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降雨类型与坡度对棕壤垄沟系统产流产沙的影响 被引量:5

Effects of Rainfall Type and Slope on Runoff and Sediment Yield in Brown Soil Furrow System
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摘要 为深入理解棕壤垄作坡耕地的土壤侵蚀机理,利用1.60 m×0.53 m的试验土槽,设计2个降雨类型,即增强型(70~70~100~100 mm/h)和减弱型(100~100~70~70 mm/h),以及2个坡度(9°和18°)的人工模拟降雨试验。每个雨型分2个阶段(阶段I、阶段II),每个阶段进行相同雨强的2个场次降雨,每个场次降雨历时20 min。结果表明:(1)雨强对径流量呈显著影响(P<0.05),100 mm/h雨强下的径流量>70 mm/h时的径流量。在减弱型雨型下,坡度对径流量影响显著(P<0.05),而增强型雨型下在不同阶段坡度对径流量的影响不同。(2)雨强对产沙量的影响显著(P<0.05),在阶段Ⅰ降雨中,100 mm/h雨强下9°和18°坡面的平均每分钟产沙量分别为70 mm/h雨强下的23.98,9.07倍。在70 mm/h雨强下,坡度对产沙量的影响显著(P<0.05),而100 mm/h雨强下不同阶段坡度对径流量的影响具有差异性。(3)100 mm/h雨强在不同雨型中出现的时序对产沙量影响不显著(P>0.05);在70 mm/h雨强下,产沙量整体较小,基本在15 g/min以下。同一雨强在不同雨型中的时序对径流量均存在显著影响(P<0.05)。(4)总径流量从大到小依次为:9°减弱型>18°减弱型>9°增强型>18°增强型;总产沙量从大到小依次为:18°增强型>18°减弱型>9°减弱型>9°增强型。不同雨型下,雨强发生改变后,累计径流量和累计产沙量增加速率和雨强的改变具有一致性。 In order to deeply understand the soil erosion mechanism of ridged farmland on brown soil,this paper used a 1.60 m×0.53 m test soil trough and designed two rainfall types,namely,intensive-type(70~70~100~100 mm/h)and reduced-type(100~100~70~70 mm/h),and artificial simulated rainfall tests on 2 slopes(9°and 18°).Each rainfall type is divided into two phases(phase I,phase II),and two sessions of rainfall of the same raininess at each stage,and each session of rainfall lasts 20 minutes.The results show:(1)Raininess has a significant effect on runoff(P<0.05).Runoff at 100 mm/h rain intensity is greater than 70 mm/h.Under the reduced rainfall type,the slope has a significant effect on runoff(P<0.05),while under the intensive rainfall type,the slope at different stages has different effects on runoff.(2)Raininess has a significant effect on sediment yield(P<0.05).During the rainfall of Phase I,the average sediment yield per minute at 9°and 18°slopes at 100 mm/h raininess was 23.98 times and 9.07 times of 70 mm/h raininess.Under 70 mm/h raininess,the slope has a significant effect on sediment yield(P<0.05),while under 100 mm/h raininess,the slope at different stages has different effects on runoff.(3)The time sequences of 100 mm/h raininess in different rainfall types has no significant effect on sediment yield(P>0.05);under 70 mm/h raininess,the overall sediment yield is smaller,basically below 15 g/min.The time sequences of the same raininess in different rainfall types had significant effects on runoff(P<0.05).(4)The total runoff is as follows:9°reduced-type>18°reduced-type>9°intensive-type>18°intensive-type;the total sediment production is in descending order:18°intensive-type>18°reduced-type>9°reduced-type>9°intensive-type.Under different rainfall type,after the change of rain intensity,the cumulative runoff and cumulative sediment yield increase rate and the change of rain intensity are consistent.
作者 徐相忠 刘前进 张含玉 XU Xiangzhong;LIU Qianjin;ZHANG Hanyu(College of Geography and Environment,Shandong Normal University,Jinan 250358;Shandong Key Laboratory of Soil Conservation and Environmental Protection,College of Resource and Environment,Linyi University,Linyi,Shandong 276005)
出处 《水土保持学报》 CSCD 北大核心 2020年第4期56-62,71,共8页 Journal of Soil and Water Conservation
基金 国家自然科学基金项目(41571261,41701311) 山东省高等学校青创人才引育计划项目(QC2019YY144) 山东省自然科学基金项目(ZR2017JL019,ZR2017PD003)。
关键词 棕壤垄沟 降雨类型 坡度 侵蚀 产流产沙 brown soil ditch rainfall type slope erosion runoff and sediment yield
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