CN102759337B - Method for monitoring dynamic fractures of underground mining working face - Google Patents
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Abstract
本发明涉及一种井工开采工作面动态裂缝的监测方法,以准确和完整的获取采动裂缝及其发育过程中的几何信息。该方法包括:布设裂缝监测基准线,建立工作面最前端裂缝位置与工作面位置之间的数学模型,通过该数学模型找到相应的最佳观测裂缝,进行持续的动态观测,获取裂缝宽度的变化数据,绘制裂缝宽度关于工作面位置的变化趋势图,以便分析前端裂缝从产生到完全闭合此全过程中所经历的所有典型阶段的特征和时间节点信息,总结和提炼工作面前端动态裂缝完整的生命周期,进而为研究该区域煤炭开采对土地生态环境的影响机理及其自修复周期的研究提供时间基准和技术支撑。The invention relates to a method for monitoring dynamic fractures in well mining working faces, which can accurately and completely obtain geometric information of mining fractures and their development process. The method includes: laying out the fissure monitoring datum line, establishing a mathematical model between the position of the front end of the working face and the position of the working face, finding the corresponding best observed crack through the mathematical model, conducting continuous dynamic observation, and obtaining the change of the width of the crack Data, draw the change trend diagram of the fracture width with respect to the position of the working face, so as to analyze the characteristics and time node information of all the typical stages experienced in the whole process from the generation of the front crack to the complete closure, and summarize and refine the complete dynamic fracture of the front of the working face. Life cycle, and then provide a time benchmark and technical support for the study of the impact mechanism of coal mining on the land ecological environment and its self-repair cycle in this area.
Description
技术领域 technical field
本发明涉及环境监测技术领域,特别涉及风沙区井工开采工作面前端动态裂缝的监测方法。The invention relates to the technical field of environmental monitoring, in particular to a monitoring method for dynamic cracks at the front end of an underground mining working face in a sandstorm area.
背景技术 Background technique
风沙区的主体矿区具有独特的土壤理化性质,比如中国神东地区,由于沙漠化及潜在的沙漠化,使得风沙区土壤颗粒组成较粗、疏松无结构、储水保肥能力差,一遇水流,沙层上赋存的薄表土层,迅速崩解,土粒容易分散。另外,土壤的理化性质与暴雨、大风等恶劣的气候因素相互作为,引发严重的土壤侵蚀。这些条件和因素最终导致矿区生态环境十分脆弱。The main mining area in the wind-sand area has unique soil physical and chemical properties. For example, in the Shendong area of China, due to desertification and potential desertification, the soil particles in the wind-sand area are relatively coarse, loose and unstructured, and have poor water storage and fertilizer retention. The existing thin topsoil layer disintegrates quickly, and the soil particles are easily dispersed. In addition, the physical and chemical properties of the soil interact with harsh climatic factors such as heavy rain and strong wind, causing serious soil erosion. These conditions and factors ultimately lead to a very fragile ecological environment in the mining area.
相关研究表明,煤炭开采导致该类型的部分区域内景观破碎度加大,水井干涸,地下水位下降,中心水位下降程度可达2-3m,土壤含水量下降,植被覆盖度减小,水土流失加重。而该区域高强度开采对土地的影响规律和机理、土地损伤(如地裂缝)的时空变化规律以及随之而导致的地表水的变化、土地损伤哪些是暂时的哪些是永久的、土地的自修复能力如何等关键问题没有进行系统研究,从而最终导致无法对该区域扰动后生态环境的修复措施的选择提供科学的决策依据。Relevant studies have shown that coal mining has led to increased landscape fragmentation in some areas of this type, dry wells, lower groundwater levels, and a drop in the central water level of up to 2-3m, decreased soil water content, reduced vegetation coverage, and increased soil erosion. . The law and mechanism of the impact of high-intensity mining on the land in this area, the temporal and spatial variation of land damage (such as ground fissures) and the resulting changes in surface water, which of the land damage is temporary and which is permanent, and the nature of the land The key issues such as the restoration ability have not been systematically studied, which ultimately leads to the inability to provide a scientific decision-making basis for the selection of restoration measures for the disturbed ecological environment in the area.
地表裂缝的生命周期是指其在地表存在的从产生到完全闭合的全过程。对于该过程的监测,是研究该区域采煤扰动前后土壤孔隙度、土壤养分、土壤含水量的时空演变规律的前提和基础,是研究该区域土地损伤机理重要组成部分。The life cycle of surface cracks refers to the whole process of their existence on the surface from creation to complete closure. The monitoring of this process is the premise and basis for studying the spatio-temporal evolution of soil porosity, soil nutrients, and soil water content before and after coal mining disturbance in this area, and is an important part of studying the land damage mechanism in this area.
