首页|胡杨(Populus euphratica)径向生长日变化特征分析

胡杨(Populus euphratica)径向生长日变化特征分析

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利用树木径向生长测定仪、自动气象站和土壤水分自动监测仪,在黑河下游胡杨河岸林内,同步监测了胡杨径向生长日变化和太阳辐射、气温、空气相对湿度及主要根系层土壤水分动态等环境因子.结果表明: 胡杨径向生长日变化呈抛物线形,每日16:00~20:00时达到最低值点,随后逐步上升至翌日06:00~09:00时达到最高值点,完成一个由收缩期、膨胀恢复期和生长期3阶段构成的日变化周期;不同季节,胡杨径向生长变动幅度存在较大差异.就监测样树而言,不同胡杨个体,胸径越大,日净生长量越大.对各环境因子统计表明,胡杨径向生长日变化与总辐射、气温和土壤体积含水率呈负相关关系,与空气相对湿度呈正相关关系.各环境因子对胡杨径向生长影响存在延时滞后作用,特别是土壤水分条件.
Study on the Sub-Diurnal Radial Growth of the Populus euphratica
Using the point-dendrometer, automatic meteorological station and the soil water content monitor, the sub-diurnal radial growth of Populus euphratica , intensity of illumination, air temperature, relative humidity and the soil water bulk content in the main root zone were measured synchronously in the riparian divers-leaf poplar forest in the downstream of Heihe River. It is revealed that: 1) the sub-diurnal radial growth of P. euphratica presents a parabola pattern, reaching the lowest in 16:00 - 20:00, and then increasing gradually to the highest in 06 : 00 - 09 : 00 in the next morning. This diurnal cycle can be divided into contraction, expansion and increment phases; 2) the sub-diurnal radial growth of P. euphratica has large difference among different seasons and specimens. The larger of the specimen's diameter, the larger of the net increment is; 3) the intensity of illumination, air temperature and the soil water bulk content have negative relations to the sub-diurnal radial growth of P. euphratica, and the relative humidity has a positive relation. And among them, the relationships of the intensity of illumination, air temperature and the soil water bulk content at the 20 cm depth reach to a high level of significance. These environmental factors, especially the soil water condition, are all likely have the lagged effect on the radial growth of P. euphratica.

point-dendrometer Populus euphraticasub-diurnal radial growthenvironmental factors

肖生春、肖洪浪、司建华、席海洋

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中国科学院,寒区旱区环境与工程研究所,内陆河流域生态水文重点实验室,阿拉善荒漠生态水文试验研究站,甘肃,兰州,730000

树木径向生长测定仪 胡杨 日变化 环境因子

国家自然科学基金国家科技支撑项目国家科技支撑项目中国科学院知识创新工程项目

409710322006BAD26B022007BAD88B07KZCX2-XB2-04-03

2010

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCDCSCD北大核心
影响因子:2.546
ISSN:1000-0240
年,卷(期):2010.32(4)
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