气体释放速率对浅层气藏中气水运移的影响

为了论证在防治浅层气地质工程灾害中预先采取的有控制性排气措施的合理性和必要性,借助非饱和水气两相渗流原理,研究浅层气藏在气体释放路径下的气水运移规律.采用数值方法描述排气井不同释放速率对地下浅层气藏中气水运移的影响.结果表明:气体释放速率对气藏中的气水运移和分布形态有显著影响,释放速率越快,"水锥"效应越明显;实际工程中需结合详勘数据,选取适宜的排气速率,实施控制性放气措施,避免过早发生淹井,导致气井快速失效;在气藏中的浅层气体释放完毕后,砂土中会残留部分以气泡形式存在的气体,施工过程中需引起重视.     

硐室爆破技术在鹅头厂铁矿的应用

说明了鹅头厂铁矿露天采场延深采用硐室爆破的理由,分析了爆破参数选择、硐室爆破参数计算、边坡安全的要求、导硐及药室布置、药室堵塞及起爆网路等,并对爆破效果进行了评价。     

软土场地预应力管桩支护结构设计与施工

以实际工程为例,介绍预应力管桩支护体系在连云港软土场地基坑中的应用。计算分析表明,软土层对管桩支护体系的稳定性影响很大,实践中采用增加支护桩长度,使桩身穿越淤泥层,以满足稳定性计算的要求。工程监测结果表明,预应力管桩支护体系在连云港软土场地具有良好的适用性,工程的成功经验可供类似软土基坑工程参考。     

水平井开发效果影响因素研究——以大庆外围油藏为例

通过统计大庆外围特低丰度薄层油藏14个区块、90口水平井、245口直井的地质、油藏工程及生产历史资料数据,利用多因素综合分类分析法,系统分析水平井开发效果与各种地质及工程因素之间的关系。研究表明,地质影响因素主要为砂体类型、注采连通关系及油水同层发育程度,开发调整措施的适应性是影响水平井生产效果的主要因素。     

改性石英砂的润湿性能研究

对经过改性处理之后的普通石英砂的润湿性能进行了研究。实验采用滴水穿透时间法（WDPT）、酒精溶液入渗法（MED）、接触角测定法三种方法。通过这三种方法来定性和定量地描述其润湿性能。实验结果表明：直接经过酸化处理的石英砂与经过硅烷化处理的石英砂的润湿性能有着明显的改变,前者较普通石英砂表现更为亲水,而后者表现出斥水性。此研究为用石英砂模拟不同润湿性能土壤提供了表面改性方法以及前期的理论准备。     

不同温度梯度冻结中砂加卸荷变形特性研究

采用K0固结,负荷冻结,加、卸荷的方法,进行了4种不同温度梯度冻结中砂的三轴试验,获得了温度梯度和加、卸荷过程对冻结中砂变形演变的影响规律.结果表明:温度梯度的存在增大了冻结中砂起始切线泊松比,抑制了冻结中砂最大体缩量;不同温度冻结中砂加、卸荷过程中均呈现出体缩—体胀趋势,但不同温度梯度以及加、卸荷条件下的体缩速率和最大体缩量差异很大,且随温度梯度增加,体缩—体胀规律逐渐向持续体胀演变;卸荷过程增大了径向变形演化速率,抑制了冻结中砂体缩的发展,这一规律能合理解释加荷过程中获得的冻土强度高于卸荷过程的基本结论.     

Asymptotic state behaviour and its modeling for saturated sand

A new double hardening elasto-plastic model is proposed in this paper based on the existing unified hardening model (UH model). By assuming that there is part coupling effect between the plastic volumetric strain and plastic shear strain, hardening parameters consisting of a coupled and an uncoupled components are adopted in this model. A unique feature of this model is that it can describe not only the conventional drained and undrained behaviors of soil, but also the stress-strain relationships of soil under partially drained conditions which can be volumetric compression or dilation. Adopting the asymptotic state concept, simple equations for estimating the limiting stress ratio under undrained or earth pressure at rest (i.e. K ₀) conditions are derived. The new model is relatively simple to be adopted in practice for two reasons. First, the same soil parameters as in Cam-clay model are used except the addition of one extra parameter, the stress ratio at the characteristic state. Second, all the parameters can be determined using conventional triaxial compression tests. Supported by the National Natural Science Foundation of China (Grant Nos. 10672010 and 50479001) and the National Earthquake Science Item (Grant No. 200808076)     

废砂/PE废地膜复合材料热老化性能的研究

以聚乙烯(PE)废地膜和工业废砂为原料,制备了不同配比的废砂/PE废地膜复合材料,研究了PE基体和复合材料的热老化规律。研究发现,经80℃人工加速热老化处理后,复合材料的玻璃化转变温度(Tg)随老化时间的增加而降低;一定条件下的热老化有助于加强PE基体和废砂间的界面作用,使复合材料的力学性能先升高后降低;废砂的加入有利于PE废地膜热老化性能的提高。     

不同支护结构的实测土压力及其分析

通过对南京某大厦深基坑支护结构侧土压力的实测研究 ,分析和研究了软土地区悬臂支护结构、单层支点混合支护结构、连拱支护结构侧土压力分布的基本规律。     

Delineating spatial distribution and thickness of unconsolidated sand along the southwest Lake Michigan shoreline using TEM and ERT geophysical methods

Erosion and accretion of various magnitudes occur along the southwest Lake Michigan shoreline. These processes are triggered by natural events and human activities, which affect the distribution and thickness of sand on the nearshore lake bottom. Significant erosion along the Illinois coastline has highlighted the need for a large-scale means of acquiring spatially rich data to build models of sand distribution along the entire shoreline. Thus, we implemented a high-resolution airborne transient electromagnetic (TEM) method, coupled with a ground-based electrical resistivity tomography (ERT) method to determine the sand distribution and thickness along the shore from the beach to ~1 km into the lake. From Kenosha, Wisconsin, to Chicago, Illinois, we acquired 1049 line-km of TEM data, and 13.43 line-km of ERT data. Our results indicated a distinct, uneven distribution and thickness of the unconsolidated sand unit covering the southwestern Lake Michigan shoreline. The unconsolidated sand unit was found to range in thickness from 0 to ~12 m. This unconsolidated sand unit was shown to be thickest (4.5 to ~10 m) in the northern part of the study site. In southern Wisconsin and Chicago, the sand layer beneath the water column was found to be very thin, ≤1 m. We propose, based on our analysis, that lake-bed conditions and wind direction are the main factors that limit southward littoral transport. Our data suggest that the current state of the shoreline is relatively analogous to how it has always behaved; however, anthropogenic disturbance has exacerbated the natural patterns of erosion and accretion.