目前,相关研究主要是针对地裂缝产生的机理、地裂缝分布规律,地裂缝几何信息的理论研究,部分文献涉及到地裂缝监测的内容:At present, relevant research is mainly aimed at the mechanism of ground fissures, the distribution of ground fissures, and the theoretical research on the geometric information of ground fissures. Some documents involve the content of ground fissure monitoring:
王金庄利用土体压缩理论,定性分析了裂缝宽度的函数模型,指出在相同条件下,裂缝d与间距L之比与地表水平变形存在线性关系(请给出对应王金庄的参考文献,谢谢);吴侃通过提出了开采引起的地表任意点动态应变分量的计算方法.将地表点的变形同地表土的力学性质结合起来,提出了地表裂缝分布规律动态计算模型,并指出裂缝在地表上显示时间大致等于T=2B/v,其中B为回采工作面上方裂缝区宽度,v为工作面平均推进速度(吴侃,胡振琪,常江,葛家新.开采引起的地表裂缝分布规律中国矿业大学学报,1997,26(2):56~59);李晓等采用自主研发的IGG-1机械式裂缝观测计,对金川二矿区10余条地裂缝的几何信息进行了不同时段的监测并进行了数据分析,得到了裂缝具有明显的三维特征,并对其成因进行了相应的剖析(李晓,路世豹,廖秋林,杜国栋.充填法开采引起的地裂缝分布特征与现场监测分析[J].岩石力学与工程学报,2006,25(7):1361~1369);姚娟根据任意两点之间的空间信息的变化情况,建立了裂缝宽度和变形计算的数学模型,指出裂缝宽度和变形是反映裂缝变化的一个重要指标(姚娟,徐工,开采引起的地表裂缝规律研究[J].山东理工大学学报(自然科学版),2009,23(6):105~108);李亮、吴侃等利用三维激光扫描的方法,获取塌陷地裂缝区地表特征的云数据,各点距起点的距离和下沉值以(x,y)的形式输入MATLAB中,对这些离散点进行插值,形成平滑的待分析曲线L,利用四种小波进行小波分析,与其实际观测数据符合,可用于提取裂缝分布规律(李亮,吴侃,陈冉丽,张舒.小波分析在开采沉陷区地表裂缝信息提取的应用[J].测绘科学,2010,35(1):165~167)。Using the theory of soil compression, Wang Jinzhuang qualitatively analyzed the function model of crack width, and pointed out that under the same conditions, there is a linear relationship between the ratio of crack d and spacing L and the horizontal deformation of the surface (please give the references corresponding to Wang Jinzhuang, thank you); Wu Kan proposed a calculation method for the dynamic strain component at any point on the surface caused by mining. Combining the deformation of the surface point with the mechanical properties of the surface soil, he proposed a dynamic calculation model for the distribution of cracks on the surface, and pointed out that the time for cracks to appear on the surface is approximately Equal to T=2B/v, wherein B is the width of the fracture zone above the mining face, and v is the average advancing speed of the working face (Wu Kan, Hu Zhenqi, Chang Jiang, Ge Jiaxin. The distribution law of surface fractures caused by mining, China University of Mining and Technology, 1997, 26(2): 56-59); Li Xiao et al. used the self-developed IGG-1 mechanical fracture observation meter to monitor the geometric information of more than 10 ground fissures in Jinchuan No. According to the analysis, the fractures have obvious three-dimensional characteristics, and their causes were analyzed accordingly (Li Xiao, Lu Shibao, Liao Qiulin, Du Guodong. Distribution characteristics and field monitoring analysis of ground fissures caused by filling mining[J]. Chinese Journal of Mechanics and Engineering, 2006, 25(7): 1361~1369); Yao Juan established a mathematical model for crack width and deformation calculation based on the change of spatial information between any two points, pointing out that crack width and deformation are reflections of An important indicator of fracture change (Yao Juan, Xu Gong, Research on the law of surface fractures caused by mining [J]. Journal of Shandong University of Technology (Natural Science Edition), 2009, 23(6): 105-108); Li Liang, Wu Kan et al. used three-dimensional laser scanning method to obtain cloud data of surface characteristics in the subsidence fissure area, and input the distance and subsidence value of each point from the starting point into MATLAB in the form of (x, y), and interpolated these discrete points to form a smooth The to-be-analyzed curve L is analyzed by four kinds of wavelets, which are consistent with the actual observation data, and can be used to extract the distribution of fractures (Li Liang, Wu Kan, Chen Ranli, Zhang Shu. Wavelet analysis in the extraction of surface fracture information in mining subsidence Application of [J]. Surveying and Mapping Science, 2010, 35(1): 165~167).
