English  |  正體中文  |  简体中文  |  Items with full text/Total items : 75035/106099 (71%)
Visitors : 19428900      Online Users : 448
RC Version 6.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
Scope Tips:
  • please add "double quotation mark" for query phrases to get precise results
  • please goto advance search for comprehansive author search
  • Adv. Search
    HomeLoginUploadHelpAboutAdminister Goto mobile version
    Please use this identifier to cite or link to this item: http://nccur.lib.nccu.edu.tw/handle/140.119/60815


    Title: 不同降雨入滲情境對蓮華池集水區水文模擬之影響
    Other Titles: The Effect of Different Rainfall-Infiltration Circumstances on Hydrological Simulation in the Lien-Hwa-Chi Watersheds
    Authors: 莊永忠;廖學誠;吳治達;詹進發;黃正良
    Chuang,Yung-Chung;Liaw,Shyue-Cherng;Wu,Chih-Da;Jan,Jihn-Fa;Hwong,Jeen-Liang
    Contributors: 政大地政系
    Keywords: 土壤水分演算模式;入滲;流量模擬;土壤體積含水量
    runoff generation mechanism;infiltration;hydrologic simulation;soil moisture content
    Date: 2010-08
    Issue Date: 2013-09-13 12:39:57 (UTC+8)
    Abstract: 本研究分別採用(1)降雨完全入滲與(2)降雨部份入滲兩種不同入滲模擬情境之土壤水分演算模式(Soil Moisture Routing Model, SMR),以南投蓮華池4號與5號集水區爲例,進行1993-1994年逐日流量估算與集水區內土壤體積含水量空間分布模擬,並對照量水堰實測流量與現地土壤含水量調查資料,以檢核兩種降雨入滲情境之模擬效度。數據指出,兩種降雨入滲情境之Nash-Sutcliffe流量模擬效度指數(R^2)差異不大(降雨完全入滲之模擬效度爲0.87與0.80;採降雨部份入滲情境之模擬效度爲0.87與0.78),但採降雨完全入滲情境之土壤體積含水量空間分布推估結果較符合現地實測值。而土壤水分演算模式無論採用何種入滲情境進行模擬,於濕季與土壤水分消退時段均具較高之流量預測能力;但乾季時其演算過程則可能受集水區地表複雜度與土壤層含水量急劇變化影響,而產生較差之模擬效果。綜合上述研究成果,可發現降雨完全入滲之設定較適用於蓮華池4號與5號集水區。
    Two different circumstances, total rainfall and partial rainfall infiltrating into soil layers, are applied in this research. We apply the Soil Moisture Routing Model (SMR) for hydrologic simulation in Lien-Hwa-Chi Watershed No. 4 and No. 5 during the period between 1993 and 1994, and compare the quantity of streamflow and spatial distribution of soil water content counted from both different circumstances. Results show that different circumstances produce almost equal accuracy of streamflow simulation. The values of Nash-Sutcliffe efficiency are 0.87 and 0.80 for the total rainfall infiltrating into soil circumstance for Watershed No. 4 and No. 5 respectively; while the values are 0.87 and 0.78 based on the partial rainfall infiltrating into soil circumstance. Comparing the different seasons, these two circumstances produce better efficiencies of streamflow simulation during wet season. Moreover, comparing the distribution of soil moisture content on watersheds, the total rainfall infiltrating into soil circumstance is more reasonable. Overall, the total rainfall infiltrating into soil mechanism is more suitable for the hydrologic simulation in the Lien-Hwa-Chi watersheds, including quantity of runoff generation and soil moisture content.
    Relation: 地理學報, 59, 39-66
    Data Type: article
    Appears in Collections:[地政學系] 期刊論文

    Files in This Item:

    File Description SizeFormat
    593966.pdf2302KbAdobe PDF488View/Open


    All items in 政大典藏 are protected by copyright, with all rights reserved.


    社群 sharing

    著作權政策宣告
    1.本網站之數位內容為國立政治大學所收錄之機構典藏,無償提供學術研究與公眾教育等公益性使用,惟仍請適度,合理使用本網站之內容,以尊重著作權人之權益。商業上之利用,則請先取得著作權人之授權。
    2.本網站之製作,已盡力防止侵害著作權人之權益,如仍發現本網站之數位內容有侵害著作權人權益情事者,請權利人通知本網站維護人員(nccur@nccu.edu.tw),維護人員將立即採取移除該數位著作等補救措施。
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - Feedback