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    中国大陆科学钻探主孔声发射法现今地应力状态的确定

    Determination of the present crustal stress state by using acoustic emission in the main borehole of the Chinese Continental Scientific Drilling

    • 摘要: 提要:对中国大陆科学钻探主孔的岩心进行了声发射测量,确定了301~1 531 m深度的最大主应力。并与钻孔崩落法(深度1 269~1 655 m)测量结果进行了对比,结果表明,声发射测量所得测值基本上落在钻孔崩落法测值的趋势线上,两种方法所得结果一致,说明测量结果可信。测量结果表明科学钻探主孔地应力大小随深度增加,在浅部301m最大主应力为13.4 MPa,在深部1 655 m为55.2 MPa 。随深度的增加率为0.0279 MPa/m。最大主应力方向为N 54°±3.3°E,且方向不随深度变化。

       

      Abstract: Abstract:The magnitude of the maximum principal stress is determined by using acoustic emission measurements of cores at 301, 598, 1003, 1258 and 1531 m depth in the main borehole of the Chinese Continental Scientific Drilling (CCSD) Project, and the measurement results of acoustic emission are compared with the measurement results of borehole breakouts. It is shown that the results from two methods are in good agreement. The results of stress measurement are reliable. The magnitude of stress in the main borehole increases with depth. The maximum principal stress is 13.4 MPa at 301 m depth and 55.2 MPa at 1655 m depth. The increase rate with depth is 0.0279 MPa/m. The direction of the maximum principal stress is N 54.2°±3.3°E and does not change with depth. It is considered that acoustic emission combined with borehole breakouts is an economic and effective method for deep in-situ stress measurement.

       

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