Sun Yuanwei, Cheng Yuanfang, Li Cui, Wang Liqiang, Dai Xiaodong, Yan Chuanliang
School of Petroleum Engineering, China University of Petroleum (East China), Qingdao, China.
College of Petroleum Engineering, Shandong Institute of Petroleum and Chemical Technology, Dongying, China.
PLoS One. 2025 Apr 17;20(4):e0319772. doi: 10.1371/journal.pone.0319772. eCollection 2025.
The shallow hydrate reservoir in the Shenhu Sea area is mainly composed of clayey silt. Clay mineral has an important impact on the mechanical properties, and the hydrate decomposition aggravates this impact. Therefore, the composition and geological conditions of shallow clay hydrate-bearing sediment in Shenhu sea area are fully considered, hydrate-bearing sediment samples with similar physical properties are synthesized in situ. Then, indoor triaxial mechanical experiments are carried out, and the effect of clay minerals on the mechanical property is analyzed. The results show that the clay content and clay type have an important impact on the mechanical properties of unconsolidated hydrate-bearing sediment. With the increase of clay content, the strain hardening characteristics are prominent, the yield stage is longer, and the plasticity is enhanced. Hydrate-bearing sediment with different clay content shows similar mechanical laws under the influence of hydrate saturation and effective confining pressure. The peak strength, elastic modulus and Poisson's ratio all show a downward trend, but the peak strength and elastic modulus change more obviously. The peak strength changes linearly with hydrate saturation, while nonlinearly with effective confining pressure, especially 0-3 MPa. This is the comprehesive result of clay particle's movement and fragmentation, clay hydration and expansion, affecting hydrate formation and sediment cementation. When the content ratio of montmorillonite/illite decreases, the peak strength and elastic modulus show an increasing trend. Because the frictional resistance and connection strength of illite crystal layer are larger with bigger particle size, weaker hydration and thinner water film. The research can provide reference for drilling and production engineering of natural gas hydrate (NGH) reservoir in the Shenhu sea area.
神狐海域浅部水合物储层主要由黏土质粉砂组成。黏土矿物对力学性质有重要影响,水合物分解会加剧这种影响。因此,充分考虑神狐海域浅部黏土水合物沉积层的组成及地质条件,原位合成了物理性质相似的水合物沉积层样品。然后开展室内三轴力学试验,分析黏土矿物对力学性质的影响。结果表明,黏土含量和黏土类型对松散水合物沉积层力学性质有重要影响。随着黏土含量增加,应变硬化特征突出,屈服阶段变长,塑性增强。不同黏土含量的水合物沉积层在水合物饱和度和有效围压影响下呈现相似力学规律。峰值强度、弹性模量和泊松比均呈下降趋势,但峰值强度和弹性模量变化更明显。峰值强度随水合物饱和度呈线性变化,随有效围压呈非线性变化,尤其是在0 - 3MPa时。这是黏土颗粒移动与破碎、黏土水化与膨胀,影响水合物生成及沉积物胶结作用的综合结果。当蒙脱石/伊利石含量比降低时,峰值强度和弹性模量呈增大趋势。因为伊利石晶层的摩擦阻力和连接强度较大,颗粒尺寸较大,水化较弱,水膜较薄。该研究可为神狐海域天然气水合物储层的钻采工程提供参考。