Characteristics of Runoff and Sediment Yield of Vegetation Measures on Slope Farmland in Anjiagou Watershed

LIU Xue-feng; ZHANG Fu; ZHANG Bai-lin; LI Xu-chun

doi:10.13961/j.cnki.stbctb.2014.04.018

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Characteristics of Runoff and Sediment Yield of Vegetation Measures on Slope Farmland in Anjiagou Watershed

- Characteristics of Runoff and Sediment Yield of Vegetation Measures on Slope Farmland in Anjiagou Watershed
- Bulletin of Soiland Water Conservation Vol. 33, Issue 4, Pages: 17-20(2014)
- 作者机构：
  
  1. 甘肃农业大学林学院,甘肃,兰州,730070
  2. 定西市水土保持科学研究所,甘肃,定西,743000
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2014.04.018
  CLC：
- Published：2014
- 稿件说明：
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LIU Xue-feng, ZHANG Fu, ZHANG Bai-lin, et al. Characteristics of Runoff and Sediment Yield of Vegetation Measures on Slope Farmland in Anjiagou Watershed[J]. Bulletin of Soiland Water Conservation, 2014, 33(4): 17-20.
DOI：

LIU Xue-feng, ZHANG Fu, ZHANG Bai-lin, et al. Characteristics of Runoff and Sediment Yield of Vegetation Measures on Slope Farmland in Anjiagou Watershed[J]. Bulletin of Soiland Water Conservation, 2014, 33(4): 17-20. DOI： 10.13961/j.cnki.stbctb.2014.04.018.

摘要

根据安家沟流域2007-2010年5-9月份径流小区观测资料

经过分析计算得到各小区的单位面积径流和累积产沙量

并对各植物措施小区的产流、产沙特征进行了研究。结果表明

5种植物措施小区的产流强度由强到弱的顺序为:油松 > 小麦 > 红豆草 > 封禁 > 沙棘;产沙强度表现为:小麦 > 红豆草 > 油松 > 封禁 > 沙棘;各种措施径流小区径流量、泥沙量与坡度呈正相关关系

且均达到显著相关水平;产沙量与径流量具有一定的相关性。

Abstract

Based on the runoff plot data of Anjiagou watershed in 2007-2010

we research the rainfall-runoff per area and the cumulative sediment load under different vegetation measure conditions were obtained

and the characteristics of runoff and sediment under different conditions were analyzed. The results show that the chinese pine slope farmland had the highest runoff and the wheat slope farmland had the highest sediment load. The relationship of runoff yield in the five slope farmlands are in order of chinese pine slope farmland > wheat slope farmland > sainfoin slope farmland > banned > seabuckthorn slope farmland. The relationship of sediment yield are in order of wheat slope farmland > sainfoin slope farmland > chinese pine slope farmland > banned > seabuckthorn slope farmland. The rainfall-runoff and sediment load are positively correlated with slope. Sediment yield has some correlation with runoff.

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references

傅涛,倪九派,魏朝富,等.坡耕地土壤侵蚀研究进展[J].水土保持学报,2001,15(3):123-128.

李晓红,韩勇,郑阳华.三峡库区坡耕地土壤侵蚀治理效益分析[J].重庆大学学报:自然科学版,2007,30(1):134-138.

南秋菊,华珞.国内外土壤侵蚀研究进展[J].首都师范大学学报:自然科学版,2003,24(2):86-95.

李登航,王立,黄高宝,等.保护性耕作对黄土高原坡耕地水土流失的影响[J].安徽农业科学,2009,37(13):6087-6088,6111.

杨建英,赵延宁.坡面侵蚀研究现状及展望[J].北京林业大学学报,1994,16(1):95-101.

于国强,李占斌,裴亮,等.不同植被类型下坡面径流侵蚀产沙差异性[J].水土保持学报,2012,26(1):1-6.

王万忠.黄土地区降雨特性与土壤流失关系的研究(Ⅲ):关于侵蚀性降雨标准的问题[J]. 水土保持通报, 1984,4(2):58-63.

江青龙,谢永生,赵婷,等.冀北山区不同土地利用类型的坡面产流产沙与降雨的关系研究[J].干旱地区农业研究,2011,29(6):202-207.

谢云,刘宝元,章文波.侵蚀性降雨标准的研究[J].水土保持学报,2000,14(4):6-11.

蒋光毅,史冬梅,卢喜平,等.紫色土坡地不同种植模式下径流及养分流失研究[J].水土保持学报,2004,18(5):54-58,63.

杨建霞,雷孝章,邱景,等.5°~25°坡耕地径流小区产流产沙规律[J].中国水土保持科学,2008,6(S):30-34.

刘松波,庄春兰,孟琳琳.坡度对坡面侵蚀产沙响应的研究[J].中国水土保持,2009(5):44-47.

高建恩.地表径流调控与模拟试验研究[D].北京:中国科学院大学,2005.

唐小娟.坡地分段雨水集蓄利用技术试验研究[D].北京:中国科学院大学,2004.

唐小娟,吴普特,高建恩.不同坡面径流调控措施的筛选试验研究[J].四川水利,2004,1(S):57-60.

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