鄂尔多斯高原中部5.8～4.5 Cal kaBP气候旋回的地层记录

通过对鄂尔多斯高原现代风成砂与PJHZ剖面沉积物粒度特征的对比分析,确定了剖面中4个层位(290~210,190~160,153.5~123.5,50~40 cm)基本属于风成砂沉积。结合粒度参数、碳酸钙含量、总有机碳含量及年代序列,认为此区域在5.8~4.5 Cal kaBP存在以下沉积旋回:~5 749 Cal aBP,沉积风成砂,反映该时期风砂活动强烈,气候干燥,冬季风强盛;5 749 Cal aBP前后,沉积物为灰绿色湖相层,表明这一时期存在短暂的湖面扩展,沙漠退缩;5 749~5 370 Cal aBP,沉积风成砂,反映了湖泊的退缩和沙漠的扩展;5 370~4 895 Cal aBP,湖相沉积物,反映了流域降水量的增多;4 895~4 580 Cal aBP沉积风成砂后,4 580 Cal aBP前后又出现了短暂的湖相沉积,之后又是风砂沉积。     

Study on the Sedimentation Rule of the Particles in Debris Flow

In this paper, according to the study on a great number of experiments and data analyses, the sedimentation rule of solid particles in debris flow is set up. Three main factors that influence the particle sedimentation in debris flow were studied; the basic reasons to influence the particle sedimentation were analyzed. The particle sedimentation in debris flow could be divided into three stages,i, e. the starting stage, the quick sedimentation stage and the accumulation stage,and detailed analysis on the sedimentation process each stage was made. The liquid viscosity, particle quality and additional water pressure have an important role on the sedimentation rule of the particle in debris flow.     

平面二维数模研究闸下淤积的缺陷

以姚江大闸和武障河闸为例，对河口水域建闸后的闸下淤积的机理进行了研究。通过应用二维悬沙模型的模拟计算，分析了数学模型在模拟近闸段的淤积时存在的缺陷，对产生问题的原因进行了初步探讨。由于闸下淤积问题存在明显的时空性和区域性特征，应积极研究解决措施。     

Mesohabitat associations of the threatened San Marcos salamander (Eurycea nana) across its geographic range

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