کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6435298 1637173 2014 11 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Effects of dissociation on the shear strength and deformation behavior of methane hydrate-bearing sediments
ترجمه فارسی عنوان
اثر انحلال بر روی مقاومت برشی و رفتار تغییر شکل رسوبات هیدرات بر متان
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات زمین شناسی اقتصادی
چکیده انگلیسی


- Both thermal recovery and depressurization method were used to dissociate methane hydrate.
- The mechanical behavior during dissociation was obtained.
- Thermal recovery method will lead to failure of specimen in certain conditions.
- Depressurization will not lead to collapse, while water pressure recovery will lead to failure in certain conditions.
- The effects of depressurization rate and reduction of pore pressure on the deformation behavior were obtained.

A series of tests were conducted in order to investigate the shear strength and deformation behavior of methane hydrate-bearing sediments during dissociation using the thermal recovery method or depressurization method. An innovative temperature-controlled high pressure triaxial apparatus which can reproduce the in situ conditions of hydrate reservoirs was used. The results indicate that: (1) the failure strength of isotropically consolidated methane hydrate-bearing sediments which dissociated completely using the thermal recovery method is less than that of pure Toyoura sand. However, the initial stiffness and volumetric strain are higher than that of pure Toyoura sand. (2) The thermal recovery method will cause the failure of methane hydrate-bearing sediments when the axial load is higher than the strength of methane hydrate-bearing sediments after dissociation. (3) The depressurization method will not cause collapse of methane hydrate-bearing sediments during depressurization. However, water pressure recovery will lead to failure when the axial load is larger than the strength of the methane hydrate-bearing sediments after dissociation. (4) The depressurization rate shows little effect on the ultimate deformation of methane hydrate-bearing sediments, while the initial deformation rate increases with increasing depressurization rate. (5) The larger the reduction of pore pressure, the larger axial strain and volumetric strain.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Marine and Petroleum Geology - Volume 51, March 2014, Pages 52-62
نویسندگان
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