古田溪三级电站坝基及扬压力异常情况分析

对我国５０年代末期有代表性的边勘测，边设计，边施工的“三边”工程之一－古田溪三级电站运行３０多年来，其大坝基础状况及部分扬压力孔发生异常等情况作了分析研究，提出一些建议，对处理类似的三边工程具有实际意义。     

储油罐模型的静态倾斜试验及理论分析

为研究地震破坏中储油罐损坏与罐体翘离的关系，设计了储油罐模型在不同地基上的静态倾斜试验，分别采用梁的小变形法和非线性有限元法，建立了储液罐翘离反应的力学模型，并进行储油罐翘离静力分析．结论为：非线性有限元法与梁的小变形法计算结果接近；软基上罐的翘离量大约是硬基上的2倍多，但硬基上罐壁轴向压力约为软基上的1．1～1．4倍；容量3000m^3及小于3000m^3的高罐比大容量的矮罐受翘离的影响大．     

塔里木盆地古隆起的形成和油气控制

塔北、巴楚和塔中隆起是塔里木盆地不同世代盆地原型结构复合的产物,对油气的分布起着重要的控制作用.其中,塔中、塔北隆起,为海西期油气运聚的主要指向区,具有良好的储盖条件,是油气重要的聚集场所.中新生代昆仑山崛起,塔西南挤榨前渊形成,致使克拉通内拗陷转化并反转形成巴楚隆起,与塔西南前渊迭加的古生代源岩构成统一的成藏系统.     

塔中地区奥陶系碳酸盐岩储层特征及其油气意义

为了探明塔中地区奥陶系碳酸盐岩储层特征及其油气意义 ,根据勘探资料分析 ,奥陶纪时期 ,发育了下奥陶统以白云岩为主 ,上奥陶统以灰岩为主的巨厚碳酸盐岩沉积 ;同时 ,在中、上奥陶统与塔里木盆地中部地区下奥陶统之间和上奥陶统顶部发育两个不整合面 .在构造、沉积和后生改造的共同作用下 ,碳酸盐岩发育有下奥陶统白云岩层系和中、上奥陶统灰岩层系两套储集岩系 ,以及白云岩内幕型、风化壳岩溶型、构造裂缝型、沉积相带控制型和深部流体改造型 5种主要储集体类型 .根据储层的发育与分布特征 ,提出今后塔中地区应重点加强塔中北斜坡、塔中西部和西北倾没端区域上的油气勘探 ;在纵向上 ,应加强对深部下奥陶统以白云岩内幕型储集体为储层的碳酸盐岩油气勘探工作     

Evolution of the East Asian monsoon and its response to uplift of the Tibetan Plateau since 1.8 Ma recorded by major elements in sediments of the South China Sea

Evolution of the East Asian monsoon and its response to uplift of the Tibetan Plateau has been investigated in the study of global change. Core sediment samples drilled in the South China Sea during ODP Leg184 are the best materials for studying long-term variability of the East Asian monsoon. R-mode factor analysis of major elements in the fine grain-sized carbonate-free sediments (<4 μm) of the upper 185 mcd splice of ODP Site 1146 drilled during Leg184 in the South China Sea shows that Ti, TFe2O3, MgO, K2O, P, CaO, and Al2O3 are representative of a terrestrial factor. The variation in the terrestrial factor score is subject to chemical erosion in the source region and thus indicates the evolution of the East Asian summer monsoon. The terrestrial factor score has three stepwise decreases at ~1.3 Ma, ~0.9 Ma, and ~0.6 Ma, indicating the phased weakening of the East Asian summer monsoon is related to wholly stepwise, quick uplifts of the Tibetan Plateau since 1.8 Ma. The periodic fluctuation of the terrestrial factor score since ~0.6 Ma indicates that the glacial-interglacial cycles have been the main force driving the evolution of the East Asian monsoon. As in the case of Chinese loess, the long-term evolution of the East Asian monsoon recorded in sediments of the South China Sea reflects a coupled effect of the glacial-interglacial cycle and uplift of the Tibetan Plateau.     

外形几何参数对双坡屋盖升力系数极值的影响

对我国浙江沿海多个风灾频发区域进行深入调研,全面地确定了新农村典型低矮建筑双坡屋盖的外形几何参数.基于此进行了刚性模型测压风洞试验,研究了屋盖升力系数极值的变化规律,讨论了最不利屋盖升力系数随建筑外形几何参数的变化,用多参数非线性最小二乘法将最不利屋盖升力系数拟合为屋盖坡角、高宽比和厚宽比的函数,并对拟合函数进行了误差...     

复合滑动面岩体稳定分析的分解平衡法

本文在分析刚性块法(Rigid Block Method)和分块法(Partition Method)的基础上,提出了一种复合滑动面岩体稳定分析方法—分解平衡法(Decomposing Equilibrium Method).该法克服了RBM法不考虑垂直于滑动方向上的横向剪力而使阻滑力偏大的缺点,考虑了PM法所没有考虑的楔形体整体作用;导出了用等K值法计算岩体稳定的计算公式;并编制相应的计算程序.最后结合工程实例用三种方法进行了稳定计算.DEM法求得安全系数K_(DEM)居RBM法和PM法之间.     

青藏高原东北边缘黄土磁化率各向异性揭示古风向的初步研究

利用磁化率各向异性系统地研究了黄土沉积时的近地面风向。根据兰州、临夏、武都三个典型剖面共计１４０个风成黄土样品的磁化率各向异性的研究发现青藏高原东北边缘地区各时代黄土沉积的近地面风向是各不相同的，自早更新世中期到中更新世直至晚更新世，随着时间的推移，古风向都存在着一个明显的逆时针方向的改变。究其原因，这可能与青藏高原的隆起和局地特殊的地形效应以及环流形式的调整有关。     

Carbon isotopic records in paleosols over the Pliocene in Northern China: Implication on vegetation development and Tibetan uplift

Carbon isotopic composition of pedogenic carbonate can be used to estimate the proportion of C₄ and C₃ plants. Here we present carbon isotopic data of carbonate in a red earth section at Xifeng, central Loess Plateau. Results show that C₄ vegetation increased in ∼4.4 Ma B.P., stabilized between 4.0 and 3.0 Ma B.P. The character and timing of C₄ expansion on the Loess Plateau are similar, but different with other localities, e.g. Pakistan and Africa, implying that regional climate changes were main factors driving the expansion of C₄ plants. This event is comparable in timing with increased aridity evidenced by Xifeng grain size and North Pacific eolian dust records. Therefore we argue that the Pliocene expansion of C₄ plants in northern China might have been caused by the increased aridity, which in turn might be related to rapid uplift of the Tibetan Plateau.     

鲁西西部壳内物性界面计算及其应用研究

利用位场(重力、航磁)对数功率谱计算了鲁西西部地壳内部的物性(密度、磁性)界面。从资料的处理和结果分析,探讨了本区深层构造的特点和深层构造与浅层构造的关系,并对壳内物性界面的计算结果在能源预测与勘探、地震等方面的应用作了讨论。