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工程科学与技术:2017,49(Z1):44-49
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山区河流河床基岩暴露与沙卵石覆盖反常关系研究——以陇西河为例
(四川大学 水利水电学院)
Abnormal Phenomena of Bedrock Exposure and Alluvial Cover in the River Bed of Mountain Area——A Case Study of Longxi River
(State Key Lab. of Hydraulics and Mountain River Eng.,College of Water Resource & Hydropower,Sichuan Univ.)
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投稿时间:2016-08-06    修订日期:2016-12-29
中文摘要: 山区河流不同河段的河床形态常处于基岩暴露与沙卵石覆盖的相间变化中。野外调查发现,至少在青藏高原与四川盆地过渡带,不少河流出现坡度大而沙卵石覆盖多,坡度小而基岩暴露多的现象。为了研究该反常规律,以岷江二级支流陇西河为例,进行多次野外观测与数据采集,通过提取流域地形数据,得到并分析其干流沿程剖面,并结合已有的室内水槽试验研究结果,进一步说明床面沙卵石的运动情况与分布特性,得到以下结论:陇西河流域岩性以砂岩为主,干流从上游向下游依次出现陡、缓、陡、缓交替的4段,平均坡度依次为8.1%、0.2%、6.2%和1.2%;较陡的两段全部沙卵石覆盖,较缓的两段全部基岩暴露。产生这种现象的原因:一是较陡段泥沙颗粒通过两侧山体崩塌滑坡侧向补给,床面大尺寸漂石与周围的较细颗粒会逐渐形成相对稳定且水流阻力大的自锁结构,且床面粗糙,有助于提高床面抗冲刷性,抑制基岩的暴露,因此导致输送到下游较缓段的输沙率很低;二是砂岩颗粒岩性较软,少量被输移到下游的颗粒容易破碎成更小的颗粒,更容易被输移,使得较缓段基岩暴露现象突出。较陡段被沙卵石覆盖,将有效抑制窄深处基岩河床的侵蚀下切速率,从而进一步影响相关流域地貌的演化,如增加河流袭夺的机率。
Abstract:River reaches in the mountain area are often in the alternation between bedrock exposure and alluvial covered.The field survey found that at least several rivers in the transition zone between Qinghai-Tibet Plateau and Sichuan Basin have the abnormal phenomena that bed rock is exposure in gentle slope reaches and alluvial deposits are covered in the steep slope reaches.In order to study the abnormal phenomena,taking the Longxi River,which is the secondary tributary of Minjiang River as a case study,field observation and data collection were carried out many times.By extracting basin’s terrain data,the longitudinal profile of the truck stream were obtained and analyzed.Moreover,combined with the pervious flume experiment results,sediment transport and distribution characteristics in Longxi River was further illustrated,and the conclusions were obtained as the lithology of Longxi River basin is mainly sandstone,from the head waters,the slopes of truck stream have four distinguish reaches with different slopes and bed surface characteristics,namely,steep,gentle,steep and gentle successively,with average slope of 8.1%,0.2%,6.2% and 1.2% respectively, the two steep reaches are alluvial covered but the two gentle reaches are bed rock exposure,The steep slope reaches are supplied from colluvially derived sediment of the hillslopes,particles from sand to large boulders will gradually form relatively stable interlock structures with high resistance,and the bed roughness of narrow and deep channel enhances the erosion resistance of the bed surface, which will inhibit bedrock exposure.The interlocked structures also result in very low sediment transport rate to the downstream gentle slope reaches;moreover,the rare sandstone grains transported downstream are easily broken into smaller ones, which are more mobile,generating the bedrock exposure phenomenon to be prominent; steep slope reaches covered by alluvial deposits will suppress the erosion rate of narrow and deep bedrock and further affect the evolution of basin geomorphology,for e.g.,promote stream piracies.
文章编号:201600777     中图分类号:    文献标志码:
基金项目:国家自然科学基金资助项目(51509172;51539007;51609160);国家重点研发计划资助项目(2016YFC0402302);国家“十二五”科技计划资助项目(2012BAB05B02);四川大学青年启动基金资助项目(2015SCU11046)
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顾继一,范念念,刘兴年.山区河流河床基岩暴露与沙卵石覆盖反常关系研究——以陇西河为例[J].工程科学与技术,2017,49(Z1):44-49.
Gu Jiyi,Fan Niannian,Liu Xingnian.Abnormal Phenomena of Bedrock Exposure and Alluvial Cover in the River Bed of Mountain Area——A Case Study of Longxi River[J].Advanced Engineering Sciences,2017,49(Z1):44-49.