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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 鄭舒婷(Su-Ting Cheng) | |
dc.contributor.author | Jia-Ying Dai | en |
dc.contributor.author | 戴嘉瑩 | zh_TW |
dc.date.accessioned | 2021-05-20T00:50:38Z | - |
dc.date.available | 2025-08-17 | |
dc.date.available | 2021-05-20T00:50:38Z | - |
dc.date.copyright | 2020-09-17 | |
dc.date.issued | 2020 | |
dc.date.submitted | 2020-08-17 | |
dc.identifier.citation | 中央氣象局(2020)。臺灣的災害性天氣。取自:https://www.cwb.gov.tw/Data/prevent/taiwan_prevent.pdf。 江昭輝、簡光佑、莊秉潔、黨美齡、李育棋、洪景山、郭珮萱、蔡徵霖(2015)。台灣區域土壤含水率觀測網之建置與資料分析。大氣科學,43(2),133–150。 行政院農委會農業試驗所(2010)。土壤資源空間資料標準(編號:NGISTD–ANC–016–2010.3)。 行政院農業委員會(2015)。2015農業灌溉白皮書。 吳怡瑩、劉哲欣、張志新(2013)。降雨量與表層土壤含水量關係之研究。社團法人中華水土保持學會102年度年會。 於幼華(2002)。環境科學大辭典。台北:文景書局。 林俐玲、黃國鋒(2011)。台灣中部崩塌地土壤水份滲透特性之研究。坡地防災學報,10(1),27–41。 財團法人農業工程研究中心(2016)。因應氣候變遷調適水利與農業跨域合作之探討。臺北市:經濟部水利署。 陳明杰(2003)。全球變遷:福山森林生態係研究─試驗集水區飽和與不飽和土壤水分移動之研究。臺北市:國立臺灣大學森林環境暨資源學系。 童慶斌、陳主惠(2001)。臺灣地區合理之蒸發散折算係數與區域蒸發散量估算方法之建立(1/2)及(2/2)。經濟部水資源局計畫報告。臺北市:經濟部水資源局。 楊清富(2014)。土壤水分感測技術及應用。臺南區農業專訊,87,18–21。 詹佳彬(2001)。應用時域反射儀觀測福山地區坡面土壤水分反應之研究。國立臺灣大學碩士論文。 臺灣省政府農林廳山地農牧局(1983)。新竹縣山坡地土壤調查報告。南投縣:臺灣省政府農林廳山地農牧局。 蔡呈奇、張瑀芳、許佳雯、杜清澤(2008)。臺灣地區森林土壤管理組之研擬。宜蘭大學生物資源學刊,4,99–107。 鍾閔光。SWAT 模式功能分析與探討–以來社溪集水區為例。中興大學水土保持學系所學位論文。 鍾閔光、林俐玲(2015)。土壤水文評估模式之介紹。水土保持學報,47(4),1539–1549。 Abrahams, A. D., Parsons, A. J. (1991). Relation between infiltration and stone cover on a semiarid hillslope, southern Arizona. Journal of Hydrology, 122(1), 49–59. Amundson, R., Berhe, A. A., Hopmans, J. W., Olson, C., Sztein, A. E., Sparks, D. L. (2015). Soil and human security in the 21st century. Science, 348(6235), 1261071. Brady, N. C., Weil, R. R. (2010). Elements of the nature and properties of soils. Pearson Prentice Hall. Breitenecker, F. (1997). An introduction to mathematical modelling. Brocca, L., Morbidelli, R., Melone, F., Moramarco, T. (2007). Soil moisture spatial variability in experimental areas of central Italy. Journal of Hydrology, 333(2–4), 356–373. Brocca, Luca, Ciabatta, L., Massari, C., Camici, S., Tarpanelli, A. (2017). Soil moisture for hydrological applications: Open questions and new opportunities. Water (Switzerland), 9(2). Brooks, R. H., Corey, A. T. (1964). Hydraulic properties of porous media. Colorado State University. Buckingham, E. (1907). Studies on the Movement of Soil Moisture. In Bulletin (United States. Bureau of Soils), no. 38. (p. 61). U.S. Government Printing Office. Cameira, M. R., Fernando, R. M., Pereira, L. S. (2003). Soil macropore dynamics affected by tillage and irrigation for a silty loam alluvial soil in southern Portugal. Soil and Tillage Research, 70(2), 131–140. Casta, P., Chopart, J. L., Janeau, J. L., Valentin, C. (1989). Mesure du ruissellement sur un sol gravillonnaire de Cote-d’Ivoire apres six ans de culture continue avec ou sans labour. Agronomie Tropicale, 44(4), 255–262. Chaturvedi, R. K., Raghubanshi, A. S., Tomlinson, K. W., Singh, J. S. (2017). Impacts of human disturbance in tropical dry forests increase with soil moisture stress. Journal of Vegetation Science, 28(5), 997–1007. Chen, C., Hu, K., Ren, T., Liang, Y. (2017). A Simple