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JOURNAL OF DESERT RESEARCH  2011, Vol. 31 Issue (2): 400-406    DOI:
沙漠与沙漠化     
Field Observation of Farmland Wind-erosion around Beijing
WANG Ren-de1,2,3, ZOU Xue-yong2,3, ZHAO Jing-yan2,3
1.Institute of Geographical Sciences, Hebei Academy of Sciences, Shijiazhuang 050011, China; 2.State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875; 3.China Center of Desert Research, Beijing Normal University, Beijing 100875, China
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Abstract  In view of relatively weak wind-erosion in semi-humid region, a new-style sand sampler and sand trapping device were used in the field observation of farmland wind-erosion in Beijing. The results showed that among three kinds of farmlands, wind-erosion of ploughed and harrowed farmland was the most serious, that of ploughed and non-harrowed farmland is the weakest and that of stubble-keeping farmland lied between them. With the wind speed increasing, wind-erosion intensity of the three types of farmlands presented a increasing trend showing significantly exponential regularity. Vertical distribution of wind-erosion sediment followed the decreasing law of power function. Vertical distribution of the largest and average particle diameters also followed the decreasing law of power and index functions, respectively. The results also showed that diameters of most wind-erosion particles were smaller than 100 μm. Therefore it can be concluded that wind-blown sand structure in the study area was mainly characterized by suspension, which may be a normal state of farmland wind-erosion in semi-humid region.
Key words:  wind-erosion      farmland      field observation      Beijing     
Received:  12 July 2010      Published:  20 March 2011
ZTFLH:  S157  
Articles by authors
WANG Ren-de
ZOU Xue-yong
ZHAO Jing-yan

Cite this article: 

WANG Ren-de;;ZOU Xue-yong;ZHAO Jing-yan;. Field Observation of Farmland Wind-erosion around Beijing. JOURNAL OF DESERT RESEARCH, 2011, 31(2): 400-406.

URL: 

http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2011/V31/I2/400

[1]叶笃正,丑纪范,刘纪远,等.关于我国华北沙尘天气的成因与治理对策[J].地理学报,2000,55(5):513-521.
[2]郑新江,杨义文,李云.北京地区沙尘天气的某些特征分析[J].气候与环境研究,2004,9(1):8-27.
[3]高庆先,苏福庆,任阵海.北京地区沙尘天气及其影响[J].中国环境科学,2002,22(5):468-471.
[4]李令军,高庆生.2000年北京沙尘暴源地解析[J].环境科学研究,2001,14(2):1-3.
[5]杨东贞,颜鹏,徐祥德.北京沙尘天气的气溶胶特征[J].应用气象学报,2002,13(特刊):185-194.
[6]郭发辉,郝京甫,宣捷.北京沙尘天气的基本特征[J].气象,2002,28(8):51-54.
[7]陈广庭.近50年北京的沙尘天气及治理对策[J].中国沙漠,2001,21(4):402-407.
[8]陈效逑,谭文肯,刘大平,等.北京平原地区裸露土地的时空分布[J].水土保持研究,2003,10(3):18-25.
[9]王升堂,赵延治,邹学勇,等.北京郊区不同土地利用类型起沙起尘的特征研究[J].地理研究,2005,25(5):601-605.
[10]冯晓静,高焕文,王丽洁,等.北京周边典型农田风蚀风洞试验与防治分析[J].农业机械学报,2008,39(7):64-67.
[11]冯晓静,高焕文,李宏文,等.北京周边保护性耕作防治土壤风蚀效果监测研究[J].农机化研究,2008(1):142-144.
[12]李晓娜,武菊英,徐彪,等.京郊延庆康庄地区不同土地利用类型对土壤风蚀的影响[J].水土保持学报,2006,20(6):22-24.
[13]吴正.风沙地貌与治沙工程学[M ].北京:科学出版社,2003.
[14]Chepil W S.Soil conditions that influence wind erosion[J].Technical Bulletin,1958,1185.
[15]董治宝,钱广强.关于土壤水分对风蚀起动风速影响研究的现状与问题[J].土壤学报,2007,44(5):935-942.
[16]哈斯.河北坝上高原土壤风蚀物垂直分布的初步研究[J].中国沙漠,1997,17(1):9-14.
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