干旱区生态环境知识资源中心(Arid): 风对极端干旱区胡杨蒸腾速率的影响

Arid

	风对极端干旱区胡杨蒸腾速率的影响
其他题名	Effect of wind speed on transpiration rate of Populus euphratica in extreme arid deserts
	赵春彦; 司建华; 冯起; 鱼腾飞; 李培都
来源期刊	冰川冻土
ISSN	1000-0240
出版年	2015
卷号	37 期号:4 页码:1104-1111
中文摘要	以2014年4-11月的胡杨蒸腾速率和风速的实测数据, 分析了风对极端干旱区胡杨蒸腾速率的影响. 结果表明: 不同风速对胡杨蒸腾速率的影响存在差异, 风速的瞬时变动并不一定都会促进蒸腾速率的升高. 0~2 m·s~(-1)风速作用对胡杨蒸腾速率的影响不大; 2~8 m·s~(-1)风速作用下, 胡杨蒸腾速率显著升高, 且随着风速的增大, 蒸腾速率上升幅度增加. 其中, 2~4 m·s~(-1)风速作用下, 其变化幅度较0~2 m·s~(-1)时增加了4.51%; 4~6 m·s~(-1)风速作用下, 其变化幅度较2~4 m·s~(-1)时增加了7.03%; 6~8 m·s~(-1)风速作用下, 其变化幅度较4~6 m·s~(-1)时增加了16.19%. 当风速大于8 m·s~(-1)时, 胡杨蒸腾速率不再上升而呈下降趋势, 且随着风速的增加, 蒸腾速率降低的幅度也越大, 其中, 8~10 m·s~(-1)风速作用下, 蒸腾速率下降了8.08%; 大于10 m·s~(-1)的风速作用下, 胡杨蒸腾速率的下降幅度高达32.91%. 胡杨蒸腾速率和风速的错位相关分析表明, 风速对胡杨蒸腾速率的影响多为实时性的, 在极少数的大风天气影响下, 蒸腾速率恢复的时间较慢, 形成了个别日期的滞后效应. 风速和胡杨蒸腾速率的指数拟合关系最显著, 且2~8 m·s~(-1)风速下, 蒸腾速率随着风速呈指数增加趋势; 8 m·s~(-1)以上风速作用下, 蒸腾速率随着风速的增加呈指数减少趋势. 在0~2 m·s~(-1)风速作用下, 蒸腾速率变化不大.
英文摘要	The transpiration rate of Populus euphratica in relation to wind speed was measured simultaneously in an extreme arid region of Northwest China during 2014 by heat ratio method in an automatic meteorological station. Response of transpiration rate of Populus euphratica to wind speed in extreme arid desert region was analyzed. It is found that the effects of wind speed on transpiration rate of Populus euphratica exist differences. Wind speed not necessarily increase transpiration rate. When wind speed reaches 0-2 m·s~(-1) wind speed has a little effect on transpiration rate. When wind speed reaches in between 2 m·s~(-1) and 8 m·s~(-1) the transpiration rate increases remarkably: compared with the wind speed of 0-2 m·s~(-1), it will increasing 4.51% as the wind speed at 2-4 m·s~(-1); compared with the wind speed of 2-4 m·s~(-1), it will increasing 7.03% as the wind speed at 4-6 m·s~(-1); compared with the wind speed of 4-6 m·s~(-1), it will increasing 16.19% as the wind speed at 6-8 m·s~(-1). Once the wind speed exceeds 8 m·s~(-1), the transpiration rate does not increase but decrease and decrease with weed speed increasing. It will decrease 8.08% and 32.91% when the weed speed exceed 8-10 m·s~(-1) and 10 m·s~(-1), respectively. In addition, it is found that the transpiration rate of Populus euphratica decreases more quickly under strongly wind speed. A correlation analysis show that time lag effect does not existent in most of date. Only under strong wind time lag effect exists owing to a slow transpiration recovery. Moreover, it is found that transpiration rate has an exponential correlation to wind speed.
中文关键词	风速 ; 蒸腾 ; 时滞效应 ; 胡杨
英文关键词	wind speed transpiration time lag Populus euphratica
语种	中文
国家	中国
收录类别	CSCD
WOS类目	AGRICULTURE MULTIDISCIPLINARY
WOS研究方向	Agriculture
CSCD记录号	CSCD:5641837
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/2XILL650/232369
作者单位	中国科学院寒区旱区环境与工程研究所阿拉善荒漠生态水文实验研究站, 中国科学院内陆河流域生态水文重点实验室, 兰州, 甘肃 730000, 中国
推荐引用方式 GB/T 7714	赵春彦,司建华,冯起,等. 风对极端干旱区胡杨蒸腾速率的影响[J]. 中国科学院西北生态环境资源研究院,2015,37(4):1104-1111.
APA	赵春彦,司建华,冯起,鱼腾飞,&李培都.(2015).风对极端干旱区胡杨蒸腾速率的影响.冰川冻土,37(4),1104-1111.
MLA	赵春彦,et al."风对极端干旱区胡杨蒸腾速率的影响".冰川冻土 37.4(2015):1104-1111.