhuu Tserenpil 《山地科学学报》2016,13(2):255-264

Ombrotrophic bogs are faithful archive of atmospheric metal deposition,but the potential for fens to reconstruct environmental change is often underestimated.In this study,some new data on the Pb depositional history in northeast China were provided using two 210Pb-dated peat sequences from a poor fen in the Fenghuang Mountain of Heilongjiang province.Anthropogenic,detritic and atmospheric soil sources were discriminated using a two-step sequential digestion(weak acid leaching to liberate mobile Pb which is often regarded as anthropogenic Pb,especially for recent samples)and a ratio of unsupported 210 Pb and supported 210 Pb with the logic of that the 214 Pb mainly represents the residual detritus(constant throughout the core)and the unsupported 210 Pb arises from atmospheric fallout.A higher 210Pb/214 Pb suggests more contributions from atmospheric deposition to the Pb content in the peat,and a ratio of 10 was defined to indicate the boundary between detritic input and atmospheric deposition.The detritic Pbwas estimated to be 10~(-1)3 mg·kg~(-1),the anthropogenic Pb ranged from 10-80 mg·kg~(-1),and the atmospheric soil-derived Pb ranged from 5 mg·kg~(-1) to 30mg·kg~(-1).The history of anthropogenic Pb pollution over the last 150 years was reconstructed,and the calculated Pb deposition rate(AR Pb) ranged from 5to 56 mg·m-2·yr~(-1).Using Ti as a reliable reference,the enrichment factor of Pb(EF Pb) relative to the upper continental crust was calculated.Both AR Pb and EF Pb increased with time,especially after the foundation of the People's Republic of China.This is consistent with increasing industrialization and coal burning in the last 60 years in northeast China.The present record of anthropogenic Pb deposition was consistent with the previous reports and an increasing trend of environmental pollution due to anthropogenic activities,in contrasts to Europe and North America which have experienced a major environmental cleanup.For the first time,this work estimates atmospheric Pb deposition via a minerotrophic peat core in China.This will enhance the use of peat archives for studies of environmental change.  相似文献   

P气田基于地质模型的储量不确定性分析          下载免费PDF全文

高玉飞  胡光义  王晖  孙立春 《山东国土资源》2016,32(10)

地质建模的最终目的是建立反映地质认识的地质模型,并对储层的不确定性以及由此带来的储量不确定性进行定量表征。南海P气田正处于开发的前期研究阶段,井点资料少,储层的纵横向变化快,储量不确定性强。该文以地质模型为载体,探讨了该气田地质储量不确定性分析的方法,总结了相似气田地质储量不确定性分析的一般方法:通过对变量的敏感性分析,确定影响该气田地质储量的主要变量,以此为基础通过拉丁超立方概率分析法进行储量评价及地质模型的优选,最终确定构造和气水界面的变化是影响该气田储量的主要因素,P50是该气田可动用储量。该方法为前期研究阶段的储量动用提供了新的思路。  相似文献   

Association of myostatin variants with growth traits of Zhikong scallop (Chlamys farreri)     

Qiang Fu  Huihui Guo  Liying Feng  Xue Li  Lingling Zhang  Shi Wang  Xiaoli Hu  Zhenmin Bao 《中国海洋大学学报(英文版)》2016,15(1):145-151

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The Impact of Large-Scale Reclamation on Hydro-Dynamic Environment——A Case Study of Xinghua Bay     

YU Jing  BAO Xianwen  DING Yang  ZHANG Wei  ZHOU Lingling 《中国海洋大学学报(英文版)》2016,15(4):583-592

A hydro-dynamic model is established on basis of MIKE21 FM to simulate the hydro-dynamic characteristics of Xinghua Bay and investigate the influence of reclamation project on the tidal elevation and tidal currents. Tidal elevation data was obtained at the six tide gauge stations around the Xinghua Bay, and another six current stations were established to observe the tidal current velocity and direction. Validation shows that the model-simulated tidal elevation and tidal currents agree well with observations made at different stations. Predictions are made according to the reclamation project proposed in the regional marine planning of Hanjiang Industrial Park around the port in Putian City. The variations of hydro-dynamic factors, such as tide, current velocity and direction and tidal influx are obtained, and the adverse effect of reclamation on marine environment is discussed. It is shown that the tidal level inside the Xinghua Bay during high tide decreases after the reclamation project is completed. The tidal currents during flooding tide generally decrease in the southeast of the reclamation region, with the maximum decreasing amplitude reaching 0.44 m s^-1. On the other hand, the tidal currents during flooding tide increase around the southeast and southwest corners of the reclamation region. The tidal currents during ebb tide increase around the southeast and southwest corners of the reclamation region, with the maximum increasing amplitude attaining 0.18 m s^-1. The results in this paper can give some guidance for the marine environment management and the effective utilization of land in Putian.  相似文献   

Feedstocks study on CO<Subscript>2</Subscript> mineralization technology     

Heping Xie  Liang Tang  Yufei Wang  Tao Liu  Zhengmeng Hou  Jinlong Wang  Tao Wang  Wen Jiang  Patrick Were 《Environmental Earth Sciences》2016,75(7):615

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