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41.
Most fault-block reservoirs in Xinmu oilfield belong to heterogeneous sandstone in characters which has low permeability, and reservoir pollution is a common phenomenon in this area. Acidizing deplugging in oil wells has become one of the major measures to improve production efficiency in the field. A compound deplugging technology in high efficiency low corrosion is developed for this kind of low permeability sandstone reservoir. On the basis of profoundly understanding of the reservoir’s physical properties and sensitivity, along with comprehensive analysis of the cause for jams in oil wells, a series of experiments are carried out in order to investigate the dissolution reaction among samples and deplugging inhibitor, sample dissolving speed, formation fluid compatibility, reduction of secondary pollution, etc. Considered reservoir condition in nearby wells the optimized compositional deplugging liquid formula is selected for this reservoir. It is featured by reducing the deplugging reaction speed, extending solution for processing radius, preventing secondary damage in dissolution processing, and removing plug pollution effectively. To implement this high efficiency low corrosion deplugging measure based on reservoir condition in the borehole and nearby wells, a relatively better result of deplugging and production increasing is achieved, which enriches the measures to increase production in Xinmu oilfield, and this method can be applied to other similar oilfields for the purpose of maintaining the crude oil production and providing assistant for increasing the production significantly.  相似文献   
42.
纳微米聚合物微球的水化膨胀封堵性能   总被引:1,自引:0,他引:1  
为改善聚合物微球的深度调剖效果,利用蒸馏沉淀聚合法制备纳微米聚合物微球,并利用激光粒度分析仪、微孔滤膜装置和驱替装置对纳微米聚合物微球的粒径、水化膨胀能力和变形封堵能力进行测试分析.结果表明:纳微米聚合物微球为较规则均匀的球形,粒径分布集中,具有良好的水化膨胀性能;随着盐矿化度增大,纳微米聚合物微球膨胀性能变差;随着温度升高,微球的膨胀性能变强;在氯化钙和氯化镁水型中,微球膨胀性能变差;在酸性和碱性环境中,微球膨胀性能变差;随着水化时间增长,微球的封堵性能和变形能力逐渐增强,对孔道产生有效封堵的同时又能变形通过孔道,在渗透率较低的岩心中具有更好的深度调剖效果.  相似文献   
43.
通过理论研究和数值分析方法,分析了钢套管桩不同的施工顺序对邻近既有隧道的影响,并结合现场实测数据对分析结果进行了验证。首先,采用理论方法分析钢套管旋转下压过程中土塞柱的受力情况,建立微分方程计算土塞柱底端的应力、土塞柱受到的剪切扭矩和自身抗剪扭矩,进而分析得到了土塞柱发生剪切破坏和土塞效应的临界深度。在此基础上按是否产生闭塞效应,分两种情况研究了钢套管旋压过程中产生的土体膨胀率。然后,利用既得的土体膨胀率,通过理论分析和数值模拟方法分析了群桩不同的施工顺序对既有多条盾构隧道的影响,得出了相对较优的群桩施工顺序方案。工程现场实测数据与数值模拟结果的对比分析表明,上述计算结果与实际情况能较好吻合。该研究对类似工程具有理论指导意义和实践参考价值。  相似文献   
44.
The stiff clays beneath Holocene strata in the Yangtze Delta are interpreted as palaeosols, based on pedogenic features including illuvial argillans, voids, cracks, iron–manganese concretions and nodules, and carbonate materials. Variations in clay content with depth, the occurrence of foraminifera, and the environmental magnetism characteristics of the palaeosols suggest that their parent materials are floodplain deposits. Anisotropy of magnetic susceptibility (AMS) parameters of the sediments correlate well both with sedimentary dynamics and depositional processes in different sedimentary environments, and AMS analysis may be a useful tool for inferring sedimentary environments. Based on their considerable thickness (> 3.0 m), vertical changes of palaeosol maturity, and occurrence of ageing argillans throughout the palaeosols, the palaeosols are inferred to be compound ones (pedocomplexes) resulting from alternating deposition and pedogenesis on the palaeointerfluve of the Yangtze River. Phytoliths in the palaeosols indicate that climates turned generally from warm and wet to cold and dry with marked fluctuations during development of the palaeosols. This suggests that the palaeosols developed mainly during the marine regression prior to the last glacial maximum. The vertical distribution of manganese materials (e.g., concretions, nodules, speckles and mottles) in the palaeosols suggests that the groundwater tables were about 2.0–3.0 m beneath the upper boundary of the palaeosols during their development. Yellow–brown streaks and speckles are abundant from the middle to lower parts of the palaeosols, and layers with high CaCO3 content occur in the strata just beneath the palaeosols, but which lack caliche, suggesting that the groundwater table fluctuated markedly during their development. Voids and cracks filled with clays, and carbonate nodules (less than 0.1 mm in diameter) with thin iron–manganese rims are abundant in the palaeosols, indicating that wet and dry seasons were marked during the palaeosol development. It is suggested that the monsoonal influence was marked in the Yangtze Delta, with both winter and summer monsoons strongly developed during the development of the late Quaternary palaeosols.  相似文献   
45.
