首页> 外文会议>Advances on coupled thermo-hydro-mechanical-chemical processes in geosystems and engineering >COUPLED NON-ISOTHERMAL MULTICOMPONENT REACTIVE GEOCHEMICAL TRANSPORT MODELS: MODELLING THE LONG-TERM GEOCHEMICAL EVOLUTION OF A HLW REPOSITORY IN CLAY WITH CORE~(2D) V4
【24h】

COUPLED NON-ISOTHERMAL MULTICOMPONENT REACTIVE GEOCHEMICAL TRANSPORT MODELS: MODELLING THE LONG-TERM GEOCHEMICAL EVOLUTION OF A HLW REPOSITORY IN CLAY WITH CORE~(2D) V4

机译:耦合的非等温多组分反应地球化学传输模型:用CORE〜(2D)V4建模黏土高放废物库的长期地球化学演化

获取原文
获取原文并翻译 | 示例

摘要

A numerical model of coupled saturated/unsaturated water flow, heat transfer and multi-component reactive solute transport under both local chemical equilibrium and kinetic conditions is presented. It has been implemented in CORE~(2D) V4. Changes in formation porosity and permeability caused by mineral dissolution/precipitation reactions are taken into account. Model and code capabilities are demonstrated with its application to modelling the long-term geochemical evolution of a HLW repository in a clay host rock.
机译:建立了在局部化学平衡和动力学条件下耦合的饱和/不饱和水流动,传热和多组分反应性溶质运移的数值模型。它已在CORE〜(2D)V4中实现。考虑到由矿物溶解/沉淀反应引起的地层孔隙度和渗透率的变化。演示了模型和代码功能,并将其用于对粘土基质岩石中的HLW储层的长期地球化学演化进行建模。

著录项

相似文献

  • 外文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号