Received July 12, 2013/ revised August 7, 2013/ accepted September 25, 2013
Copyright ⵑ 2013 by the Korean Society of Civil Engineers
This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/by-nc/3.0)
ǣǣȀȀǤǤȀͳͲǤͳʹͷʹȀ ǤʹͲͳ͵Ǥ͵͵ǤǤʹʹͺͷ Ǥ ǤǤ
⽾㬖⟖Ⳃ#≾ᦗ#㬲⛛ᤶⴖ#ᇚ⇚(II): 㬦⭏#㡷⛯
ْȵଗ୨ȵ୨ଵࢂ
Kim, Nam Won*, Kim, Youn Jung**, Chung, Il-Moon***
Development of Analyzing Model of Groundwater Table Fluctuation(II): Characteristics of Recharge
ABSTRACT
In this study, daily based groundwater recharge was estimated under unsteady state by using groundwater table fluctuation model developed by Kim et al. (2013). This technique analyzes groundwater variation characteristics by using reaction factor related with groundwater flow and specific yield related with recharge. For the application of this model, measured groundwater level at JD Yongdam 1 and JW Konghang for 5 years were used. This model can estimate daily based groundwater recharge and the computed groundwater levels showed good agreement with measured groundwater levels. At JD Yongdam 1 and JW Konghang, the estimated recharges (rates) were 520.4904.0mm (32.761.8%) and 447.4633.4mm (24.045.1%), respectively. The developed model can be suggested as an efficient and precise method to estimate daily based groundwater recharge by using groundwater level data.
Key words : Groundwater level, Groundwater recharge, Reaction factor, Specific yield
Ⅹಾ
ᅙᩑǍᨱᕽ۵Kim et al. (2013)ᯕ}ၽ⦽ᇡᱶඹᔢ┽ᨱᕽ᮹ḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙᮥᯕᬊ⦹ᩍ݉᭥eᄥ⧉᧲పᮥᔑᱶ⦹ᩡ݅. ḡ⦹ᙹ᭥
ᄡ࠺⧕ᕾ༉ߙᮡḡ⦹ᙹ᮹⮱ŝšಉࡽၹ᮲ĥᙹ᪡⧉᧲ᨱšಉࡽእᔑ⇽ᮉᮥๅ}ᄡᙹಽᯕᬊ⦽݅. ⧕ᕾ༉ߙ᮹ᱢᬊᮥ᭥⧕ᱽᵝࠥ⦽ḡ ᩎ᮹š⊂ᱶᵲvᬑᨱݡ⦽ၹ᮲ᯕ᧲⪙⦽JW Ŗ⧎ŝJD ᬊݕ1ḡᱱᨱݡ⦽5֥(2006-2010)e᮹ḡ⦹ᙹ᭥š⊂ᯱഭෝᯕᬊ⦹ᩡ݅. ḡ⦹ᙹ᭥
⧕ᕾ༉ߙᮡǎḡᱢᯙȽ༉ᨱᕽ᮹݉᭥eᄥ(ᯝᄥ) ⧉᧲పᔑᱶᯕa܆⦹໑ḡ⦹ᙹ᭥ᯱഭ᪡እƱ⦽đŝ, ⧉᧲పŝๅ}ᄡᙹaḡ⦹ᙹ᭥ෝ
ၹᩢ⦹Łᯩᨩ݅. ⧉᧲పᔑᱶđŝJD ᬊݕ1 ḡᱱᮡ520.4904.0mm (32.761.8%), JW Ŗ⧎ḡᱱᮡ447.4633.4mm (24.045.1%) ಽӹ┡ԍ݅. }ၽࡽ⧕ᕾ༉ߙᮡḡ⦹ᙹ᭥ᯱഭෝᯕᬊ⦹ᩍๅ}ᄡᙹෝ⇵ᱶŝ݉᭥eᄥ⧉᧲పᮥᔑᱶ⦹۵ႊᦩᮝಽ⪽ᬊࡹʑෝʑݡࡽ݅.
áᔪᨕ ḡ⦹ᙹ᭥, ḡ⦹ᙹ⧉᧲, ၹ᮲ĥᙹ, እᔑ⇽ᮉ
1. ᕽು
ḡ⦹ᙹ⧉᧲పᮡḡᩎ᮹ḡ⦹ᙹšญĥ⫮ၰᙹᯱᬱᱶ₦ᙹพᯕa܆⦹ࠥಾ⦹ʑ᭥⦽ᵲ⦽ᗭᯕ໑ᙹᯱᬱᨱݡ⦽ḡ⦹ᙹ᮹᳕ᖒᯕ
ⓑḡᩎᯝᙹಾᬒᵲ⦽᮹ၙෝw۵݅. ✚⯩ᱽᵝࠥᨱ۵ྜྷᔑᨦᯕ⪽ᖒ⪵ࡹᨕḡ⦹ᙹ᮹ᙹa᷾a⦹ᩍḡ⦹ᙹ᮹ᦩᱶᱢᯙŖɪŝ
ᙹప ⪶ᅕෝ ᭥⦽ šญa Ǎࡽ݅.
Cho and Park (2008)ᨱ໕ 1990֥ݡ ᯕ⬥ ḡ⦹ᙹ᮹⧉᧲పᮥ ᗱᛞí ʑ ᭥⧕ ᱥℕ vᬑపᵲ ⧉᧲పᯕ ₉ḡ⦹۵ እᮉᮥ
սėॡ
‘ḡ⦹ᙹ⧉᧲ᮉ’ᯕ⦹ᩍ⪽ᬊࡹŁᯩ݅. K-water (2003)ᨱ
໕ᱽᵝࠥ᮹⧉᧲పᮥⅾvᙹప᮹46.1%ಽaᱶ⦹ᩍᱢᬊ⦹ᩡ݅.