Representative images of split sediment cores document geological records, serve as visual aids for multimedia, and provide samples for image analysis. Existing core imaging systems, often containing integrated hardware and software, are capable of providing excellent images; unfortunately these systems are also bulky and expensive, and are therefore limited to labs that process large volumes of core and those actively involved in image analysis. For most research groups such systems are unfeasible to buy and maintain. Producing good quality core images with a hand-held digital camera is very difficult without a consistent lighting source, and changes in camera angle (in all three spatial dimensions) between photographs may prevent accurate image compositing. Tripods allow for camera stability, but typically do not accommodate downward-facing photography. Presented here is an easily constructed core-imaging system that minimizes many of the drawbacks of personal digital cameras. Software necessary for using this system is readily available and can be run from a personal computer.  相似文献   
46.
During the Anyang period in Shang dynasty (13c.BC ∼ 11c.BC), the bronze manufacture of Ancient China reached its maximum glory and splendor, as evidenced by the casting moulds and cores unearthed in the Yinxu. The pre-casting firing temperature of the moulds, one of the key technologies in the casting system, is still a controversial issue. In this article, the firing temperature of the mould and the core, unearthed at the Xiaomintun Site, Yin ruins, is estimated to be 600°C–700 °C, analyzed by luminescence techniques. This study can settle down the dispute in the results of the thermal expansion analysis.  相似文献   
47.
静压预应力混凝土管桩土塞效应试验研究   总被引:2,自引:0,他引:2  
张忠苗  刘俊伟  俞峰  谢志专 《岩土力学》2011,32(8):2274-2280
对淤泥质黏土互层以及粉土两种土层条件下静压预应力混凝土管桩的土塞效应进行了试验研究。现场及室内试验结果显示,管桩径厚比越大、土层条件越为坚硬则形成的土塞相对高度越大。上硬下软的土层分布易形成闭塞现象,而上软下硬的情况则易导致土塞的滑动。沉桩过程中,管壁端阻与静力触探锥尖阻力具有极为相似的变化规律,两者比值不随土塞高度变化率及沉桩深度的变化而改变。管壁端阻与锥尖阻力的相关性与土层条件密切相关,对于淤泥质黏土和粉土而言,两者比值分别为0.59和0.81。土塞的分层与地基土层分布基本一致,且分层界面为向上凸起的曲面。土塞形成过程中挤密效应是显著的,黏聚力则因扰动的影响有不同程度的降低。直剪试验显示,土塞抗剪强度的时效性是显著的。粉土中预应力混凝土管桩有效土塞高度约为5~6倍桩径,为整个土塞高度的70%;而淤泥质黏土中有效土塞高度大于4倍桩径。试验结果与已有的研究结果较为接近  相似文献   
48.
韩城区块煤层气钻井堵漏技术措施的探讨   总被引:1,自引:0,他引:1  
通过对韩城区块5口煤层气钻井漏失情况的分析,发现主要漏失层位为上部的孙家沟组和上、下石盒子组,漏失层的岩性以砂岩为主,且大都发生在岩性变化处。该区井漏形式主要为砂泥岩层段漏失及纵向裂隙漏失,据此提出了相应的堵漏措施:在渗透、纵向裂隙发育的砂泥岩中加入丹封、锯末及复合材料进行堵漏;在纵向裂隙发育的砂岩,漏失量较大时,采用大颗粒材料加水泥封堵,必要时用水泥固井进行堵漏。并针对该区的地层特性漏失原因,提出了相应的井漏预防措施。  相似文献   
49.
江陵凹陷深层富钾卤水井内降温析盐情况探讨   总被引:1,自引:1,他引:0       下载免费PDF全文
江陵凹陷位于湖北省江汉盆地西南部,其赋存有高温高压深层富钾卤水,该卤水资源在开发过程中遇到的主要问题是采卤过程中的结盐堵井。不考虑压力等其它因素,只探讨单一因素温度对氯化钠溶解度的影响,资料分析显示在50~150℃之间时,温度与溶解度线性关系较好;探索了岗钾1井井内析盐规律,发现在井深为1 600~2 400 m时析盐量最大。根据此规律,建议采用注入淡水法,使井内卤水得到稀释,以达到防止结盐的目的;建议稀释到对氯化钠溶液浓度略小于28.3%,注水井深2 400 m。  相似文献   
50.
Abstract

The superconducting-gravimeter data of Melchior and Ducarme (1986) has been interpreted as internal motion in the Earth's core by Aldridge and Lumb (1987) using a Poincaré model. Several low-order modes with periods of 13–16 hours have been tentatively identified in the core which is taken to be an incompressible, homogeneous fluid within a rigid, rotating container. The identification is based on asymptotic values of the frequencies which change slowly with time while the modes decay with an e-folding time of about 280 days. The slow change in frequency with time implies a small temporal variation in the rotation rate of the core. This mean flow is a nonlinear effect often observed in laboratory experiments designed to excite Poincaré modes. Interaction among modes during free ringdown is also observed in those experiments and apparently in the data of Melchior et al. (1988) as well. Laboratory work thus provides the link to extend the Poincaré model to include viscous and nonlinear effects in order to interpret the gravimetric observations as core modes.  相似文献   
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