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標題: 土壤水分特性曲線與不飽和水力傳導度之研究
Study of Soil Water Characteristic curve and Unsaturated Hydraulic Conductivity
作者: 張舒婷
Chang, Shu-Ting
關鍵字: Hydraulic conductivity;水力傳導度;Water characteristic curve;TDR;van Genuchten Model;水分特性曲線;TDR;van Genuchten Model
出版社: 水土保持學系所
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本研究設置水力傳導度室內實驗系統,配合土壤水分特性曲線壓力鍋排水法,得到三種不同土壤質地(砂質壤土、坋質壤土、壤土)之水分特性曲線及不飽和水力傳導度後,使用GOSA軟體擬合van Genuchten Model求得水力傳導度參數,並將擬合所得之傳導度作為室內實驗結果之驗證,以瞭解本研究設置之實驗系統是否足以取代繁雜費時的壓力鍋實驗,並探討在不同質地土壤下van Genuchten Model之適用參數。
本研究中壓力鍋排水所得到水分特性曲線經GOSA軟體擬合vG Model後,得到砂質壤土之α=0.00194、n=2.455;壤土之α=0.00168、n=2.695;粘質壤土之α=0.00137、n=3.151。α值隨砂含量增加而有增加之趨勢。

The experimental system of hydraulic conductivity in the laboratory were setup, and the water characteristic curves were measured by pressure plate. Water characteristic curves and unsaturated hydraulic conductivity of different soil texture (sandy loam, clayey loam, loam) were obtained. The parameters of van Genuchten Model were obtained by curve fitting technique and then to calculate hydraulic conductivity. In order to understand whether this experiment could substitute for the pressure plate, and discusses the usable parameter of these three soils.
The result shows that our experiment can obtain the best water characteristic curve in the clayey loam, next is the sandy loam, latter is the loam. The result of the unsaturated conductivity experiment shows that the most correct experiment is in the clayey loam, next is the loam, latter is the sandy loam.
The parameters of the van Genuchten Model are α=0.00194, n=2.455; α=0.00168, n=2.695; α=0.00137, n=3.151 for sandy loam, loam and clayey loam respectively in this study.
其他識別: U0005-2507200713524900
Appears in Collections:水土保持學系

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