ə్ӹḡ⦹ᙹ⧉᧲ᮡๅḩ᮹ᙹญḡḩ⦺ᱢᩢ⨆ᮥၼʑভྙᨱ
Ŗeᱢaᄡᖒᮥaḥ݅. ᕽzᮡḡᩎᯕࠥǎḡᱢᮝಽ
݅᧲⦽sᮥaḡအಽḡ⦹ᙹ⧉᧲పᮥᔑᱶ⦹ʑ᭥⧕ᕽ۵݉᭥
eᄥ ⧉᧲పᮥ ᔑᱶ⦹ᩍ Ƚࡹᨕ ⦽݅.
⩥ᰍ⧉᧲పᔑᱶᮥ᭥⧕ᱢᬊ⦹۵ႊჶᮝಽ۵ᙹྙᖒᇥᇥญჶ, ʑᱡᮁ⇽ᇥญჶ, ḡ⦹ᙹ᭥ᄡ࠺ჶ, ḡ⦹ᙹ᭥ᄡ࠺༉ߙ॒ᱢᬊࡹ۵
}ֱᨱ ݅᧲⦹í ᇥඹࡹŁ ᯩ݅. b ⇵ᱶႊჶॅᮡ ᵝᨕḥ
⪹ĞᨱⓍíᩢ⨆ᮥၼᮝ໑, ᩑǍᯱӹᩑǍ}ֱᨱᔢݡᱢ ᯙ ᪅₉᪡ ᰆ݉ᱱᯕ ᳕ᰍ⦹ʑࠥ ⦽݅(Yun et al., 2009).
ḡ⦹ᙹ᭥ ᄡ࠺ᯱഭෝ ᯕᬊ⦽ ႊჶ᮹ ݡ⢽ᱢᯙ ᮁ⩶ᮝಽ۵
Healy and Cook (2002)ᨱ᮹⧕ᱽᦩࡽvᙹၽᔾ⦹۵ḡ⦹ᙹ᭥
᮹ᄡ⪵పᨱݡᙹ⊖᮹እᔑ⇽ශᮥŒ⦹ᩍḡ⦹ᙹ⧉᧲పᮥᔑ⇽⦹
۵ ḡ⦹ᙹ᭥ ᄡ࠺ჶᯕ ᯩ݅. ᯕᨱࠥ }ֱŝ ᱢᬊႊჶᨱ
ḡ⦹ᙹ᭥ v⦹ჶ, ٥ᱢḡ⦹ᙹ᭥ v⦹ჶ, ॒᮹ ݅᧲⦽ ⋎ᮝಽ
ᔍᬊࡹŁᯩ݅(Choi et al., 2011; Healy and Cook, 2002; Kim et al., 2010; Choi and Ahn, 1998; Moon and Woo, 2001).
ᯕႊჶॅᮡ✚ᱶᔢੱ۵⦹vǍeᨱݡ⦹ᩍ⧉᧲ᮉᮥᔑᱶ⦹
ᩍᱥǍeᨱᱢᬊ⦹အಽ⧉᧲పᯕŝ⇵ᱶࡹÑӹ݉ʑe᮹⧉᧲ప
ᮥᔑᱶ⧁ᙹᨧ݅۵⦽ĥaᯩ݅. ᯕᨱࠥCho and Park (2008)ᨱ
᮹⧕ ᱽࡽ ∊ḥŖɚᮉᮥ ᯕᬊ⦽ ḡ⦹ᙹ᭥ ᄡ࠺ ༉ߙᯕ ᯩ݅.
ᱽᦩ⦽ ᮡ ᯕುᱢ ɝÑෝ ᱽ⦹Ł ᯩᮝӹ ๅ}ᄡᙹ ᔑᱶ
ᇡᙹᱢᯙ᳑ᔍၰᝅ⨹ᯕǍࡽ݅. ᔢʑᨱʑᚁ⦽ၵ᪡zᯕ⧉᧲ప
⇵ᱶᨱݡ⦽ฯᮡᩑǍaḥ⧪ࡹŁᯩᮝӹbᔑᱶჶॅᮡᙹᔢ᮹
᪅ඹ᪡ᱢᬊᔢ᮹⦽ĥෝḡܭ݅. ə్ӹḡ⦹ᙹ᭥ᄡ࠺ᯱഭෝᯕᬊ
⦹۵ႊჶᮡᙹྙᖒᇥᇥญჶ᮹᷾ÑᯱഭᯕŁʑᱡᮁ⇽ჶŝࠥᯝš ᖒᮥᮁḡ⦹໑ᬒᯕš⊂ᯱഭᨱ᯦b⦽ႊჶᯕ۵ᱱᨱᕽ∊ᇥ
⯩Łₑ⧁⦥aᯩ݅. ᯕ᪡zᮡ݉ᱱᮥᅕ᪥⦹۵ႊჶᮝಽKim et al., (2013)ᮡ⧉᧲ŝḡ⦹ᙹ᭥ᩩ⊂ᮥ᭥⦽ḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉
ߙᮥᱽ⦹ᩡ۵ߑᯕ۵ḡ⦹ᙹ⮱ŝšಉࡽၹ᮲ĥᙹ᪡ḡ⦹ᙹ
⧉᧲ŝšಉࡽእᔑ⇽ᮉᮥʑၹᮝಽ⧕ᕾ⦽݅. ᅙᩑǍᨱᕽ۵Kim et al., (2013)ᯕ}ၽ⦽ḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙᮥᱢᬊ⦹ᩍǎḡᱢ
Ƚ༉᮹݉᭥eᄥ⧉᧲పᮥᔑᱶ⦹Łə✚ᖒᮥȽ⦹Łᯱ⦽݅.
