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首页> 外文期刊>Arabian journal of geosciences >In situ stress measurements of two hydropower projects in Iran by hydraulic fracturing method
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In situ stress measurements of two hydropower projects in Iran by hydraulic fracturing method

机译:水力压裂法测量伊朗两个水电项目的原地应力

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Hydraulic fracturing is one of the best-known methods of in situ stress measurement at great depths. In the last two decades, this method has been used as an important tool for pre-excavation designing of large projects, e.g., hydroelectric power plants, tunnels, mines, waste disposal galleries, etc. In this paper, some methods of stress calculation in fractured and intact rocks by means of hydraulic fracturing test are described, and the in situ stress states of Aras hydropower project and Roudbar Lorestan pumped-storage project are determined afterwards. The hydraulic fracturing (HF) and hydraulic tests on preexisting fractures (HTPF) tests were carried out in four vertical boreholes at shallow depth (100-190 m) at Aras and two vertical boreholes at almost great depth (440-520 m) at Roudbar Lorestan. The in situ stress magnitudes and orientations are calculated by classical and inversion methods in HF method (great depths) and by differential evolution and Gauss-Newton algorithms in HTPF method (shallow depths). The results of stress measurements illustrate that differential evolution provides better solutions than Gauss-Newton method. It is also demonstrated that the maximum horizontal stress orientation falls in southeast quarter which is in good agreement with the reports published from focal mechanism analysis and the direction of existing faults in Aras Project but deviates from world stress map data in the Rudbar site where it is influenced by the local joints and fractures in the test zone. Eventually, it should be mentioned that the ratio of horizontal to vertical stresses is significantly affected by topography and geology of the test areas. However, this ratio decreases as the depth increases.
机译:水力压裂是大深度现场应力测量的最著名方法之一。在过去的二十年中,该方法已被用作大型项目(例如水力发电厂,隧道,矿山,废物处置场等)的预开挖设计的重要工具。通过水力压裂试验描述了裂缝和完好无损的岩石,然后确定了阿拉斯水电站工程和鲁德巴尔·洛雷斯坦抽水蓄能工程的现场应力状态。在Aras的浅深度(100-190 m)的四个垂直井眼和Roudbar的两个大深度(440-520 m)的垂直井眼中进行了水力压裂(HF)和预先存在的裂缝的水力测试(HTPF)试验洛尔斯坦。通过HF方法的经典和反演方法(大深度)以及HTPF方法的差分演化和Gauss-Newton算法(浅深度)来计算原位应力的大小和方向。应力测量的结果表明,差分演化提供了比高斯-牛顿法更好的解决方案。研究还表明,最大水平应力方向在东南部,与震源机制分析报告和Aras项目中现有断层的方向一致,但与Rudbar现场的世界应力图数据有出入。受测试区局部关节和裂缝的影响。最后,应该提到的是,水平应力与垂直应力之比受测试区域的地形和地质的影响很大。但是,该比率随着深度的增加而减小。

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