多圈管分期冻结施工法温度场现场实测与分析     

宗翔 《冰川冻土》2012,34(5):1179-1183

在深厚表土中进行冻结法施工常产生由于冻胀应力造成的冻结管断裂, 为减小深井冻结壁在形成过程中产生的内部冻胀应力, 采取外圈辅助冻结孔滞后于主圈孔冻结的施工方案, 能有效地防止冻结管断裂. 应用有限元方法对淮南某煤矿主井冻结井筒分期冻结过程进行了瞬态温度场数值模拟, 和现场实测十分接近. 分期冻结方案能减少冻结壁内部水分聚集, 以达到减少冻胀应力的目的, 并形成相对比较均匀的温度场. 相同冻结条件下采用分期冻结方案, 冻结壁有效厚度增大约15%. 数值模拟的系统分析可为深井冻结壁的设计与施工提供科学依据.  相似文献   

晋江龙湖湖盆古凹陷内古河流形成与消亡及与地震关系     

徐起浩  施建生 《海洋地质与第四纪地质》2012,(2):53-63

根据野外调查及龙湖湖内和沿岸共78个钻孔岩心揭示的龙湖及沿岸混合花岗岩及其风化土、残坡积层和晚更新世以来的沉积层展布,分析了龙湖成湖前的凹陷和发育在凹陷内的古河流环境。研究发现龙湖湖盆内下游古河床相对邻近上游河床被大幅度抬升达3m余。龙湖的最早湖相沉积年龄为2 430±90aBP,其年龄落在导致古森林更深沉没于海的深沪湾晚全新世强古地震的时间范围内,认为龙湖的形成可能与2 430aBP左右深沪湾大地震,导致控制深沪湾陆地地堑的衙口—氵丙州断裂西北侧地块翘起掀升,使得湖盆凹陷内下游古河床被快速抬升,古河流被堵塞有关。龙湖是地震断塞湖,不同于断陷湖,是向斜坳陷湖的又一种构造湖。研究得出龙湖成湖前的古河流约在7 000aBP开始形成,这正是导致深沪湾古森林首次沉没于海的深沪湾早全新世强古地震大致年龄,结合古河床形成前的凹陷形态,认为龙湖湖盆内古河流的形成可能与7 000aBP左右深沪湾大地震导致龙湖地区环境改变有关。  相似文献   

Uplift of deck or footings in bridges with distributed mass subjected to transverse earthquake          下载免费PDF全文

Michael N. Fardis 《地震工程与结构动力学》2015,44(15):2755-2773

The eigenvalue problem is analytically formulated in symmetric bridges with distributed mass and moment of inertia under transverse earthquake. The piers are elastically supported on the ground. The deck is monolithically connected to one or two piers for all degrees of freedom and restrained or transversely free at the abutments. The characteristic equation, symmetric normal modes, modal participation factors, and participating mass ratios are given analytically. The problem is expressed in terms of few dimensionless parameters: (i) the radius of gyration of the deck mass divided by the pier height; (ii) the ratio of the rotational stiffness of a footing to that of the pier at the base; (iii) the ratio of flexural stiffness of the outer spans to those of the pier; (iv) the ratio of torsional stiffness of side spans to the rotational stiffness of the pier top; (v) for two piers, the side‐to‐central‐span ratio. Modal response spectrum analysis gives the moment at the base of the footings and the torque in the deck at its supports on the abutments as ratios to the values at incipient uplifting from the ground or the bearings. The peak ground acceleration of the motion at the onset of either one of these two types of nonlinearity is depicted as a function of the dimensionless parameters and the fundamental period of an elastic deck supported only at the abutments, or of a rigid deck on piers fixed against rotation at top and bottom. Copyright © 2015 John Wiley & Sons, Ltd.  相似文献   

中国西部大开发的时序与战略思考   总被引：1，自引：1，他引：0  

谭传凤  陈峰云  李祥妹  李荣 《地理与地理信息科学》2003,19(1):47-50

该文通过对中国和美国西部开发有关时序,战略等问题比较分析,认为我国西部开发在时序上应采取渐进式,开发战略重点的确定应慎重,指出应把发展教育作为先行战略,把生态建设作为核心战略,并且应制定一套完整的政策作为西部开发的保证体系。  相似文献   

河北省涞水县野三坡国家地质公园：地质遗迹的地质意义和4期节理的导控作用   总被引：4，自引：1，他引：3  

梁定益赵崇贺  聂泽同宋志敏 《地质通报》2005,24(2):189-195

野三坡国家地质公园位于太行山断隆与燕山“台褶带”的结合部,两构造单元以紫荆关大断裂为界。公园内地质遗迹丰富,其地质内涵是华北地质的精髓。发育4期宏大构造节理,分别与印支期华南板块、燕山期伊佐奈歧板块、华北期太平洋板块和喜马拉雅期印度板块的挤压有关。4期节理,特别是喜马拉雅期南北向“追踪张节理”,对园区构造地貌景观的形成起着关键作用。  相似文献   

Dispersal and recruitment of blue crab larvae in Delaware Bay,U.S.A.     

