泡沫油稳定性主控因素实验研究     

吴永彬  李晓玲  赵欣  李松林  李秀峦 《现代地质》2012,26(1):184-190

泡沫油在天然能量开采过程中具有"原油粘度高、生产气油比低、原油日产水平高、产量递减慢、天然能量开采采收率高"等特有的开采特征;而泡沫的稳定性是决定"泡沫油现象"存在时间长短的最关键因素。为定量描述泡沫稳定性的主控因素,自主研制了高温高压泡沫油可视化稳定性测试模型,并利用该模型开展了温度、溶解气油比、降压速度及孔隙尺寸对泡沫稳定性的单因素影响规律评价实验。实验结果表明,泡沫油中泡沫稳定存在的最高温度为60℃,最低极限原始溶解气油比为5 m3/m3,最低降压速度为0.08 MPa/min;同时发现,在越接近油藏实际孔隙尺寸的多孔介质中,泡沫的存在时间越长,表明在实际油藏天然能量开发过程中,"泡沫油现象"将会长期存在。以上认识有效地指导了MPE-3油藏天然能量开发,对于类似稠油/超稠油油藏确定合理的开发操作策略,实现经济高效开发具有重要指导意义。  相似文献   

连续时间随机游动理论模拟多孔介质中溶质运移的研究进展     

李娜  任理 《水科学进展》2012,23(6):881-886

近年来,基于连续时间随机游动(Continuous Time Random Walk, CTRW)理论所建立的模拟非均质多孔介质中溶质运移的方法已在大量的数值实验、室内实验、野外实验中得到了广泛的验证,为非均质多孔介质中的溶质运移行为提供了一种有效的模拟方法。简述了提出和发展CTRW的研究背景、基础理论以及与经典的对流-弥散方程等其他模拟方法的关系,综述了该理论在模拟溶质运移中的发展和应用,分析了实际应用中的关键问题,并展望了将其进一步发展应用于模拟反应性溶质运移的前景。  相似文献   

Analytical and numerical investigation of uniqueness and localization in saturated porous media     

H.W. Zhang  B.A. Schrefler 《国际地质力学数值与分析法杂志》2002,26(14):1429-1448

This paper presents first the applications of uniqueness and strain localization analysis of saturated porous media, where localization of deformation into well defined narrow zones in a saturated porous medium is studied in terms of discontinuous bifurcation theory. A generalized plasticity constitutive model and a Mohr–Coulomb model are used in both the theoretical and numerical analyses of shear band formations. The critical hardening moduli and shear band angle for localization are computed, and quantitative results are given for both constitutive models. Numerical results previously obtained and new ones are confirmed by this analytical and numerical investigation. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献   

Modelling of cement suspension flow in granular porous media     

Z. Saada  J. Canou  L. Dormieux  J. C. Dupla  S. Maghous 《国际地质力学数值与分析法杂志》2005,29(7):691-711

A theoretical model of cement suspensions flow in granular porous media considering particle filtration is presented in this paper. Two phenomenological laws have been retained for the filtration rate and the intrinsic permeability evolution. A linear evolution with respect to the volume fraction of cement in the grout has been retained for the filtration rate. The intrinsic permeability of the porous medium is looked for in the form of a hyperbolic function of the porosity change. The model depends on two phenomenological parameters only. The equations of this model are solved analytically in the one‐dimensional case. Besides, a numerical resolution based on the finite element method is also presented. It could be implemented easily in situations where no analytical solution is available. Finally, the predictions of the model are compared to the results of a grout injection test on a long column of sand. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献   

A re‐investigation of the low Reynolds number uniform flow past a porous spherical shell     

H. J. Hsu  L. H. Huang  P. C. Hsieh 《国际地质力学数值与分析法杂志》2004,28(14):1427-1439

This work reinvestigates the flow field of a uniform flow past a porous spherical shell based on Song and Huang's (2000) theory of laminar poroelastic media flow with proper boundary conditions. The analytical solution of this study not only indicates viscous effects inside the porous spherical shell, but it also preserves the continuities of tangential velocity and shear stress at the interfaces. The result reveals that as the porosity approaches unity, the flow is entirely comprised of the incident stream; as the porosity approaches zero, the well‐known Stokes' solution of a uniform flow past a sphere with low Reynolds number is obtained. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   

Mechanical behaviour and failure of cohesive granular materials     

Jean‐Yves Delenne  Moulay Saïd El Youssoufi  Fabien Cherblanc  Jean‐Claude Bnet 《国际地质力学数值与分析法杂志》2004,28(15):1577-1594

