Geothermics, Vol.32, No.4-6, 743-761, 2003
Reinjection of cooled geothermal brines into sandstone reservoirs
Injection of heat-depleted brines into elastic sedimentary reservoirs with alternating clay, sand and sandstone sequences has long been considered a delicate subject among petroleum and geothermal operators. Not only is injection an environmental pre-requisite in waste disposal, but it is also a means of achieving sound reservoir management as regards optimum heat sweep and recovery and pressure maintenance. However, without thorough and careful planning, injection can turn to disaster, for example where the formation and reinjected waters prove incompatible, or there is particle entrainment, capture and release, or unsuccessful well completion, which often leads to irreparable damage to the well and formation. This paper reviews the physics and chemistry governing these critical areas, and the problems likely to occur while pumping cooled brines into sandstone reservoirs: (i) water incompatibilities and subsequent supersaturation/precipitation of solid particles and clay swelling; (ii) fine particle migration/settling processes and relative pore throat bridging, pore retention/ bridging and formation plugging; (iii) flow velocities and near well or well completion erosion impairment; and (iv) temperature-related electrokinetic and water-rock interaction effects. The foregoing are illustrated by laboratory experiments, model runs and field trials. Application of these studies to water injection in the Upper Pannonian elastic reservoir in the Great Hungarian Plain is also discussed. (C) 2003 CNR. Published by Elsevier Ltd. All rights reserved.