1. 福建农林大学资源与环境学院,福州,350002
2. 安溪县水土保持委员会办公室, 福建 安溪,362000
[ "蒋芳市(1979-),男,福建大田人,讲师,博士,主要从事土壤侵蚀与治理研究。E-mail:jfsfafu@163.com" ]
纸质出版:2019
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蒋芳市, 张海东, 陈培松, 等. 土石混合崩积体坡面细沟跌坑发育试验研究[J]. 水土保持学报, 2019,33(6):27-33.
JIANG Fangshi, ZHANG Haidong, CHEN Peisong, et al. Experimental Study on the Drop Pit Development of Rill Erosion on Soil-rock Mixed Colluvial Deposit Slopes[J]. 2019, 33(6): 27-33.
蒋芳市, 张海东, 陈培松, 等. 土石混合崩积体坡面细沟跌坑发育试验研究[J]. 水土保持学报, 2019,33(6):27-33. DOI: 10.13870/j.cnki.stbcxb.2019.06.004.
JIANG Fangshi, ZHANG Haidong, CHEN Peisong, et al. Experimental Study on the Drop Pit Development of Rill Erosion on Soil-rock Mixed Colluvial Deposit Slopes[J]. 2019, 33(6): 27-33. DOI: 10.13870/j.cnki.stbcxb.2019.06.004.
为了探究土石混合崩积体坡面细沟跌坑发育情况,采用室内放水冲刷试验,通过设置4个流量(2,4,8,12 L/min)和4种砾石含量的土石混合崩积物(砾石质量比例0,10%,30%,50%),研究不同条件下细沟跌坑的发育特征。结果表明:在不同冲刷时段,跌坑数量变化为3~17个,跌坑平均深度为1.10~5.93 cm,细沟纵断面形态系数为2.97~19.97。各跌坑参数随冲刷时间的延长总体呈增大趋势,部分坡面在5 min或7.5 min时出现最大值;跌坑参数随流量的增加总体呈先增大后减小趋势,8 L/min流量条件下出现最大值,而随着砾石含量增加总体呈增大趋势;流量对跌坑发育的影响大于砾石含量。各跌坑参数与流速、阻力系数及曼宁粗度系数密切相关,径流剪切力是描述跌坑发育的最适合水动力学指标,可用线性函数表达。
In order to explore the drop pit development on soil-rock mixed colluvial deposit slopes
a scouring test was conducted in laboratory. Four soil-rock mixed colluviums (0
10%
30%
50% gravel in mass ratio) under different flow discharges (2
4
8
12 L/min) were tested.The results were as followed:the number of drop pit varied from 3 to 17
the average depth of drop pit was between 1.10 to 5.93 cm
and the profile form indices were between 2.97 and 19.97. The number of drop pit
the depth of drop pit
and the profile form indices all showed the increasing trend overall with the increase of scouring duration
whereas the maximum value appeared in some slopes at 5 min or 7.5 min. All drop pit parameters first increased and then decreased with the increase of flow discharge as a whole
and the maximum value appeared under the discharge of 8 L/min. The number of drop pit
the depth of drop pit
and the profile form indices increased with the increase of gravel content.The influence of flow discharge on the all parameters of drop pit was greater than those of gravel contents. Drop pit parameters were significantly correlated with flow velocity
resistance coefficient and Manning roughness coefficient. Shear stress was the best hydrodynamic parameter to describe the development of drop pit development as a linear function.
王礼先.中国水利百科全书·水土保持分册[M].北京:中国水利水电出版社,2004.
季翔,黄炎和,林金石,等.基于CA-Markov模型与ANUDEM内插法的崩岗侵蚀量预估[J].农业工程学报,2018,34(21):128-136.
Chen J L, Zhou M, Lin J S, et al. Comparison of soil physicochemical properties and mineralogical compositions between noncollapsible soils and collapsed gullies[J].Geoderma,2018,317:56-66.
Jiang F S, Huang Y H, Wang M K, et al. Effects of rainfall intensity and slope gradient on steep colluvial deposit erosion in southeast China[J].Soil Science Society of America Journal,2014,78(5):1741-1752.
蒋芳市,陈培济,黄炎和,等.集中水流下土石混合崩积体坡面侵蚀水动力特征试验研究[J].水土保持学报,2017,31(6):11-17,102.
Liu X L, Qiu J A, Zhang D L. Characteristics of slope runoff and soil water content in benggang colluvium under simulated rainfall[J].Journal of Soils and Sediments,2018,18:39-48.
盛贺伟,孙莉英,蔡强国.黄土坡面细沟发育形态对侵蚀特征的影响[J].应用基础与工程科学学报,2017,25(4):679-688.
覃超,吴红艳,郑粉莉,等.黄土坡面细沟侵蚀及水动力学参数的时空变化特征[J].农业机械学报,2016,47(8):146-154,207.
沈海鸥,郑粉莉,温磊磊,等.降雨强度和坡度对细沟形态特征的综合影响[J].农业机械学报,2015,46(7):162-170.
Jiang F S, Zhan Z Z, Chen J L, et al. Rill erosion processes on a steep colluvial deposit slope under heavy rainfall in flume experiments with artificial rain[J].Catena,2018,169(23):46-58.
邵明安,马东豪,朱元骏,等.黄土高原土石混合介质土壤水分研究[M].北京:科学出版社,2010.
Zhang Y H, Zhang M X, Niu J Z, et al. Rock fragments and soil hydrological processes:Significance and progress[J].Catena,2016,147:153-166.
牛耀彬,高照良,李永红,等.工程堆积体坡面细沟形态发育及其与产流产沙量的关系[J].农业工程学报,2016,32(19):154-161.
董旭,张宽地,王光谦,等.黄土细沟流跌坑的形成与作用机理[J].四川大学学报(工程科学版),2016,48(5):28-35.
白清俊,马树升.细沟侵蚀过程中水流跌坑的发生机理探讨[J].水土保持学报,2001,15(6):62-65.
严冬春,文安邦,史忠林,等.紫色土坡面水流跌坑形态特征及其成因[J].山地学报,2012,30(1):30-35.
马小玲,张宽地,杨帆,等.坡面细沟侵蚀断面形态发育影响因素分析及动力特性试验[J].农业工程学报,2017,33(4):209-216.
赵本山,王生新,徐奎,等.山前洪积扇坡面细沟侵蚀跌坑特征的试验研究[J].干旱区地理,2017,40(2):348-354.
严冬春,文安邦,史忠林,等.紫色土坡面跌坑贯穿发生细沟的水动力过程[J].长江流域资源与环境,2012,21(1):94-99.
倪世民,冯舒悦,王军光,等.不同质地重塑土坡面细沟侵蚀形态与水力特性及产沙的关系[J].农业工程学报,2018,34(15):149-156.
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