摘要
在分析厚松散层薄基岩下开采水砂突涌工程地质模式的基础上,设计自制了水砂混合流运移及突涌模型。试验以0.05 MPa和0.10 MPa水压力条件下的不同水砂混合物成分、不同通道裂缝宽度为例,揭示了孔隙水压力在裂缝通道中不同位置的变化特征。通过设置的模型试验,定量化地研究水砂混合物运移及涌出的多种地质信息,获得不同模型试验水砂混合流运移通道中不同位置监测的水压力变化曲线,同时分析裂缝通道水砂流速度与通道宽度的关系,观测水砂流通道溢出口出砂量与时间的变化关系。
Based on the engineering geological modes of quicksand inrush induced by coal mining under the thin bedrock and thick unconsolidated formations,a test model of the mixed water and sand flow transfer and inrush was designed.The variation characteristics of water pressure in different position of the fissure channel were revealed by considering the various compositions of the flow and variations of the width of the fractured channel under the water pressure of 0.05 MPa and 0.10 MPa.Geological information of the mixed water and sand flow transfer for the various compositions of the flow,water pressure and the channel feature was quantitatively studied.The water pressure variation curves in the different positions were gained from different model tests.The relations between the channel width and the velocity of the mixed water and sand flow in the fractured channel were analyzed.The relationship between time and sand production volume of the mixed water and sand flow channel overflows was obtained from observational results.
出处
《煤炭学报》
EI
CAS
CSCD
北大核心
2012年第1期141-146,共6页
Journal of China Coal Society
基金
国家自然科学基金青年科学基金资助项目(40802076)
中国博士后科学基金面上资助项目(20110491476)
江苏高校优势学科建设工程资助项目
关键词
薄基岩
裂缝通道
水砂流
模型试验
thin bedrock
fissure channel
mixed water and sand flow
model test