谋杀团的密度正增加的现象-它对斜坡运动方式的模糊依赖的结果

B. Stepanov, R. K. Yafyazova
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摘要

泥石流各局部体积的特征根据其运动路径(坡度、河道宽度和粗糙度)、泥石流形成过程中所涉及的泥沙、碎屑的粒度和矿物学组成、泥石流体的密度、粘度和塑性等特征而不断变化。迄今为止,人们认为泥石流质量密度与泥石流路径的坡度有明确的关系。在哈萨克斯坦水文气象研究所(KazNIGMI)进行的实验和理论研究发现,泥石流过程的过程取决于泥石流质量的密度。从泥石流路径坡度中识别出泥石流质量密度的模糊性,发现了一种自然现象:当泥石流路径坡度超过临界值时,泥石流质量密度会发生突变(Stepanov效应)。考虑泥石流路径坡度对泥石流质量密度的模糊性是计算泥石流特征的关键因素。
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THE PHENOMENON OF AN EPOSITIVE INCREASE IN THE DENSITY OF THE MURDER MASS – THE CONSEQUENCE OF ITS AMBIGUOUS DEPENDENCE ON THE SLOPE WAYS OF MOVEMENT
The characteristics of each local volume of debris flow are continuously changing depending on the characteristics: a path of its movement (slope, width and roughness of channel), dis-charge, granulometric and mineralogical compositions of debris involved in debris-flow-formation, density, viscosity and plasticity of debris-flow mass, etc. Up to now, it believes that the debris-flow mass density depends unambiguously on the slope of path of a debris-flow. As a result of experimental and theoretical studies carried out at the Kazakh Research Hydrometeorological Institute (KazNIGMI), it was found that the course of the debris-flow process depends on the density of debris-flow mass. Identification of the ambiguity of the debris-flow mass density from the slope of the debris flow path led to the discovery of a nat-ural phenomenon: an abrupt change of the density of debris-flow mass when the critical val-ue of the slope of the debris flow path is exceeded (the Stepanov’s effect). Taking into ac-count the ambiguity of the debris-flow mass density from the slope of the debris flow path is a key element in computing debris flow characteristics.
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