然而,上述研究多以整体裂缝作为研究对象,着重体现在裂缝的分布规律,部分对裂缝的监测研究,裂缝最初监测时间较严重滞后于裂缝出现的时间,获取的数据也不能完全包含裂缝最初状态的信息,监测频率不规范,不适合神东矿区现代化开采造成裂缝在地表显示特征的快速变化。However, most of the above studies focus on the overall fracture as the research object, emphasizing on the distribution of fractures. In some monitoring studies on fractures, the initial monitoring time of fractures is seriously lagging behind the time of crack appearance, and the obtained data cannot fully contain the initial state of fractures. The monitoring frequency is not standardized, and it is not suitable for modern mining in the Shendong mining area, resulting in rapid changes in the characteristics of cracks on the surface.
总体来说,对于裂缝从产生时的最初状态到表征在地表上完全或者基本消失所经历的阶段、过程,特别是对于薄基岩风沙区工作面前端裂缝的生命周期的监测还没有开展没有进行相应研究,该过程中裂缝对土地生态环境的研究也就无从谈起。Generally speaking, the monitoring of the stages and processes experienced by fractures from their initial state to their complete or basic disappearance on the surface, especially for the life cycle monitoring of fractures at the front of the working face in the thin bedrock sandstorm area, has not been carried out. Corresponding research, the study of the cracks on the land ecological environment in this process is out of the question.
风沙区工作面前端裂缝生命周期的监测方法的难题在于:The difficulty of monitoring the life cycle of the front cracks in the working face in the sandstorm area lies in:
1)观测对象的辨别与选取难度很大:薄基岩风沙区地表被松散层覆盖,冲刷层以上的土壤构成主要是黄沙,且流动性较大,加之大风、雨水天气对于小区域内地貌重塑的影响较大,地表裂缝最初产生阶段在地表上的表征相对较弱,其特征辨别和选取相对于其他类型区域非常困难,从而对地裂缝产生时最初状态的数据以及最终裂缝生命周期的获取造成了很大的影响;1) The identification and selection of observation objects is very difficult: the surface of the wind-blown sand area with thin bedrock is covered by loose layers, and the soil above the scour layer is mainly composed of yellow sand with high mobility. The influence of plasticity is greater, and the representation of the initial stage of surface cracks on the surface is relatively weak. Compared with other types of areas, it is very difficult to distinguish and select its characteristics. Therefore, the data of the initial state of the ground cracks when they are generated and the final life cycle of the cracks are obtained. had a great impact;
2)裂缝几何信息的获取难度较大:风沙区地表流动沙层的存在,裂缝两侧的土壤过砂、质地松散,裂缝在开裂、闭合等发育过程中,裂缝壁的部分土壤容易出现塌落现象,给裂缝宽度数据的获取带来了很大的困难,不确定的偶然误差引入粗差,无法取得预期的效果,最终也无法获得前端裂缝的生命周期。2) It is difficult to obtain the geometric information of fractures: the presence of floating sand layers on the surface in the sandstorm area, the soil on both sides of the cracks is too sandy and loose in texture, and part of the soil on the crack wall is prone to collapse during the cracking and closing process of the cracks. phenomenon, which brings great difficulties to the acquisition of crack width data. Uncertain accidental errors introduce gross errors, and the expected effect cannot be achieved, and ultimately the life cycle of the front crack cannot be obtained.
发明内容 Contents of the invention
有鉴于此,本发明的目的在于,提出一种井工开采工作面动态裂缝的监测方法,以准确和完整的获取动态裂缝及其发育过程中的几何信息,为研究由区域地表裂缝导致的土壤理化性质的时空演变规律提供基础,最终为该区域生态修复方案和措施提供科学的依据。In view of this, the object of the present invention is to propose a method for monitoring dynamic fractures in well mining working faces, to accurately and completely obtain dynamic fractures and geometric information in the development process thereof, and to study soil fractures caused by regional surface fractures. The spatio-temporal evolution of physical and chemical properties provides a basis, and ultimately provides a scientific basis for ecological restoration programs and measures in this area.
