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[黄土高原小流域淤地坝泥沙颗粒粒径剖面分布]

[Profile distribution of sediment particle sizes at a check dam in a small watershed of Loess Plateau].

作者信息

Wang Ya-Feng, Fu Bo-Jie, Chen Li-Ding, Lü Yi-He, Wang De, Song Cheng-Jun

机构信息

State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2009 Oct;20(10):2461-7.

Abstract

Sediment gyration sampling was conducted in June 2006 to analyze the profile distribution of sediment particle sizes at a check-dam built in 1954 in a typical small watershed of hilly and gully Loess plateau. There were at least 28 layers of sediment gyration at the check-dam, with the layer depth varied from 2 cm to 60 cm. In the sediment profile, silt (0.05-0.002 mm) occupied > 60%, its particle size being mainly within the range of 0.01-0.05 mm, while coarse sand (> 0.05 mm) accounted for 23.09%. The variation degree of sediment particle sizes increased with increasing depth, and an abrupt change was observed at the depth 2 m. Both longitudinal gradient and hydrodynamic condition caused the variation of sediment particle sizes. There was an accumulated plough layer of 72 cm thickness in the profile, which had indicative role for the sediment erosion environment of check dam.

摘要

2006年6月进行了沉积物旋转采样,以分析黄土高原丘陵沟壑区典型小流域内一座建于1954年的淤地坝沉积物粒径的剖面分布。该淤地坝沉积物旋转至少有28层,层深从2厘米到60厘米不等。在沉积物剖面中,粉砂(0.05 - 0.002毫米)占比> 60%,其粒径主要在0.01 - 0.05毫米范围内,而粗砂(> 0.05毫米)占23.09%。沉积物粒径的变化程度随深度增加而增大,在2米深度处观察到突变。纵向坡度和水动力条件均导致沉积物粒径变化。剖面中有一层厚度为72厘米的累积犁底层,对淤地坝的沉积物侵蚀环境具有指示作用。

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