王河煤矿矿井突水特征与防治水对策

王河煤矿位于荥巩矿区中部,单一开采太原组一1煤层,属带压开采,为荥巩矿区矿井水害最为严重的矿井之一.该矿自投产以来累计发生突水事故达50余次,并造成淹井2次.本文通过对王河井田地质、水文地质条件、突水点分布规律和突水强度特征的分析研究,阐明了矿井突水事故频发的原因,论述了地质构造条件、一1煤层底板隔水层厚度、含水层富水性、矿山压力、水压与突水的关系.在此基础上,提出了矿井防治水害的方法和措施,为今后该矿的安全生产指明了方向.     

煤层底板突水机理及评价

针对我国北方地区煤矿开采时煤层底板突水问题,介绍了我国矿井水害的现状和防治水技术发展的情况,阐明了喀斯特裂隙水的赋存条件、运移规律以及奥陶系灰岩喀斯特发育的规律;结合国外治水理论,论述了煤层底板突水机理,总结出煤层底板突水的水害特点、突水机理和评价方法,通过突水事例说明"突水系数法"的实际治水效果,最后对煤层底板突水提出了对策.     

浅析峰峰矿区矿井突水原因及防治

峰峰矿区是华北大水矿区 ,水害严重威胁着下组煤层的开采。本文通过对该矿区典型突水事例的分析 ,探讨了造成突水的原因 ,并提出了防治的措施。     

浅析峰峰矿区矿井突水原因及防治

峰峰矿区是华北大水矿区,水害严重威胁着下组煤层的开采。本文通过对该矿区典型突水事例的分析,探讨了造成突水的原因,并提出了防治的措施。     

煤矿水害及防治方法探讨

1　煤矿水害的种类1 .1　地表水体及大气降水水害地表水水害系指大气降水或地表水体通过区内含水层露头、塌陷区、古井溃入矿井造成的水害事故 ,尤其是暴雨、洪水溃入矿井造成淹井以及泥石流、滑坡造成的淹埋矿井及工业场所的灾害 .此类水害水量大 ,影响面广 ,破坏严重 .其特点是煤层埋藏较浅 ,第四系覆盖层薄 ,矿区浅部岩溶含水层发育 ,易接受地表水的补给 ,地表植被破坏严重 ,地面防洪排水工程不完善 .1 .2　老窑水及采空区积水水害老窑水一般处在埋藏较浅、开采年代较久的煤层 ,煤层开采的情况难以掌握 ,积水量、积水范围不清 .因积水中…     

采煤工作面煤层底板突水预报泛决策分析理论研究综述

自 2 0世纪 60年代以来 ,随着我国煤炭工业的长足发展 ,开采技术条件中的矿井水害问题越来越提到煤矿安全生产的高度来认识 .与此相适应 ,煤层底板突水预报问题一直是一个极为活跃的研究领域 ,其中泛决策分析理论是煤层底板突水预报的一个独立分支 ,本文系统地总结了泛决策分析理论的发展情况 .     

采煤工作面煤层底板突水预报泛决策分析理论研究综述

自20世纪60年代以来,随着我国煤炭工业的长足发展,开采技术条件中的矿井水害问题越来越提到煤矿安全生产的高度来认识.与此相适应,煤层底板突水预报问题一直是一个极为活跃的研究领域,其中泛决策分析理论是煤层底板突水预报的一个独立分支,本文系统地总结了泛决策分析理论的发展情况.     

郭二庄9~#煤带压开采底板突水灰色风险评价

针对郭二庄井田下组9#煤带压开采中存在的底板突水风险影响因素的不确定性,采用灰色风险计算模型和方法,结合井田已有突水、出水点水位标高、矿井最大涌水量及单位涌水量等相关信息统计,构建灰色风险计算模型,对井田受采动影响后煤层底板发生突水风险的概率和风险性变异进行评价。计算结果表明郭二庄井田下组9#煤带压开采存在底板突水风险性大,煤层开采前应慎重作出避让和分区隔离开采、探治结合等有效的补救措施,减少突发水害事故的发生。     

郭二庄9#煤带压开采底板突水灰色风险评价

针对郭二庄井田下组9#煤带压开采中存在的底板突水风险影响因素的不确定性,采用灰色风险计算模型和方法,结合井田已有突水、出水点水位标高、矿井最大涌水量及单位涌水量等相关信息统计,构建灰色风险计算模型,对井田受采动影响后煤层底板发生突水风险的概率和风险性变异进行评价。计算结果表明郭二庄井田下组9#煤带压开采存在底板突水风险性大,煤层开采前应慎重作出避让和分区隔离开采、探治结合等有效的补救措施,减少突发水害事故的发生。     

米村矿一1煤底板奥灰水突水危险性分析

带压开采过程中,防止底板突水是安全生产的关键.为了解突水原因,通过对生产现场地质资料进行疏理,并运用地质理论和矿山压力理论,对拟开采的一1煤层突水危险性进行了分析,认为煤层直接底板本溪组铝土质泥岩隔水层厚度过薄,井田内小断层比较发育,间接底板奥陶系灰岩的富水条件是矿井突水的主要因素.分析结果可为今后预测一1煤底板突水危险性提供理论依据.     

