水分胁迫条件下化控物质浸种对小麦根苗生长的影响

采用水培溶液添加PEG6000模拟干旱胁迫的方式，研究了化学调控物质浸种对不同程度水分胁迫下小麦根系及幼苗生长影响。结果表明，水分胁迫不同程度地降低了小麦幼苗的株高、叶面积、地上部及根的干重、根系活力、SOD、POD活性等，并明显增加了根系MDA含量水平。化学调控物质浸种处理可以增加各种条件下小麦的总根长、叶面积、根活力及SOD与POD活性，且表现出在干旱胁迫下增加幅度高于正常处理的现象。化学调控物质浸种有利于缓解干旱胁迫带来的不良影响。利用FA、GA、MET及稀土等化学调控物质浸种具有促进根系生长、培育小麦壮苗的突出作用。图3，表2，参14。     

直线电机地铁车辆曲线通过建模与仿真

分析了直线电机轮轨交通系统车辆与轨道结构的特点，针对广州地铁4号线车轨系统的特征，建立了其动态曲线通过模型。通过仿真计算得到了曲线半径、超高以及行车速度对车辆曲线通过时动力特性的影响规律。通过此项研究，为进一步探讨直线电机车辆曲线通过动力特性、优化线路设计参数以及轨道的养护维修工作打下了良好的基础。     

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.     

深部高应力巷道的非对称大变形

针对深部巷道尤其是倾斜岩层中的巷道围岩大变形问题,根据和分解有限变形力学理论,采用深部工程软岩大变形力学设计与分析系统(LDEAS)对旗山-1000 m 水平北翼轨道联络大巷的开挖过程进行了数值模拟.结果表明,倾斜岩层中巷道出现底板臌起、两帮缩进,顶板出现大面积的下沉;底板臌起、两帮缩进量的最大值和顶板的最大下沉量均随着巷道底板下岩层弹性模量的降低而呈增大的趋势.和分解增量法分析模型下巷道顶板的最大下沉量要小于两帮的最大收缩量,但是极分解增量法分析模型下巷道顶板的最大下沉量却大于两帮的最大收缩量.     

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.     

西藏措勤地区典中组火山岩地球化学特征及构造背景

措勤盆地位于西藏冈底斯构造-岩浆岩带的西段北侧,该区古新世火山活动十分强烈,形成了一套厚度大于1 000 m的中酸性火山岩地层,火山岩K-Ar和Rb-Sr同位素年龄为63.9～61.0 Ma,区域上可与古近纪林子宗群下部层位相对比,归为古新统典中组.火山岩岩石化学、地球化学特征分析表明,该火山岩系属高钾钙碱性-钙碱性系列,轻稀土富集,负Eu异常明显.与原始地幔相比,微量元素Rb,Ba,K,Th,U富集;Ti,P,Sr,Ta(Nb)亏损.锶、氧同位素组成显示岩浆来源与陆壳物质关系密切,推测是来自于俯冲带的幔源基性岩浆与陆壳重熔酸性岩浆以不同比例混合所形成.综合研究认为,这套火山岩形成于陆缘弧构造环境,与喜马拉雅特提斯洋壳向北俯冲消减作用有关.     

水电站深部洞室群应力场相关性研究

结合新疆某水电站的深部洞室群稳定性研究工作,利用三维弹塑性有限元方法,详细研究了水电站3个洞室的应力场在开挖过程中的变化规律,发现了"洞室群应力恶化效应",即后期的洞室施工对邻近洞室的应力场有恶化作用,加剧了前期开挖洞室的应力集中效应;以及"洞室群圆弧拱顶应力优化效应",即后期的洞室施工对邻近洞室拱顶的应力场有优化作用,减缓了前期开挖洞室拱顶的应力集中效应,这一规律的发现将对深部洞室群稳定性控制具有一定的意义.图5,表2,参10.     

岩巷快速爆破掘进的探讨

对影响岩巷掘进速度的循环进尺、巷道成型、爆破效率、炮眼深度、组织管理等因素进行了分析探讨。     

加载方式对大理岩碎块分布影响的试验研究

通过对大理岩的标准岩石试件进行单轴压缩和巴西劈裂试验，探讨了不同加载方式对破坏后岩石碎块分布的影响．结果表明：径向劈裂加载破坏后的大理岩碎块在0．5～20．0mm的粒径范围内是一个分形分布，平均分维数Dt为1．9761．单轴压缩破坏后大理岩的碎块分布存在双重尺度下的自相似分形，在0．1～1．0mm和2．0—40．0mm两个粒径范围内均呈分形分布，其平均分维数Dc1,Dc2分别为2．135 0，1．5499．分维数在一定程度上表现出随抗压强度增加而增加的趋势，但与抗拉强度的关系不明显，这与大理岩的各向异性密切相关．岩样破坏后碎块分布的分维数也是岩样荷载形式的恰当表征，引入岩石破碎过程的等效概率模型，从理论上给予了较好的解释．