⧕ᕾ༉ߙᮥᱢᬊ⦹ʑ᭥⧕, ᱽᵝࠥ✚ᄥᯱ⊹ࠥᙹᯱᬱᅙᇡᨱᕽᬕ
ᩢᵲᯙᱽᵝࠥḡᩎ᮹⦽⦹ඹḡᱱᵲJD ᬊݕ1ŝJW Ŗ⧎ḡᱱ᮹
ḡ⦹ᙹ᭥ᯱഭෝᯕᬊ⦹ᩡ݅. ᯕෝᯕᬊ⦹ᩍbš⊂ḡᱱ᮹ḡ⦹ᙹ
᭥᮹ ᄡ࠺ᮥ ᳭ᬑ⦹۵ ๅ}ᄡᙹᯙ ၹ᮲ĥᙹ(reaction factor)᪡
እᔑ⇽ᮉ(specific yield)ᮥ⇵ᱶ⦹ᩍᇡᱶඹᔢ┽ᨱᕽ᮹⧉᧲ప
ၰ ⧉᧲✚ᖒᨱ ݡ⦹ᩍ ם⦹ᩡ݅.
2. ḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙ᮹}
2.1 ࣡ܛැজࡦ܄ଭԹڄ
De Zeeuw and Hellinga (1958)۵݉᭥e(ⱀt)࠺ᦩ᮹⧉᧲ప (Rⱀt)ᯕᯝᱶ⦹݅Łaᱶ⧁ভ, ᇡᱶඹᔢ┽ᨱᕽ᮹ḡ⦹ᙹ᭥ᄡ࠺
ᮥ ᱽᦩ⦹ᩡ݅. ᯕ۵ ḡ⦹ᙹ᭥ෝ ᱥ ḡ⦹ᙹ᭥(hi-1)᪡ ၹ᮲ĥᙹ,
⧉᧲ప əญŁ ݡᙹ⊖᮹ እᔑ⇽ᮉᨱ ݡ⦽ ᮝಽ ⢽⩥ࡽ݅. ᅙ
ᩑǍᨱᕽ۵ᯕෝḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙ᮹ʑᅙᮝಽ⦹ᩍ݉᭥
eᄥ ⧉᧲పᮥ ᔑᱶ⦹ᩡ݅(Kim et al., 2013).
ƆƇá ƆƇ àÎãà ķƒäâ ćÕ×׳ķ
«ƒÞÎ à ãà ķƒäß
(1)
ᩍʑᕽhi۵iᯝᨱᕽ᮹ḡ⦹ᙹ᭥(L), hi-1۵i-1ᯝᨱᕽ᮹ḡ⦹ᙹ᭥
(L), ⶸt۵݉᭥e(T), Rⶸt۵݉᭥eᨱᕽ᮹ݡᙹ⊖⧉᧲ప(L) ᯕ݅.
2.2 ઑ߆ॺ୨ࢺ࣑
De Zeeuw and Hellinga (1958)aᱽᦩ⦹۵ḡ⦹ᙹ᭥ᄡ࠺ᮥ
ᄡ⩶⦹ᩍ⧉᧲పᮥᔑᱶ⦹ᩡᮝ໑݉᭥e࠺ᦩ᮹⧉᧲ప, Rⱀtᨱ
ݡ⧕ ݅ ᱶญ⦹໕ Eq. (2)᪡ zᯕ ⢽⩥ࡽ݅.
«ƒá ćåƆƇà ƆƇ àÎÎ à ãà ķƒäãà ķƒäæZ Õ×׳ķ (2)
ᯕভ, ᩑᗮᱢᯙḡ⦹ᙹ᭥š⊂ᯱഭෝ⫮ा⦽݅໕hi, hi-1ᨱᕽ᮹
ḡ⦹ᙹ᭥sᮥᯕᬊ⦹ᩍๅ}ᄡᙹᯙၹ᮲ĥᙹ(ⱕ, reaction factor)
᪡እᔑ⇽ᮉ(µ, specific yield)ᮥ⇵ᱶ⧉ᮝಽ៉ᇡᱶඹᔢ┽ᨱᕽ᮹
݉᭥eᄥ ⧉᧲ప(Rⱀt)ᮥ ᔑᱶ⧁ ᙹ ᯩ݅.
2.3 ࢱଦծॺ୨
ᇡᱶඹḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙᨱ۵ࢱ}᮹ๅ}ᄡᙹaᯩ۵ߑ
əᵲ᮹⦹ӹaၹ᮲ĥᙹ(ⱕ, reaction factor)ಽ, ݡᙹ⊖ᨱᕽḡ⦹ᙹ ᮹ ႑⇽⩶┽ෝ ᖅ⦹۵ ᯙᯱᯕ݅.