为实现上述发明目的,本发明采用以下技术方案:In order to realize the above-mentioned purpose of the invention, the present invention adopts the following technical solutions:
一种井工开采工作面动态裂缝的监测方法,所述方法包括以下步骤:A method for monitoring dynamic fractures in an underground mining face, the method comprising the following steps:
(1)布设裂缝监测基准线:在采煤工作前,布设裂缝监测基准线,所述基准线由若干个地表移动观测站组成,所述观测站从开切眼处的后方沿工作面走向的中心线布设,基准线的两端应保证超出采动影响范围,并在布设后测定各观测站的空间坐标位置;(1) Lay out the fissure monitoring datum line: before the coal mining work, lay out the fissure monitoring datum line, the datum line is made up of several surface mobile observation stations, and the said observation station is from the rear of the cut hole along the working face. For center line layout, the two ends of the reference line should be guaranteed to be beyond the scope of influence of mining, and the spatial coordinate positions of each observation station should be measured after the layout;
(2)找出最前端裂缝:当工作面推进到第一位置为A时,对其前方新出现的疑似裂缝进行标记观测,找出这些疑似裂缝中随工作面的后续推进而发育的裂缝,这些发育的裂缝中与第一位置距离最大的裂缝即为最前端裂缝,测定最前端裂缝的第二位置为B,得到第二位置与第一位置之间的距离C;(2) Find the frontmost crack: when the working face advances to the first position A, mark and observe the new suspected cracks in front of it, and find out the cracks that develop with the subsequent advancement of the working face among these suspected cracks. Among these developed cracks, the crack with the largest distance from the first position is the front end crack, and the second position of the front end crack is measured as B, and the distance C between the second position and the first position is obtained;
(3)建立数学模型:重复步骤2得到多个工作面的第一位置Ai,以及与其相应的最前端裂缝的第二位置Bi和第一位置与第二位置的距离Ci,建立三者的数学模型,Bi=Ai+C’,其中C’为多个Ci的数学期望,i=1,2..n;(3) Establish a mathematical model: Repeat
(4)根据步骤3建立的数学模型,在距离工作面C’的位置,选定该位置两侧最相邻的多条裂缝作为观测裂缝,测定该多条裂缝随工作面推进的多个宽度变化,测定频率大于1天/次,直至裂缝不再发育,在地表上完全闭合为止,从中选出发育最为明显的一条裂缝作为最佳观测裂缝;(4) According to the mathematical model established in step 3, at the position C' from the working face, select the most adjacent multiple cracks on both sides of the position as observation cracks, and measure the multiple widths of the multiple cracks as the working face advances change, the measurement frequency is greater than 1 day/time, until the fracture no longer develops and is completely closed on the surface, and the most obvious fracture is selected as the best observation fracture;
(5)在不同的工作面位置,重复步骤4,得到多个最佳观测裂缝的宽度变化数据;(5) At different working face positions, repeat
(6)根据步骤4和5得到的最佳观测裂缝随工作面推进的多个宽度变化数据,绘制裂缝宽度关于工作面位置的变化趋势图。(6) According to the multiple width change data of the best observed cracks as the working face advances obtained in
优选地,根据开采沉陷学相关理论,所述基准线的布设遵循如下原则:在地表能达到充分采动的条件下,基准线通过移动盆地的平底部分即可;在地表不能达到充分采动的条件下,基准线需设在移动盆地的主断面上。Preferably, according to the relevant theory of mining subsidence, the layout of the baseline follows the following principles: under the condition that the surface can be fully mined, the baseline can pass through the flat bottom of the mobile basin; Under these conditions, the baseline should be set on the main section of the mobile basin.
优选地,在步骤1中,所述观测站间隔10-40米布设。Preferably, in
优选地,在观测裂缝宽度的同时,还观测裂缝的长度、深度和落差的变化。Preferably, while observing the width of the crack, changes in the length, depth and drop of the crack are also observed.
优选地,步骤4中观测裂缝宽度时,在裂缝两侧距离裂缝5-10cm处垂直于裂缝布设观测棒,测量裂缝初始宽度Lo,以及两端观测棒的距离Do,后期测量观测棒的距离Di,通过公式Li=Lo+(Di-Do)计算裂缝宽度Li,其中i=1,2..n。Preferably, when observing the width of the crack in
优选地,在每条裂缝上布设多个宽度测量点,宽度测量点之间的间距为3-5米。Preferably, multiple width measurement points are arranged on each crack, and the distance between the width measurement points is 3-5 meters.
优选地,每条裂缝的观测周期T>2B/V,其中B为工作面走向方向连续裂缝带的带宽,V为工作面日推进速度,观测工作直至地裂缝的地面表征消失、且持续无变化为止,其中T的单位为天,B的单位为米,V的单位为米/天。Preferably, the observation period of each fracture is T>2B/V, where B is the bandwidth of the continuous fracture zone in the strike direction of the working face, and V is the daily advancing speed of the working face. So far, the unit of T is day, the unit of B is meter, and the unit of V is meter/day.
