Arid
DOI10.1016/j.still.2003.08.001
Wind erosion and airborne dust deposition in farmland during spring in the Horqin Sandy Land of eastern Inner Mongolia, China
Li, FR; Zhao, LY; Zhang, H; Zhang, TH; Shirato, Y
通讯作者Li, FR
来源期刊SOIL & TILLAGE RESEARCH
ISSN0167-1987
EISSN1879-3444
出版年2004
卷号75期号:2页码:121-130
英文摘要

In the Horqin Sandy Land of eastern Inner Mongolia in northern China, wind erosion in farmland is very common in a period from thawing of frozen surface soil in mid-March to sowing of crops in the end of April, largely because of dry and windy weather. However, little is known about the magnitude of wind erosion and associated nutrient losses due to erosion and the addition of nutrients by airborne dust deposition to farmlands during this period. A field experiment was conducted in an Entisol with sand origin under corn (Zea mays L.) production to investigate daily changes in wind speed and wind erosion intensity (as measured by soil transport rate) over a period from 20 March to 30 April 2001. We also measured daily rates of airborne dust deposition during the spring seasons with the high frequency of dust storm occurrence. The rates of soil transport by wind varied greatly from 13.2 to 1254.1 kg ha(-1) per day, averaging 232.1 kg ha(-1) per day, largely attributable to great variation between days in wind speed within the study period. The potential losses of nutrients through wind erosion were 0.26-24.95 kg ha(-1) per day (averaging 4.62 kg ha(-1) per day) in organic matter, 0.02-1.64 kg ha(-1) per day (averaging 0.31 kg ha(-1) per day) in nitrogen and 0.01-0.7 kg ha(-1) per day (averaging 0.13 kg ha(-1) per day) in phosphorus. The mean rates of airborne dust deposition ranged from 4.0 to 48.9 kg ha(-1) per day, averaging 19.9 kg ha(-1) per day, during the spring seasons. The potential addition of organic matter, nitrogen and phosphorus by dust input to the experimental field was, on average, 0.54, 0.04 and 0.02 kg ha(-1) per day, respectively. Although the addition was a fraction of the losses due to erosion, nevertheless, dust input in the spring seasons is one of the major suppliers of soil nutrition. The fact that the addition of nutrients by dust is about 1/10 of the losses of soil nutrients through wind erosion suggests that developing and adopting more effective management practices to reduce soil erosion losses and to improve soil fertility are crucial to achieve a sustainable agricultural system in a fragile, semiarid sandy land environment. (C) 2003 Elsevier B.V. All rights reserved.


英文关键词dust input nutrient addition sandy soils soil erosion losses soil transport rate
类型Article
语种英语
国家Peoples R China ; Japan
收录类别SCI-E
WOS记录号WOS:000188498200003
WOS关键词SOIL QUALITY ; TRANSPORT ; SYSTEMS ; SURFACE ; DESERT
WOS类目Soil Science
WOS研究方向Agriculture
来源机构中国科学院西北生态环境资源研究院
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/148077
作者单位(1)Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China;(2)Natl Inst Agroenvironm Sci, Tsukuba, Ibaraki 3058604, Japan
推荐引用方式
GB/T 7714
Li, FR,Zhao, LY,Zhang, H,et al. Wind erosion and airborne dust deposition in farmland during spring in the Horqin Sandy Land of eastern Inner Mongolia, China[J]. 中国科学院西北生态环境资源研究院,2004,75(2):121-130.
APA Li, FR,Zhao, LY,Zhang, H,Zhang, TH,&Shirato, Y.(2004).Wind erosion and airborne dust deposition in farmland during spring in the Horqin Sandy Land of eastern Inner Mongolia, China.SOIL & TILLAGE RESEARCH,75(2),121-130.
MLA Li, FR,et al."Wind erosion and airborne dust deposition in farmland during spring in the Horqin Sandy Land of eastern Inner Mongolia, China".SOIL & TILLAGE RESEARCH 75.2(2004):121-130.
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