Method for Determining the Critical Point of the Soil Water Retention Curve. Soil Science Society of America Journal, 81(2), 250. Cheng, L. P., Liu, W. Z. (2014). Long Term Effects of Farming System on Soil Water Content and Dry Soil Layer in Deep Loess Profile of Loess Tableland in China. Journal of Integrative Agriculture, 13(6), 1382–1392. Cheng, S., Huang, J., Ji, F., Lin, L. (2017). Uncertainties of soil moisture in historical simulations and future projections. In Journal of Geophysical Research (Vol. 122, Issue 4, pp. 2239–2253). Croney, D., Coleman, J. D. (1961). Pore pressure and suction in soil. In Proc. of the Conf. on Pore Pressure and Suction in Soils, 31–37. Daly, E., Porporato, A. (2005). A Review of Soil Moisture Dynamics: From Rainfall Infiltration to Ecosystem Response. Environmental Engineering Science, 22(1), 9–24. Darcy, H. (1856). Les fontaines publiques de la ville de Dijon: exposition et application des principes à suivre et des formules à employer dans les questions de distribution d’eau. Victor Dalmont. Devia, G. K., Ganasri, B. P., Dwarakish, G. S. (2015). A Review on Hydrological Models. Aquatic Procedia, 4, 1001–1007. Entekhabi, D., Rodriguez-Iturbe, I. (1994). Analytical framework for the characterization of the space-time variability of soil moisture. Advances in Water Resources, 17(1), 35–45. Famiglietti, J. S., Rudnicki, J. W., Rodell, M. (1998). Variability in surface moisture content along a hillslope transect: Rattlesnake Hill, Texas. Journal of Hydrology, 210(1), 259–281. Fan, J., McConkey, B., Janzen, H., Wang, H. (2016). Root distribution by depth for temperate agricultural crops. Field Crops Research, 189, 68–74. Fayer, M. J. (2000). UNSAT-H Version 3.0: Unsaturated Soil Water and Heat Flow Model. Theory , User Manual , and Examples. Model Manual, June, 184. Forrester, J. W. (1997). Industrial Dynamics. Journal of the Operational Research Society, 48(10), 1037–1041. Foster, G. R. (1982). Modeling the erosion process. Hydrologic Modeling of Small Watersheds, 297–380. Fredlund, D. G. (1967). Comparison of Soil Suction and one-dimensional consolidation characteristics of a highly plastic clay. In Canadian Geotechnical Journal. Gray, D., Norum, D. (1967). The effect of soil moisture on infiltration as related to runoff and recharge. Proceedings of Hydrology Symposium, November(6), 133–153. Gupta, H. V., Bastidas, L. A., Sorooshian, S., Shuttleworth, W. J., Yang, Z. L. (1999). Parameter estimation of a land surface scheme using multicriteria methods. In Journal of Geophysical Research Atmospheres (Vol. 104, Issue D16, pp. 19491–19503). Gysi, M., Klubertanz, G., Vulliet, L. (2000). Compaction of an Eutric Cambisol under heavy wheel traffic in Switzerland — field data and modelling. Soil and Tillage Research, 56(3), 117–129. Hacke, U. G., Sperry, J. S., Ewers, B. E., Ellsworth, D. S., Schäfer, K. V. R., Oren, R. (2000). Influence of soil porosity on water use in Pinus taeda. Oecologia, 124(4), 495–505. Hannon, B., Ruth, M. (2014). Modeling Dynamic Biological Systems. In Modeling dynamic biological systems (pp. 3–28). Springer, Cham. Hardie, M. A. (2011). Effect of antecedent soil