gas pore volume 气体孔隙体积
gas pore in weld metal 焊缝中的气孔
pore gas flow 渗气阻力
pore gas pressure 孔隙气压
pore gas expelling 渗气阻力
The elemental geochemical anomaly of pore water in Marine sediments during the formation of gas hydrate is a significant indication for Marine gas hydrates in the deep sea floor.
海洋天然气水合物在生成过程中会引起周围沉积物孔隙水中元素地球化学异常,这些异常是指示天然气水合物存在的重要标志。
The experimental results show that the mean pore diameter decreases with increasing solidification pressure (the overall gas pressure).
结果表明,随着凝固压力(气体总压)的增大,气孔平均直径不断降低。
Besides temperature and pressure, the controlling factors for gas hydrate stability also include pore water composition, gas concentration in the fluid and Marine sediment types in the seafloor.
海洋天然气水合物的生成除了受温度和压力的影响外,还要受到孔隙水的化学组成、流体中气体的浓度及沉积物类型的影响。
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