焦作矿区突水特点及矿井综合防治

焦作矿区以水大、水文地质条件复杂而闻名, 在生产过程中, 突水频繁, 突水原因及类型的多变, 多次造成淹井、淹采区的事故． 因此, 根据多年的治理突水及淹井经验, 对突水规律及特点进行了分析、总结; 制定出相应的防治水技术措施, 对水害进行的综合防治取得了较明显的效果．     

Influential factors and control of water inrush in a coal seam as the main aquifer

In this paper, a combination of field measurement, theoretical analysis and numerical simulation were used to study the main control factors of coal mine water inrush in a main aquifer coal seam and its control scheme. On the basis of revealing and analyzing the coal seam as the main aquifer in western coal mine of Xiao Jihan coal mine, the simulation software of PHASE-2D was applied to analyze the water inflow under different influencing factors. The results showed that water inflow increases logarithmically with the coal seam thickness, increases as a power function with the permeability coefficient of the coal seam, and increases linearly with the coal seam burial depth and the head pressure; The evaluation model for the factors of coal seam water inrush was gained by using nonlinear regression analysis with SPSS. The mine water inrush risk evaluation partition within the scope of the mining field was obtained,through the engineering application in Xiao Jihan coal mine. To ensure the safe and efficient production of the mine, we studied the coal mine water disaster prevention and control measures of a main aquifer coal seam in aspects of roadway driving and coal seam mining.     

基于断层影响因子与断层分维特征的断层突水危险性定量化分析

断层是诱发矿井突水事故的重要影响因素,新汶煤田受奥灰岩溶突水威胁严重,针对断层诱发突水问题,在系统总结新汶煤田矿井断层构造分布特征基础上,建立了断层对奥灰岩溶突水影响定量化分析体系。引入断层影响因子概念,对底板突水危险性进行了定量分析;采用非线性理论对煤矿地质构造发育特征进行定量化研究,揭示了矿井断层分维特征,提出了断层分维特征及其对突水影响危险性分区的原则及方法。采用断层影响因子等值线和断层分维等值线相互融合技术,得到新汶煤田协庄煤矿奥灰岩溶裂隙分布规律。根据不同单元岩溶的富水性,圈定出煤层突水危险区,对煤炭开采防治突水灾害具有指导意义。     

Analysis and control on anomaly water inrush in roof of fully-mechanized mining field

Caving of mine roofs from water inrush due to anomalous pressure is one of the major disasters and accidents that can occur in mines during production. Roof water inrush can trigger a wide range of roof collapse, causing major accidents from breaking roof supports while caving. These failures flood wells and do a great deal of damage to mines and endanger mine safety. Our objective is to analyze the anomalies of water inrush crushing the support at the #6301 working face in the ]isan Coal Mine of the Yanzhou Mining Group. Through information of water inrush to the roof, damage caused by tectonic movements, information on the damage caused by roof collapse and the theory about the distribution of pressure in mine abutments, we advice adjusting the length of the working face and the position of open-off cut relatively to the rich water area. In the case of anomalous roof pressure we should develop a state equation to estimate preventive measures with "transferring rock beam" theory. Simultaneously,we improve the capacity of drainage equipment and ensured adequate water retention at the storehouse.These are all major technologies to ensure the control and prevention against accidents caused by anomalous water inrush in roofs, thus ensuring safety in the production process of a coal mine.     

Risk assessment of fault water inrush during deep mining

With the gradual depletion of shallow coal resources, the Yanzhou mine in China will enter the lower coal seam mining phase. However, as mining depth increases, lower coal seam mining in Yanzhou is threatened by water inrush in the Benxi Formation limestone and Ordovician limestone. The existing prediction models for the water burst at the bottom of the coal seam are less accurate than expected owing to various controlling factors and their intrinsic links. By analyzing the hydrogeological exploration data of the Baodian lower seam and combining the results of the water inrush coefficient method and the Yanzhou mine pressure seepage test, an evaluation model of the seepage barrier capacity of the fault was established. The evaluation results show the water of the underlying limestone aquifer in the Baodian mine area mainly threatens the lower coal mining through the fault fracture zone. The security of mining above confined aquifer in the Baodian mine area gradually decreases from southwest to northeast. By comparing the water inrush coefficient method and the evaluation model of fault impermeability, the results show the evaluation model based on seepage barrier conditions is closer to the actual situation when analyzing the water breakout situation at the working face.     

五图-双系数法在煤矿突水评价中的应用

为安全开采受承压水威胁的一1煤层,分析了郑州矿区大平煤矿主要底板突水因素,并用单一突水系数公式对底板突水进行了预测分区.研究表明,用单一的突水系数公式来预测突水事故并不准确.在突水系数法的基础上,把含水层奥灰岩富水区、矿山压力、大中型断层、小断层密集带等主要突水因素考虑进去,对突水系数法进行修正,用五图-双系数法对大平矿底板突水进行预测分区,其预测结果可以指导煤矿安全开采.     

米村矿一_1煤底板奥灰水突水危险性分析

带压开采过程中,防止底板突水是安全生产的关键.为了解突水原因,通过对生产现场地质资料进行疏理,并运用地质理论和矿山压力理论,对拟开采的一1煤层突水危险性进行了分析,认为煤层直接底板本溪组铝土质泥岩隔水层厚度过薄,井田内小断层比较发育,间接底板奥陶系灰岩的富水条件是矿井突水的主要因素.分析结果可为今后预测一1煤底板突水危险性提供理论依据.     

基于岩体极限平衡理论的煤层底板突水危险性预测

基于岩体极限平衡理论,研究了完整近水平煤层底板突水力学机制。综合考虑底板隔水层厚度、工作面斜长及隔水层岩性组合特征,推导出了底板突水极限水压值计算公式。以保德煤矿为例,将突水极限水压值法运用到保德煤矿13＃煤底板突水危险性预测中。通过与传统突水系数法对比分析,阐明了突水极限水压值法的优越性:突水极限水压值法改进了传统突水系数法,可更有效地进行工作面斜长较大时的底板突水危险性预测。