อ᧞, ⧉᧲ᯕᨧ݅Łaᱶ⧁ভḡ⦹ᙹa႑⇽ࢉᨱḡ⦹ᙹ᭥
۵⦹v⦹íࡹ۵ߑ, ᯕভ᮹qᙹłᖁᮥᯕᬊ⦹ᩍၹ᮲ĥᙹෝᔑᱶ
⦽݅. ݅ั⧕Eq. (1)ᮡ⧉᧲ᯕᨧ۵Ğᬑ(Rⱀt= 0ᯝĞᬑ)ᨱ
݉᭥eⱀtෝ1 day⦹໕ḡ⦹ᙹ᭥ᯱഭෝᯕᬊ⦹ᩍၹ᮲ĥᙹෝ
ᔑᱶ⧁ ᙹ ᯩí ࡽ݅.
ķ á Þ ćƆƇ
ƆƇ àÎ
ß (3)
Fig. 1. Location of Groundwater Monitoring Wells in Jeju Island (Figure from Kim et al. (2013))
(a) (b)
Fig. 2. Observed Rainfall and Groundwater Level at JD Yongdam1(a) and JW Konghang(b)
2.4 णॺౢଘॺ୨ࢺ࣑
༉ߙ᮹ࢱჩṙๅ}ᄡᙹ۵እᔑ⇽ᮉ(µ, specific yield)ಽ, ᯕ۵
ḡ⦹ᙹ᮹⧉᧲✚ᖒᮥӹ┡ԕ۵ᵝᯙᯱᯕ݅. Eq. (1)ᮥእᔑ⇽ᮉ ᨱ ݡ⧕ ᱶญ⦹໕ Eq. (4)ŝ zᯕ ⢽⩥⧁ ᙹ ᯩ݅.
ł á ćÕ××ķÞƆƇà ƆƇ àÎãà ķƒäß
«ƒÞÎ àãàķƒäß
(4)
ə్ӹEq. (4)᮹እᔑ⇽ᮉᮡၹ᮲ĥᙹ᪡⧉᧲పᮥၙญᦥ
⦹ʑভྙᨱḢᱲᔑᱶ⧁ᙹᨧ݅. ʑ᳕ᩑǍᨱᕽ۵⧉᧲పݡᝁᨱ
vᙹపᮥᱲ༊⦹ӹᅙᩑǍᨱᕽ۵ḡ⦹ᙹ᮹⧉᧲ᨱ᮹⦽ၽᔾ⦹۵
ḡ⦹ᙹ᭥ᔢǍeᨱݡ⧕ᙹྙ༉⩶(SWAT-K)ᨱᕽ᮹ษḡส☁
᧲⊖ᨱᕽ᮹⋉ࡽ᧲ᯕ༉ࢱ⧉᧲ࡽ݅Łaᱶ⦹ᩍᯕෝ⧉᧲పᮝ ಽᯕᬊ⦹ᩡ݅. ᙹྙ༉⩶(SWAT-K)᮹ᇥᕾđŝ۵Chung et al.
(2011)ᯕᇥᕾ⦽⦽ᮁᩎᯱഭෝᯕᬊ⦹ᩡ݅. እᔑ⇽ᮉᮡǍeᄥ
ḡ⦹ᙹ᭥ᄡ࠺ᯱഭ᪡ᙹྙ༉⩶᮹⋉పᮥᯕᬊ⦹ᩍᅕᱶᮥ⦹ᩍ
⧕ᕾ༉ߙᨱ ᱢᬊ⦹ᩡ݅.
3. ᩑǍḡᩎ
⧕ᕾ༉ߙ᮹ ᱢᬊᮥ ᭥⧕ ᱽᵝࠥ᮹ ⦽ᮁᩎᮥ ᖁᱶ⦹ᩡᮝ໑
ḡ⦹ᙹ᭥ᯱഭ۵ᱽᵝࠥ✚ᄥᯱ⊹ࠥᙹᯱᬱᅙᇡ(www.jejuwater.
go.kr)ᨱᕽᬕᩢᵲᯙJD ᬊݕ1, JW Ŗ⧎ḡᱱ᮹š⊂ᯱഭෝᯕᬊ⦹
ᩡ݅(Fig. 1). ḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙᮡḡ⦹ᙹ᭥ᯱഭෝᯕᬊ⦹ᩍ
⧉᧲పᮥᔑᱶ⦹ʑভྙᨱᝅ⊂ᯱഭᨱݡ⦽᮹᳕ࠥaๅᬑ׳݅.
ᕽvᬑᨱݡ⦽ᙹ᭥ᄡ⪵aӹ┡ӹ۵∊ᱢ⊖ᨱš⊂ḡᱱᮥ
ᖁᱶ⦹ᩡ݅(Kim et al., 2013).
ᱽᵝࠥ᮹ᇢᵲᦺ⧕ᦩaᨱ᭥⊹⦽⦽ᮁᩎᮡ᳑໕⩥ྕᦵඹ
᪡᳑໕ᦵၰ⩥ྕᦵඹಽǍᖒࡹᨕᯩ۵ߑ, ✚⯩⩥ྕᦵᨱၽݍ⦽
ⓕญ⍅⊖ᯕḡ⦹ᙹ᮹⧉᧲ŝᮁ࠺ᨱᵲ⇵ᩎ⧁ᮥ⦽݅. ᯕ్⦽ᱽᵝ ᮹ḡḩ⦺ᱢ✚ᖒᮡḡ⦹ᙹ᮹⋉⚍᪡⧉᧲ᨱᮁญ⦹ᩍ┡ԕයḡᩎ ᅕ݅ ⧉᧲పᯕ Ⓧí ӹ┡ӽ݅(Choi et al., 2011).