moisture on infiltration and preferential flow in texture contrast soils. University of Tasmania. Haverkamp, R., Debionne, S., Angulo-Jaramillo, R., de Condappa, D. (2016). Soil properties and moisture movement in the unsaturated zone. In The handbook of groundwater engineering. Heber Green, W., Ampt, G. A. (1911). Studies on Soil Phyics. The Journal of Agricultural Science, 4(1), 1–24. Hillel, D. (2013). Fundamentals of soil physics. Academic Press. Jackson, C., Xia, Y., Sen, M. K., Stoffa, P. L. (2003). Optimal parameter and uncertainty estimation of a land surface model: A case study using data from Cabauw, Netherlands. Journal of Geophysical Research D: Atmospheres, 108(D18). Jiang, M. H., Lin, T. C., Shaner, P. J. L., Lyu, M. K., Xu, C., Xie, J. S., Lin, C. F., Yang, Z. J., Yang, Y. S. (2019). Understory interception contributed to the convergence of surface runoff between a Chinese fir plantation and a secondary broadleaf forest. Journal of Hydrology, 574, 862–871. Jury, W. A., Horton, R. (1991). Soil physics. John Wiley Sons. Jyrkama, M. I., Sykes, J. F. (2007). The impact of climate change on spatially varying groundwater recharge in the grand river watershed (Ontario). Journal of Hydrology, 338(3), 237–250. Klute, A., Klute, A., Dirksen, C. (1986). Hydraulic Conductivity and Diffusivity: Laboratory Methods. Methods of Soil Analysis: Part 1 Physical and Mineralogical Methods, 687–734. Lebedeff, A. F. (1927). The movement of ground and soils waters. First In Ternational Congress of Soil Science Procedings, 1, 459–494. Li, B., Rodell, M., Zaitchik, B. F., Reichle, R. H., Koster, R. D., van Dam, T. M. (2012). Assimilation of GRACE terrestrial water storage into a land surface model: Evaluation and potential value for drought monitoring in western and central Europe. Journal of Hydrology, 446–447, 103–115. Liu, H. H., Birkholzer, J. (2012). On the relationship between water flux and hydraulic gradient for unsaturated and saturated clay. Journal of Hydrology, 475(510), 242–247. Liu, H., Zhao, W., He, Z., Zhang, L. (2007). Stochastic modelling of soil moisture dynamics in a grassland of Qilian Mountain at point scale. Science in China Series D Earth Sciences, 50, 1844–1856. Lu, N., Godt, J. W., Wu, D. T. (2010). A closed-form equation for effective stress in unsaturated soil. Water Resources Research, 46(5), 1–14. Luckner, L., Van Genuchten, M. T., Nielsen, D. R. (1989). A consistent set of parametric models for the two‐phase flow of immiscible fluids in the subsurface. Water Resources Research, 25(10), 2187–2193. Millington, R. J., Quirk, J. P. (1961). Permeability of porous solids. Transactions of the Faraday Society, 57, 1200–1207. Moriasi, D., Arnold, J., Van Liew, M., Bingner, R., Harmel, R. D., Veith, T. (2007). Model Evaluation Guidelines for Systematic Quantification of Accuracy in Watershed Simulations. Transactions of the ASABE, 50(3), 885–900. Mualem, Y. (1976). A new model for predicting the hydraulic conductivity of unsaturated porous media. Water Resources Research, 12(3). Nunes, J. P., Seixas, J., Keizer, J. J., Ferreira, A. J. D. (2009). Sensitivity of runoff and soil erosion to climate change