Pore capillary pressure and saturation of methane hydrate bearing sediments

Sun Shicai Liu Changling Ye Yuguang Liu Yufeng

孙始财, 刘昌岭, 业渝光, 刘玉峰. 沉积物孔隙毛细管压力与甲烷水合物饱和度关系研究[J]. 海洋学报英文版, 2014, 33(10): 30-36. doi: 10.1007/s13131-014-0538-y
引用本文: 孙始财, 刘昌岭, 业渝光, 刘玉峰. 沉积物孔隙毛细管压力与甲烷水合物饱和度关系研究[J]. 海洋学报英文版, 2014, 33(10): 30-36. doi: 10.1007/s13131-014-0538-y
Sun Shicai, Liu Changling, Ye Yuguang, Liu Yufeng. Pore capillary pressure and saturation of methane hydrate bearing sediments[J]. Acta Oceanologica Sinica, 2014, 33(10): 30-36. doi: 10.1007/s13131-014-0538-y
Citation: Sun Shicai, Liu Changling, Ye Yuguang, Liu Yufeng. Pore capillary pressure and saturation of methane hydrate bearing sediments[J]. Acta Oceanologica Sinica, 2014, 33(10): 30-36. doi: 10.1007/s13131-014-0538-y

沉积物孔隙毛细管压力与甲烷水合物饱和度关系研究

doi: 10.1007/s13131-014-0538-y
基金项目: The Open Fund of State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University under contract No. PLN1206; the National Natural Science Foundation of China under contract No. 51376114; the Ministry of Land and Resources research of China in the Public Interest under contract No. 201111026; the Open Fund of Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals, Shandong University of Science & Technology under contract No. DMSM201007; the National Basic Research Program (973 program) of China under contract No. 2009CB219503.

Pore capillary pressure and saturation of methane hydrate bearing sediments

  • 摘要: 为了更好地理解沉积物中孔隙毛细管压力和水合物饱和度的关系,论文提出了一种新的方法。首先,测定了细颗粒石英砂中甲烷水合物的相平衡。根据相平衡数据,计算了孔隙毛细管压力和甲烷水合物的饱和度。结果表明细颗粒石英砂中由于孔隙水活度的降低,甲烷水合物的相平衡发生改变。分析认为孔隙水活度的降低是由于石英砂颗粒表面基团、负电荷性以及孔隙毛细管压力共同所致。随着甲烷水合物饱和度的增加,孔隙有效空间减小,孔隙毛细管压力随之增加。由于水合物生长的随机性特点,孔隙压力-饱和度关系还无法定量描述。
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出版历程
  • 收稿日期:  2013-05-24
  • 修回日期:  2013-12-26

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