Effects of Different Tillage Practices on the Yield of Runoff and Sediment in Peanut Podding Stage

ZHANG Jiehao; LIANG Xinlan; HUANG Hongliang; TANG Kai; WANG Qingzhen; ZHOU Cangning; MAO Xi

doi:10.13870/j.cnki.stbcxb.2021.01.010

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Effects of Different Tillage Practices on the Yield of Runoff and Sediment in Peanut Podding Stage

更新时间：2025-03-12

- Effects of Different Tillage Practices on the Yield of Runoff and Sediment in Peanut Podding Stage
- Vol. 35, Issue 1, Pages: 71-78(2021)
- 作者机构：
  
  四川农业大学水利水电学院,四川,雅安,625014
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2021.01.010
  CLC： S157.1
- Published：2021
- 稿件说明：
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ZHANG Jiehao, LIANG Xinlan, HUANG Hongliang, et al. Effects of Different Tillage Practices on the Yield of Runoff and Sediment in Peanut Podding Stage[J]. 2021, 35(1): 71-78.
DOI：

ZHANG Jiehao, LIANG Xinlan, HUANG Hongliang, et al. Effects of Different Tillage Practices on the Yield of Runoff and Sediment in Peanut Podding Stage[J]. 2021, 35(1): 71-78. DOI： 10.13870/j.cnki.stbcxb.2021.01.010.

摘要

为了研究不同耕作措施在花生结荚期时对紫色土区产流产沙过程的影响，通过对顺坡垄作、横坡垄作、穴播、平作这4种耕作措施种植花生以及对照组平坡裸地进行野外模拟降雨试验，得到其径流泥沙特征。利用滑动秩和检验法找出产流产沙过程变异时刻点，对变异时刻点后用Mann-Kendall趋势检验法分析产流产沙过程趋势。结果表明：产流产沙过程变异时刻点后均处于一个较为稳定状态，平坡裸地的稳定径流率、侵蚀率均最大，顺坡垄作次之，然后是平作，再是穴播，横坡垄作最小；而各耕作措施初始产流时间则与稳定径流率和侵蚀率相反。在减流减沙效益方面，相对于平坡裸地，不同耕作措施均表现出减流减沙效果，具体表现为横坡垄作 > 穴播 > 平作 > 顺坡垄作。

Abstract

In order to study the effects of different tillage practices on the yield of runoff and sediment in purple soil area in peanut podding stage. Field rainfall simulation experiments were carried out to study the yield of runoff and sediment in four tillage practices and one control group (longitudinal ridge

cross ridge

bunch planting

flat planting and bare land on flat slope). The sliding-rank-sum-test was used to find out the catastrophe point of runoff and sediment production process. The Mann-Kendall trend test method was used to analyze the trend of runoff and sediment yield process after the catastrophe point. The results showed that the runoff and sediment yield process was in a relatively stable state after the catastrophe point. The stable rate of runoff and sediment yield in bare land was the largest

followed by longitudinal ridge

then flat planting

bunch planting

and cross ridge was the smallest. However

the initial runoff yield time of each tillage practice was opposite to the stable rate of runoff and sediment yield. Compared to bare land on flat slope

all tillage practices showed the effects of runoff and sediment reduction. The specific performance was cross ridge > bunch planting > flat planting > longitudinal ridge.

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references

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CHEN Lei1,2,LI Zhan-bin1,LI Peng1,MU Jun3,JIA Lian-lian1(1.Key Lab.of Northwest Water Resources and Environment Ecology of MOE at Xaut,Xian,Shaanxi 710048,2.Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Fesources,Yangling,Shaanxi 712100,3.Xian Research Academic of Environmental Sciences,,)

中科院水利部水土保持研究所,陕西杨凌7121002. 西安理工大学西北水资源与环境生态教育部重点实验室,陕西西安,7100483. 西安市环境保护科学院

College of natural resources and environment, Northwest A&F University, Yangling of Shaanxi

College of Environmental Science and Engineering, Hunan University

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