in two Mediterranean watersheds. Part II: assessing impacts from changes in storm rainfall, soil moisture and vegetation cover. Hydrological Processes, 23(8), 1212–1220. Osunbitan, J. A., Oyedele, D. J., Adekalu, K. O. (2005). Tillage effects on bulk density, hydraulic conductivity and strength of a loamy sand soil in southwestern Nigeria. Soil and Tillage Research, 82(1), 57–64. Panigrahi, B., Panda, S. N. (2003). Field test of a soil water balance simulation model. Agricultural Water Management, 58(3), 223–240. Peek, A. J., Watson, J. D. D. (1979). Hydraulic conductivity and flow in non-uniform soil. Workshop on Soil Physics and Field Heterogeneity, 31–39. Peng, F., Mu, M., Sun, G. (2020). Evaluations of Uncertainty and Sensitivity in Soil Moisture Modeling on the Tibetan Plateau. Tellus, Series A: Dynamic Meteorology and Oceanography, 72(1), 1–16. Petropoulos, G. P. (2013). Remote sensing of energy fluxes and soil moisture content. CRC Press. Philip, J. R., De Vries, D. A. (1957). Moisture movement in porous materials under temperature gradients. Eos, Transactions American Geophysical Union, 38(2), 222–232. Poesen, J., Ingelmo-Sanchez, F. (1992). Runoff and sediment yield from topsoils with different porosity as affected by rock fragment cover and position. Catena, 19(5), 451–474. Rawls, W. J., Brakensiek, D. L., Saxtonn, K. E. (1982). Estimation of Soil Water Properties. Transactions of the ASAE, 25(5), 1316–1320. Ray, R. L., Jacobs, J. M. (2008). Landslide susceptibility mapping using remotely sensed soil moisture. International Geoscience and Remote Sensing Symposium (IGARSS), 3(1), 2–4. Ray, R. L., Jacobs, J. M., de Alba, P. (2010). Impacts of Unsaturated Zone Soil Moisture and Groundwater Table on Slope Instability. Journal of Geotechnical and Geoenvironmental Engineering, 136(10), 1448–1458. Remesan, R., Mathew, J. (2016). Hydrological data driven modelling. Springer International Pu. Richards, B. G. (1965). Measurement of the free energy of soil moisture by the psychrometric technique using thermistors (pp. 39–46). Richards, L. A. (1931). Capillary conduction of liquids through porous mediums. Journal of Applied Physics, 1(5), 318–333. Richards, L., Weaver, L. (1944). Moisture retention by some irrigated soils as related to soil moisture tension. Journal of Agricultural Research, 69(6), 215–234. Rodriguez-Iturbe, I, Porporato, A., Ridolfi, L., Isham, V., Coxi, D. R. (1999). Probabilistic modelling of water balance at a point: the role of climate, soil and vegetation. Proceedings of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 455(1990), 3789–3805. Rodriguez-Iturbe, Ignacio, Entekhabi, D., Bras, R. L. (1991). Nonlinear Dynamics of Soil Moisture at Climate Scales: 1. Stochastic Analysis. Water Resources Research, 27(8), 1899–1906. Roels, J. M. (1984). Flow resistance in concentrated overland flow on rough slope surfaces. Earth Surface Processes and Landforms, 9(6), 541–551. Rosolem, R., Gupta, H. V., Shuttleworth, W. J., de Gonçalves, L. G. G., Zeng, X. (2013). Towards a comprehensive approach to parameter estimation in land surface parameterization schemes. Hydrological Processes, 27(14), 