辽宁弓长岭铁矿二矿区构造特征分析   总被引：1，自引：0，他引：1       下载免费PDF全文

牛树银  孙爱群  张建珍  王宝德  马宝军  李斌  王铮 《地质找矿论丛》2013,28(2):167-175

辽宁弓长岭铁矿不仅发现较早、规模较大、开采历史较长,而且向下延深较大且富铁矿增多。针对弓长岭二矿区的构造解剖研究表明,二矿区至少经历了4期构造变形:第一期为小型塑性流变褶皱,第二期为区域规模的倒转同斜褶皱,第三期属于横跨叠加褶皱,第四期为区域规模的隆升。伴随着四期褶皱作用的断裂构造,从早到晚,则表现为韧性剪切带-脆韧性剪切带-韧脆性剪切带-脆性破裂。构造变形对铁矿的形成有一定的控制作用。  相似文献   

含水量累积区与冰雹增长行为之数值模拟   总被引：2，自引：0，他引：2  

郑凯琳  陈宝君 《大气科学》2011,35(2):298-310

利用三维冰雹云模式联合三维粒子增长运行模式,对一例具有累积区的雹云进一步展开研究.结果表明:(1)累积区既是雹胚和冰雹的形成区,也是二者初期的快速增长区,但并非主要的增长区;(2)源于累积区的雹胚粒子,至少要达到毫米以上才有可能最终长成中等以上大小的冰雹,而且初始粒径越大最终产生的大冰雹的尺度越大、数目越多;(3)大冰...  相似文献   

塔里木盆地西南坳陷周缘的滑脱构造   总被引：2，自引：1，他引：1       下载免费PDF全文

王步清  谢会文  陈汉林  王清华  杨宝俊 《地质科学》2011,(3):733-742

西南坳陷主要发育两套滑脱层序,一套是中寒武统和田河组膏盐岩,另一套是古近系底部阿尔塔什组和齐姆根组的夹灰岩、白云岩的膏泥岩;前者厚度500 m左右,后者厚度在100 ～700 m左右.和田河组膏盐岩主要影响中生代及中新世末的构造变形,古近系底部的膏泥岩主要影响上新世末及第四纪的构造变形,构造变形样式均以顺层滑脱构造为主...  相似文献   

Modeling the effects of completion techniques and formation heterogeneity on CO₂ sequestration in shallow and deep saline aquifers   总被引：1，自引：1，他引：0  

Fang Yang  Baojun Bai  Shari Dunn-Norman 《Environmental Earth Sciences》2011,64(3):841-849

This work studied the effect of completion techniques and reservoir heterogeneity on CO₂ storage and injectivity in saline aquifers using a compositional reservoir simulator, CMG-GEM. Two reservoir models were built based on the published data to represent a deep saline aquifer and a shallow aquifer. The effect of various completion conditions on CO₂ storage was then discussed, including partial perforation of the reservoir net pay (partial completion), well geometry, orientation, location, and length. The heterogeneity effect was addressed by considering three parameters: mean permeability, the vertical to horizontal permeability ratio, and permeability variation. Sensitivity analysis was carried out using iSIGHT software (design of experiments) to determine the dominant factors affecting CO₂ storage capacity and injectivity. Simulation results show that the most favorable option is the perforation of all layers with horizontal wells 250–300 m long set in the upper layers. Mean permeability has the most effect on CO₂ storage capacity and injectivity; k _v/k _h affects CO₂ injectivity storage capacity more than permeability variation, V _k. More CO₂ can be stored in the heterogeneous reservoirs with low mean permeability; however, high injectivity can be achieved in the uniform reservoirs with high mean permeability.  相似文献   

Factors affecting CO2 storage capacity and efficiency with water withdrawal in shallow saline aquifers     

Fang Yang  Baojun Bai  Shari Dunn-Norman  Runar Nygaard  Andreas Eckert 《Environmental Earth Sciences》2014,71(1):267-275

