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泥石流、冰碛和河湖沉积物的粒度特征及判别 被引量:19

PRELIMILARY EXPLORATION ON GRAIN CHARACTERISTIC AND DISCRIMINATION OF DEBRIS FLOW DEPOSIT , MORAINE AND RIVER & LAKE DEPOSIT
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摘要 根据福克(Folk)公式,计算出几个典型地区泥石流、冰碛和河湖沉积物的粒度特征参数,用核心区域图解法和判别分析方法认识和分析参数的分布特征和联系,初步建立判别的图形模型和数学模型,用以反推和判别参数反映的沉积类型和沉积环境。 Few research results on how to deduce and determine the corresponding deposit types and enviromments of sediment are satisfied though much research work has been done due to their monotonous and unintelligible qualitative methods.In accordance with the grain characteristic parameters of debris flow deposit,moraine and river_lake deposit in four typical regions,which are obtained with Folk formula,this article analyzes the distributing characteristics and the relationships between these parameters by means of core_area graphic method and discriminatory_analytical method,then,a prelimilary discriminatory model of graph has been established as the following. 1.the discriminatory model of graph is “Fig 2;the relationbetween the parameters of grain characteristics” and“ Table 1 the analytical result of the three deposits′ parmeters”,respectively. 2.the discriminatory equations for the deposits of deris flow(df),moraine(mr),and river_lake(rl)are: Y( df:mr )=0.86486Mz-0.70819Q-5.01804S k+0.01084K Y<-2.6415,for df;Y>-2.6415, for mr Y( df:rl )=0.71345Mz-4.04274Q+0.18417S k-0.52035K Y<-11.8405, for df ;Y>-11.8405, for rl Y( mr:rl )=-0.07021Mz-7.6609Q+0.09191S k-1.98192K Y<-23.4333, for mr ;Y>-23.4333, for rl Using the model,one can confer to deduce and determine the corresponding deposit types and environments of sediment.
出处 《山地学报》 CSCD 1999年第1期50-54,共5页 Mountain Research
基金 成都理工学院地质灾害专业实验室基金
关键词 粒度特征 泥石流 冰碛 河流 湖泊 沉积物 Grain characteristic, core _area graph, discriminatory_analysis
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参考文献7

  • 1陈怀录 韩敏.武都地经石流粒度分析及其特征[M].成都:四川科学技术出版社,1986.146.
  • 2中国科学院南京地理所 等.云南断陷湖泊与沉积 滇池、洱海、扶仙湖[M].北京:科学出版社,1989.295-296.
  • 3张超 杨秉赓.计量地理学基础(第2版)[M].北京:高等教育出版社,1993.138,144.
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  • 7成都地质学院陕北队,沉积岩(物)粒度分析及其应用,1978年

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