Please wait a minute...
img

Wechat

Adv search
JOURNAL OF DESERT RESEARCH  2012, Vol. 32 Issue (4): 980-984    DOI:
Biology and Soil     
Discussion on Wind Factor Influencing the Distribution of Biological Soil Crusts on Surface of Sand Dunes
WU Yong-sheng1,2, Has Erden2, QU Zhi-qiang3
1.Institute of Water Resources for Pastoral Area, Ministry of Water Resources of China, Huhhot 010020, China;
2.College of Resource Science and Technology, Beijing Normal University,Beijing 100875, China;
3.Ministry of Civil Affair & Ministry of Education Academy of Disaster Reduction and Emergency Management, Beijing Normal University, Beijing 100875, China
Download:  PDF (1599KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  Biological soil crusts are widespread in arid and semi-arid areas, and their formation and development have significant effects on rehabilitation process of desert ecosystem. Air flow pattern and developmental characteristics of biological soil crusts on fixed sand dunes are studied by field observation method. Results indicate that near surface air flow on windward slope of sand dunes shows an increasing trend from the base to the top and reaches the highest point at the crest. At lee side, although near surface air flow has a little increase at lower part of the slope after initial sudden decrease at upper part of the slope, but its overall trend turns up to decreasing from the crest. Wind velocity variation coefficient is varied at different heights over each observation site. The thickness, gear strength and percentage of fine particles of biological soil crusts decrease from the base of slope to the upper part, showing biological soil crusts are less developed in high wind speed area and well developed in low wind speed area. This indicates that change of airflow pattern caused by topography could be the key factor affecting the distribution of biological soil crusts at different location of sand dunes.
Key words:  biological soil crusts      wind      distribution     
Received:  25 November 2011      Published:  20 July 2012
ZTFLH: 

P931.3

 
Articles by authors
HA Si
WU Yong-sheng
QU Zhi-qiang

Cite this article: 

WU Yong-sheng, HA Si, QU Zhi-qiang. Discussion on Wind Factor Influencing the Distribution of Biological Soil Crusts on Surface of Sand Dunes. JOURNAL OF DESERT RESEARCH, 2012, 32(4): 980-984.

URL: 

http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2012/V32/I4/980

[1]魏美丽,张元明.脱水对生物结皮中齿肋赤藓光和色素含量和叶绿体结构的影响[J].中国沙漠,2010,30(6):1311-1318.

[2]Belnap J.The potential roles of biological soil crusts in dryland hydrologic cycles[J].Hydrological Processes,2006,20:3159-3178.

[3]Belnap J,Budel B,Lange O L.Biological soil crusts:Characteristics and distribution[M]//Belnap J,Lange O L.Biological Soil Crusts:Structure,Function and Management.Berlin:Springer-Verlag,2001:3-30.

[4]Kidron G J,Barzilay E,Sachs E.Microclimate control upon sand microbiotic crusts,western Negev Desert,Israel[J].Geomorphology,2000,36(1-2):1-18.

[5]Li X R,Zhou H Y,Wang X P,et al.The effects of revegetation on cryptogam species diversity in Tengger Desert,Northern China[J].Plant and Soil,2003,251:237-245.

[6]Bowker M A,Belnap J,Davidson D W,et al.Evidence for micronutrient limitation of biological soil crusts:Importance to arid-land restoration[J].Ecological Applications,2005,15:1941-1951.

[7]Eldridge D J.Environmental factors relating to the distribution of terricolous bryophytes and lichens in semi-arid Australia[J].Bryologist,1997,100:28-39.

[8]张元明,潘惠霞,潘伯荣,等.古尔班通古特沙漠不同地貌部位生物结皮的选择性分布[J].水土保持学报,2004,14(4):61-65.

[9]Li X R,He M Z,Zerbe S,et al.Micro-geomorphology determines community structure of biological soil crusts at small scale[J].Earth Surface Processes and Landforms,2010,35: 932-940.

[10]吴永胜,哈斯,李双权,等.毛乌素沙地南缘生物土壤结皮的发育特征[J].水土保持学报,2010,24(5):258-261.

[11]哈斯,庄燕美,王蕾,等.毛乌素沙地南缘横向沙丘粒度分布及其对风向变化的响应[J].地理科学进展,2006,25(6):42-52.

[12]张元明,曹雪芹.准噶尔荒漠生物结皮研究[M].北京:科学出版社,2008:2-10.

[13]段争虎,刘新民,屈建军.沙坡头地区土壤结皮形成机理的研究[J].干旱区研究,1996,13(2):31-37.

[14]Fang H Y,Cai Q G,Chen H,et al.Mechanism of formation of physical soil crust in desert soils treated with straw checkerboards[J].Soil & Tillage Research,2007,93:222-230.

[15]吴楠,潘伯荣,张元明.土壤微生物在生物结皮形成中的作用及生态意义[J].干旱区研究,2004,21(4):444-450.

[16]Hu C X,Liu Y D,Song L R,et al.Effect of desert soil algae on the stabilization of fine sands[J].Journal of Applied Phycology,2002,14:281-292.

[17]Hu C X,Liu Y D,Zhang D L,et al.Cementing mechanism of algal crusts from desert area[J].Chinese Science Bulletin,2002,47(16):1361-1368.

[18]贾荣亮,李新荣,谭会娟,等.沙埋干扰去除后生物土壤结皮光合生理恢复机制[J].中国沙漠,2010,30(6):1299-1304.

[19]Nickling W G,Neuman C M,Lancaster N.Grainfall processes in the lee of transverse dunes,Silver Peak,Nevada[J].Sedimentology,2002,49(1):191-209.

[20]张正偲,赵爱国,董治宝,等.藻类结皮自然恢复后抗风蚀特性研究[J].中国沙漠,2007,27(4):558-562.

[21]王继和,马全林,刘虎俊,等.干旱区沙漠化土地逆转植被的防风固沙效益研究[J].中国沙漠,2006,26(6):903-909.

[22]杨文斌,卢崎,吴波,等.低覆盖度不同配置灌丛内风流结构与防风效果的风洞实验[J].中国沙漠,2007,27(5):791-796.
No Suggested Reading articles found!