云南盈江浑水沟粘性泥石流浆体的理化特性

CORC > 成都山地灾害与环境研究所 > 中国科学院水利部成都山地灾害与环境研究所 > 成都山地所知识仓储（2009年以前）

	云南盈江浑水沟粘性泥石流浆体的理化特性
语种	中文
	王裕宜
	1981-12
页码	74-78
出版者	科学技术出版社重庆分社
出版地	重庆
关键词	理化特性泥石流浑水沟盈江云南
交替题名	Physical and chemical Properties of Viscuos Debris Flow Slurry in Hunshui Gully, Yingjiang, Yunnam
英文摘要	The volume weight of viscous debris flows in Hunshui Gully is 1.87-2.24 t/m3, of which the gravel with a size>2mm makes up 50.5%. The probabilistic accumulation curve shows that in the flow the particles are not screened, and the flow moves as a whole. Sodium montmorillonite predominates in the clay component of the flow. The salt content both in the water of the ordinary flow and in the cleared water of the debris flow is relatively high. Thus, the physical properties of the debris flow are of high dispersion expansion, and thixotropy. It is seen from the rheologic curve of the slurry comprising coarse grain with a size<1mm that this slurry is pseudo-Bingham fluid, which properties are controlled by its volume weight, free porosity ratio, grain composition and clay content. Laboratory experoments show that the viscosity of the slurry comprising fine grain with a size<0.1mm is varied with the difference in electrolyte concentration, ionic bond and pH value. All these affect the formation and movement of viscous debris flow in certain degree.
内容类型	专著章节文集论文
源URL	[http://ir.imde.ac.cn/handle/131551/26989]
专题	成都山地灾害与环境研究所_成都山地所知识仓储（2009年以前）
作者单位	中国科学院成都地理研究所
推荐引用方式 GB/T 7714	王裕宜. 云南盈江浑水沟粘性泥石流浆体的理化特性. 重庆:科学技术出版社重庆分社,1981:74-78.