Please wait a minute...
img

Wechat

Adv search
JOURNAL OF DESERT RESEARCH  2011, Vol. 31 Issue (2): 415-419    DOI:
生物土壤与生态     
Stem Sap Flow of Caragana korshinskii and Its Influence Factors in a Revegetated Desert Area
HUANG Lei1, ZHANG Zhi-shan1, ZHOU Xiao-kun2
1.Shapotou Desert Research and Experiment Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China; 2.Department of Mathematics, Northeastern University, Shenyang 110004, China
Download:  PDF (2179KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  Stem sap flows of 18-year-old Caragana korshinskii plants were monitored continuously with Dynamax stem flow recorder for the entire growing season under nature conditions in a revegetated desert area. Environmental factors such as solar radiation, air temperatures, relative humidity, wind speed, and precipitation were measured meanwhile with eddy correlation system. Results show that the curves of stem sap flow rate in the whole growing season are obviously single-peak. Sap flow usually starts at 00:00 and increases gradually, reaches peak point at about 08:30—11:30, then gradually decreases to the minimum point at the middle night. Sap flow rate is significantly correlated with solar radiation, vapour pressure deficit, relative humidity, air temperature and wind speed, among which the solar radiation and relative humidity are two main factors that affect the sap flow rate of Caragana korshinskii. The close correlation between daily sap flow rate and meteorological factors in the whole growing season provides us an accurate estimation of the transpiration of Caragana korshinskii and rational water carrying capacity of sand dunes in the revegetated desert areas. Lastly, multiple linear equation of sap flow rate and environmental factors is established through stepwise regression.
Key words:  sap flow      Caragana korshinskii      environmental factors      revegetated desert area     
Received:  26 July 2010      Published:  20 March 2011
ZTFLH:  Q945.17  
Articles by authors
HUANG Lei
ZHANG Zhi-shan
ZHOU Xiao-kun

Cite this article: 

HUANG Lei;ZHANG Zhi-shan;ZHOU Xiao-kun. Stem Sap Flow of Caragana korshinskii and Its Influence Factors in a Revegetated Desert Area. JOURNAL OF DESERT RESEARCH, 2011, 31(2): 415-419.

URL: 

http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2011/V31/I2/415

[1]夏桂敏,康绍忠,李王成,等.甘肃石羊河流域干旱荒漠区柠条树干液流的日季变化[J].生态学报,2006,26(4):6-13.
[2]李新荣,张景光,刘立超,等.我国干旱沙漠地区人工植被与环境演变过程中植物多样性的研究[J].植物生态学报[J].2000,24(3):257-261.
[3]Shen Y C.Consideration and actions for ecology construction in the Loess Plateau[J].Nature,2005:15-19.
[4]夏永秋,邵明安.黄土高原半干旱区柠条(Caragana korshinskii)树干液流动态及其影响因子[J].生态学报,2008,28(4):1376-1382.
[5]陈崇,李吉跃,王玉涛.绦柳树干液流变化及其影响因子研究[J].北京林业大学学报,2008,30(4):82-88.
[6]严昌荣,Downey A,韩兴国,等.北京山区落叶阔叶林中核桃楸在生长中期的树干液流研究[J].生态学报,1999,19(6):793-797.
[7]孙慧珍,周晓峰,赵惠勋.白桦树干液流的动态研究[J].生态学报,2002,22(9):1387-1391.
[8]王瑞辉,马履一,奚如春,等.元宝枫生长旺季树干液流动态及影响因素[J].生态学杂志,2006,25(3):231-237.
[9]王华田,马履一,孙鹏森.油松、侧柏深秋边材木质部液流变化规律的研究[J].林业科学,2002,38(5):31-37.
[10]马履一,王华田,林平.北京地区几个造林树种耗水性比较研究[J].北京林业大学学报,2003,25(2):2-7.
[11]曹云,黄志刚,欧阳志云,等.南方红壤区杜仲树干液流动态[J].生态学报,2006,26(9):2887-2895.
[12]段玉玺,秦景,贺康宁,等.白榆、新疆杨液流动态比较研究[J].中国沙漠,2008,28(6):1136-1144.
[13]周孝明,陈亚宁,李卫红,等.塔里木河下游胡杨树干液流特征研究[J].中国沙漠,2008,28(4):673-678.
[14]司建华,冯起,张小由,等.极端干旱区荒漠河岸林胡杨生长季树干液流变化[J].中国沙漠,2007,27(3):442-447.
[15]张宁南,徐大平,Morris J,等.雷州半岛尾叶桉人工林树液茎流特征的研究[J].林业科学研究,2003,16(6):661-667.
[16]张志山,张小由,谭会娟,等.热平衡技术与气孔计法测定沙生植物蒸腾[J].北京林业大学学报,2007,29(1):60-66.
[17]李新荣,张志山,王新平,等.干旱区土壤植被系统恢复的生态水文学研究进展[J].中国沙漠,2009,29(5):845-852.
[18]张志山,李新荣,王新平,等.沙漠人工植被区蒸腾测定[J].中国沙漠,2005,25(3):374-379.
[19]Wullschleger S D,Meinzer F C,Vertessy R A.A review of whole plant water use studies in trees[J].Tree Physiology,1998,18(8/9):499-512.
[20]潘颜霞,王新平.荒漠人工植被区浅层土壤水分空间变化特征分析[J].中国沙漠,2007,27(2):250-256.
[21]潘颜霞,王新平,苏延桂,等.荒漠人工固沙植被区浅层土壤水分动态的时间稳定性特征[J].中国沙漠,2009,29(1): 81-86.
No Suggested Reading articles found!