Fig. 2۵JD ᬊݕ1ŝJW Ŗ⧎ḡᱱ᮹ᝅ⊂ḡ⦹ᙹ᭥᪡vᙹప
ᯱഭෝӹ┡ԙäᯕ݅. vᙹ۵ᱽᵝvᬑš⊂ᗭ᮹ᯱഭᯕ໑ḡ⦹ᙹ
᭥۵bḡᱱᨱᕽ5֥e(2006-2010) š⊂⦽ᯱഭᯕ݅. ḡ⦹ᙹ᭥᪡
vᙹᯱഭ᪡᮹šĥෝšₑ⦽đŝࢱḡᱱ༉ࢱvᬑᨱݡ⦽ᙹ᭥
ᔢၹ᮲ᯕෙäᮝಽӹ┡ԍ݅. ੱ⦽ḡ⦹ᙹ᭥qᙹ᪡ᔢǍe ᯕ૽ಘ⦹íӹ┡ӹ༉ߙᱢᬊᨱᬊᯕ⦽äᮝಽ❱݉ࡹᨩ݅. ᯱഭa
đ⊂ࡽǍeᨱݡ⧕ᕽ۵ᖁ⩶ᅕe⦹ᩍᯱഭෝᅕ᪥⦹ᩡ݅. 2007֥
᮹ ḡ⦹ᙹ᭥ ᯱഭ ᵲ ݉ʑeᨱ vᙹపᯕ ɪ᷾⦹ᩍ ḡ⦹ᙹ᭥᮹
ᔢᇡa℉ࢱ⩶┽ಽๅᬑɪĞᔍෝᯕŁᯩ۵ߑᯕ۵݉ʑeᨱ
ԕฑ݅ప᮹vᙹಽᯙ⧕ၽᔾ⦽ḡ⦹ᙹ᭥ᔢŝš⊂ᱶᨱvᙹa
Ḣᱲᱢᮝಽ ᮁ᯦ࢉᮝಽᕽ ŝ⊂ᱶࡹᨕ ӹ┡ӽ đŝಽ ❱݉ࡽ݅.
ḡ⩶ᱢᮝಽᯙᱲ⦽ࢱš⊂ḡᱱᮡvᙹ᪡ḡ⦹ᙹ᭥ᄡ࠺⩶┽۵
ᱥၹᱢᮝಽ ᮁᔍ⦽ ⩶┽ෝ ᅕᯕŁ ᯩ݅.
4. ⧉᧲ᇥᕾ
ḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙᨱᱢᬊ⦹ᩍJD ᬊݕ1, JW Ŗ⧎ḡᱱᨱ ᕽ᮹݉᭥eᄥ⧉᧲పᮥᔑᱶ⦹ᩡ݅. ᔑᱶࡽḡ⦹ᙹ᮹ᯝᄥ⧉᧲
పᮥ ᯕᬊ⦹ᩍ ᳑ᔍḡᱱ᮹ ⧉᧲⩶┽ ၰ ✚ᖒᮥ ᔕ⠕ᅕᦹ݅. ᅙ
⧕ᕾ༉ߙ᮹ᝅᱽᱢᬊa܆ᖒᨱݡ⧕ᇥᕾ⧕ᅕᦹᮝ໑ᔑᱶࡽๅ}
Table 1. Applied Parameters
Location Reaction factor(쩀) Specific yield(쩋)
JD Yongdam1 0.039 0.023
JW Konghang 0.028 0.009
c
d
(a)
c
d
(b)
Fig. 3. Observed Groundwater Level and Simulated Recharge at JD Yongdam1(a) and JW Konghang(b)
Table 2. Estimated Recharge at JD Yongdam1
Date Precipitation (mm)
Simulated recharge (mm)
Recharge ratio (%) (Year) (Months)
2006
1~3 271.7 99.1 36.5
4~6 190.8 135.9 71.2
7~9 1,414.5 280.8 19.9
10~12 262.8 183.4 69.8
Total 2,139.8 699.2 32.7
2007
1~3 237.0 131.6 55.5
4~6 162.4 111.4 68.6
7~9 988.4 346.0 35.0
10~12 221.5 315.0 142.2
Total 1,609.3 904.0 56.2
2008
1~3 222.6 170.0 76.4
4~6 445.4 175.1 39.3
7~9 353.4 135.2 38.2
10~12 152.3 89.0 58.4
Total 1,173.7 569.3 48.5
2009
1~3 186.4 103.3 55.4
4~6 308.4 109.0 35.4
7~9 479.2 161.0 33.6
10~12 167.2 147.1 88.0
Total 1,141.2 520.4 45.6
2010
1~3 219.6 130.0 59.2
4~6 396.8 176.9 44.6
7~9 638.0 303.6 47.6
10~12 151.2 258.1 170.7
Total 1,405.6 868.7 61.8
ᄡᙹෝᯕᬊ⦹ᩍ⧉᧲పᮥᔑᱶ⦹ᩡ݅. JD ᬊݕ1ŝJW Ŗ⧎ḡᱱ᮹
⧉᧲పᇥᕾᨱᯕᬊࡽḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙ᮹ๅ}ᄡᙹ۵Table 1ŝ z݅.
4.1 ઑଭ෴
Fig. 3ᮡࢱḡᱱᨱݡ⧕᳑ᔍʑe࠺ᦩ᮹ᯝᄥvᙹపŝ⧉᧲ప
ᮥࠥ⦽đŝᯕ݅. vᬑపᨱ⧉᧲పᯕ۹ᨕӹḡอvᬑa
ၽᔾ⦹ḡᦫ۵ʑeᨱࠥ⧉᧲ᯕᯝᨕӹŁᯩ۵äᮥᙹᯩ݅.