2075–2097. Russam, K. (1958). An investigation into the soil moisture conditions under roads in Trinidad, BWI. Géotechnique, 8(2), 57–71. Saito, H., Šimůnek, J., Mohanty, B. P. (2006). Numerical Analysis of Coupled Water, Vapor, and Heat Transport in the Vadose Zone. Vadose Zone Journal, 5(2), 784. Sakai, M., Jones, S. B., Tuller, M. (2011). Numerical evaluation of subsurface soil water evaporation derived from sensible heat balance. Water Resources Research, 47(2), 1–17. Saraiva, J. P., Lima, B. S., Gomes, V. M., Flores, P. H. R., Gomes, F. A., Assis, A. O., Reis, M. R. C., Araújo, W. R. H., Abrenhosa, C., Calixto, W. P. (2017). Calculation of sensitivity index using one-at-a-time measures based on graphical analysis. 2017 18th International Scientific Conference on Electric Power Engineering (EPE), 1–6. Sentís, I. P. (1997). A soil water balance model for monitoring soil erosion processes and effects on steep lands in the tropics. Soil Technology, 11(1), 17–30. Shaver, T. M., Peterson, G. A., Sherrod, L. A. (2003). Cropping intensification in dryland systems improves soil physical properties: regression relations. Geoderma, 116(1), 149–164. Simic, E., Destouni, G. (1999). Water and solute residence times in a catchment: Stochastic-mechanistic model interpretation of 18O transport. Water Resources Research, 35(7), 2109–2119. Soares, J. V, Almeida, A. C. (2001). Modeling the water balance and soil water fluxes in a fast growing Eucalyptus plantation in Brazil. Journal of Hydrology, 253(1–4), 130–147. Strobbia, C., Cassiani, G. (2007). Multilayer ground-penetrating radar guided waves in shallow soil layers for estimating soil water content. Geophysics, 72(4), J17–J29. Susha Lekshmi, S. U., Singh, D. N., Shojaei Baghini, M. (2014). A critical review of soil moisture measurement. Measurement, 54, 92–105. Tan, K. H. (2009). Environmental soil science (3rd ed.). CRC Press. Traff, D. C., Niemann, J. D., Middlekauff, S. A., Lehman, B. M. (2015). Effects of woody vegetation on shallow soil moisture at a semiarid montane catchment. Ecohydrology, 8(5), 935–947. van Genuchten, M. T. (1980). A Closed-form Equation for Predicting the Hydraulic Conductivity of Unsaturated Soils1. Soil Science Society of America Journal, 44(5), 892. van Genuchten, M. T., Leij, F. J., Yates, S. R. (1991). The RETC code for quantifying the hydraulic functions of unsaturated soils. Vanapalli, S. K. (1996). Simple test procedures and their interpretation in evaluating the shear strength of an unsaturated soil. Veihmeyer, F. J., Hendrickson, A. H. (1928). Soil moisture at permanent wilting of plants. Plant Physiology, 3(3), 355–357. Veihmeyer, F. J., Hendrickson, A. H. (1931). The moisture equivalent as a measure of the field capacity of soils. Soil Science, 32(3), 181–193. Vereecken, H. (1995). Estimating the unsaturated hydraulic conductivity from theoretical models using simple soil properties. Geoderma, 65(1–2), 81–92. Wang, T., Kumar, S., Bárdossy, A. (2019). On the use of the critical event concept for quantifying soil moisture dynamics. Geoderma, 335, 27–34. Wild, A. (1993a). Soils and the Environment. Cambridge University Press. Wild, A. (1993b). Soils