期刊文献+

宁夏平罗盐碱地排水渠道抗冲性野外水槽试验 被引量:4

The Field Flume Experiment of Drainage Channel Erosion Resistance in the Pingluo Saline Land of Ningxia
下载PDF
导出
摘要 采用水槽试验的方法来分析宁夏平罗西大滩地区分别以白僵土、沙土所铺设成的排水渠道的稳定性。结果表明,用白僵土铺成的渠道有很强的抗冲性,白僵土的侵蚀及渠道的冲淤变化,主要归因于反复对白僵土的浸润湿化与脱水干燥;沙土粘性小,抗冲性弱,用沙土铺成的渠道在水流作用下纵向横向变形都很大,随着试验的进行,沙土逐渐被河流冲刷带走,渠道中出露的白僵土颗粒能起到抗冲铺盖层的作用,阻止渠道进一步在纵向上的变形。对比西大滩常见的白僵土和沙土的抗冲性发现,用白僵土铺成的渠道稳定性好,如果能够很好的解决白僵土浸润湿化与脱水干燥问题,则以白僵土构建排水渠道将会维持其稳定性。 This paper use flume experiments to analyze the stability of the drainage channels,the two different channels were paved by Baijiangtu and sand in the saline land of Ningxia,respectively.From the experiments,we can draw conclusions that the channel which paved by Baijiangtu has a strong resistance to water flow erosion.The minor change of the channel erosion and deposition is due to the repeated wetting and air drying.The sand is easy erosion by water flow,so the channel which paved by the sand has a large deformation in the longitudinal and transverse under the water flow.But the mud-gravel composed of the Baijingtu on the channel bed restrict the further longitudinal deformation.Comparing the two test we can draw a conclusion that the Baijiangtu could be used to construct the drainage channel in the Pingluo saline land of Ningxia,if the wetting and air drying problems can be solved.
出处 《灌溉排水学报》 CSCD 北大核心 2011年第2期55-59,共5页 Journal of Irrigation and Drainage
基金 中国科学院西部行动计划项目(KZCX2-XB2-13)
关键词 白僵土 砂土 水槽试验 宁夏 盐碱地 Baijiangtu sand flume simulation experiment Ningxia saline land
  • 相关文献

参考文献5

二级参考文献33

  • 1金德生.边界条件对曲流发育影响的过程响应模型实验研究[J].地理研究,1986,5(3):12-21. 被引量:23
  • 2Jones, L.S., Schumm, S.A. Causes of avulsion: an overview. In: Smith, N.D., Rogers, J. (Eds.), Fluvial Sedimentology Ⅵ.Special Publication of the International Association of Sedimentologists 28, Blackwell, Oxford, 1999, 171~178.
  • 3Kraus, MJ. Avulsion deposits in lower Eocene alluvial rocks, Bighorn Basin, Wyoming. Journal of Sedimentary Research,1996, 66(2): 354-363.
  • 4Bryant, M., Falk, P., Paola, C. Experimental study of avulsion frequency and rate of deposition. Geology, 1995, 23(4): 365-368.
  • 5McCarthy, T. S., Ellery, W. N. And Stanistreet, I. G. Avulsion mechanisms on the Okavango fan, Botswana: the control of a fluvial system by vegetation. Sedimentology, 1992, 39: 779-795.
  • 6Makaske, B., Smith, D. G. and Berendsen, H. J. A. Avulsion, channel evolution and floodplain sedimentation rates of the anastomosing upper Columbia River, British Colubia, Canada. Sedimentology, 2002, 49: 1049~1071.
  • 7Knighton, A. D. and Nanson G. C. Flow transmission along an arid zone anastomosing river, Cooper Creek. Australia. Hydrological Processes 1994, 8: 137-154.
  • 8Smith D G and Smith N D. Sedimentation in anastomosed river systems: examples from alluvial vallays near Banff, Alberta.Journal of Sedimentary Petrology, 1980, 50: 157-164.
  • 9Rust, B.R. Sedimentation in an arid-zone anastomosing fluvial system: Cooper's Creek, central Australia. Journal of Sedimentary Petrology, 1981, 51: 745-755.
  • 10Smith, D.G. Anastomosed fluvial diposits: modern exampies from western Canada. In: J. D. Collinson and J. Lewin(eds.),Modern and ancient fluvial systems. Spec. Pubis. Int. Ass. Sediments. Blackwell, London. 1983: 155~168.

共引文献27

同被引文献70

引证文献4

二级引证文献16

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部