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Titlebook: Rough Sets and Knowledge Technology; First International Guo-Ying Wang,James F. Peters,Yiyu Yao Conference proceedings 2006 Springer-Verla

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Zdzisław Pawlak mankind plays a dominant role on climate change due to CO emissions from en- 2 ergy consumption, and that a significant reduction in CO emissions is necessary 2 within decades. At the same time, the supply of fossil energy sources like coal, oil, and natural gas becomes less reliable. In spring 200
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Tsau Young Lindriving force of global geodynamics. The feature of this convection is that it is accompanied by very large changes in the properties of the material. The paper presents an overview of numerical models of the authors that reproduce the main global geodynamic processes. Presented models are as follow
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Wojciech Ziarkooultz-sous-Forêts (France). 2D temperature model built along a magnetotelluric profile crossing Travale (Italy) geothermal system enabled to constrain the location of potential supercritical reservoir at large depth by two seismic reflection horizons, which correspond to isotherm T. = 400 °C charact
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Yixin Zhongporoelastic medium induced by them. The process is stimulated by fluid injection into a borehole as well as by natural movement of water and melt. The Stokes hydrodynamic equations describe the flow in the fracture. The external problem is governed with the equations of poroelasticity. An ordered se
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Andrzej Czyzewskiatical viewpoint the description of the HF dynamics requires mathematical modeling and numerical simulation of the process of controllable growth of a large scale fracture in porous and permeable geological medium. For correct and comprehensive description of the HF process it is required to account
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Jerzy W. Grzymala-Bussehort time periods, at temperatures from 150°C. The greatest problem which arises in writing a monograph on such materials is the tremendous amount of data that is available. More than 2000 references have been published on one heat-resistant polymer system alone over a period of little more than two
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