The effects of stress and fluid pressure on the anisotropy of interconnected cracks     

S. R. Tod 《Geophysical Journal International》2002,149(1):149-156

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Separation of intrinsic and scattering seismic attenuation in the Southern Apennine zone, Italy   总被引：4，自引：0，他引：4  

F. Bianco  E. Del Pezzo  M. Castellano  J. Ibanez  F. Di Luccio 《Geophysical Journal International》2002,150(1):10-22

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Bed-limited cracks in effective medium theory     

S. R. Tod 《Geophysical Journal International》2003,152(2):344-352

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Statistical properties of reflection traveltimes in 3-D randomly inhomogeneous and anisomeric media   总被引：1，自引：0，他引：1  

Yu. A. Kravtsov  T. M. Müller  S. A. Shapiro  S. Buske 《Geophysical Journal International》2003,154(3):841-851

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An anisotropic fractured poroelastic effective medium theory   总被引：1，自引：0，他引：1  

S. R. Tod 《Geophysical Journal International》2003,155(3):1006-1020

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我国传压介质材料--叶蜡石矿物的基本特征   总被引：2，自引：1，他引：2  

徐文炘  李蘅  郭陀珠 《矿产与地质》2003,17(5):636-638

通过赵家台叶蜡石各种特征的研究，发现我国使用的传压介质材料不是纯的叶蜡石矿物，化学成分具有SiO2低、Al2O3高的特点；叶蜡石矿物与杂质矿物热膨胀系数绝缘程度应相近，并呈交织结构。  相似文献   

高放废物处置库选址中低渗透介质地质研究的几个问题   总被引：3，自引：0，他引：3  

郭永海  吕川河 《工程地质学报》2003,11(2):133-137

低渗透介质是阻碍有害物质在地下迁移良好的天然屏障, 因此成为高放废物处置库围岩类型的首选。本文通过对高放废物处置库选址中地质研究的回顾, 阐述了低渗透介质地质研究的特点, 对地质参数测定、取样、水流模拟、地球化学模拟进行了重点介绍。  相似文献   

探地雷达检测中如何计算速度   总被引：5，自引：1，他引：5  

袁明德 《物探与化探》2003,27(3):220-222,236

雷达波的传播速度随介质而变,这给准确定位探测目标带来了一些困难,因为目标深度取决于速度与讯号反射时间的乘积.但另一方面,利用速度变化与介质的关系,反过来可以推断介质的物质架构.作者结合实用例举了7种求速度的方法,以供使用探地雷达的同行们选用.  相似文献   

不同电阻率测深方法对旁侧不均匀体的反映   总被引：2，自引：0，他引：2  

强建科  阮百尧 《物探与化探》2003,27(5):379-382

利用三维有限元数值模拟,重点研究了旁侧三维不均匀体所产生的视电阻率的影响问题,展示了4种常规电阻率测深法在旁侧不均匀体上的异常分布特点;探讨了测深点正下方目标体异常与旁侧不均匀体异常的区别问题,指出旁侧不均匀体的影响是产生电阻率法假异常的主要原因之一.  相似文献   

A mathematical model of concentrate solids content for the wet drum magnetic separator     

John G. Rayner  T. J. Napier-Munn   《International Journal of Mineral Processing》2003,70(1-4):53-65

Low concentrate density from wet drum magnetic separators in dense medium circuits can cause operating difficulties due to inability to obtain the required circulating medium density and, indirectly, high medium solids losses. The literature is almost silent on the processes controlling concentrate density. However, the common name for the region through which concentrate is discharged—the squeeze pan gap—implies that some extrusion process is thought to be at work. There is no model of magnetics recovery in a wet drum magnetic separator, which includes as inputs all significant machine and operating variables.A series of trials, in both factorial experiments and in single variable experiments, was done using a purpose built rig which featured a small industrial scale (700 mm lip length, 900 mm diameter) wet drum magnetic separator. A substantial data set of 191 trials was generated in this work. The results of the factorial experiments were used to identify the variables having a significant effect on magnetics recovery.It is proposed, based both on the experimental observations of the present work and on observations reported in the literature, that the process controlling magnetic separator concentrate density is one of drainage. Such a process should be able to be defined by an initial moisture, a drainage rate and a drainage time, the latter being defined by the volumetric flowrate and the volume within the drainage zone. The magnetics can be characterised by an experimentally derived ultimate drainage moisture. A model based on these concepts and containing adjustable parameters was developed. This model was then fitted to a randomly chosen 80% of the data, and validated by application to the remaining 20%. The model is shown to be a good fit to data over concentrate solids content values from 40% solids to 80% solids and for both magnetite and ferrosilicon feeds.  相似文献