冲击载荷下含瓦斯煤动力学破坏特征与瓦斯渗流规律分析

为探究不同冲击载荷和瓦斯压力作用下的含瓦斯煤动力学特征、裂隙扩展及瓦斯渗流变化规律,采用含瓦斯煤岩冲击损伤-渗流试验系统开展含瓦斯煤冲击试验以及原位渗流测试,并结合工业CT扫描系统进行试样裂隙结构的三维重构,分析含瓦斯煤内部裂隙扩展特征及其对瓦斯渗流的影响规律。研究结果表明,冲击载荷和瓦斯压力对含瓦斯煤的动力学性质、变形过程、裂隙扩展和渗流规律均具有重要影响,具体表现在:①受围压和轴压的影响,冲击载荷耦合瓦斯压力条件下的含瓦斯煤应力-应变曲线无明显压密阶段;含瓦斯煤的变形过程主要经历了弹性变形阶段、应变强化阶段及破坏阶段。②冲击载荷的增加对含瓦斯煤动力学参数具有强化作用,气体压力的升高则劣化了含瓦斯煤动力学参数;冲击载荷越大,瓦斯压力越高,含瓦斯煤的裂隙扩展愈充分,所形成的裂隙结构愈复杂。③含瓦斯煤的渗流规律受控于裂隙扩展,冲击载荷耦合瓦斯压力作用下,含瓦斯煤中存在孔隙流动、孔隙流动-裂隙流动并存及裂隙流动等3种气体流动形式;含瓦斯煤冲击破坏后,随着气体压力增加以及气楔作用的增强,瓦斯流动形式可由孔隙流动依次转变为孔隙流动-裂隙流动并存和裂隙流动;裂隙扩展和流动形式共同影响含瓦斯煤渗流规律,含瓦斯煤渗透率随瓦斯压力的增大总体上符合先增大后减小的变化趋势。

计算煤层透气系数的新方法

煤层透气系数是研究煤层瓦斯动力学的重要参数之一.本文提出计算煤层透气系数的简捷、准确的新方法.

An integrated approach to study of strata behaviour and gas flow dynamics and its application

This paper presents an advanced and integrated research approach to longwall mining-induced strata move- ment, stress changes, fractures, and gas flow dynamics with actual examples of its application from recent studies for coextraction of coal and methane development at Huainan Mining Group in China, in a deep and multi-seam mining environment. The advanced approach takes advantage of the latest techniques in Australia for mine scale geotechnical characterisation, field measurement, monitoring and numerical modelling. Key techniques described in this paper include coal mine site 3D geotechnical characterisation methods, surface deep downhole multi-point extensometers and piezometers for overburden displacement and pore pressure measurements during mining, tracer gas tests for goal gas flow patterns, and advanced numerical modelling codes for coupled coal mine strata, water and gas simulations, and longwall goaf gas ttow investigations. This integrated approach has resulted in significant insights into the complex dynamic imeraction between strata, groundwater, and gas during mining at Huainan Mining Group in recent years. Based on the lindings from the extensive field monitoring and numerical modelling studies, a three-dimensional annular-shaped over-lying zone along the perimeter of the longwall panel was identified for optimal methane drainage during mining.

Application of Discrete Lumped Kinetic Modeling on Vacuum Gas Oil Hydrocracking

The kinetic model of vacuum gas oil （VGO） hydrocracking based on discrete lumped approach was investigated, and some improvement was put forward at the same time in this article. A parallel reaction scheme to describe the conver- sion of VGO into products （gases, gasoline, and diesel） proposed by Orochko was used. The different experimental data were analyzed statistically and then the product distribution and kinetic parameters were simulated by available data. Fur- thermore, the kinetic parameters were correlated based on the feed property, reaction temperature, and catalyst activity. An optimization code in Matlab 2011b was written to fine-me these parameters. The model had a favorable ability to predict the product distribution and there was a good agreement between the model predictions and experiment data. Hence, the ki- netic parameters indeed had something to do with feed properties, reaction temperature and catalyst activity.

Kinetic characteristics of coal gas desorption based on the pulsating injection

In order to understand the kinetic characteristics of coal gas desorption based on the pulsating injection （PI）, the research experimentally studied the kinetic process of methane desorption in terms of the PI and hydrostatic injection （HI）. The results show that the kinetic curves of methane desorption based on PI and HI are consistent with each other, and the diffusion model can best describe the characteristics of meth- ane desorption. Initial velocity, diffusion capacity and ultimate desorption amount of methane desorption after P! are greater than those after HI, and the ultimate desorption amount increases by 16.7-39.7%. Methane decay rate over the time is less than that of the HI. The PI influences the diffusion model param- eters, and it makes the mass transfer Biot number B＇_i decrease and the mass transfer Fourier series F＇_0 increase. As a result, PI makes the methane diffusion resistance in the coal smaller, methane diffusion rate greater, mass transfer velocity faster and the disturbance range of methane concentration wider than HI. Therefore, the effect of methane desorption based on PI is better than that of HI.

DYNAMICS OF GAS SEEPAGE AND ITS APPLICATIONS

Dynamics of gas seepage as a borderline subject of geosciences mainly studies the flow and distribution of gas in coalseams or gas-bearing strata. In this paper new dynamic models for coal gas flow are developed.Using in-situ measured parameters of coal gas dynamics, the new models are tested with three existing dynamic models in the world. The results show that the new models approach the reality more cIose than the other three models.In addition, the other relations or indices helped to evaluate gas flow in coalseam are proposed.

Geological division of gas in the Pingdingshan mine area based on its tectonic dynamics characteristics

In this paper,we used tectonic dynamics theories to study the tectonic evolution characteristics of the Pingdingshan mine area,and analyzed the impact of tectonic progressive control on gas occurrence.The study results are as follows:the Pingdingshan mine area has been mainly controlled by multiple squeezing and shearing actions of the Qinling orogenic belt since early and middle Yanshan,forming the tectonic control characteristics of master control in two directions,namely NWW trending and NNE trending;the NWW trending structure is dominated by squeezing and shearing,while the NNE trending structure is dominated by tension.Progressively controlled by the structure,the gas occurrence presents partition and zonation,i.e.compared with the western structure,the eastern NWW-NW trending structure of the mine area is more highly developed,resulting in the mine area gas occurrence distribution characteristics are distinct in the east while indistinct in the west.Based on this,the mine area can be divided into the following two geological dynamic areas:the western half of mine area,namely the Guodishan fault control area,where the NW-SE trending synchronous tension action suffered by the northeast side(footwall) is relatively strong,and compared with the southwest side(hanging wall),its coal and gas outburst seriousness is weak;and the eastern half of mine area,namely the NWW-NW thrust nappe fracture fold control area,which is a serious area of coal and gas outburst,in particular the axial area of the Likou syncline is the intersection compound and combination position of the NW and NE trending structures,a tectonic concentrated area,and the gas pressure and content here are the largest.