PDF Download

[1]WANG Yu-xia,LIU Guo-bin,WANG Guo-liang,et al.Effect of Artemisia capillaries Distribution Patterns on Runoff and Sediment Production in Loess Hilly and Gully Region[J].Research of Soil and Water Conservation,2010,17(01):62-66.

Copy

Effect of Artemisia capillaries Distribution Patterns on Runoff and Sediment Production in Loess Hilly and Gully Region

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 17 Number of periods: 2010 01 Page number: 62-66 Column: Public date: 2010-02-20

Title:: Effect of Artemisia capillaries Distribution Patterns on Runoff and Sediment Production in Loess Hilly and Gully Region

Author(s):: WANG Yu-xia¹, LIU Guo-bin^1,2, WANG Guo-liang^1,2, YUAN Zi-cheng¹, QU Qiu-ling¹; 1. Northwest A&F University, Yangling, Shanxi, 712100, China;
2. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shanxi, 712100, China

Keywords:: Artemisia capillaries communities; distribution patterns; runoff and sediment production; loess hilly and gully region

CLC:: S157;S315

DOI:: -

Abstract:: Vegetation pattern has a great affection on its soil conservation function.Different combination of vegetation and bare land play a different role in regulating runoff and sediment yield.By simulated rainfall in the field,an experiment of runoff and sediment production and its characteristics was conducted in various Artemisia capillaries community distribution patterns at preliminary succession stages in Loess Hilly Gully Region.The results showed that under the same rainfall intensity of 2.43 mm/min and vegetation coverage,the runoff-reducing benefit of pattern B uniformly distributed by small plaque was greater than pattern C distributed by large plaque.Whereas,the sediment-reducing benefit was smaller.Compared to bare plot,the runoff in pattern B and C was decreased by 14.7% and 9.5%,and the sediment reduced of 36.14%,63.86% respectively.The accumulative runoff of the band-shaped plot increased with the rainfall duration with a linear relation.The accumulated sediment yield increased with rainfall time and then gradually decreased,such relation could be described by quadratic function.Also,the initial sediment yield was increased with runoff volume,then decreased.The changes in accumulative sediment yield with runoff was also conformed binomial function.

References:: [1] 朱显谟,祝一志.试论中国黄土高原土壤与环境[J].土壤学报,1992,29(4):351-357.
[2] 邱扬,傅伯杰,王勇.土壤侵蚀时空变化及其环境因子的时空关系[J].水土保持学报,2002,16(1):108-111.
[3] 朱显谟.黄土高原植被因素对于水土流失的影响[J].土壤学报,1960,8(2):110-120.
[4] 李勇,吴钦孝.黄土高原植被根系提高土壤抗冲性能研究:I.油松人工林根系对土壤抗冲性能的增加效应[J].水土保持学报,1990,4(1):1-5.
[5] 查轩,唐克丽,张科利,等.植被对土壤特性及土壤侵蚀的影响研究[J].水土保持学报,1992,6(2):52-59.
[6] 王晗生,刘国彬.植被结构及其防止土壤侵蚀作用分析[J].干旱区资源与环境,1999,13(2):62-68.
[7] 焦菊英,王万中,李靖.黄土高原林草水土保持有效盖度分析[J].植物生态学报,2000,24(5):608-612.
[8] 许炯心.黄土高原植被-降水关系的临界现象及其在植被建设中的意义[J].生态学报,2005,25(6):1233-1239.
[9] 徐宪立,马克明,傅伯杰,等.植被与水土流失关系研究进展[J].生态学报,2006,26(9):3137-3143.
[10] Valentin C D,Herbes J M,Poesen J.Soil and water components of banded vegetation patterns[J].Catena,1999,37:1-24.
[11] Ludwig J A,Tongway D J,Maraden S G.Strips.strands on stipples:modeling the influence of three landscape banding patterns on resource capture and productivity in a semi-arid woodlands Australia[J].Catena,1999,37(1/2):257-273.
[12] 游珍,李占斌,蒋庆丰,等.坡面植被分布对降雨侵蚀的影响研究[J].泥沙研究,2005,12(6):40-43.
[13] 郭忠升.水土保持植被建设中的三个盖度:潜势盖度、临界盖度和有效盖度[J].中国水土保持,2000(4):30-31.
[14] 汪有科,刘保元,焦菊英.恢复黄土高原林草植被及其盖度的前景[J].水土保持通报,1992,12(2):55-60.
[15] 吴钦孝,赵鸿雁,汪有科.黄土高原油松林地产流产沙及其过程研究[J].生态学报,1998,18(2):151-157.
[16] 李勉,姚文艺,陈江南,等.坡面草被覆盖对坡沟侵蚀产沙过程的影响[J].地理学报,2005,60(5):725-732.
[17] 黄明斌,刘贤赵.黄土高原森林植被对流域径流的调节作用[J].应用生态学报,2002,13(9):1057-1060.

Similar References:

Memo

Last Update: 1900-01-01