Carbon sequestration in shallow aquifers can be facilitated by water withdrawal. The factors that optimize the injection/withdrawal balance to minimize potential environmental impacts have been studied, including reservoir size, well pattern, injection rate, reservoir heterogeneity, anisotropy ratio, and permeability sequence. The effects of these factors on CO₂ storage capacity and efficiency were studied using a compositional simulator Computer Modeling Group-General Equation of State Model, which modeled features including residual gas trapping, CO₂ solubility, and mineralization reactions. Two terms, storage efficiency and CO₂ relative breakthrough time, were introduced to better describe the problem. The simulation results show that simultaneous water withdrawal during CO₂ injection greatly improves CO₂ storage capacity and efficiency. A certain degree of heterogeneity or anisotropy benefits CO₂ storage. A high injection rate favors storage capacity, but reduces the storage efficiency and CO₂ breakthrough time, which in turn limits the total amount of CO₂ injected.  相似文献   

Observational Indicators of Formation Excitation of H2     

S. Tiné  D.A. Williams  D.C. Clary  A.J. Farebrother  A.J. Fisher  A.J.H.M. Meijer  J.M.C. Rawlings  C.J. Davis 《Astrophysics and Space Science》2003,288(3):377-389

Theoretical predictions by Farebrother et al. and Meijer et al. of rovibrational excitation probabilities in H₂ arising from formation by Eley-Rideal processes on a graphite surface are incorporated into a model of the chemistry and excitation of interstellar H₂. The model includes the usual radiative and collisional pumping of H₂ rotational and vibrational states, in addition to the formation processes. Predictions are made for HH₂ rovibrational emission line intensities for representative points in diffuse and in dark interstellar clouds. We find that – if all the interstellar HH₂ is formed by this Eley-Rideal process – then the consequences of formation pumping, as distinct from collisional and radiative pumping, should be clearly evident in both cases. In particular, we predict a clear spectral signature of this direct HH₂ formation process on graphite, distinct from radiative and collisional pumping; this signature should be evident in both diffuse and dark clouds; but the emissivity for dark clouds is predicted to be some 500 times greater than that in diffuse clouds in which the dense material may be embedded. An observational search for this signature in two dark cloud sources was made, but a preliminary analysis of the data did not yield a detection. The implications of and possible reasons for this preliminary conclusion are discussed. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

超级单体风暴中大冰雹增长机制的模拟研究   总被引：5，自引：3，他引：2  

陈宝君  郑凯琳  郭学良 《气候与环境研究》2012,17(6):767-778

为调查超级单体中大冰雹的运行增长机制,使用三维冰雹分档对流云模式结合三维粒子运行增长模式,对一例超级单体风暴进行了数值模拟.实测风暴的结构如中气旋、弱回波区、前悬回波等被很好地模拟再现,显示了模式对超级单体具有良好的模拟能力.雹胚在风暴发展阶段由过冷雨滴冻结产生,主要分布在主上升气流区上部,在主上升气流区西北侧中高层也有相当数量的雹胚粒子,冰雹主要分布在主上升气流区东侧.风暴发展阶段产生的雹胚有7％～8％增长到1 cm以上,1％左右增长到2 cm以上,这些大冰雹绝大多数起源于主上升气流区北侧的高层云区,气旋性进入主上升气流区按照简单的上—下形式增长,少数大冰雹起源于主上升气流区西北侧风暴后部中高层,气旋性地沿着主上升气流区的边缘按照下—上—下形式运动增长,表明了超级单体中大冰雹存在两条增长路径.  相似文献   