优选地,步骤4和5中,根据公式计算出最大下沉速度滞后距L,其中,Ho代表采煤工作面的平均采深,为最大下沉速度滞后角,在工作面与观测裂缝之间的距离D<2L时,加大观测频率,当D>2L时,减小观测频率。Preferably, in
由上述技术方案可知,本发明提供的动态裂缝的监测方法构建了工作面和裂缝的空间参考体系;通过建立工作面最前端裂缝与工作面位置之间的数学模型,提供了裂缝特征的测量方法(观测方法、观测周期与频率),为任意工作面位置处最佳观测裂缝(观测对象)的准确选取提供了科学依据,并且通过测定包括地裂缝产生发育的最初阶段在内的裂缝几何信息,绘制了裂缝宽度关于工作面位置的变化趋势图,以便分析前端裂缝从产生到完全闭合此全过程中所经历的所有典型阶段的特征和时间节点信息,为裂缝生命周期的获取提供完整可靠的数据;进而为研究该区域煤炭开采对土地生态环境的影响机理及其自修复周期的研究提供时间基准和技术支撑。It can be seen from the above technical solution that the dynamic crack monitoring method provided by the present invention constructs the spatial reference system of the working face and cracks; by establishing a mathematical model between the frontmost crack of the working face and the position of the working face, a measurement method of crack characteristics is provided (observation method, observation period and frequency), providing a scientific basis for the accurate selection of the best observation fracture (observation object) at any working face position, and by measuring the fracture geometry information including the initial stage of ground fissure generation and development, The change trend diagram of the fracture width with respect to the position of the working face is drawn to analyze the characteristics and time node information of all typical stages experienced in the whole process from the creation to the complete closure of the front fracture, and provide complete and reliable data for the acquisition of the fracture life cycle ; and then provide a time benchmark and technical support for the study of the impact mechanism of coal mining on the land ecological environment and its self-repair cycle in this area.
附图说明 Description of drawings
图1为本发明中基准线和监测点的布设示意图;Fig. 1 is the layout schematic diagram of datum line and monitoring point among the present invention;
图2为本发明中裂缝宽度的观测示意图;Fig. 2 is the observation schematic diagram of crack width in the present invention;
图3为本发明的一个实施例中裂缝宽度随工作面推进的变化趋势图。Fig. 3 is a graph showing the variation trend of the crack width as the working face advances in one embodiment of the present invention.
具体实施方式 Detailed ways
下面以本发明所述方法在薄基岩风沙区工作面前端裂缝生命周期监测中的实际应用为例,对本发明进行详细说明。然而本领域技术人员应该认识到,本发明并不因此而受到任何限制。Hereinafter, the present invention will be described in detail by taking the practical application of the method of the present invention in the life cycle monitoring of front end cracks in the thin bedrock sandstorm area as an example. However, those skilled in the art should realize that the present invention is not limited thereby.
本发明所述方法包括以下步骤:The method of the present invention comprises the following steps:
第一步:布设裂缝监测基准线。Step 1: Lay out crack monitoring baselines.
所述基准线由若干个地表移动观测站组成,所述观测站从开切眼处的后方沿工作面走向的中心线布设,基准线的两端应保证超出采动影响范围,其布设工作应超前于采煤工作。优选地,所述基准线根据开采沉陷学相关理论,所述基准线的布设遵循如下原则:在地表能达到充分采动的条件下,基准线通过移动盆地的平底部分即可;在地表不能达到充分采动的条件下,基准线需设在移动盆地的主断面上。The reference line is composed of several mobile observation stations on the surface. The observation stations are arranged from the rear of the cutout along the center line of the working face. Ahead of coal mining work. Preferably, the reference line is based on the relevant theory of mining subsidence, and the layout of the reference line follows the following principles: under the condition that the surface can be fully mined, the reference line can pass through the flat bottom of the mobile basin; Under the condition of full mining, the baseline shall be set on the main section of the mobile basin.
如图1所示,其中1为开切眼位置,2为基准线,3为布设在基准线上的观测站。所述观测站间隔10-40米布设,并在布设后使用比如经纬仪导线和水准测量的方法测定观测站的空间坐标。As shown in Figure 1, 1 is the position of the incision, 2 is the baseline, and 3 is the observation station arranged on the baseline. The observation stations are laid out at intervals of 10-40 meters, and the spatial coordinates of the observation stations are determined by methods such as theodolite wire and leveling survey after the arrangement.
第二步:找出最前端裂缝。Step 2: Find the frontmost crack.
工作面最前端裂缝是裂缝发育全过程最好的监测对象,而在风沙区,地表可能被松散层所覆盖,导致工作面最前端裂缝的产生初期在地表的表征很微弱。此外,一些沙生植物的根系生长也可能导致地表的开裂,从而最前端裂缝的辨别带来很多干扰信息。故此,需要结合工作面开采的位置,采取措施找出最前端裂缝。The fracture at the front end of the working face is the best monitoring object for the whole process of fracture development, but in the windy and sandy area, the surface may be covered by loose layers, resulting in very weak indications on the surface at the initial stage of the fracture at the front end of the working face. In addition, the root growth of some psammophytes may also lead to cracks on the ground surface, so the identification of the front cracks brings a lot of interference information. Therefore, it is necessary to take measures to find out the most frontal cracks in combination with the mining position of the working face.
