The effects of methane hydrate dissociation at different temperatures on the stability of porous sediments
详细信息    查看全文
文摘
The strength of porous sediments during hydrate dissociation was studied. Mathematical expressions for the variation of strength of sediments were proposed. The Duncan-Chang model related to temperature and dissociation time was proposed.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700