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  1. 防災科研関係論文

地表面温度を用いた土壌熱物性値及び地中熱流量の逆推定法の提案

https://nied-repo.bosai.go.jp/records/6656
https://nied-repo.bosai.go.jp/records/6656
c8dc0785-ce5f-4eab-a01d-3edc686cc7b6
Item type researchmap(1)
公開日 2024-06-03
タイトル
言語 ja
タイトル 地表面温度を用いた土壌熱物性値及び地中熱流量の逆推定法の提案
タイトル
言語 en
タイトル Direct Estimation of Ground Thermometric Parameter and Ground Conductive Heat Flux, from Ground Surface Temperature
著者 森脇 亮

× 森脇 亮

ja 森脇 亮

en MORIWAKI Ryo

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神田 学

× 神田 学

ja 神田 学

en KANDA Manabu

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横山 仁

× 横山 仁

ja 横山 仁

en Yokoyama Hitoshi

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抄録
内容記述タイプ Other
内容記述 The object of this study is to develop a method for estimating both the ground thermometric parameter (ρ c λ) and ground conductive heat flux (G) simultaneously by using the ground surface temperature (Ts). This method is based on the Fourier series expressions of the result of heat transfer equation. The method is tested by a field-measurement. The following results are obtained: 1) The estimated ρ c λ have a reasonable value. 2) Estimated diurnal variations of G agree very well with that observed. 3) The spatial distribution of ρ c λ is also estimated from the surface temperature distribution obtained by the thermo-graphy.
言語 ja
抄録
内容記述タイプ Other
内容記述 The object of this study is to develop a method for estimating both the ground thermometric parameter (ρ c λ) and ground conductive heat flux (G) simultaneously by using the ground surface temperature (Ts). This method is based on the Fourier series expressions of the result of heat transfer equation. The method is tested by a field-measurement. The following results are obtained: 1) The estimated ρ c λ have a reasonable value. 2) Estimated diurnal variations of G agree very well with that observed. 3) The spatial distribution of ρ c λ is also estimated from the surface temperature distribution obtained by the thermo-graphy.
言語 en
書誌情報 ja : 水工学論文集
en : PROCEEDINGS OF HYDRAULIC ENGINEERING

号 41, p. 1097-1100, 発行日 1997
出版者
言語 ja
出版者 公益社団法人 土木学会
出版者
言語 en
出版者 Japan Society of Civil Engineers
ISSN
収録物識別子タイプ ISSN
収録物識別子 0916-7374
DOI
関連識別子 10.2208/prohe.41.1097
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