《Table 2 Parameters measured in different rainfall simulations during soybean growth stages》
本系列图表出处文件名:随高清版一同展现
《Effect of soil management on soil erosion on sloping farmland during crop growth stages under a large-scale rainfall simulation experiment》
Note:R1,seedling stage;R2,initial blossoming stage;R3,full flowering stage;R4,pod bearing stage;R5,initial filling stage.LAI,leaf area index;NH,no soil management practice;HT,hoeing tillage applied.
The runoff initiation time considerably differed among soybean growth stages in two treatments(Table 2).For NH treatment,a faster response to simulated rainfall was observed in R3 where the runoff was generated 87′′after beginning the rainfall simulation.From R1 to R3,the runoff initiation time decreased from 4′38′′(R1)to 1′27′′(R3),thereby indicating that generation of runoff occurred faster.From R3 to R5,the runoff initiation time increased slightly from 1′27′′(R3)to 3′30′′(R5).By contrast,under HT treatment,the minimum runoff initiation time occurred in R3,where it varied between 5′13′′in R3 and 28′10′′in R5.These results can be explained by the differences in the canopy among growth stages,which directly affected the partitioning of rainfall.For instance,stemflow may have contributed to the faster generation of runoff from R1 to R3,as found by Ma et al.(2013),who reported that stemflow increased with leaf area due to crop leaves could intercept rainfall,thus contributing to an increased flow along the stems.Alternatively,the high leaf retention capacity may increase the time of runoff initiation from R3 to R5(Zhang et al.,2015).In addition,the longer time required for runoff generation under HT treatment compared to NH treatment in the same growth stage may be attributed to hoeing tillage,which destroyed the physical soil crust and increased soil surface roughness,thereby improving rainwater storage capacity as well as providing more opportunity for infiltration.Ultimately,this led to an increased runoff generation threshold and an extended runoff generation time in HT plot,which was also observed by Gómez et al.(2005).
图表编号 | XD0020365300 严禁用于非法目的 |
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绘制时间 | 2018.12.01 |
作者 | WANG Linhua、WANG Yafeng、Keesstra SASKIA、Cerdà ARTEMI、MA Bo、WU Faqi |
绘制单位 | State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences、Institute of Soil and Water Conservation, Northwest A&F University、State Key Laboratory of Urban and Regional Ecology, Research |
更多格式 | 高清、无水印(增值服务) |
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