电渗前后淤泥质土的物理力学性质对比研究          下载免费PDF全文

田震  王宝军  卢毅  李飞  马楠诘 《高校地质学报》2018,24(3):460

为深入研究电渗排水对土体工程性质的影响,采用铁丝为电极,在模型箱内对南京市某河道淤泥质土进行电渗排水 模拟试验。电渗前后土的物理力学性质对比分析表明：电渗后土体的液、塑限与塑性指数均降低;电渗前后土体在相同含 水量和干密度情况下进行直接剪切试验,发现电渗后土体的凝聚力和内摩擦角均降低,即电渗后土体在特定情况下出现了 强度衰减的现象。论文基于土中阳离子流失机理对土体在特定情况下的强度衰减现象进行了微观解释。另外,利用提出的 新的电渗机理从微观角度解释了电渗过程中土体开裂现象,阳极因快速失水,最早出现裂隙,但裂隙延展范围较小;阴极 含水量始终高于阳极,且失水速度较慢,裂隙延展范围较大。值得一提的是,在以往的研究中并未关注到电渗加固过程中 土中阳离子流失对电渗后土体性质的影响。  相似文献   

珠江口盆地白云凹陷深层砂岩储层中碳酸盐胶结作用及成因探讨     

王代富  罗静兰  陈淑慧  胡海燕  马永坤  李弛  柳保军  陈亮 《地质学报》2017,91(9):2079-2090

通过各类薄片显微镜下鉴定与定量统计,阴极发光、扫描电镜、电子探针、碳、氧及锶同位素、流体包裹体均一温度测试等分析,开展了白云凹陷深水区珠江组和珠海组砂岩储层中碳酸盐胶结物的类型与期次、地球化学特征、成因机制研究。结果显示,存在三期碳酸盐胶结作用,早期主要为方解石,以高Ca、低Fe、低Mg为特征。但珠江组早期碳酸盐胶结物的同位素组成(δ~(13)C_(PDB):-2.43‰~0.29‰,δ~(18)OPDB:-9.79‰~-3.08‰,87 Sr/86Sr:0.7084~0.7109)与珠海组(δ~(13)C_(PDB):-9.37‰~-8.13‰,δ~(18)OPDB:-7.11‰~-7.09‰,87Sr/86Sr:0.7138~0.7142)有一定差异,前者是在浅埋藏阶段从碳酸盐过饱和碱性海水介质中沉淀出的产物;后者与碳酸盐过饱和的碱性淡水有关。中期主要为铁方解石,以高Ca、较高Fe、低Mg、碳和锶同位素组成变化范围较大(δ~(13)C_(PDB):-20.88‰~-5.29‰,δ~(18)OPDB:-11.1‰~-8.99‰,87Sr/86Sr:0.7093~0.7151)为特征,其部分碳源与有机酸脱羧作用产生的CO_2有关,另一部分碳源(δ~(13)C_(PDB):-5.38‰~-5.29‰)可能与深部物质有关。形成碳酸盐胶结物所需的Ca2+、Mg2+、Fe2+等离子来源于砂岩中长石等碎屑的溶蚀、黏土矿物的转化以及深部热液流体。晚期主要为铁白云石(δ~(13)C_(PDB):-2.83‰~-1.83‰,δ~(18)OPDB:-9.45‰~-5.77‰,87Sr/86Sr:0.7101~0.7162),以高Fe、高Mg、较低Ca、碳同位素组成与同期海水基本一致为特征,87Sr/86Sr值低于正常成岩演化形成的碳酸盐,该期碳酸盐胶结物的形成与砂岩中生物碎屑以及先期碳酸盐胶结物的溶蚀再沉淀有关,部分可能受到深部热液流体的影响。  相似文献   

播撒碘化银实施雹云催化的数值试验--个例研究   总被引：9，自引：3，他引：6  

周毓荃  陈宝君  肖辉  黄毅梅  李子华 《大气科学》2003,27(1):8-22

在三维冰雹云模式基础上,采用湿热泡扰动方式激发对流云,对1998年7月21日发生在河南北部地区的一次冰雹过程进行模拟并做催化试验.结果表明,该例雹云具有含水量累积区,对累积区中心播撒碘化银能够减雹、增雨;而在此中心之下较低的高度作业,或播撒时间选取不当,则有可能增加冰雹.  相似文献