宽级配卵石河床表层大多为不同粗化程度的粗化层覆盖,现有大多数公式只能反映特定粗化程度下的输沙特性,限制了这些公式的适用性。理论分析和试验结果表明:在同样的来水来沙条件下,粗化程度越高,输沙率越小,在计算中引入粗化程度参数可以较好地提升公式的适用性;粗化层的稳定性对卵石推移质输沙有重要影响,粗化层遭受破坏后,推移质输沙率剧增,现有公式计算结果明显偏小。因此,在计算推移质输沙率时需要科学合理地考虑粗化层破坏导致的输沙率剧增问题。
Abstract
Surface layers of gravel bed of wide gradation are usually covered by armoring layer with different coarsening degrees. Most of the existing bed-load transport formulas could just reflect the characteristics of sediment transport in a certain coarsening degree, hence are of poor applicability. Theoretical analysis and experiment results show that bed-load transport rate decreases as the coarsening degree of armoring layer increases under the same incoming flow and sediment condition. Introducing the parameter of coarsening degree into the calculation could solve this problem. The stability of armoring layer plays an important role in bed-load transport in gravel bed. Bed-load transport rate increases sharply when the armoring layer is broken. The calculation results of the existing formulas are obviously small. Therefore, the sharp increase of sediment transport rate caused by the failure of armoring layer should be considered in calculating the bed-load transport rate.
关键词
卵石河床 /
推移质输沙率 /
粗化程度 /
粗化层稳定性 /
临界条件
Key words
gravel bed /
bed-load transport rate /
coarsening degree /
stability of armoring layer /
critical conditions
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参考文献
[1] DUBOYS P. Le Rhône et Les Rivières à Lit Affouillable[J].Annales des Ponts et Chaussées, 1879, 18(5): 141-195.
[2] MEYER-PETER E, MüLLER R. Formula for Bed-load Transport[C]∥Proceedings of 2nd Meeting, International Association for Hydraulic Research.Stockholm, June,1948: 39-64.
[3] BAGNOLD R A. An Approach to the Sediment Transport Problem from General Physics[R]. U.S.:U.S. Geological Survey Profession Paper 422-I, 1966:37.
[4]EINSTEIN H A. Bed Load Transport as a Probability Problem[D]. Colorado: Colorado State University,1937.(in German).Translated by SAYRE W W, in Sedimentation, Appendix C, 1972.
[5] PARKER G, KLINGEMAN P C, MCLEAN D G. Bedload and Size Distribution in Paved Gravel-bed Streams[J]. Journal of the Hydraulics Division, 1982, 108(4): 544-571.
[6] WILCOCK P R. Toward a Practical Method for Estimating Sediment Transport Rates in Gravel-bed Rivers[J]. Earth Surface Processes and Landforms, 2001, 26(13):1395-1408.
[7] 韩其为.泥沙起动规律及起动流速[M].北京:科学出版社,1999.
[8] 秦荣昱,王崇浩.河流推移质运动理论及应用[M].北京:中国铁道出版社,1996.
[9] 孙志林,田 林.非均匀沙分级推移质公式[J].水利学报,2001,(5):65-70.
[10]刘兴年,黄 尔,曹叔尤,等.宽级配推移质输移特性研究[J].泥沙研究,2000,(4):14-17.
[11]钱 宁. 推移质公式的比较[J].水利学报,1980,(4):1-11.
[12]曹叔尤,刘兴年,方 铎,等.山区河流卵石推移质的输移特性[J].泥沙研究,2000,(4):1-5.
[13]GOMEZ B, CHURCH M. An Assessment of Bed Load Sediment Transport Formulae for Gravel Bed Rivers[J]. Water Resources Research,1989,25(6):1161-1186.
[14]VAN DER SCHEER P,RIBBERINK J S,BLOM A. Transport Formulas for Graded Sediment,Behavior of Transport Formulas and Verification with Experimental Data[M]. Enschede: Civil Engineering University of Twente,The Netherlands,2002.
[15]REID I, LARONNE J B, POWELL D M. The Nahal Yatir Bedload Database: Sediment Dynamics in a Gravel-bed Ephemeral Stream[J]. Earth Surface Processes and Landforms, 1995, 20(9):845-857.
[16]HASSAN M A,CHURCH M. Experiments on Surface Structure and Partial Sediment Transport on a Gravel Bed[J]. Water Resources Research,2000,36(7):1885-1895.
[17]WITTENBERG L,NEWSON M D. Particle Clusters in Gravel-bed Rivers: an Experimental Morphological Approach to Bed Material Transport and Stability Concepts[J]. Earth Surface Processes and Landforms,2005,30(11):1351-1368.
[18]PARKER G. Surface-based Bedload Transport Relation for Gravel Rivers[J]. Journal of Hydraulic Research,1990,28(4):417-436.
[19]卢金友,金中武,郭 炜,等.长江上游推移质泥沙输移研究[J].长江科学院院报,2009,26(1):5-8.
[20]徐海涛,卢金友,刘小斌.不连续宽级配床沙推移质输沙率特性试验分析[J].长江科学院院报,2011,28(10):26-30,36.
[21]魏 丽,卢金友,徐海涛.天然河道不连续宽级配床沙特性及形成条件探讨[J].长江科学院院报,2012,29(10):6-10,15.
[22]王 涛,刘兴年,黄 尔,等.卵石河床清水冲刷粗化层破坏临界条件试验研究[J].四川大学学报(工程科学版),2008,40(4):36-40.
[23]聂锐华,刘兴年,杨克君,等.粗化层破坏过程中的最大推移质输沙率试验研究[J].四川大学学报(工程科学版),2013,45(2):1-5.
[24]ENGELUND F,FREDSØE J. A Sediment Transport Model for Straight Alluvial Channels[J]. Hydrology Research,1976,7(5):293-306.
[25]VERICAT D,BATALLA R J,GARCIA C. Breakup and Reestablishment of the Armour Layer in a Large Gravel-bed River below Dams: The Lower Ebro[J].Geomorphology,2006,76(1/2):122-136.