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史莉红, 武守鑫, 刘冲, 安羽枫, 王金龙, 张宏伟, 张卫强. 断层带承压水导升模拟试验系统研制与应用[J]. 煤炭科学技术, 2019, (7).
引用本文: 史莉红, 武守鑫, 刘冲, 安羽枫, 王金龙, 张宏伟, 张卫强. 断层带承压水导升模拟试验系统研制与应用[J]. 煤炭科学技术, 2019, (7).
SHI Lihong, WU Shouxin, LIU Chong, AN Yufeng, WANG Jinlong, ZHANG Hongwei, ZHANG Weiqiang. Development and application of simulation test system for confined water conduction in fault zone[J]. COAL SCIENCE AND TECHNOLOGY, 2019, (7).
Citation: SHI Lihong, WU Shouxin, LIU Chong, AN Yufeng, WANG Jinlong, ZHANG Hongwei, ZHANG Weiqiang. Development and application of simulation test system for confined water conduction in fault zone[J]. COAL SCIENCE AND TECHNOLOGY, 2019, (7).

断层带承压水导升模拟试验系统研制与应用

Development and application of simulation test system for confined water conduction in fault zone

  • 摘要: 在相似材料试验方面对断层带承压水导升高度数据的采集缺乏有效的监测手段,因此仅从应力变化、裂隙扩展2个角度去研究断层的活化突水规律缺乏一定的系统性。为研究工作面推进过程中断层带的活化特性及注浆工艺对断层突水行为的影响,以新元煤矿的地质条件为背景,运用二维相似材料试验平台和自制的承压水导升系统,对注浆前后工作面推进过程中断层带及附近岩层的应力演化规律、裂隙发育规律、承压水导升特性进行了系统研究。研究结果表明:承压水导升系统不仅使得含水层对底板岩体的力学效用得以表征,且实现了采动过程中水流导升高度数据的连续采集;在工作面推进过程中底板岩体会先后经历采前压缩、采后膨胀、应力恢复3个基本阶段,断层带的“屏障”作用会造成其邻近区域内底板应力集中,破坏区范围加大;随着防水煤柱尺寸的减小,断层带及两盘灰岩含水层受采动应力的扰动越加明显,当煤柱尺寸缩减到小于30 cm后,断层带下盘区域离层量陡〖JP2〗增,并且对盘三灰~四灰含水层中原先被浆液封堵的裂隙再次张开;断层带内承压水的导升高度与煤柱尺寸宽度密切相关,注浆工艺有效保证了煤柱尺寸在从36 cm减到30 cm的过程中,水流高度一直保持在9.6 cm,但是工作面在30 cm宽煤柱的基础上再向前推进时断层带内承压水的高度又会急速递增。

     

    Abstract: Currently, there is no effective monitoring method to collect the data of confined hydraulic conductivity rise in fault zone in similar material test. Therefore, it is not systematic to study the law of activated water inrush of fault only from the perspective of stress change and fracture propagation. To study the activation characteristics of fault zone and the influence of grouting technology on the water inrush behavior of faults in the course of longwall face advancing, this paper takes the geological data of the Xinyuan Coal Mine as the background. Two-dimensional similar material test platform and self-made confined water conduction system were used to study the stress evolution law, fracture development law and confined water conduction characteristics of the fault zone and adjacent strata before and after grouting in the course of longwall face advancing. Systematic research had been carried out. The results show that the confined water conduction system not only characterizes the mechanical effect of aquifer on the rock mass in the floor, but also realizes the continuous acquisition of water conduction height data during mining process. In the process of the longwall face advancing, floor rock mass will undergo three basic stages: pre-mining compression, post-mining expansion and stress recovery. The ‘barrier’,effect of fault zone will cause stress concentration occurring in the bottom of its adjacent area and expansion of the damaging area. With the decreasing of the waterproof coal pillar size, the disturbance of mining stress on fault zone and slate limestone aquifer becomes more obvious. When the coal pillar size is reduced to less than 30 cm, the amount of strata separating from the lower wall of fault zone increases sharply, and the cracks previously blocked by grout in Pansan limestone-limestone aquifer opened again. The height is closely related to the size and width of the coal pillar. The grouting technology effectively ensures that the flow height of the coal pillar maintained at 9.6 cm in the process of reducing the size of the coal pillar from 36 cm to 30 cm. However, when the longwall face advances on the basis of the width of the coal pillar at 30 cm, the height of the confined water in the fault zone will increase rapidly.

     

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