具体地,当工作面推进到第一位置为A时(工作面与开切眼之间的距离),对其前方新出现的疑似裂缝进行标记观测,利用其周边的地表移动观测站作为控制点,架设全站仪或者其它测量设备,根据现场情况,在一段合适的时间内(比如4-10天)观察这些疑似裂缝的发育情况,找出这些疑似裂缝中随工作面的后续推进而发育的裂缝(即长度或宽度会变化的裂缝),这些发育的裂缝中与第一位置A距离最大的裂缝即为最前端裂缝,测定最前端裂缝的第二位置位B,得到第二位置B与第一位置A之间的距离C。Specifically, when the working face advances to the first position A (the distance between the working face and the incision hole), the new suspected cracks in front of it are marked and observed, and the surrounding surface mobile observation stations are used as control points , set up a total station or other measuring equipment, observe the development of these suspected cracks within a suitable period of time (such as 4-10 days) according to the site conditions, and find out the development of these suspected cracks with the subsequent advancement of the working face. cracks (that is, cracks whose length or width can change), among these developed cracks, the crack with the largest distance from the first position A is the frontmost crack, and the second position B of the frontmost crack is measured, and the second position B and the first position A are obtained. A distance C between locations A.
第三步:建立数学模型。重复第二步的方法,得到多个工作面第一位置Ai,以及与其相应的最前端裂缝的第二位置Bi和第一位置Ai与第二位置Bi之间的距离Ci(i=1,2..n),利用最小二乘法建立三者的数学模型,Bi=Ai+C’,其中C’为多个Ci的数学期望,从而为下一步观测对象的选取及其最初状态的几何信息的获取奠定基础。The third step: establish a mathematical model. Repeat the method of the second step to obtain the first positions Ai of multiple working faces, as well as the second positions Bi of the corresponding front-end cracks and the distance Ci between the first positions Ai and the second positions Bi (i=1, 2 ..n), using the least square method to establish the mathematical model of the three, Bi=Ai+C', where C' is the mathematical expectation of multiple Ci, so as to provide the next step for the selection of the observation object and the geometric information of the initial state Get laid.
第四步:根据第三步建立的数学模型,在与当前工作面距离为C’的位置,选定该位置两侧最相邻的多条裂缝(比如4条裂缝)作为观测裂缝,可以利用全站仪以及邻近地表移动观测站标定其初始状态时的空间位置,并同时测定该多条裂缝随工作面推进的多个宽度变化,测定频率大于1天/次,直至裂缝不再发育,在地表上完全闭合为止,并从中选出发育最为明显的一条裂缝作为最佳观测裂缝。Step 4: According to the mathematical model established in the third step, at a position with a distance of C' from the current working face, select the most adjacent cracks (for example, 4 cracks) on both sides of the position as observation cracks, which can be used The total station and the adjacent surface mobile observation station calibrate the spatial position of its initial state, and simultaneously measure the multiple width changes of the multiple fractures as the working face advances. Until the surface is completely closed, the most obvious fracture is selected as the best observed fracture.
如图2所示,其中4为体表裂缝,5为观测棒,6为钢尺。裂缝宽度的变化情况可采用如下方法测量:As shown in Figure 2, 4 is a body surface crack, 5 is an observation rod, and 6 is a steel ruler. The change in crack width can be measured by the following methods:
在裂缝两侧距离裂缝5-10cm处垂直于裂缝布设观测棒,测出该处裂缝初始宽度Lo(可直接使用钢尺测量),以及两端观测棒的距离Do,后期只需测量观测棒的距离Di(i=1,2..n,为测量次数),通过公式Li=Lo+(Di-Do)计算出每次测量时的裂缝宽度Li。另外,由于裂缝较长,因此每条裂缝上可以设置多组观测棒,间隔3-5米设置,实际操作中,还可根据裂缝的发育情况及时加设观测棒。此外,观测棒应尽量垂直于地面,嵌入土中,埋深不少于20cm。Arrange observation rods perpendicular to the crack at a distance of 5-10cm on both sides of the crack, measure the initial width Lo of the crack at this place (can be directly measured with a steel ruler), and the distance Do between the observation rods at both ends, and only need to measure the distance of the observation rod in the later stage For the distance Di (i=1, 2..n, the number of measurements), the crack width Li for each measurement is calculated by the formula Li=Lo+(Di-Do). In addition, because the cracks are long, multiple groups of observation rods can be installed on each crack, with an interval of 3-5 meters. In actual operation, observation rods can also be added in time according to the development of cracks. In addition, the observation rod should be as vertical as possible to the ground, embedded in the soil, and the buried depth should not be less than 20cm.
其中,为尽量减少野外工作量,可以进一步利用经验公式确定观测的周期及频率。Among them, in order to minimize the workload in the field, empirical formulas can be further used to determine the observation period and frequency.
