Numerical simulation of pore size dependent anhydrite precipitation in geothermal reservoirs

被引:4
|
作者
Muermann, Mario [2 ]
Kuehn, Michael [1 ]
Pape, Hansgeorg [2 ]
Clauser, Christoph [2 ]
机构
[1] GFZ German Res Ctr Geosci, Sect Hydrogeol 5 3, Potsdam, Germany
[2] Rhein Westfal TH Aachen, Inst Appl Geophys & Geothermal Energy, EON Energy Res Ctr, Aachen, Germany
关键词
mineral precipitation; numerical simulation; anhydrite; geothermal reservoirs; Allermohe; SHEMAT; pore scale; COUPLED PROCESS MODELS; HYDROTHERMAL SYSTEMS; CHEMICAL-REACTIONS; HEAT-TRANSFER; MOUNT-ISA; FLOW; CONVECTION; TRANSPORT; GERMANY;
D O I
10.1016/j.egypro.2013.08.014
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Porosity and permeability of reservoirs are key parameters for an economical use of hydrogeothermal energy. Both may be significantly reduced by precipitation of minerals. The Allermohe borehole near Hamburg (Germany) represents a case in which precipitation of anhydrite resulted in a failed reservoir development. We introduce a new numerical approach for better understanding of this, considering both the spatial variations of supersaturation on the pore scale and the pore space structure. Besides pore size this requires consideration of the effects of surface charge density on the fluid supersaturation in porous media and of the role of fluid flow velocity. (C) 2013 The Authors. Published by Elsevier Ltd.
引用
收藏
页码:107 / 116
页数:10
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