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贺西煤矿巷道围岩地质力学测量与分析 被引量:4
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作者 闫永林 《煤炭技术》 CAS 北大核心 2021年第9期76-79,共4页
采用自主研制的水压致裂地质力学测试成套装置,在贺西煤矿进行了地应力、煤岩体强度及结构井下现场测量。结果表明,矿井四采区为高应力区,三采区为中等水平应力区,形成以构造应力为主的地应力场,水平主应力方向为N42.5°E~N69.6... 采用自主研制的水压致裂地质力学测试成套装置,在贺西煤矿进行了地应力、煤岩体强度及结构井下现场测量。结果表明,矿井四采区为高应力区,三采区为中等水平应力区,形成以构造应力为主的地应力场,水平主应力方向为N42.5°E~N69.6°E,巷道应加强右顶底角部位的支护强度;巷道顶板锚杆锚索控制区域由泥质砂岩和细砂岩组成,其单轴抗压强度均值分别为44.34 MPa和50.68 MPa,巷道围岩内部无薄弱结构面,围岩强度保持平稳;锚杆锚索支护范围岩层整体完整无明显弱层,巷道适宜采用树脂锚杆锚索进行支护。测试结果为贺西煤矿锚杆支护等采矿工程参数设计提供了基础数据。 展开更多
关键词 地质力学测量 地应力 强度 结构 巷道支护
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Equivalent materials simulation experimental study on bed separations developing and mining subsidence in constant humidity and constant temperature conditions
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作者 付志亮 王素华 高延法 《Journal of Coal Science & Engineering(China)》 2008年第4期585-590,共6页
A new experiment was made on the developing of bed separations and mining subsidence from Tangshan T2192 working face by equivalent materials simulation.The overburden deformation and the developing of bed separations... A new experiment was made on the developing of bed separations and mining subsidence from Tangshan T2192 working face by equivalent materials simulation.The overburden deformation and the developing of bed separations with working face advanc- ing was simulated by a new model.The results show that the maximum value of bed separations moved forward gradually along with the working face advancing;the maxi- mum value of bed separations is 0.31~0.50 times of mining thickness.The key strata have a great influence upon surface subsidence during the overburden movement process.The mechanics parameters of new experiment are fitted with results in fields perfectly. 展开更多
关键词 SUBSIDENCE bed separations constant humidity constant temperature equivalent simulation experiment
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Application of superconductive gravity technique on the constraints of core-mantle coupling parameters 被引量:2
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作者 CUI XiaoMing SUN HePing +1 位作者 XU JianQiao ZHOU JiangCun 《Science China Earth Sciences》 SCIE EI CAS 2012年第3期513-520,共8页
The parameters, i.e. the Period and the Quality factor, of the Earth's free core nutation (FCN) are closely related to the dissipative coupling between the core and the mantle. Based on the FCN parameters obtained... The parameters, i.e. the Period and the Quality factor, of the Earth's free core nutation (FCN) are closely related to the dissipative coupling between the core and the mantle. Based on the FCN parameters obtained from the actual observations and theoretical simulation, significantly constrained in this study were several key parameters near the core-mantle boundary (CMB), related to the core and mantle coupling, including viscosity at the top of liquid core, conductivity at the bottom of the mantle, and dynamic ellipticity of the CMB. In order to choose high quality observations from global stations of the superconducting gravimeters (SG) on the Global Geodynamics Project (GGP) network, we adopted two criteria, the standard deviations of harmonic analysis on tidal observations and the quality of the FCN parameters calculated with the observations from single station. After the mean ocean tidal effects of the recent ocean tidal models were removed, the FCN parameters were retrieved by stacking the tidal gravity observations from the GGP network. The results were in a good agreement with those in the recent research by using the SG and/or the VLBI observations. Combined with an FCN theoretical model deduced by angular momentum method, the viscous and electromagnetic coupling parameters near the CMB were evaluated. Numerical results indicated that the viscosity at the top of the liquid core was in the range from 6.6×102 to 2.6×103 Pa·s, which was in good agreement with those obtained from the Earth's nutation, the FCN and variations in the length of day (LOD). The conductivity at the bottom of the mantle should be as large as 2.6×106-1.0×107 S m-1 to match the FCN quality factors from the actual observations. The dissipative coupling had a little influence of 1-2 sidereal days for the FCN period. 展开更多
关键词 SG observations free core nutation core-mantle boundary viscosity CONDUCTIVITY dynamic ellipticity
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