C.E. Epifanio  C.C. Valenti  A.E. Pembroke 《Estuarine, Coastal and Shelf Science》1984,18(1):1-12

Results of a three-year survey of the occurrence of Callinectes sapidus larvae in the mouth of Delaware Bay indicated that stage I zoea larvae were most abundant insurface water as compared to mid-depths and near bottom. The major peak in abundance of stage I zoea larvae occurred in early August with a secondary peak in early September. Peaks in abundance of megalopae occurred five weeks after the respective peaks in zoeal abundance. Zoea stages II–VIII were not collected in the bay mouth. Results of sampling every 3 h over consecutive tidal cycles showed that stage I zoea larvae were most common in the water column on ebbing tidal currents. Megalopae were most common in the water column on flooding tidal currents, suggesting a tidally related, vertical migration. It was concluded that stage I zoea larvae are flushed from the estuary and undergo development on the continental shelf. Megalopae are then transported back to inshore waters by a combination of winds and currents and invade the estuary by means of migration into the water column on flooding tidal currents and migration to the bottom on ebbing tidal currents.  相似文献   

用树木年轮重建博尔塔拉河流域的降水量序列   总被引：3，自引：1，他引：3  

潘娅婷  袁玉江  喻树龙  崔宇 《沙漠与绿洲气象(新疆气象)》2005,28(6):1-3

根据采自天山北坡西段博尔塔拉河流域18个采点的树木年轮样本,建立了每个采点的3种年表。通过相关普查分析,发现年表序列与上年10月至当年7月降水相关显著。用查干哈尔尕(t+1)、依和浑迪(t、t+1)、哈夏(t+2)4个树轮标准化年表序列可较好地重建该流域392a的该时段的降水量。分析重建结果发现:在这392a中,具有较明显的5个干期和6个湿期:有2a、3a、4a、12a、29a和43a的变化准周期:在1730,1753,1778和1831年发生突变。  相似文献   

基于多因复成矿床理论探讨阿合勒铜矿的成因   总被引：1，自引：4，他引：1  

曾乔松  陈广浩王核 李鹏春 《大地构造与成矿学》2005,29(4):545-550

新疆北部阿舍勒铜锌多金属矿床为海相火山岩型块状硫化物矿床，形成于晚古生代西伯利亚西南缘活动陆缘环境。在西伯利亚、哈萨克斯坦-准噶尔板块多阶段的俯冲、碰撞、拼合过程中，矿床所处的大地构造环境经历了多个开合演化阶段，为该矿床提供了良好的先天、临产及后天条件。成矿以喷气-沉积作用为主，其后经历了变质改造、岩浆热液叠加及表生氧化作用。矿床控制因素显示出“地层一岩控-构控和时控”多位一体的特点。同位素及微量元素研究表明，成矿物质具有多源性。根据陈国达历史-因果论大地构造学提出的多因复成矿床概念和时空四维兼顾研究思路，讨论了阿舍勒铜矿的多因复成矿床特征，厘定其为一个多因复成型矿床。  相似文献   

First finds of Permian conodonts in eastern Iran and once again on the Guadalupian series base in Permian sections of the Tethyan realm     

E. Ja. Leven  A. N. Reimers  H. W. Kozur 《Stratigraphy and Geological Correlation》2007,15(1):57-66

Conodonts found for the first time in eastern Iran (the Bage-Vang section) are characterized. Beds with conodonts also yield fusulinids that is suitable for refining correlation of conodont and fusulinid zonations. Stratigraphic ranges of different conodont species in the Bage-Vang section are correlated with those in the Luodian section (South China), where conodonts are also accompanied by fusulinids. As a result, some previous inferences concerning position of the Guadalupian Series base in the Tethyan sections are refined.  相似文献   

郯庐断裂带的两大发展阶段——广义的逆冲推覆断裂带和狭义的平移断裂带   总被引：2，自引：1，他引：2       下载免费PDF全文

侯明金  Jacques  Mercier  Pierre  Vergely  王永敏 《中国地质》2006,33(6):1267-1275

笔者总结了近年来的研究成果认为．中国东部的郯庐断裂带白海西期以来经历了两个主要发展阶段：第一阶段是广义的郯庐断裂带发展阶段，晚三叠世-早侏罗世由于扬子地块与华北地块的碰撞，成为两地块的对接边界，具有逆冲推覆的性质，属广义的特提斯构造域。第二发展阶段从早白垩世以来，发展成为一条平移断裂带，属于狭义的环太平洋构造域的平移系统。岩相古地理资料显示了扬子地块与华北地块的对接始于晚二叠世早期：印支期的郯庐断裂带是一条由NE、NNE向展布的缓‘S’型的地块拼贴边界．在现今的郯庐断裂带上表现为残留的由北北西向南南东的斜向逆冲推覆的性质，中下构造层次表现为韧性逆冲推覆变形，上部构造层即前陆褶皱冲断带内的变形：应力场分析资料显示：早三叠世晚期开始地表浅部就有近南北向的挤压作用，左行走滑平移作用开始发育：早白垩世晚期开始转入引张伸展阶段．与中国东部的伸展作用一致：新近纪又转为近东西向挤压．发育逆冲兼右行走滑作用．  相似文献