and the Environment. Cambridge University Press. Wilson, G. W., Fredlund, D. G., Barbour, S. L. (1994). Coupled soil-atmosphere modelling for soil evaporation. Canadian Geotechnical Journal, 31(2), 151–161. Xie, Z., Yuan, F., Duan, Q., Zheng, J., Liang, M., Chen, F. (2007). Regional Parameter Estimation of the VIC Land Surface Model: Methodology and Application to River Basins in China. Journal of Hydrometeorology, 8(3), 447–468. Yang, L., Wei, W., Chen, L., Jia, F., Mo, B. (2012). Spatial variations of shallow and deep soil moisture in the semi-arid Loess Plateau, China. Hydrology and Earth System Sciences, 16(9), 3199–3217. Ziadat, F. M., Taimeh, A. Y. (2013). Effect of rainfall intensity, slope, land use and antecedent soil moisture on soil erosion in an arid environment. Land Degradation Development, 24(6), 582–590. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/8243 | - |
dc.description.abstract | 土壤水分動態在自然界中扮演十分重要的角色,如地表與地中的能量交換等,易受雨量、氣溫及地文等條件影響,對森林及集水區管理而言,是個重要的考量因子。然而,相較其他地面水文的資料,臺灣土壤水的現地資料相對短缺。為能有效評估土壤水分動態,本研究欲建立一淺層土壤水系統動態模型,藉由物理機制模擬不同土壤質地下不同深度的淺層土壤水含水率,以及入滲、滲漏、蒸發、飽和流及漫地流等水文過程。於模型建立後,本研究於玉峰集水區設置四個樣區,用以校正與驗證本模型,並驗證此模型的可行性與精確度。 研究結果發現利用物理機制所建立而成的淺層土壤水動態模型,以玉峰集水區現地土壤水資料做校正與驗證,可得到擬合度佳且具可信度的小時土壤水模擬。該地區的淺層土壤水的實測值介於1.50 %~35.40 %,模擬值介於3.00 %~43.40 %,模擬結果的平均誤差(ME)介於-2.33~2.38,平均絕對誤差(MAE)介於1.08~6.24,均方根誤差(RMSE)介於1.37~8.15,平均絕對百分比偏差(MAPE)介於28.31 %~57.78 %。依據敏感度分析結果顯示,雨量、含石率、孔隙形狀參數、飽和含水率、田間含水率及細切土層數等皆為土壤含水率及各水文過程變化的敏感因子。 本研究新建立的淺層土壤水動態模型,利用當地氣候觀測資料及土壤性質特性,模擬土壤水含量的小時變化,可協助補足土壤水資料不足的情況。此外,因本模型係以物理機制為基礎,能夠適用於多數場域,並具有分析未來氣候變遷情境的潛力,對於農業、災害等議題,可提供相關水文過程及土壤水變動等資訊,作為決策參考。 | zh_TW |
dc.description.abstract | The soil moisture dynamics plays a key role in natural processes, such as heat exchange between surface and subsurface, and response to the magnitude of precipitation, air temperature and landscape conditions. As such, the soil moisture has been considered as an important factor for forest and watershed management. However, compared to surface hydrological measurements, soil moisture information is very scarce in many watershed areas in Taiwan. To provide soil moisture estimations, I constructed a physically–based model considering multiple processes, including infiltration, percolation, evaporation, saturation and overland flow, to simulate soil moisture at various depths in different soil textures. Modeling results were calibrated and validated with field measurements from four sampling sites in the Yufeng watershed, to examine the feasibility and accuracy of the model. Calibration and validation results from the Yufeng watershed showed that the dynamic shallow soil moisture model performed well in providing reasonable well-fitted and reliable simulations of soil water contents in an hourly time frame. The field measurements of the soil water contents were between 1.50 % to 35.40 %, while the simulation results ranged between 3.00 % to 43.40 %. Modeling mean error (ME) ranged between -2.33 to 2.38, mean absolute error (MAE) between 1.08 to 6.24, root mean square error (RMSE) between 1.37 to 8.15, and mean absolute percentage error (MAPE) between 28.31 % to 57.78 %. Based on the sensitivity