随着工作面的推进,对裂缝进行持续观测,根据盆地内走向方向连续裂缝带的宽度B,和工作面日推进速度V,优选地,每条裂缝的观测周期T>2B/V,观测工作直至地裂缝的地面表征消失、且持续无变化为止,其中T的单位为天,B的单位为米,V的单位为米/天。As the working face advances, continuous observation of fractures is carried out. According to the width B of the continuous fracture zone in the strike direction in the basin, and the daily advancing speed V of the working face, preferably, the observation period T>2B/V for each fracture, the observation work Until the surface representation of ground fissures disappears and remains unchanged, the unit of T is day, the unit of B is meter, and the unit of V is meter/day.
裂缝宽度的变化与地表活动剧烈程度有关,可以用地表下沉速度以及地表达到最大下沉速度时与工作面距离L(通常表述为最大下沉速度滞后距)反映,因此,优选地,应该与根据被观测的裂缝的位置与工作面位置之间的距离d与L的贴近程度调整观测频率,当裂缝宽度变化较大时,需要加大观测频率;当裂缝宽度变化较小时,减小观测频率。通常情况下,可以利用最大下沉速度滞后角根据公式计算出最大下沉速度滞后距L,其中,Ho代表采煤工作面的平均采深。根据先前布设的裂缝观测基准线上地表移动观测站在采动过程中高程的变化数据,即可计算出最大下沉速度以及进而得到L的大小。在工作面与观测对象二者之间的距离D<2L时,观测频率相对较大,尤其是在0.5L<D<1.5L时,应进行加密观测,当D>2L时,观测频率应相应减小。The change of fracture width is related to the intensity of surface activity, which can be reflected by the subsidence velocity of the surface and the distance L from the working face when the surface reaches the maximum subsidence velocity (usually expressed as the lag distance of the maximum subsidence velocity). Therefore, preferably, it should be compared with Adjust the observation frequency according to the closeness of the distance d and L between the position of the observed crack and the position of the working face. When the crack width changes greatly, the observation frequency needs to be increased; when the crack width changes small, the observation frequency should be reduced. . Normally, the maximum sinking velocity lag angle can be used According to the formula Calculate the maximum sinking velocity lag distance L, where Ho represents the average mining depth of the coal face. The maximum subsidence velocity and Then get the size of L. When the distance between the working face and the observation object is D<2L, the observation frequency is relatively high, especially when 0.5L<D<1.5L, intensive observation should be carried out; when D>2L, the observation frequency should be corresponding decrease.
为更好地获取裂缝的变化情况,优选地,在测定裂缝宽度变化的同时,还可以同时测量裂缝的长度和落差变化情况。例如,通过最近的观测站,用全站仪在裂缝的两端用导线测量的方法确定裂缝两端的坐标位置,并绘制到工作面的井上下对照图,利用两点坐标求的裂缝长度。In order to better obtain the change of the crack, preferably, while measuring the change of the crack width, the length of the crack and the change of the drop can also be measured simultaneously. For example, through the nearest observation station, use the total station to determine the coordinates of the two ends of the fracture by wire measurement, and draw the up-and-down comparison map of the working face, and use the two-point coordinates to calculate the fracture length.
第五步:为了更加全面地观测裂缝随工作面的推进的生长发育情况,重复第四步的方法,以便在不同的工作面位置,得到多个最佳观测裂缝的发育情况。Step 5: In order to more comprehensively observe the growth and development of fractures with the advancement of the working face, repeat the method of the fourth step, so as to obtain the development of multiple best observed fractures at different positions of the working face.
第六步:利用获取的裂缝的宽度信息绘制单条裂缝宽度信息的变化趋势图,分析各主要典型性阶段的持续时间和工作面推进量,通过多条裂缝的统计信息,总结该区域地表裂缝的完整的生命周期。Step 6: Use the obtained fracture width information to draw a trend chart of the width information of a single fracture, analyze the duration of each main typical stage and the advance amount of the working face, and summarize the surface fractures in this area through the statistical information of multiple fractures. complete life cycle.
实施例:针对某矿区的采动裂缝监测,使用上述方法获取的裂缝宽度信息绘制了裂缝宽度随工作面推进的趋势图,如图3所示,该裂缝上设有5个观测点,其中■代表1#、●代表2#、▲代表3#、代表4#和代表5#。Embodiment: For the monitoring of mining cracks in a certain mining area, the crack width information obtained by the above method is used to draw a trend diagram of the crack width advancing with the working face. As shown in Figure 3, there are 5 observation points on the crack, of which Represents 1#, ● represents 2#, ▲ represents 3#, Represents 4# and Represents 5#.