ᯕ۵ᦿᕽᖅ⦽ၵ᪡zᯕ⧉᧲ᮡ☁᧲⊖ŝእ⡍⪵ݡෝᯕ࠺⦹۵
ີ⍅ܩ᷹ᨱ ᮹⧕ၽᔾ⦹໑ ๅḩ᮹ ✚ᖒᨱ᮹⧕ ə ᧲ŝ⩶┽a
đᱶࡽ݅۵äᮥၹ᷾⦹۵äᯕ݅. ࢱḡᱱ᮹⧉᧲⩶┽ෝᔕ⠕ᅕ໕
ᱥℕᱢᯙ ⧉᧲᮹ ᄡ⪵᧲ᔢᮡ ᮁᔍ⦹í ӹ┡۵ߑ ᯕ۵ Fig. 2᮹
ḡ⦹ᙹ᭥š⊂ᯱഭᨱᕽࠥᙹᯩ۵äౝḡ⦹ᙹ᭥ᄡ࠺᧲ᔢᯕ
እ⦽ࢱḡᱱᯕအಽ⧉᧲ࡹ۵ŝᱶࠥᮁᔍ⦹݅۵äᮥӹ┡ԙ݅.
ə్ӹFig. 3᮹(d)᪡zᯕᯕᄅ✙vᬑᨱෙ݉ʑe᮹⧉᧲
᧲ᔢᮡ ݅ᗭ₉ᯕෝ ᅕᯕ۵ߑ ᯕ۵⋉⚍ࡽ ᧲ᯕ ☁᧲⊖ᮥ☖⧕
ᯕ࠺⦹۵ŝᱶᨱ⧉᧲ŝ႑⇽᮹⩶┽aݍḡʑভྙᯕ݅.
݅ั⧕, ᯙɝḡᩎᯕ⦹ࠥݡᙹ⊖᮹ᙹญḡḩ⦺ᱢ✚ᖒᨱ
ๅ}ᄡᙹa ݍᲙ ၽᔾ⦹۵ äᯕ݅.
ᅙᩑǍᨱᕽᱽ⦽༉ߙᮥᯕᬊ⦹ᩍᔑᱶ⦽⧉᧲పᵲᯝᇡa
ᮭᙹੱ۵0᮹sᮝಽӹ┡ӹFig. 3᮹(c)᪡zᯕ݅ప᮹vᬑ
⬥⧉᧲ᮥ⇵ᱶ⦹ḡ༜⦹۵Ğᬑaၽᔾ⦹ʑࠥ⦽݅. ᯕᨱݡ⧕
⩥ᰍಽᕽ۵םญᱢᯙᖅᯕᨕಅᬑ໑༉ߙᯱℕ᮹᪅₉ᯕÑӹv ᙹ᪡ḡ⦹ᙹ᭥š⊂ᯱഭ᮹᪅ඹੱ۵⧉᧲పᅕ݅႑⇽ࡹ۵᧲ᯕ
ฯᦥӹ┡ӹ۵⩥ᔢᮝಽ⇵ᱶ⧁ᙹᯩᮝӹᯕ⩥ᔢᨱݡ⧕ᕽ۵
⇵aᱢᯙ ᩑǍa ᯕᨕᲙ ⧁ äᮝಽ ᅕᯙ݅.
4.2 ઑ߆
Tables 2 and 3ᮡḡ⦹ᙹ᭥ᄡ࠺ᯱഭෝᯕᬊ⦹ᩍᯝᄥಽᔑᱶࡽ
⧉᧲పᮥ ᇥʑᄥ, ᩑᄥಽ ⧊ᔑ⦹ᩍ ӹ┡ԙ đŝᯕ݅.
JD ᬊݕ1ḡᱱ᮹⧉᧲పᇥᕾđŝෝᔕ⠕ᅕ໕, ᱥၹᱢᮝಽ1~3
ᬵᨱ aᰆ ԏí ӹ┡ӹŁ ᱱᱱ ᷾a⦹݅a 7~9ᬵᨱ aᰆ ׳í
ӹ┡ӽ݅. 2007֥ᮡ1~6ᬵʭḡ۵ԏíӹ┡ӹŁ9~12ᬵʭḡĥᗮ
Table 3. Estimated Recharge at JW Konghang
Date Precipitation (mm)
Simulated recharge (mm)
Recharge ratio (%) (Year) (Months)
2006
1~3 271.7 92.7 34.1
4~6 190.8 110.4 57.8
7~9 1,414.5 183.6 13.0
10~12 262.8 126.3 48.1
Total 2,139.8 513.0 24.0
2007
1~3 237.0 100.9 42.6
4~6 162.4 91.5 56.4
7~9 988.4 213.8 21.6
10~12 221.5 207.2 93.5
Total 1,609.3 613.4 38.1
2008
1~3 222.6 125.8 56.5
4~6 445.4 126.6 28.4
7~9 353.4 121.7 34.4
10~12 152.3 99.5 65.3
Total 1,173.7 473.6 40.4
2009
1~3 186.4 97.7 52.4
4~6 308.4 105.0 34.1
7~9 479.2 124.9 26.1
10~12 167.2 119.8 71.7
Total 1,141.2 447.4 39.2
2010
1~3 219.6 107.6 49.0
4~6 396.8 137.3 34.6
7~9 638.0 209.7 32.9
10~12 151.2 178.8 118.2
Total 1,405.6 633.4 45.1
(a)
(b)
(c)
(d)
Fig. 4. Comparison of Rainfall and Simulated Recharge at JD Yongdam 1 :(a) Daily, (b) Monthly, (c) Quarterly, (d) Annual
⧉᧲పᯕ׳ᦥḡ۵ߑᯕ۵ᯕᱥvᬑ᮹ᩢ⨆ᮝಽᔢ⦽ḡ⦹ᙹᨱ
᮹⦽äᮝಽᅕᩍḥ݅. ᩑࠥᄥⅾ⧉᧲పᮡ520.4ⴇ904.0mmಽ
ӹ┡ԍ݅. 2008֥ᨱaᰆᱢí⧉᧲ࡹᨩᮝ໑ᯕʑ᮹vᙹప
ᩎԏíӹ┡ԍ݅. 2006֥ŝ2007֥᮹vᙹ᪡⧉᧲పᮥእƱ⧕
ᅕ໕, vᙹపᮡ2006֥ᯕ2,139mmಽฯᮝӹ⧉᧲పᮡ2007֥
ᨱ⧉᧲పᯕ׳íӹ┡ԍ݅. ᯕ۵2006֥᮹7~9ᬵe᮹Ḳᵲࡽ
vᙹ᮹݅ᙹa⧉᧲ࡹḡ ༜⦹Łḡ⢽ᮁ⇽ᯕӹḢᱲᮁ⇽॒ᮝಽ
႑⇽ࡹᨕ ӹ┡ӽ äᮝಽ ❱݉ࡽ݅.