analysis, precipitation, soil–gravel mixture content, shape parameter, saturated water content, field water capacity and divided layers appeared critical factors to influence the soil moisture dynamics and the associated hydrological processes. In sum, this newly constructed dynamic shallow soil moisture model uses meteorological data and soil information to simulate hourly change of soil water contents, and can be applied to assist the provision of required soil water information that were often insufficient in many places. As the model is based on physical mechanisms, it can be generally applied to other regions. More importantly, it has the ability to provide forecasts dealing with agricultural or natural disaster issues in future climate change scenarios to find mitigation strategies, and to offer science–based information for decision making copping with potential changes in hydrological processes and soil moistures. | en |
dc.description.provenance | Made available in DSpace on 2021-05-20T00:50:38Z (GMT). No. of bitstreams: 1 U0001-1208202012473200.pdf: 92359161 bytes, checksum: 70c023cdc0d2b5d47c819e2539e00680 (MD5) Previous issue date: 2020 | en |
dc.description.tableofcontents | 口試委員會審定書 I 謝誌 II 中文摘要 IV Abstract V 目錄 VII 圖目錄 X 表目錄 XIII 第一章 緒論 1 1.1 研究背景與動機 1 1.2 研究目的 3 第二章 文獻回顧 4 2.1 地下水文模型類別與發展 4 2.2 地下水文模型基本概念 6 2.2.1 土壤組成 7 2.2.2 孔隙率(Porosity) 7 2.2.3 土壤質地(Soil texture) 8 2.2.4 土系(Soil series) 9 2.2.5 土壤含水量(Soil water content) 9 2.2.6 水力傳導係數(Hydraulic conductivity) 12 2.2.7 水勢能(Water potential) 12 2.2.8 水分特性函數(Water characteristic function) 13 第三章 材料與方法 15 3.1 研究架構 15 3.2 研究流程 15 3.3 淺層土壤水動態模型之建立 17 3.3.1 模型概述與架構 17 3.3.2 模型建構工具簡介 28 3.3.3 模型校正與驗證 28 3.4 淺層土壤水動態模型之應用 30 3.4.1 試驗地概述 30 3.4.2 驗證樣區土壤質地測試 33 3.4.3 土壤含水率測定 36 3.4.4 模型設定 37 3.5 敏感度分析(Sensitivity analysis) 39 3.5.1 敏感度分析方法 39 3.5.2 模型參數敏感度分析 40 第四章 結果 41 4.1 Stella Architect模型展示 41 4.2 模型校正與驗證 42 4.2.1 樣區A、B、C之校正與驗證 42 4.2.2 測試樣區—樣區T之驗證 53 4.3 各樣區水文過程及含水率模擬結果 56 4.3.1 水文過程模擬結果 56 4.3.2 含水率模擬結果 59 4.4 敏感度分析 63 4.4.1 含水率(VWC)分析結果 65 4.4.2 入滲量(I)分析結果 69 4.4.3 滲漏量(qp)分析結果 71 4.4.4 蒸發量(E)分析結果 72 4.4.5 飽和流量(qs)分析結果 73 4.4.6 漫地流量(Q)分析結果 74 第五章 討論 79 5.1 水文過程中各因子之影響 79 5.1.1 土壤水分傳輸及滲漏 79 5.1.2 入滲及超滲漫地流 83 5.1.3 蒸發 83 5.1.4 飽和流及飽和漫地流 87 5.2 模型應用 87 5.3 誤差討論與研究限制 89 第六章 結論與建議 92 引用文獻 93 | |
dc.language.iso | zh-TW | |
dc.title | 淺層土壤水動態模型之建立與應用 | zh_TW |
dc.title | Dynamic Shallow Soil Moisture Model Development and Applications | en |
dc.type | Thesis | |
dc.date.schoolyear | 108-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 張斐章(Fi-John Chang),黃國文(Gwo-Wen Hwang),鄭智馨(Chih-Hsin Cheng) | |
dc.subject.keyword | 土壤含水率,物理模型,系統動態,水文過程,土壤含水率分佈,敏感度分析, | zh_TW |
dc.subject.keyword | Soil moisture,Physically–based model,System dynamics,Hydrological processes,Soil moisture distribution,Sensitivity analysis, | en |
dc.relation.page | 103 | |
dc.identifier.doi | 10.6342/NTU202003072 | |
dc.rights.note | 同意授權(全球公開) | |
dc.date.accepted | 2020-08-18 | |
dc.contributor.author-college | 生物資源暨農學院 | zh_TW |
dc.contributor.author-dept | 森林環境暨資源學研究所 | zh_TW |
dc.date.embargo-lift | 2025-08-17 | - |
顯示於系所單位: | 森林環境暨資源學系 |
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