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多形態裂隙砂巖水力耦合破壞過程與增透機理試驗研究

Experimental investigation on hydromechanical coupling-induced failure and permeability evolution for sandstone with multiple-shape prefabricated fractures

  • 摘要: 水力耦合激活巖石天然裂隙,誘導裂隙擴展形成復雜裂隙網絡,增加巖石滲透性是礦產地熱共采體系中的關鍵技術。本文通過預制含單裂隙、T型裂隙和Y型裂隙的砂巖試樣,進行三軸水力耦合試驗,研究多形態裂隙砂巖的關鍵閾值(閉合應力、起裂應力、損傷應力、峰值強度)、彈性模量、泊松比以及破壞模式等力學特性,同時開展裂隙漸進演化過程中聲發射和滲透率的演化規律研究,進一步分析水力耦合作用下裂隙巖石增透機理。結果表明:多形態預制裂隙砂巖試樣在水力耦合作用下,既有裂隙均通過拉伸、剪切或混合模式擴展形成次生裂紋,構成裂隙網絡,試樣滲透率顯著增加。單裂隙試樣的次生裂隙以剪切破壞為主,T型和Y型裂隙試樣的次生裂隙為剪切破壞和張拉-剪切破壞兩類。此外,多形態裂隙對試樣強度的影響大于水的弱化作用。隨著軸壓增大,巖石滲透率峰前階段先減小后增大,達到強度破壞時突跳增大。當試樣達到峰值后應力突然下降時,滲透率達到最大值,滲透率增透效果最好。預制裂隙角度和形態的變化對突跳系數的影響幅度較小,單裂隙的平均突跳系數值大于Y型裂隙大于T型裂隙。研究結果有助于理解裂隙破壞和流體流動行為,進而指導礦產地熱共采的工程。

     

    Abstract: In mineral and geothermal resource co-mining, the underground rock is often affected by mining stress, and fractures of different shapes, such as single fractures, T-shaped fractures, and Y-shaped fractures, are generated. To increase the reservoir permeability, the existing fractures need to be reactivated, causing them to expand under force and propagate in shear and tension modes, generating new fractures and finally forming a fracture network to increase permeability. Waterjet cutting and wire cutting equipment are used to prefabricate sandstone samples with different inclinations and single, T-shaped, and Y-shaped fractures on standard samples. This paper conducts hydromechanical coupling experiments to investigate the possibility of increasing permeability by expanding and merging fractures in prefabricated fractured sandstone samples under triaxial conditions. In addition, the focus is on mechanical properties, such as critical thresholds (crack closure stress, crack initiation stress, damage stress, and peak strength), elastic moduli, and Poisson's ratio, and the failure modes of multiple-shape prefabricated fracture sandstone samples are mainly studied. Simultaneously, the evolution law of acoustic emission and permeability during the progressive failure of fractured rock is studied, and the mechanism of permeability enhancement of fractured rocks under the action of hydraulic coupling is analyzed. The results show that under the action of hydromechanical coupling, all multi-shape prefabricated fracture specimens form secondary cracks that expand in tensile, shearing, or mixed modes through the existing fractures and generate new fractures or fracture networks, which can effectively increase the flow rate. All single-fracture specimens are shear failures, and the T-shaped and Y-shaped fracture specimens have two types of shear failure and tension-shear failure. Furthermore, the weakening effect of water has a smaller effect on strength than the effect of multiple-shape prefabricated fractures. With increasing axial pressure, the rock permeability first decreases and then increases in the pre-peak stage, and the jump coefficient increases when reaching the strength failure. When the stress suddenly drops after the peak of the sample, the permeability reaches the maximum value, and the permeability enhancement effect is the best. The change in the prefabricated fracture angles and shapes has a small influence on the jump coefficient. The average value of the jump coefficients of a single fracture is larger than that of a Y-shaped fracture, which is larger than that of a T-shaped fracture, and the jump coefficients are more than doubled. These observational and experimental results will help to understand fracture failure and fluid flow behavior, which will guide the engineering applications of mineral and geothermal resource co-mining.

     

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