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Title
  • ja 多雪域にある湿原の地下水変動について
Alternative
  • VARIATION IN GROUNDWATER LEVEL OF A MIRE IN A SNOWY REGION
Creator

中津川, 誠

NRID 1000010344425

佐藤, 嘉昭

工藤, 啓介

Rights
    • Copyright 2005 土木学会 ダウンロードを含むこの著作物の利用は、著作権法の私的使用及び引用の範囲に限り認められます。その範囲外の利用については、土木学会 の承諾が必要です。
Subject
  • Other bog
  • Other invasion of sasa bamboo
  • Other groundwater variation
  • Other snowmelt
  • Other snowy region
  • NDC 510
Description
Other
  • In Sarobetsu Mire, the groundwater level has been dropping for the past few decades. There is great concern regarding the increase in sasa bamboo distribution and the displacement of the original vegetation. In the region of the mire, snow plays an important role in stabilizing the ground water level, especially in the bog area, because it recharges abundant amount of water to the groundwater. Observation data showed that the ground water level in the bog area is kept high in winter by meltwater recharge from the bottom of the accumulated snow. An attempt was made to analyze the effect of snowmelt on groundwater level variation using a two-dimensional unsteady model. The simulation results indicated that lowering of groundwater level in the bog area could strongly relate to a decrease in snowmelt water. This means that mire conservation must take into account not only artificial influences like reclamation but also climate influences.
Publisher土木学会
Date Created 2016-02-15 , Issued 2005-02
Languagejpn
NIItypejournal article
VersiontypeVoR
Identifier URI http://hdl.handle.net/10258/1508
Relation
  • isIdenticalTo DOI https://doi.org/10.2208/prohe.49.79
  • isIdenticalTo NAID 130003842223
Journal
    • NCID AN10426673
    • ISSN 0916-7374
    • 水工学論文集
    49, 79-84
File
Oaidate2020-02-10T09:11:23Z