[1]郭红艳,王百田,靳新红.黄土高原8种树种蒸腾速率与日蒸散量比较[J].水土保持研究,2008,15(02):136-138.
　GUO Hong-Yan,WANG Bai-Tian,JIN Xin-Hong.Studies on Transpiration Rate and Evapotranspiration of 8 Tree Species in the Loess Plateau[J].Research of Soil and Water Conservation,2008,15(02):136-138.
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黄土高原8种树种蒸腾速率与日蒸散量比较

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 15 期数: 2008年02期 页码: 136-138 栏目: 出版日期: 2008-04-20
Title:
Studies on Transpiration Rate and Evapotranspiration of 8 Tree Species in the Loess Plateau
作者:
郭红艳1, 王百田1, 靳新红2
1. 北京林业大学水土保持与荒漠化防治教育部重点实验室, 北京, 100083;
2. 北京市水利规划设计研究院, 北京, 100044
Author(s):
GUO Hong-Yan1, WANG Bai-Tian1, JIN Xin-Hong2
1. Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing Forestry University, Beijing 100083, China;
2. Beijing Institute of Hydraulic Engineering Planning, Design & Research, Beijing 100044, China
关键词:
黄土高原; 造林树种; 蒸腾速率; 蒸散量
Keywords:
the Loess Plateau; main afforestation tree species; transpiration rate; evapotranspiration
分类号:
S715.4
摘要:
以侧柏、华北落叶松、油松、新疆杨、臭椿、核桃、枣树、榆树为研究对象,在2006年7月,对供试苗木进行定时的称重、蒸腾观测.一天中,其平均蒸腾速率的大小为:新疆杨>臭椿>华北落叶松>侧柏>榆树>油松>核桃>枣树,日蒸散量的大小依次为新疆杨>侧柏>臭椿>华北落叶松>油松>核桃>枣树>榆树,蒸腾速率大者蒸腾耗水不一定大,反之亦然.新疆杨、臭椿的耗水量较大;侧柏、落叶松和油松耗水量较少、抗旱性较强;榆树、枣树和核桃,耗水量居中,应大力提倡种植,且作为经济树种可增加当地群众的收入.
Abstract:
The dissertation chose Patycladusorientalis,Larixprinapiam-rupprechtii,Pinus tabulae formis,Populus bolleana,Ailanthusaltissima,Zizyphus jujube,Ulmus pumila and Juglans regia on the Loess Plateau to be our subjects.In July of 2006,we had their transpiration rate and other factors.The results show:in one day,the decreasing orders of average transpiration rate of the eight tree species is Populus bolleanaAilanthus altissimaLarix prinapiam-rupprechtiiPatycladus orientalisUlmus pumilaPinus tabulae formisJ uglans regiaZizyphus jujube.But the decreasing orders of average daily evapotranspiration is Populus bolleanaPatycladus orientalisAilanthus altissimaLarix prinapiam-rupprechtiiPinus tabulaeformisJuglans regiaZizyphus jujubeUlmus pumila.So we can see that the average transpiration rate and the average daily evapotranspiration of the eight tree species is not consistent,when the former was high,the later maybe very low,just so so.The results also show that the Populus bolleana and the Ailanthu saltissima consume more water than other species,Patycladus orientalis,Larix prinapiam-rupprechtii and Pinus tabulaeformis consume lower water,the Ulmus pumila,Zizyphus jujube and Juglans regia don’t consume lots of water and have economic benefit to local people,so they are precede to other tree species.

参考文献/References:

[1] Norman J.Rosenberg.Microclimsate:The Biological Environment[M].John Wiley &Sons.,1974.
[2] 吕一河,傅伯杰.生态学中的尺度及尺度转换方法[J].生态学报,2001,21(12):2096-2015.
[3] 吴钦孝,杨文治.黄土高原植被建设与可持续发展[M].北京:科学出版社,1998:37-70.

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[9]赵安成.陇东黄土高原沟壑区典型小流域治理模式剖析[J].水土保持研究,1994,1(01):45.
　Zhao Ancheng.Analysis of Control Models of Typical Small Watershedin Gully Area of Loess Plateau, the East Part of Gansu Province[J].Research of Soil and Water Conservation,1994,1(02):45.
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备注/Memo

收稿日期:2007-6-5;改回日期:。
基金项目:国家自然科学基金项目(3007063);国家攻关项目(2001BA51080304)
作者简介:郭红艳(1982- ),女,硕士研究生,主要从事生态环境工程研究.E-mail:guohongyan1024@163.com
通讯作者:王百田(1958- ),男,教授.硕士,主要从事林业生态工程、水土保持研究.E-mail:wbaitian@bjfu,edu.cn
通讯作者:王百田(1958- ),男,教授.硕士,主要从事林业生态工程、水土保持研究.E-mail:wbaitian@bjfu,edu.cn

更新日期/Last Update: 1900-01-01