ᩑ݉᭥᮹vᬑݡእ⧉᧲ప᮹እෝᔕ⠕ᅕ໕32.7ⴇ61.8(%)ᔍ ᯕಽӹ┡ԍ݅. ੱ⧉᧲పŝݍญ7~9ᬵᯕԏíӹ┡۵ߑᯕ۵
7~9ᬵ࠺ᦩԕฑvᙹపᯕ┡ʑᅕ݅⍅⧉᧲పᯕ₉ḡ⦹۵እᮉ ᯕԏíӹ┡ӽäᯕ݅. ၹݡಽ10~12ᬵᯕ׳ᮡእᮉᮥᅕᯕ໑
ᯝᇡʑ۵100%ෝⅩŝ⦹ᩍӹ┡ӹʑࠥ⦹۵ߑᯕ۵ĉᬙ℁
vᙹపᮡ ԏᦥḡŁ ᯕᱥ 7~9ᬵ ࠺ᦩ ԕฑ vᬑᨱ ᮹⦽ ḡℕࡽ
(a) (b)
(c) (d)
Fig. 5. Comparison of Rainfall and Simulated Recharge at JW Konghang :(a) Daily, (b) Monthly, (c) Quarterly, (d) Annual
⧉᧲ŝḡ⦹ᙹ⮱ᨱ᮹⦽ᩢ⨆ᮝಽ❱݉ࡽ݅. ə్ӹᯕ్⩥ᔢᯕ
ᯝၹᱢᯙ äᯙḡᨱ ݡ⦽ ❱݉ᮡ ⪶⊹ ᦫ݅.
JW Ŗ⧎ḡᱱ᮹⧉᧲పᇥᕾđŝෝᔕ⠕ᅕ໕, ᱥၹᱢᮝಽᱱᱱ
᷾a⦹݅a7~9ᬵᨱaᰆ׳íӹ┡ӹŁ݅ĉᬙ℁qᗭ⦹۵
᧲ᔢᮝಽJD ᬊݕ1ḡᱱŝᮁᔍ⦽⩶┽ಽӹ┡ӽ݅. ᩑࠥᄥ⧉᧲ప
ᮡ447.4ⴇ633.4mmಽӹ┡ԍ݅. JW Ŗ⧎ḡᱱᨱᕽࠥJD ᬊݕ1ḡ ᱱŝ࠺ᯝ⦹í2010֥10~12ᬵᔍᯕ᮹⧉᧲ᮉᯕ100%ෝⅩŝ⦹
ᩍӹ┡ԍ݅. ᯙɝḡᩎᯙJD ᬊݕ1ŝእƱ⧁ভ⧉᧲పŝ⧉᧲ᮉᯕ
₉ᯕෝ ᅕᯕ۵ߑ ࢱ ḡᱱ᮹ ᯱഭ᮹ ᪅ඹᯕÑӹ ḡ⦹ᙹ᮹ Ñ࠺
⩶┽aݍӹ┡ӹ۵⩥ᔢᮝಽ❱݉ࡽ݅. JW Ŗ⧎ḡᱱ᮹vᬑݡ እ⧉᧲ప᮹እෝᔕ⠕ᅕ໕ᩑᄥ⧉᧲እ۵24.0ⴇ45.1(%)ᔍᯕಽ, ᱥၹᱢᮝಽ JD ᬊݕ1ḡᱱᅕ݅ ԏí ӹ┡ԍ݅.
