升降温作用下裂隙演化对单裂隙花岗岩渗流特性影响研究
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太原理工大学

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山西省基础研究计划项目(20210302124353)


Study on the Effect of Fracture Evolution on Seepage Characteristics of Single Fracture Granite under Heating and Cooling
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Taiyuan University of Technology

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    摘要:

    为研究高温高压下粗糙单裂隙表面形貌演化特征及水力流动特性,开展了在不同应力与渗透压条件下,一次温度循环的单裂隙渗流试验,采用三维形貌扫描技术描述不同围压下升降温作用后裂隙表面演化特征,分析了其对单裂隙花岗岩渗流特性的影响,结果表明:单裂隙花岗岩经温度循环及渗流作用后,裂隙表面局部岩体消失,其整体轮廓高度降低,轮廓线趋于平滑;在不同应力下,升温阶段裂隙水力开度和渗透系数先减小后增大,在降温阶段,同一温度下的裂隙水力开度和渗透系数均高于升温阶段时的值;高温高压渗流作用导致裂隙表面岩体产生不可逆的热破坏,裂隙面粗糙度降低,裂隙水力开度与渗流系数因此增大。

    Abstract:

    In order to study the surface morphology evolution characteristics and hydraulic flow characteristics of single rough fracture under high temperature and high pressure, single fracture seepage experiment of temperature cycle was carried out under different stress and osmotic pressure conditions. The surface evolution characteristics of fracture after rising and cooling were described by three-dimensional topography scanning technology. Its influence on the seepage characteristics of single fracture granite was analyzed. After the seepage action of high temperature and high pressure, the local body of the fractured surface of the single fractured granite destroyed, and the height of the contour decreases, the fracture surface contour becomes smoother; Under different triaxial pressures, the hydraulic fracture aperture and permeability coefficient drops first and then increase with the increase of temperature, with the decrease of temperature, the hydraulic fracture aperture and permeability coefficient at the same temperature are higher than those at the heating stage; The hydraulic fracture aperture and seepage coefficient increased with the decreased of the overall roughness of the fracture surface, which is subjected to the irreversible thermal destruction of the action of high temperature and high pressure seepage.

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  • 收稿日期:2023-03-06
  • 最后修改日期:2023-03-20
  • 录用日期:2023-03-28
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