检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:魏勇[1,2] 许开立[3] 熊琳[1] 李梦[1] WEI Yong XU Kaili XIONG Lin LI Meng(School of Environment and Resource, Southwest University of Science and Technology, Mianyang Sichuan 621010,China Key Laboratory of Solid Waste Treatment and Resource Recycle, Ministry of Education, Mianyang 621010, China School of Resources & Civil Engineering, Northeastern University, Shenyang Liaoning 110819, China)
机构地区:[1]西南科技大学环境与资源学院,四川绵阳621010 [2]固体废物处理与资源化省部共建教育部重点实验室,四川绵阳621010 [3]东北大学资源与土木工程学院
出 处:《中国安全科学学报》2017年第4期122-126,共5页China Safety Science Journal
基 金:国家自然科学基金资助(51004014);四川省安全监管局(四川煤监局)安全生产科技项目(scaqjgjc_stp_20150011)
摘 要:为提高尾矿库区下游的防灾减灾能力,以北京首云铁矿和尚峪尾矿库为例,开展物理模型试验研究,探究砂流体积分数、溃口形态及下游坡度对溃坝砂流流动特性及规律的影响。试验结果表明,随着溃坝砂流体积分数的增大,砂流到达堆积深度峰值时间越长,峰值就越大;随着溃坝口门的增大,砂流到达堆积深度峰值时间越短,峰值越大,溃口就越大,砂流在下游演进运动的范围就越广,砂流覆盖面积也越大;随着库区下游坡度的增大,砂流到达堆积深度峰值时间越短,峰值越小,下游坡度对砂流演进运动过程及覆盖面积影响也较小。In order to improve the ability of disaster prevention and reduction in tailings reservoir downstraeam, taking Beijing Heshangyu tailing reservoir as an example, physical model experiments were carried out to explore effects of dam-break flow's volume fractions, collapse forms and downstream slopes on flow charateristics and regularity of tailing dam-break flow . The experimental results show that with in- creasing of tailing flow volume fraction, the time that tailing dam-break flow reaches accumulation depth peak is longer and accumulation depth peak is greater. With increasing of collapse gate, the time that tailing dam-break flow reaches accumulation depth peak is shorter and accumulation depth peak is greater. The larger collapse gate of tailing dam-break is, the more widely tailing flow moves in the downstream and the greater coverage area of tailing flow is.With increasing of downstream slope, the time that tailing dambreak flow reaches accumulation depth peak is shorter and accumulation depth peak is smaller.Downstream slope has only a fairly weak effect on the movement process and coverage area of tailing dambreak flow.
关 键 词:溃坝砂流 流动特性 砂流浓度 溃口形态 下游坡度
分 类 号:X928.03[环境科学与工程—安全科学]
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.3