设计了一套空气-活性炭的声发射信号检测装置,结合经典声发射理论与现代信息处理技术,对气固两相流过程中固相的质量流率、粒径以及碰撞速度等因素做细致分析。对4.00,2.80,1.18,085,0.43 mm 5种不同粒径的活性炭颗粒分别在不同质量流...设计了一套空气-活性炭的声发射信号检测装置,结合经典声发射理论与现代信息处理技术,对气固两相流过程中固相的质量流率、粒径以及碰撞速度等因素做细致分析。对4.00,2.80,1.18,085,0.43 mm 5种不同粒径的活性炭颗粒分别在不同质量流率、不同碰撞速度下的声发射信号进行采样,并采用功率谱估计算法对其进行分析。实验发现碰撞速度对信号的频率影响较小,但对信号的功率强度影响较大,此外,功率谱估计的频率、面积与固相颗粒的粒径、质量流率有很好相关性,拟合出二者的相关方程并通过试验验证,得到各参数的相对误差小于5.5%。因此,采用声发射测量技术与功率谱估计相结合的方法对于气固两项流相关参数的检测是可行有效的。展开更多
Granular mass flows （e.g., debris flows/avalanches） in landslide-prone areas are of great concern because they often cause catastrophic disasters as a result of their long run-out distances and large impact forces. ...Granular mass flows （e.g., debris flows/avalanches） in landslide-prone areas are of great concern because they often cause catastrophic disasters as a result of their long run-out distances and large impact forces. To investigate the factors influencing granular mass flow mobility, experimental tests were conducted in a flume model. Granular materials consisting of homogeneous sand and non- homogeneous sandy soil were used for studying particle size effects. Run-out tests with variable flow masses, water contents, and sloping channel confinement parameters were conducted as well. The results indicated that granular mass flow mobility was significantly influenced by the initial water content; a critical water content corresponding to the smallest flow mobility exists for different granular materials. An increase in the total flow mass generally induced a reduction in the travel angle （an increase in flow mobility）. Consistent with field observations, the travel angles for different granular materials decreased roughly in proportion to the logarithm of mass. The flume model tests illustrate that the measured travel angles increase as the proportion of fine particles increases. Interestingly, natural terrain possesses critical confinement characteristics for different granular mass flows.展开更多
文摘设计了一套空气-活性炭的声发射信号检测装置,结合经典声发射理论与现代信息处理技术,对气固两相流过程中固相的质量流率、粒径以及碰撞速度等因素做细致分析。对4.00,2.80,1.18,085,0.43 mm 5种不同粒径的活性炭颗粒分别在不同质量流率、不同碰撞速度下的声发射信号进行采样,并采用功率谱估计算法对其进行分析。实验发现碰撞速度对信号的频率影响较小,但对信号的功率强度影响较大,此外,功率谱估计的频率、面积与固相颗粒的粒径、质量流率有很好相关性,拟合出二者的相关方程并通过试验验证,得到各参数的相对误差小于5.5%。因此,采用声发射测量技术与功率谱估计相结合的方法对于气固两项流相关参数的检测是可行有效的。
基金financial support from the Science and Technology Service Network Initiative Program of the Chinese Academy of Sciences (grant no.KFJ-EW-STS-094-2)"Hundred Talents" Program of the Chinese Academy of Sciences (Sulijun)+2 种基金the National Natural Science Foundation of China (grant no.41201012, 51208218)the Hundred Young Talents Program of the Institute of Mountain Hazards and Environment (grant no.SDSQB-2013-01)the Chinese Academy of Sciences Visiting Professorship for Senior International Scientists (grant no.2012T1Z0042)
文摘Granular mass flows （e.g., debris flows/avalanches） in landslide-prone areas are of great concern because they often cause catastrophic disasters as a result of their long run-out distances and large impact forces. To investigate the factors influencing granular mass flow mobility, experimental tests were conducted in a flume model. Granular materials consisting of homogeneous sand and non- homogeneous sandy soil were used for studying particle size effects. Run-out tests with variable flow masses, water contents, and sloping channel confinement parameters were conducted as well. The results indicated that granular mass flow mobility was significantly influenced by the initial water content; a critical water content corresponding to the smallest flow mobility exists for different granular materials. An increase in the total flow mass generally induced a reduction in the travel angle （an increase in flow mobility）. Consistent with field observations, the travel angles for different granular materials decreased roughly in proportion to the logarithm of mass. The flume model tests illustrate that the measured travel angles increase as the proportion of fine particles increases. Interestingly, natural terrain possesses critical confinement characteristics for different granular mass flows.
