河南老湾花岗岩的源区成分模拟

老湾花岗岩的岩石化学、稀土元素和同位素特征指示出老湾花岗岩源于下地壳经部分熔融作用形成。源岩中含有壳源和幔源物质,具类似于高钾钙碱性安山岩的岩石化学特点。详细的研究表明了早元古界桐柏山群不能成为老湾花岗岩的源岩。模拟的太古代岩系岩石化学成分经高程度的部分熔融作用可以形成老湾花岗岩。     

岩体动态响应分析程序的微机化及其应用

开发微机化的数值分析程序是推广数值方法在岩体工程中应用的一条有效途径。本文首先介绍一种微机数值分析程序的内存数据处理方法，然后介绍据此对岩体动态响应分析的二维非线性有限元程序ＤＹＮＰＡＫ的微机化改造和应用实例。     

用地球化学特征判别川北含铀砂岩

文章阐述了川北砂岩型铀矿床的地球化学特征。根据能谱测量，用Ｕ，Ｔｈ，Ｋ元素的丰度和比值，获得铀富集的有利条件、不利条件。通过伽马能谱法（测Ｕ，Ｔｈ，Ｋ）和Ｘ射线荧光法（测Ａｓ，Ｂａ），区分含铀浅色砂岩和不含铀浅色砂岩，区分红色砂岩（红色泥岩）与浅色砂岩，缩小川北砂岩找铀矿的范围。     

聚苯乙烯凝胶平均孔径尺寸的研究

研究了聚苯乙烯凝胶合成及其孔径的控制,并用两种不同的方法计算了各类凝胶的平均孔径。     

新疆若羌县赤石山变质核杂岩研究

新疆北山裂谷带西缘若羌县赤石山地区存在大型变质核杂岩构造。其下拆离盘为古元古界结晶基底杂岩 ,上拆离盘为中元古界白湖群变质岩系 ,滑脱拆离带为已变形的大型韧性正断层。核杂岩南、北侧发育上叠盆地 ,北侧形成“年轻”正断层及同构造期岩浆岩。变质核杂岩的形成与晚古生代北山陆内裂谷区域伸展有直接联系。该区变质核杂岩的首次厘定 ,对深化北山裂谷的研究具有重要意义     

高应力软岩巷道壁后充填支护研究

高应力软岩巷道属非线性大变形问题,巷道支护必须满足其变形要求。总结了白皎煤矿高应力软岩砌碹巷道变形破坏特征,分析了砌碹巷道破坏机理,并对碹体壁后充填粉煤灰基材料改善"支护-围岩"关系的作用机理进行了分析,最后得到了现场验证。     

采矿岩体动态稳定性CA模型的建立与系统分析

运用元胞自动机的演化建模方法构建深部采矿岩体的动态稳定性演化模型.定义岩体的工作状态变化概率和岩体完整性影响系数,创建了一种实现采矿岩体的动力学仿真模型.通过数字模拟实验,分析了岩体中不同状态下的元胞相互作用的关系,得到了以离散度作为岩体动态稳定性的度量指标.     

孔隙结构表征陶粒滤料净水效能的方法

在分析陶粒的吸附性能和孔隙结构的基础上,采用浊度和UV254等动态实验方法研究了陶粒滤料的净水效能,建立了陶粒滤料过滤性能的表征方法.结果表明,陶粒的比表面积和碘吸附值、孔体积和单宁酸吸附值、最可几孔径与全部吸附值的相关系数分别是0.99、0.92和1.00.其表征方法所得的陶粒滤料评价结果与陶粒滤料净水效能的实验结果相符,为评价陶粒滤料的净水效能和针对不同水质选择陶粒滤料提供了标准.     

Kinematics analysis of a robotic rock grinder

With the aim to discover water, life and resources in other planets, robotic sampling instrument is a crucial part of the space exploration robot. To remove dusty and weathered surfaces and expose the fresh rock underneath the planetary surface, a robotic rock grinder is considered to replace the geolo- gist’s rock hammer to carry out the geological investigation. A primary prototype of the robotic rock grinder with three degrees of freedom has been developed in this paper. Planetary transmission system is used in the grinding driving system with two inputs (rotation motor and revolution motor) and two outputs (grinding wheel and cutting brush). The grinding wheel with two teeth has been used to abrade the rock. The cutting brush is used to sweep the debris. The third actuator is to feed the grinding sys- tem. Kinematics of the grinding system has been analyzed. To get a continuous and smooth fresh face over the rock, grinding trajectory of the grinding wheel has been discussed and planned. Lastly, abra- sion experiments have been made to testify the feasibility and the basic function of this system.     

The controlling factors and distribution prediction of H_2S formation in marine carbonate gas reservoir,China

Generally, there are some anhydrites in carbonate reservoir, as H2S is also familiar in carbonate oil and gas reservoirs. Nowadays, natural gas with high H2S concentration is usually considered as TSR origin, so there is close relationship between H2S and anhydrite. On the contrary, some carbonate rocks with anhydrite do not contain H2S. Recently, researches show that H2S is only a necessary condition of H2S formation. The reservoir porosity, sulfate ion content within formation water, reservoir temperature, oil/gas and water interface, hydrocarbon and some elements of reservoir rock have great controlling effects on the TSR occurrence. TSR deoxidizes hydrocarbon into the acidic gas such as H2S and CO2, and the H2S formation is controlled by TSR occurrence, so the relationship among reaction room, the contact chance of sulfate ion and hydrocarbon, the reservoir temperature has great influence on the TSR reaction. H2S has relatively active chemical quality, so it is still controlled by the content of heavy metal ion. Good conditions of TSR reaction and H2S preservation are the prerequisite of H2S distribution prediction. This paper builds a predictive model based on the characteristic of natural gas reservoir with high H2S-bearing. In the porosity reservoir with anhydrite, the formation water is rich in sulfate and poor in heavy metal ion. Oil and gas fill and accumulate in the gas reservoir with good preservation conditions, and they suffered high temperature later, which indicates the profitable area of natural gas with high H2S-bearing.