三峡地区枯水期强降水前期指标分析

利用三峡地区东部６个站１９６１－１９９４年１０月－１月的逐日降水量资料和逐日历史天气图资料，统计分析了５００ｈＰａ环流形势呈“大Ｕ”型的条件下，三峡地区有无区域性强降水的前期指标，并用１９９５年资料进行检验，１９９６年资料进行试报。结果表明可根据５００ｈＰａ天气图上小槽位置，孟加拉湾槽位置及地面天气图上锋面位置３个指标的组合并结合其它消空条件能较好地预报“大Ｕ”型环流形势下三峡地区有无区域性强降水     

深循环热水型煤田地区温度场的特点及测量方法

本文根据福建省龙岩盆地王坑井田的部分测温资料,分析了井田近地表温度在水平方向和垂直方向上的分布规律及灰岩含水层中地下水的运动对温度场的影响。在此基础上,提出了在地下水运动较强烈的地区进行稳态和非稳态测温方法以及孔底温度半对数直线校正法。     

Response of dry- and liquid-filled porous rocks to static and dynamic loading by variously-shaped projectiles

Summary The present investigation was undertaken to study the response of both dry and liquid-filled porous rocks to static and dynamic loading of penetrators with various tip shapes. Eighteen static and forty-eight dynamic tests were conducted involving 6.35 mm diameter indenters featuring flat, hemispherical and 60° conical tip shapes on three different rocks in the energy range from 1.57 to 5.63 J. Force-penetration data were collected by means of strain gages attached to the penetrators. For all three materials, the magnitude of the resistive forces for a given input energy decreased in the following order: (i) dynamic penetration into a dry sample, (ii) dynamic penetration into a fluid-filled specimen, (iii) static loading of the fluid-filled rock, and (iv) static, loading of the dry rock.An unusual observation for the dynamic force-penetration curves was the temporal disparity between the peak force and maximum deformation, which must be attributed to inertial factors. Based on the experimental data, an analytical rigid-body model was constructed that contained both a static and a dynamic component of the resistive force with the objective of quantifying the effect of dynamic loading and the presence of fluid on the response of the rocks. The dynamic component was portrayed as a viscous resistance proportional to the velocity of the penetrator and the contact surface area which is a function of the indentation. It was found that the model provides a good predictive capability for the dynamic force-indentation relations for prescribed materials and tip geometries upon use of but a single constant for the viscosity.This paper is dedicated to the memory of Corwin O. Rogers.     

冰沟门盆地晚二叠世晚期肃南组河流相特征

甘肃冰沟门异常区在晚二叠世晚期肃南组(P_2~s)时发育了两种类型古河流。以大磁窑河为代表的网状支流河,蚀源区铀源丰度低,河床坡降大,流程短,水流急,不利于铀矿化的形成。古梨园河发育的中-晚期为低-高弯蛇曲河,边滩发育,规模适中(河宽<300m),铀源丰富,河水中富含植物碎屑等有机质,铀在沉积一成岩阶段于河流转弯处和主、支流交汇处形成聚集,为后生阶段的工业富集提供了良好的前提。     

A study on volatilization of antimony and bismuth by heating with ammonium iodide—A method for separation and determination of trace antimony and bismuth in geological samples

A decomposition apparatus was established consisting of a reaction tube and a long air-cooling condenser for the separation of antimony and bismuth through volatilization. It is demonstrated that the reaction Sb₂O₃+6NH₄I=2SbI₃+6NH₃+3H₂O starts at 300°C and completes at 380°C in 8 min. In comparison, the reaction Bi₂O₃+6NH₄I=2BiI₃+6NH₈+3H₂O will not take place below 450°C and will complete at 550°C. The differences in volatilizing temperature between antimony and bismuth iodide are large enough to make them separate at different temperatures. Experimental data show that antimony iodide was sublimated at 380°C without any loss of bismuth, and upon the completion of SbI₈ volatilization the long condenser tube can be substituted for by a clean one to collect volatilizing bismuth iodide at the temperature of 550°C. Results are in good agreement with those obtained from thermodifferential-thermogravimetric analyses. Determination of antimony was done using extraction spectrophotometric method with the reagent 5Br-PADAP, and that of bismuth using spectrophotometric method with Xylenol Orange. The method is simple, rapid, accurate and suitable for rock and other geological samples containing antimony and bismuth in the range of X-X · 10² ppm.     

中国东部沿海基岩海岛地下水资源分布特点——以庙岛群岛为例

本文依据对庙岛群岛基岩裂隙水进行的地质构造、水文地质、物探等方面的研究,提出了适用于我国东部沿海基岩海岛的地下淡水蘑菇体新模式。以新构造控水为指导思想,探讨了基岩海岛裂隙水的赋存条件及富集规律,指出了地下水资源开发方向,并且结合生产实际,比较有效地解决了研究区变质岩海岛找淡水难的问题。     

50米气象塔风、温、湿自动采集处理系统

本文介绍五层风速、温度、湿度及三层风向观测系统。选用Apple-Ⅱ微机作为采样处理机,采样时间为10秒。主要工作为1.软件设计。2.用干湿球温度表进行测湿。为保证精度,对测湿系数A值作了重新测定,并对测湿误差作了详实分析。     

地图设计与生产彩色管理系统的研究

本文以色度学理论为指导,根据地图设计与生产的实际需要,建构了一个用于地图颜色设计与分色的彩色管理系统。该系统通过数学模型完成对所含的七种颜色空间的相互交换,其中ＹＭＣＫ空间和ＨＶＣ空间直接与输入输出设备（介质）的颜色特征相关。在这一研究中,作者提出了一种不区分网点扩大性质的数学模型,改进了ＣＩＥＸＹＺ与ＭＲＧＢ空间的变换方法。     

不同桩型情况下的桩基差异沉降三维有限元分析

近年来，以控制差异沉降为目标的桩基础变刚度调平方法在我国岩土工程界正受到越来越多的重视和应用。该文用三维有限元方法研究在同一基础下采用不同桩型情况时各桩沉降和刚度的关系，探讨通过改变桩型来调整刚度，最后控制差异沉降的方法，并通过一个工程实例阐述运用不同桩型进行设计的概念和方法，达到减小差异沉降。     

虚拟城市中地物数据三角剖分的探讨与实现

在构建虚拟城市时,对用户采集的矢量地物数据进行Delauney三角剖分,并以VisualC 得以实现,在建成的“虚拟小区”三维视景模型中证明其是有效的。