岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2014年
10期
2769-2775
,共7页
唐巨鹏%杨森林%王亚林%吕家庆
唐巨鵬%楊森林%王亞林%呂傢慶
당거붕%양삼림%왕아림%려가경
煤与瓦斯突出%深部开采%地应力%瓦斯压力%突出强度
煤與瓦斯突齣%深部開採%地應力%瓦斯壓力%突齣彊度
매여와사돌출%심부개채%지응력%와사압력%돌출강도
coal and gas outbursts%deep mining%ground stress%gas pressure%outburst intensity
基于目前煤与瓦斯突出模拟试验均为人为控制突出口打开的实际情况,自主研制了可改变轴压、围压和孔隙压,实现突出口自行打开的煤与瓦斯突出模拟仪。以典型高瓦斯矿井-阜新孙家湾矿为例,试验模拟了煤层开采深度分别为900、1100、1300 m时,突出煤层临近工作面区域在地应力和瓦斯压力共同作用下诱导发生煤与瓦斯突出全过程。试验利用轴压、围压模拟地应力作用,孔隙压模拟瓦斯压力作用。经相似理论计算确定了3种开采深度下轴压和围压值、孔隙压逐级增加得到了突出时瓦斯压力,并拟合了关系曲线。研究结果表明:开采深度、轴压、围压、瓦斯压力与突出距离、突出强度间均呈幂指数增加规律。随深度增加,地应力与瓦斯压力对突出影响增量逐渐减小。瓦斯压力对突出影响作用存在3阶段特征,分别为急剧影响增加阶段、稳定影响增加阶段和缓慢影响增加阶段,确定了瓦斯压力对突出影响变化率最大值,即瓦斯压力变化异常区与稳定区分界点为0.75 MPa,对应开采深度为350 m,与前人理论分析结果基本吻合。由此可以推断,随深部开采,地应力与瓦斯压力共同作用下煤与瓦斯突出频度将增加,但强度和破坏程度增加率将趋于平缓。所得结论对该矿深部煤与瓦斯突出机制认识和预测防治具有参考意义。
基于目前煤與瓦斯突齣模擬試驗均為人為控製突齣口打開的實際情況,自主研製瞭可改變軸壓、圍壓和孔隙壓,實現突齣口自行打開的煤與瓦斯突齣模擬儀。以典型高瓦斯礦井-阜新孫傢灣礦為例,試驗模擬瞭煤層開採深度分彆為900、1100、1300 m時,突齣煤層臨近工作麵區域在地應力和瓦斯壓力共同作用下誘導髮生煤與瓦斯突齣全過程。試驗利用軸壓、圍壓模擬地應力作用,孔隙壓模擬瓦斯壓力作用。經相似理論計算確定瞭3種開採深度下軸壓和圍壓值、孔隙壓逐級增加得到瞭突齣時瓦斯壓力,併擬閤瞭關繫麯線。研究結果錶明:開採深度、軸壓、圍壓、瓦斯壓力與突齣距離、突齣彊度間均呈冪指數增加規律。隨深度增加,地應力與瓦斯壓力對突齣影響增量逐漸減小。瓦斯壓力對突齣影響作用存在3階段特徵,分彆為急劇影響增加階段、穩定影響增加階段和緩慢影響增加階段,確定瞭瓦斯壓力對突齣影響變化率最大值,即瓦斯壓力變化異常區與穩定區分界點為0.75 MPa,對應開採深度為350 m,與前人理論分析結果基本吻閤。由此可以推斷,隨深部開採,地應力與瓦斯壓力共同作用下煤與瓦斯突齣頻度將增加,但彊度和破壞程度增加率將趨于平緩。所得結論對該礦深部煤與瓦斯突齣機製認識和預測防治具有參攷意義。
기우목전매여와사돌출모의시험균위인위공제돌출구타개적실제정황,자주연제료가개변축압、위압화공극압,실현돌출구자행타개적매여와사돌출모의의。이전형고와사광정-부신손가만광위례,시험모의료매층개채심도분별위900、1100、1300 m시,돌출매층림근공작면구역재지응력화와사압력공동작용하유도발생매여와사돌출전과정。시험이용축압、위압모의지응력작용,공극압모의와사압력작용。경상사이론계산학정료3충개채심도하축압화위압치、공극압축급증가득도료돌출시와사압력,병의합료관계곡선。연구결과표명:개채심도、축압、위압、와사압력여돌출거리、돌출강도간균정멱지수증가규률。수심도증가,지응력여와사압력대돌출영향증량축점감소。와사압력대돌출영향작용존재3계단특정,분별위급극영향증가계단、은정영향증가계단화완만영향증가계단,학정료와사압력대돌출영향변화솔최대치,즉와사압력변화이상구여은정구분계점위0.75 MPa,대응개채심도위350 m,여전인이론분석결과기본문합。유차가이추단,수심부개채,지응력여와사압력공동작용하매여와사돌출빈도장증가,단강도화파배정도증가솔장추우평완。소득결론대해광심부매여와사돌출궤제인식화예측방치구유삼고의의。
Based on the practical situation that the opening of outburst mouth is man-made controlled in experiments of coal and gas outbursts, the simulation device of outburst is designed and developed which can change axial pressure, confining pressure and pore pressure. The outburst mouth can open by itself. Sunjiawan coal mine in Fuxin is a typical high gassy mine as example, the whole processes of outburst induced are simulated by experiments on conditions of joint action of stress and gas pressure near working face when mining depth is respectively 900 m, 1 100 m and 1 300 m. In experiments, axial pressure and confining pressure are used to simulate ground stress. And pore pressure is used to simulate gas pressure. According to similarity theory, axial pressure and confining pressure are determined in advance on condition of 900 m, 1 100 m and 1 300 m. With the step-by-step increment of pore pressure, the gas pressure of outburst is obtained. The relationship curves are presented. The results show that the relationship curves are all power exponent among mining depth, axial pressure, confining pressure, gas pressure and outburst distance, outburst intensity. With depths increasing, the influences of stress and gas pressure on the intensity increment of gas outburst are gradually decreased. The effect of the gas pressure on outburst presents three stages characteristics, dramatic stage, steady stage and slow stage of impact increasing. The gas pressure of 0.75 MPa is the threshold influenced on maximum rate of outburst. That is also cut-off point of gas pressure between abnormal and steady region, corresponding mining depth of 350 m, which is consistent with previous theoretical results. On the basis of analysis above, it can be presented that with deep mining, the frequency of coal and gas outbursts will increase on the joint action of stress and gas pressure. But the increment of impact strength and damage will decrease. The conclusions will have reference significance to mechanism, forecasting and prevention of gas outburst for Sunjiawan coal mine.