应用地层测试流动段资料确定油井稳定产能方法研究

提出了一种根据地层测试流动段压力资料预测油井稳定产能的方法，该方法以比采油指数作为对比参数，对测试比采油指数的计算进行了推导，采用回归分析方法建立了测试比采油指数和生产比采油指数之间的关系式。应用建立的关系式对其它井的稳定产能进行了预测，误差分析表明预测结果比较正确。     

高含酸性气碳酸盐岩气藏流体敏感性实验研究

对川东北雷口坡组、嘉陵江组、飞仙关组、长兴组高含H，S及032的碳酸盐岩储层流体敏感性进行了实验研究，结果表明岩样速敏损害弱～强，水敏和盐敏损害中偏弱～极强，碱敏损害严重。岩石学分析揭示，川东北高含酸性气碳酸盐岩储层发育伊利石、微晶石英、白云石、方解石、硫化钙等潜在损害物质。钻井完井液侵入会破坏储层各物质间的原始动态平衡，诱发储层损害。主要损害机理为：①储层流体pH增加引起黏土矿物以及微晶石英失稳；②碱液与微晶石英、长石、白云石反应生成硅酸盐、高岭石、水镁石等新矿相；③流体矿化度改变可降低伊利石微粒间的连接力；④硫化钙水解产生OH^-，过量的OH-与Ca^2＋结合形成氢氧化钙沉淀；⑤储层含水饱和度和流体离子浓度改变，致使焦沥青脱附并在储层深部沉积；⑥硬石膏水化膨胀、分散运移。针对该气藏损害机理，可采用屏蔽暂堵技术以形成优质滤饼，有效降低储层流体敏感性损害。图5表2参10。     

川东北板东地区长兴组生物礁型储层研究

四川盆地东北部板东地区长兴组地层主要由含生物(屑)灰岩-生物(屑)灰岩、礁灰岩、泥-粉晶白云岩和细-中晶白云岩构成,其中以细-中晶白云岩的储集性能最好。以礁顶部测井曲线变化特征为依据,认为该礁至少是由3个旋回叠加而成。成岩作用中对储层影响最大主要是胶结充填作用、白云石化作用、溶蚀作用。经镜下观察认为胶结充填作用分3期,充填了大部分的原生孔隙;混合水云化作用使生物屑灰岩演变成具或不具生物(屑)残余结构的细—中晶白云岩;溶蚀作用形成的晶间溶孔、不规则溶孔、溶洞构成了生物礁主要储集空间。     

琼东南盆地异常地层压力与深部储集层物性

以琼东南盆地的实际资料为基础,分析了琼东南盆地异常地层压力分布及其成因机制,查明了琼东南盆地深部储层异常物性分布特征和异常地层压力对深部储层物性的影响并提出了深部储层的预测方法.认为琼东南盆地体现了晚期超压的特点,次生孔隙发育段与异常超压发育段对应,异常压力通过烃类的次生孔隙生成和原生孔隙保护、欠压实的孔隙保护以及阻止胶结物的形成3种方式对深部储层孔隙保存和发育产生影响.最后验证了Gluyas和Cade提出的有效埋藏深度是计算和预测超压条件下储集层孔隙度与深度关系的方法,认为该方法对琼东南盆地深部超压条件下储集层孔隙度的预测是-种行之有效的方法.     

沁水盆地煤层气安全钻井工艺

在煤层气钻井过程中，经常出现煤岩坍塌、井漏、煤层气气侵等问题，极大地影响了钻井安全。为了减少钻井事故及井下复杂情况的发生，提高钻井速度，在调研了国内外煤层钻井的现场经验和资料的基础上，结合目前煤层气钻井技术的发展状况，以及华北石油管理局近年来40多口煤层气井的钻井实践，针对沁水盆地在煤层气钻井过程中产生的复杂问题，及对安全钻井影响较大的井漏、坍塌和低密度水泥浆固井等问题，做了一些研究和总结，并提出了相应的解决办法，为同类煤层气的开采提供了借鉴。     

Continuous formation of slurry ice by cooling water–oil emulsion in a tube

Water-silicone oil emulsion with an additive, (C₂H₅O)₃SiC₃H₆NH₂, was examined as a heat storage material. A spiral tube used as a heat exchanger was immersed in a low temperature bath and the emulsion was circulated in the tube to make ice continuously. Ice was separated from the ice–liquid suspension in an outlet tank. The amount of formed ice, the temperatures of the inlet and the outlet of the heat exchanger, and the temperatures in the tube wall were measured and the overall heat transfer coefficient and the heat flux through the tube were calculated. Experiments were carried out, varying the flow rate, the temperature of cooling brine, and the thickness of tube wall. The condition under which slurry ice was formed continuously without adhesion of ice to the cooling wall was clarified. Though decrease in the thermal resistance of the tube increased the rate of ice formation or raised the brine temperature, it narrowed the range of the flow rate and of the brine temperature in which slurry ice was formed continuously.     

In Situ Formation of a Novel Nanocomposite Structure Based on MCM-41 and Polyethylene

M41S materials are prepared by in situ assembly of inorganic precursors and organic template and can be viewed as nanocomposites of the siliceous phase and organic surfactant. Calcination of these precursors gives the M41S materials that have been used to prepare novel nanocomposite structures, in which the organic phase inside the nano-sized pores is isolated by the nano-sized inorganic pore walls. The nanocomposite structures can be formed by in situ polymerization of monomers inside the channels. Polymerization of ethylene takes place inside the nano-sized pores, producing the desired nanocomposite structure. The resulting polyethylene was found to be a mixture of crystalline and amorphous phases.     

A new Thermo-viscoplastic Material Model for Finite-Element-Analysis of the Chip Formation Process

A new material model for describing the thermo-viscoplastic flow behavior of workpiece material in metal cutting is presented. In order to express the complex flow behavior which depends on the local strain, strain rate and temperature, a new methodology for sequential formulation is proposed. The material parameters which are achieved by using the flow stress data available at low strain rates are enhanced by matching the results of the experimental investigations and finite element simulations of the orthogonal cutting process. As a result, a material model which has a wide validity range of strain, strain rate and temperature is established.     

活性炭中甲烷水合物的生成动力学

在温度275．75－279．95K和压力5．6－9．6MPa的静置条件下，测定了14组甲烷水合物在活性炭中的生成动力学数据（压力－时间关系），分析了甲烷水合物在活性炭中生成的物理过程，结合边界层理论和结晶学原理，提出了单液膜传质控制机理的生成动力学模型，并求得了解析解,使用Levenberg-Marquardt方法拟合模型参数，模型预测值与实验值符合良好。     

分层测试工艺在中原油田的应用

对含有多层油藏的合注井，改变注水压力，测试各层压力、流量的变化，采用层面流量卷积法确定各单层油藏的渗透率、表皮因子和压力等参数。应用实例说明，该方法切实可行，资料可靠，是复杂油气藏动态监测的一种有效工艺。