2022
DOI: 10.1016/j.enggeo.2022.106782
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Hydrate-bearing sediment of the South China Sea: Microstructure and mechanical characteristics

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Cited by 88 publications
(32 citation statements)
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“…In the GMGS1, GMGS3, and GMGS4 Wells, clay accounted for about 40% of the total. The proportion of silt is about 60%. , The particle size ranges from 40 to 90 μm, and the corresponding mesh number is 160. , In addition, in the drilling area, in addition to the silty sand type, there are also sandy clay reservoirs with large sand particle size. The particle size range is about 200 μm, and the corresponding mesh number is 70.…”
Section: Methodsmentioning
confidence: 99%
“…In the GMGS1, GMGS3, and GMGS4 Wells, clay accounted for about 40% of the total. The proportion of silt is about 60%. , The particle size ranges from 40 to 90 μm, and the corresponding mesh number is 160. , In addition, in the drilling area, in addition to the silty sand type, there are also sandy clay reservoirs with large sand particle size. The particle size range is about 200 μm, and the corresponding mesh number is 70.…”
Section: Methodsmentioning
confidence: 99%
“…Natural gas hydrates (cage compounds) are transparent or translucent solid compounds formed by hydrogen bonding of guest molecules such as methane gas or carbon dioxide with water. In the natural environment, gas hydrate exists stably in the form of methane and water crystallization under low-temperature and high-pressure conditions, which is also widely distributed in offshore areas and permafrost zones. Under the background of the exhaustion of traditional fossil resources and continuously increasing energy demand, as a clean and efficient unconventional fossil energy with wide distribution and large reserves, natural gas hydrate can provide critical support for solving the energy shortage problem. , However, the geological characteristics of hydrate-bearing sediments are complex and the sedimentary environment is sensitive, , and the exploitation of hydrate is accompanied by the decomposition of hydrate. , The decomposition of hydrate will reduce the sediment strength, which will lead to landslide, deposition, and another marine geological disaster. Therefore, the study of the mechanical characteristics of methane hydrate-bearing sediment (MHBS) under triaxial stress is of great importance to the safety and stability exploitation and commercialization of hydrate engineering …”
Section: Introductionmentioning
confidence: 99%
“…Previous studies have shown that important factors influence hydrate decomposition such as permeability (k), porosity (Φ), and hydrate saturation (S H ). k is the measurement index of the hydrate reservoir seepage capacity and largely controls the production potential of the hydrate reservoir; reservoir Φ and S H would obviously influence methane gas and water production in the depressurization process. So, accurately describing the 3D heterogeneity characteristics of k, Φ, and S H in the geological model is the necessary prerequisite to exactly study the hydrate reservoir production, spatial evolution of temperature and pressure field, and productivity effect of reservoir reconstruction.…”
Section: Introductionmentioning
confidence: 99%