We investigate the stress–strain behaviour and failure of a cohesive granular material both by experiments and numerical simulations. The material is an assembly of aluminium rods glued together by means of an epoxy resin. The behaviour of cohesive bonds (force–displacement relationship, failure conditions) is characterized by performing simple loading tests (tension/compression, shear…) on a couple of rods. Then, this local behaviour is introduced in a numerical code based on a discrete element method in order to perform numerical compression tests on large samples. The validation of this approach was the main goal of the present investigation that is essentially achieved by a direct comparison between the numerical results and similar experimental tests. As a basic application, we derive the macroscopic cohesion and friction characteristics of random cohesive materials by systematic numerical simulations in a biaxial geometry. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   

Preparation and characteristics of porous ceramics   总被引：1，自引：0，他引：1  

References： 《东北亚地学研究》2007,10(2):166-170

Pyrophyllite is always used for making porous ceramics. In order to design the preparation technics of porous ceramics with pyrophyllite reasonably we must know the classifications, characteristics, properties and applications of porous ceramics. The classification and characteristics of porous ceramics are reviewed in this article; and several common preparations with their advantages and disadvantages are also introduced. The authors discussed the problems existing in researching and developing process for porous ceramics, and forecasted the development prospect of porous ceramics.  相似文献   

饱和孔隙弹性介质中的Rayleigh波及一维动力学问题     

黄江  曾心传 《大地测量与地球动力学》1993,(3)

本文依饱和孔隙介质动力学的基本方程组,对Rayleigh波在二相介质中的传播及一维土层动力学问题进行了探讨。数值计算表明:Rayleigh波速度在饱和孔隙弹性介质中大大小于在非饱和弹性介质中传播的速度;一维土层地面位移对有惯性力作用(a≠0)与忽略惯性力作用(a=0)也有很大差异。并对一维土层在阶梯形加载、脉冲式加载、正弦加载状态进行求解,为在实践中定性估计地基由于这类荷载作用产生的运动性态提供参考。  相似文献   

Multi-stage melt–rock interaction in the Mt. Maggiore (Corsica, France) ophiolitic peridotites: microstructural and geochemical evidence     

Elisabetta Rampone  Giovanni B. Piccardo  Albrecht W. Hofmann 《Contributions to Mineralogy and Petrology》2008,156(4):453-475

Spinel and plagioclase peridotites from the Mt.Maggiore (Corsica, France) ophiolitic massif record a composite asthenosphere–lithosphere history of partial melting and subsequent multi-stage melt–rock interaction. Cpx-poor spinel lherzolites are consistent with mantle residues after low-degree fractional melting (F = 5–10%). Opx + spinel symplectites at the rims of orthopyroxene porphyroclasts indicate post-melting lithospheric cooling (T = 970–1,100°C); this was followed by formation of olivine embayments within pyroxene porphyroclasts by melt–rock interaction. Enrichment in modal olivine (up to 85 wt%) at constant bulk Mg values, and variable absolute REE contents (at constant LREE/HREE) indicate olivine precipitation and pyroxene dissolution during reactive porous melt flow. This stage occurred at spinel-facies depths, after incorporation of the peridotites in the thermal lithosphere. Plagioclase-enriched peridotites show melt impregnation microtextures, like opx + plag intergrowths replacing exsolved cpx porphyroclasts and interstitial gabbronoritic veinlets. This second melt–rock interaction stage caused systematic chemical changes in clinopyroxene (e.g. Ti, REE, Zr, Y increase), related to the concomitant effects of local melt–rock interaction at decreasing melt mass, and crystallization of small (<3%) trapped melt fractions. LREE depletion in minerals of the gabbronoritic veinlets indicates that the impregnating melts were more depleted than normal MORB. Preserved microtextural evidence of previous melt–rock interaction in the impregnated peridotites suggests that they were progressively uplifted in response to lithosphere extension and thinning. Migrating melts were likely produced by mantle upwelling and melting related to extension; they were modified from olivine-saturated to opx-saturated compositions, and caused different styles of melt–rock interaction (reactive spinel harzburgites, vs. impregnated plagioclase peridotites) depending on the lithospheric depths at which interaction occurred. Electronic supplementary material  The online version of this article (doi:) contains supplementary material, which is available to authorized users.  相似文献   

下伏煤层瓦斯压力消散数值模拟     

戎涛  雷文杰 《中国地质灾害与防治学报》2008,19(1):91-94

平煤五矿己15煤层为低瓦斯煤层,下伏己16-17煤层为高瓦斯煤层,相对层间距比例1.0-4。己16-17煤层煤厚3.5m,为主采煤层。为降低己16-17煤层的瓦斯压力,实现安全高效生产,该矿以已15煤层为保护层,采用上保护层开采技术改变具有突出危险的煤层瓦斯赋存状态,降低被保护层的瓦斯压力。基于多孔介质流体流动理论,利用有限元数值模拟技术,模拟平顶山五矿超近上保护层的开挖过程,分析被保护煤层的瓦斯流动过程和煤层瓦斯压力的变化规律,论证保护层开采技术可以改变高突、高瓦斯煤层瓦斯赋存状态的可行性。  相似文献