当前工作面距离开切眼的位置为454m时,该裂缝最早出现,超前工作面7m;工作面向前推进19m时,裂缝呈现出最大表征,其中5#信息采集点由3.3mm递增到25mm左右,变化速度约为1.158mm/m。该区域对应的为A1阶段,在此阶段内,#1、#2、#3、#4四个信息采集点的裂缝宽度均递增,属于裂缝发育阶段。When the front working face is 454m away from the cutting hole, the crack appears first, 7m ahead of the working face; when the working face advances 19m, the crack shows the largest sign, and the 5# information collection point increases from 3.3mm to about 25mm, The change speed is about 1.158mm/m. This area corresponds to the A1 stage. In this stage, the fracture widths of the four information
工作面继续向前推进42m时,5个信息采集点的宽度整体处于下降状态,在515m处信息采集点的宽度值趋于0,从地面表征上来看,裂缝整体也处于愈合状态。当工作面继续推进至565m时,裂缝基本无发育,对应的区域为图上的A2阶段;在裂缝发育的第一个半周期,从出现-发育-闭合及其稳定,工作面总计推进了约111m,此时工作面超前裂缝的位置为104m。When the working face continued to move forward for 42m, the width of the five information collection points decreased as a whole, and the width value of the information collection point tended to 0 at 515m. Judging from the ground representation, the cracks were also in a healing state as a whole. When the working face continues to advance to 565m, there is basically no fracture development, and the corresponding area is the A2 stage on the map; in the first half cycle of fracture development, from appearance-development-closure and stability, the working face has advanced about 111m, at this time the position of the leading crack in the working face is 104m.
当工作面继续向前推进至577m时,裂缝在先前位置重新裂开,5个信息采集点处裂缝的宽度均小于第一个阶段发育为最大值的情况,该阶段对应的A3区域,属于地表松动阶段,此时工作面超前裂缝116m。When the working face continued to advance to 577m, the fractures re-opened at the previous positions, and the widths of the fractures at the five information collection points were all smaller than the maximum value in the first stage. The A3 area corresponding to this stage belongs to the surface In the loosening stage, the working face is 116m ahead of the crack at this time.
从577m处直至613m处,裂缝宽度的变化很微弱,该阶段对应的为A4区域,定义为渐稳定阶段,此时工作面超前裂缝152m;后期裂缝逐渐趋于闭合状态,该阶段对应的A5区域,定义为完全愈合阶段,后续的观测结果显示,裂缝没有继续裂开的现象,此时工作面超前裂缝219m.各阶段,裂缝与工作面位置分别为:A1(-7m~12m);A2(12m~104m);A3(104m~116m);A4(116m~152m);A5(152m~219m),其中“-”代表工作面滞后于裂缝出现的位置。From 577m to 613m, the change of the fracture width is very weak. This stage corresponds to the A4 area, which is defined as the gradually stable stage. At this time, the working face is ahead of the fracture by 152m; in the later stage, the fracture gradually tends to close, and this stage corresponds to the A5 area. , which is defined as the complete healing stage. Follow-up observation results show that the cracks do not continue to crack. At this time, the working face is ahead of the cracks by 219m. At each stage, the positions of the cracks and the working face are: A1 (-7m ~ 12m); A2 ( 12m ~ 104m); A3 (104m ~ 116m); A4 (116m ~ 152m); A5 (152m ~ 219m), where "-" means that the working face lags behind the position where the crack appears.
从出现至完全闭合这个全过程,这个具有周期性变化情形的,称之为裂缝的生命周期。The whole process from emergence to complete closure, this periodic change is called the life cycle of cracks.
其它观测对象亦具有相似规律,因此可以将风沙区该工作面上方动态裂缝的生命周期划分为5个阶段:A1发育阶段(最初出现,由小到大);A2愈合阶段(由大变小,初次愈合);A3地表松动阶段(裂缝重新裂开,但较之发育阶段程度要小);A4渐稳定阶段(裂缝几乎不变化,处于稳定阶段);A5完全闭合阶段(裂缝再次愈合,不再张开)。Other observation objects also have similar rules, so the life cycle of dynamic fractures above the working face in the wind-sand area can be divided into five stages: A1 developmental stage (initial appearance, from small to large); A2 healing stage (from large to small, initial healing); A3 surface loosening stage (cracks re-open, but to a lesser extent than the development stage); A4 gradual stabilization stage (cracks hardly change, in a stable stage); A5 complete closure stage (cracks heal again, no longer open).
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CN103076437B (en) * | 2012-12-30 | 2014-10-01 | 中国矿业大学(北京) | Coal mining ground fissure moisture damage detection method taking space-time difference and rainfall impact into consideration |
CN105719342B (en) * | 2016-01-05 | 2018-10-02 | 首都师范大学 | A kind of the three-dimensional modeling method for visualizing and device of ground fissure geologic body |
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CN112288692B (en) * | 2020-10-16 | 2023-04-07 | 上海同禾工程科技股份有限公司 | Crack monitoring and management system and monitoring and management method |
CN113095643B (en) * | 2021-03-31 | 2022-05-13 | 内蒙古科技大学 | Multi-index comprehensive evaluation method for surface mining cracks of shallow coal seam |
CN113739661A (en) * | 2021-08-24 | 2021-12-03 | 同济大学 | Measuring scale and method for detecting surface cracks of component |
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