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Forest-hydrological Study on Transpiration in a Mountainous Watershed

Forest-hydrological Study on Transpiration in a Mountainous Watershed
山区流域蒸腾作用的森林水文学研究
批准号:
63560150
负责人:
SUZUKI Masakazu
金额:
$1.6万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for General Scientific Research (C)
财政年份:
1988
资助国家:
日本
项目状态:
已结题
起止时间:
1988 至 1989

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中文摘要
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英文摘要
Attempt has been made to estimate transpiration rate from mountainous watershed using three methods in a forested watershed for detail description on forest transpiration. In the Kiryu Experimental watershed, annual and monthly transpiration rate had been estimated by the short term water budget method and intercepted rainfall observation. In this study, transpiration rate has been estimated using the Penman-Monteith model with the meteorological data observed above the forest canopy in a mixed stand of Japanese Red Pine and Japanese Cypress. Measurement of sap flow velocity using the heat-pulse method also has been carried out around the tower for meteorological observation in the Kiryu watershed.Sap flow velocity using the heat-pulse method has been measured continuously more than two years by an automatic heat-pulse velocity measuring system composed of a handheld computer and a A-D converter with relay switch output. The characteristic of the seasonal variations in transpiration ra … More te estimated by these three methods agreed well one another. Diurnal variations in transpiration estimated by the Penman-Monteith method and by the sap flow measurement also agreed well. However, the relationships between estimated rate by the Penman-Monteith method and sap flow measurement shows a non-linear curve. The reason of the non-linear relationships may caused by the non-linear relationships between the heat-pulse velocity calculated by a simple method and the actual sap flow velocity.For the accurate estimation of transpiration rate using the heat- pulse method, simultaneous observation of heat-pulse method and water absorption rate measurement for a cut tree of Japanese Cypress has been conducted. The relationships between water absorption rate and the heat- pulse velocity calculated by a simple method shows is the nearly same curve as the relationships between estimated value by the Periman-Monteith method and the heat-pulse method. This relationships can be reproduced a simulation model using numerical calculation of an advection-diffusion equation with actual heat-pulse transfer conditions. Less
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Ranpisela,D.A.,Suzuki,M.,Fukushima,Y.: "Application of the Penman-Monteith model to the estimation of the evapotranspiration rate of a forsted watershed." Journal of the Japanese Forestry Society(日本林学会誌). 72. 1-10 (1990)
Ranpisela, D.A.、Suzuki, M.、Fukushima, Y.:“Penman-Monteith 模型在森林流域蒸发蒸腾率估算中的应用。” 日本林业学会杂志 72. 1-10 (1990)。
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小南裕志: 京都大学農学部演習林報告. 60. 190-197 (1987)
小波浩:京都大学农学部森林研究报告 60. 190-197 (1987)。
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通讯作者:
鈴木雅一: 日本林学会誌.
铃木正和:日本林业学会杂志。
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