工程荷载作用下缓倾角反倾似层状岩质边坡变形稳定性分析

在反倾层状边坡的破坏机制和稳定性分析方面,由于其稳定性一般较好,系统深入地研究其破坏机制和稳定性的反而不多。以火山岩地层多次火山喷发旋回形成的缓倾角反倾似层状岩质边坡为研究对象,利用有限元分析其位移矢量图,揭示边坡的变形破坏机制和稳定性控制要素,利用极限平衡法、矢量和法,评价其稳定性,利用强度折减法分析塑性区的扩展规律,揭示滑动面发展的时间空间规律,结果表明,（1）类似层状反倾岩质边坡的潜在破坏模式为剪切–张拉破坏,滑面形态表现为近似折线状：顺坡向穿过凝灰岩夹层和强风化岩体,后缘通过陡倾结构面;（2）极限平衡法、矢量和法的边坡稳定性综合评价表明边坡浅层稳定性不满足工程稳定性要求,深层稳定性满足工程稳定性要求,且三维矢量和安全系数大于二维结果,是三维效应造成;（3）塑性区扩展揭示滑面的空间发展序列为滑面4、5、3。文中的技术路线和分析方案可用于缓倾角反倾层状岩质边坡稳定性评价。     

黑龙江嫩江县银多金属矿45°斜孔钻探施工技术

在黑龙江省嫩江县二道坎村开展银多金属矿普查工作中使用MP-1000型便携式钻机进行了45°斜孔施工,该钻机占地小,搬迁方便,适合斜孔施工。针对斜孔施工中出现的钻孔漏失、坍塌掉块、钻孔偏斜的问题,通过采用改性刚性水泥堵漏剂对钻孔漏失段进行封堵,取得了良好的封堵效果;选用合适护壁性能的冲洗液减少了钻孔坍塌掉块;为防止孔斜,采用锚杆固定的方式稳固钻机,钻进过程中使用高胎体钻头,减少起下钻次数,避免掉块挤压钻具引起孔斜。通过选择合适的冲洗液以及不断优化施工工艺,45°斜孔施工取得了良好的效果。     

斜孔长螺旋钻进技术的试验研究

重点阐述了作者在分析、研究试验成果资料基础上得出的有关斜孔长螺旋钻进功率消耗、规程参数、孔弯规律及相应技术措施的初步结论。     

Inversion of breakout data from inclined boreholes for stress state of the upper crust in Jizhong depression

ＩｎｖｅｒｓｉｏｎｏｆｂｒｅａｋｏｕｔｄａｔａｆｒｏｍｉｎｃｌｉｎｅｄｂｏｒｅｈｏｌｅｓｆｏｒｓｔｒｅｓｓｓｔａｔｅｏｆｔｈｅｕｐｐｅｒｃｒｕｓｔｉｎＪｉｚｈｏｎｇ　ｄｅｐｒｅｓｓｉｏｎＹＡＮ－ＸＩＡＮＧＹＵ（俞言祥）ａｎｄＺＨＯＮＧ－ＨＵＡＩＸＵ（...     

静止环境中平面负浮力排放近区特性的数值研究

运用k-ε湍流模型,建立静止环境中平面负浮力倾斜射流的二维数学模型,采用D.M.Shahrabani和J.D.Ditmars的试验资料进行检验,并且对这类流动进行了数值预报。在此基础上,提出了将射流影响区域划分成为三个区的概念,即:射流区、回流区和水平扩展区,也给出了射流区和水平扩展区及射流区内部分区的界限。给出了收缩断面的位置及该断面物理量的分布,为远区特性计算给出了定解条件。     

利用主成分分析法研究余干地震台接收函数

对模型合成的理论接收函数进行主成分分析,研究在倾斜界面和各向异性影响下主成分形态变化规律,分析倾斜界面倾角和各向异性强度对接收函数R分量主成分贡献率的影响。对江西余干地震台的接收函数R分量主成分进行分析,结果发现:Ps震相的平均走时为3.4 s;台站下方介质的各向异性和倾斜界面同时存在,各向异性快轴大致呈NE向,倾斜界面倾向约170°。     

我国心脑血管病的医学气象研究

回顾了20世纪80年代以来我国心脑血管病医学气象研究的主要成果，总结分析了这些研究的结论、进展和不足，提出加强和改进此类研究的建议和对策。     

Double Porosity Finite Element Method for Borehole Modeling

Summary. This paper considers the mechanical and hydraulic response around an arbitrary oriented borehole drilled in a naturally fractured formation. The formation is treated as a double porosity medium consisting of the primary rock matrix as well as the fractured systems, which are each distinctly different in porosity and permeability. The poro-mechanical formulations that couple matrix and fracture deformations as well as fluid flow aspects are presented. A double porosity and double permeability finite element solution for any directional borehole drilled in the fractured porous medium is given. Compared with conventional single-porosity analyses, the proposed double-porosity solution has a larger pore pressure in the matrix and a smaller tensile stress in the near-wellbore region. The effects of time, fracture, mud weight, and borehole inclination in the double-porosity solution are parametrically studied to develop a better understanding of physical characteristics governing borehole problems.     

用几何规划解决弹簧的优化设计

介绍了几何规划的基本理论和在工程机械设计中的应用方法，将几何规划用于ＸＲＣ－１型斜井人车的弹簧优化设计，与传统设计方法相比显著地提高了经济效益。     

Tidal-channel deposits on a delta plain from the Upper Miocene Nauta Formation, Marañón Foreland Sub-basin, Peru

Miocene siliciclastic sediments of the Marañón Foreland Sub‐basin in Peru record the sedimentary response to regional marine incursions into Amazonia. Contrary to previous interpretations, the Late Miocene Nauta Formation provides evidence of the last known marine incursion before the current Amazonia river basin became established. Sedimentological, ichnological and palynological data from well‐exposed outcrops along a ca 100 km road transect suggest that the Nauta Formation represents a shallow, marginal‐marine channel complex dominated by tidal channels developed in the inactive, brackish‐water portions of a delta plain. The main facies associations are: FA1 – slightly bioturbated mud‐draped trough cross‐stratified sand; FA2 – locally, pervasively bioturbated inclined heterolithic stratification (IHS); and FA3 – moderately bioturbated horizontally bedded sand–mud couplets. These identify subtidal compound dunes, tidal point bars and shallow subtidal to intertidal flats, respectively. Bi‐seasonal depositional cycles are ascribed to the abundant metre‐ to decimetre‐scale sand–mud couplets that are found mainly in the IHS association: semi‐monthly to daily tidal rhythmicity is inferred from centimetre‐ and millimetre‐scale couplets in the mud‐dominated parts of the decimetre‐scale couplets. The ichnology of the deposits is consistent with brackish depositional conditions; the presence of Laminites, a variant of Scolicia, attests to episodic normal marine conditions. Trace fossil suites are assigned to the Skolithos, Cruziana and mixed Skolithos–Cruziana ichnofacies. Pollen assemblages related to mangrove environments (e.g. Retitricolporites sp., Zonocostites sp., Psilatricolporites maculosus, Retitricolpites simplex) support a brackish‐water setting. Uplift of the Mérida Andes to the North and the consequent closure of the Proto‐Caribbean connection, and the onset of the transcontinental Amazon drainage, constrain the deposition of the Nauta sediments with around 10 to 8 Ma, probably contemporaneous to similar marine incursions identified in the Cuenca (Ecuador), Acre (Brazil) and Madre de Dios (Southern Peru) (sub)basins, and along the Chaco‐Paranan corridor across Bolivia, Paraguay and Argentina.