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黄金科学技术 ›› 2021, Vol. 29 ›› Issue (6): 843-853.doi: 10.11872/j.issn.1005-2518.2021.06.057

• 采选技术与矿山管理 • 上一篇    下一篇

基于空隙量守恒的覆岩裂隙带发育高度模型

黄丹1,2,3(),陈何1,3,郑志杰1,3   

  1. 1.矿冶科技集团有限公司,北京 100160
    2.中南大学资源与安全工程学院,湖南 长沙 410083
    3.国家金属矿绿色开采国际联合研究中心,北京 102628
  • 收稿日期:2021-05-17 修回日期:2021-11-07 出版日期:2021-12-31 发布日期:2022-03-07
  • 作者简介:黄丹(1987-),男,河北衡水人,博士,高级工程师,从事矿山采矿技术研究工作。huangdan@bgrimm.com
  • 基金资助:
    国家重点研发计划重点专项“煤与共伴生战略性金属矿产协调开采成套方法”(2021YFC2902102);国家重点研发计划政府间国际科技创新合作重点专项“地下金属矿规模化绿色开采关键技术合作研究”(2018YFE0123000)

Model of the Height of Overburden Fracture Zone Based on Void Conservation

Dan HUANG1,2,3(),He CHEN1,3,Zhijie ZHENG1,3   

  1. 1.BGRIMM Technology Group, Beijing 100160, China
    2.School of Resources and Safety Engineering, Central South University, Changsha 410083, Hunan, China
    3.National Center for International Joint Research on Green Metal Mining, Beijing 102628, China
  • Received:2021-05-17 Revised:2021-11-07 Online:2021-12-31 Published:2022-03-07

摘要:

预测与控制矿体开采覆岩裂隙带发育高度,是沉积型层系矿体上行开采与保水开采的关键。基于空隙量守恒理论,分析了上覆岩层随采动空隙扩散的岩移规律,以矿体采高、覆岩碎胀系数、裂隙带残余空隙率、顶板垮落和放顶高度为主控因素,建立了预测覆岩裂隙带发育高度的裂隙拱模型H1=fH,k,ε1,h。结合山西某煤下铝土矿采区上行开采的技术条件与采矿方案,开展了相似模拟试验,分析了覆岩空隙扩散规律。同时,在煤下铝土矿开采裂隙带高度模型的基础上,分析了采高、放顶高度与裂隙带高度之间的关系,提出了确定煤下铝土矿采高与放顶高度的方法。通过数值模拟和“三带”理论验证了基于空隙率守恒的裂隙带高度预测模型的有效性和煤下铝土矿开采技术方案的可行性。本文提出的覆岩裂隙带高度模型为预测裂隙带高度与制定覆岩移动控制方案提供了新方法和有益借鉴。

关键词: 空隙量守恒, 数值模拟, 裂隙带高度, 空隙率, 放顶高度, 煤下铝土矿

Abstract:

Prediction and control of the development height of overburden fracture zone in ore-mining is the key of upward mining and water-retaining mining for sedimentary stratum series.When mining in layered strata,the process of caving zone and fractured zone of overlying strata movement tending to bending subsidence zone can be regarded as the result of the diffusion of voids in goaf from bottom to top.When the seam mining span is small,fractures in the overburden arched upward,and formed “fracture arch”. As the voids in the fracture arch continue to spread upwards,when the rock voidage in the fractured arch reaches the residual dilatancy coefficient under the action of rock pressure compound extrusion,the stress equilibrium state is formed between the mining affected area and the outer rock strata. At this time,the fracture arch no longer rise upward. Increasing the mining span of the seam will break the form of fracture arch and make the range of fracture arch to fracture zone. The highest arch height of the fracture arch the same as the height of the fracture zone. Above the height range of the fracture arch is the bending subsidence zone.Based on the theory of void conservation in this paper,the strata movement rule of overlying strata with mining void diffusion was analyzed. By analyzing the limiting geometry condition of fractured arch developing upward with mining-induced voids,while taking mining height,expansion coefficient of overburden rock,residual voidage,height of roof caving as main control factors,the fissure arch model for predicting development height of overburden fracture zone was established H1=fH,k,ε1,h. Combined with the technical condition and upward mining method of a bauxite ore under coal seams in Shanxi,the similar simulation test was carried out to study and analyze the diffusion rule of overlying rock voids.When the movement range of overburden grows to the integral sinking horizon with excavation steps,increasing the stope width leads to the development of fracture zone from arch to inverted trapezoid or saddle shape.The movement zone in the overburden gradually develops upward to the integral sinking horizon,which is characterized by bending subsidence zone.The bauxite dilatancy coefficient of alu-minum strata under coal is about 10%.Based on the height model of fracture zone in under-coal bauxite mining,the relationship among mining height,caving height and fracture zone height was analyzed.When the distance between coal and bauxite is 32.0 m and the mining height of bauxite is 3.0 m,the caving height is 4.0 m. A method for determining the mining height and caving height of under-coal bauxite ore was proposed. Through numerical simulation and “three zone theory” analysis,the effectiveness of fracture zone height prediction model based on void conservation and the feasibility of mining method for under-coal bauxite ore were proved. The prediction model proposed in this paper provides a new method and a useful reference for predicting the height of overburden fracture zone and making the control scheme of overlying rock movement.

Key words: void conservation, numerical simulation, fracture zone height, voidage, roof caving height, under-coal bauxite

中图分类号: 

  • TD325

图1

覆岩内空隙扩散岩移结构示意图"

图2

裂隙拱剖面简化为三角形示意图"

图3

垮落体边界与水平面夹角α的最小值"

表1

煤下铝土矿研究区地层和地质条件"

统(群)地层代号岩性描述
古生界二叠系下统下石盒子组P1x

上部为灰黄色石英砂岩、黄绿色砂质页岩和紫红色泥岩;

下部为黄绿色石英砂岩及黄绿、灰绿色砂质泥岩

山西组P1s灰白色石英砂岩和灰色砂质泥岩,中夹煤层
石炭系上统太原组C3t

底部为厚约12 m的灰白、白色厚层中粗粒含砾砂岩、砂质粘土岩,中部夹煤层,

厚度约10 m,上部由细砂岩、黑色泥岩、炭质泥岩、砂质泥岩和煤层组成

中统本溪组C2b

二段底部为细砂岩和砂质粘土岩,向上依次为杂色粘土岩、砂质粘土岩、

薄层细砂岩和黑色泥岩,顶部局部夹1~2层不稳定的生物碎屑灰岩;

一段为山西式铁矿、铝土矿和硬质耐火粘土矿的赋存层位

奥陶系中统峰峰组O2 f泥灰岩、泥质白云岩及角砾状泥灰岩
上马家沟组O2s顶部为灰岩,中下部为泥灰岩、白云质灰岩、豹皮状灰岩和角砾状灰岩

图4

相似模拟试验及覆岩移动范围示意图"

图5

覆岩移动范围面积随开采时间的变化"

图6

覆岩移动范围高度随开采时间的变化"

图7

覆岩移动范围内空隙率随开采时间的变化"

图8

煤下铝土矿开采裂隙带高度、采高及放顶高度的关系图"

图9

煤下铝土矿开采数值模型(a)与回采顺序(b)"

图10

房柱法开采后不处理空区与放顶处理空区的覆岩移动数值模拟结果比较(走向Y=150剖面)"

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