4.3 ઑন
Figs. 4~5۵⧉᧲పᮥᯝᄥ(a), ᬵᄥ(b), ᇥʑᄥ(c), ᩑᄥ(d)ಽ
ӹ٥ᨕvᙹపŝ⧉̹ࠥ⦽đŝᯕ݅. bḡᱱᨱᕽ᮹ᯝᄥ⧉᧲ప
ᮡvᙹపŝᯝᱶ⦽ᔢšᖒᮥᅕᯕḡᦫ۵݅. ᬵᄥᨱᕽᇥʑᄥಽ
⧉᧲ప⧊ᔑʑeᯕʙᨕḩᙹಾᔢšᖒᯕᯩᨕᅕᯕӹᇥᔑᩎ
Ⓧíӹ┡ԍ݅. Tables 2 and 3ᨱᕽᅝᙹᯩॐvᙹపݡእ⧉᧲ప
᮹እᮉᯕๅ֥ݍญӹ┡ԉᮥᙹᯩ݅. ੱFigs. 4 and 5᮹
(c)᪡(d)ᨱᕽᙹᯩॐ, vᙹప᮹᷾aa⧉᧲ప᮹᷾aಽḢđࡹ
ḡᦫ۵äᮥᙹᯩ݅. vᙹపᯕ☁᧲⊖᮹⋉⚍܆ᮥⅩŝ⦹໕
ḡ⢽⦹ಽ⋉⚍⦹ḡ༜⦹ŁḢᱲᮁ⇽॒ᮝಽᯙ⧕⮹్ӹaʑভྙ
ᨱ⧉᧲పᯕ᷾a⦹۵ߑ⦽ĥaᯩ݅. ᕽvᙹప᮹ᯝᱶእᮉᮥ
⧉᧲పᮝಽaᱶ⦹ᩍ⧉᧲ᮥᖅ⦹۵äᮡฯᮡ᪅₉ෝ⡍⧉⦹í
ࡹအಽ⧉᧲పᔑᱶ݉᭥eᄥᨱෙ ⧉᧲పᮥᱢᬊ⦹ᩍ
ᝁᖒᮥ ׳ᯝ ᙹ ᯩᮥ äᯕ݅.
5. ᧞ၰđು
Ŗeᱢᮝಽᄡ࠺⦹۵ḡ⦹ᙹ⧉᧲పᮥᔑᱶ⦹ʑ᭥⧕ǎḡᱢ
Ƚ༉᮹݉᭥eᄥḡ⦹ᙹ⧉᧲పᮥᔑᱶ⦹Łᯱ⦹ᩡ݅. De Zeeuw and Hellinga (1958)aᱽᦩ⦽ḡ⦹ᙹ᭥ᄡ࠺ᮥᄡ⩶⦹ᩍ}ၽࡽ
ḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙᮥᯕᬊ⦹ᩍ⧉᧲పᮥᔑᱶ⦹ᩡ݅. ⧕ᕾ༉
ߙᮥᱢᬊ⦹ʑ ᭥⧕ እƱᱢvᙹᨱ ݡ⦽ ၹ᮲ᯕ᧲⪙⦽ ᱽᵝࠥ
⦽ḡᩎ᮹ḡ⦹ᙹš⊂ᵲJW Ŗ⧎, JD ᬊݕ1 ḡᱱ᮹ḡ⦹ᙹ᭥
š⊂ᯱഭ(2006-2010)ෝᯕᬊ⦹ᩡ݅. ᱢᬊࡽๅ}ᄡᙹ۵JD ᬊݕ1 ḡᱱ᮹ၹ᮲ĥᙹ۵0.039, እᔑ⇽ᮉᮡ0.023ᯕ໑JW Ŗ⧎ḡᱱᮡ
bb0.028ŝ0.009ᯕ݅. ᩑᄥ⧉᧲పᮥᔑᱶđŝෝእƱ⦹໕JD ᬊݕ1ḡᱱᮡ 520.4ⴇ904.0mmᯕ໑ JW Ŗ⧎ḡᱱᮡ 447.4ⴇ 633.4mmಽᇥᕾࡹᨩ݅. ࢱḡᱱ᮹ᱥၹᱢᯙᄡ࠺᧲ᔢᮡᮁᔍ⦹ӹ
⧉᧲పŝ vᙹݡእ እᮉᮡ ݅ᗭ ₉ᯕෝ ᅕᯙ݅.
}ၽࡽḡ⦹ᙹ᭥ᄡ࠺⧕ᕾ༉ߙᮡḡ⦹ᙹ᭥ᯱഭෝᯕᬊ⦹ᩍ
ๅ}ᄡᙹ᪡݉᭥eᄥ⧉᧲పᮥᔑᱶ⦹۵ႊჶᮝಽᝅᱽᱢᬊđ ŝ, ḡ⦹ᙹ᮹ ⧉᧲ᨱ ݡ⦽ ✚ᖒᮥ ᖅ⧁ ᙹ ᯩᨩᮝ໑ ᯕᨱ
ḡ⦹ᙹ᮹⧉᧲పᮥᔑᱶ⦹۵ႊჶᮝಽ⪽ᬊa܆⧁äᮝಽ❱݉ࡽ
݅. ੱ⦽ḡ⦹ᙹ᭥ᨱ᮹⦽⧉᧲పၰ⡍⪵ݡᨱᕽ᮹ๅ}ᄡᙹ⇵ᱶ⦹
۵ ᙹ݉ᮝಽࠥ ⪽ᬊࡹʑෝ ʑݡ⦽݅.
qᔍ᮹ɡ
ᅙᩑǍ۵ǎ☁Ʊ☖ᇡÕᖅƱ☖ʑᚁḡᩎ✚ᖒ⪵ᔍᨦ᮹ᩑǍእ
ḡᬱ(10ḡᩎʑᚁ⩢ᝁB02, ᱽᵝᙹᯱᬱᩑǍ݉)ᨱ᮹⧕ᙹ⧪ࡹᨩ
ܩ݅.
References
Cho, J. W. and Park, E. G. (2008). “A study on delineation of groundwater recharge rate using water-table fluctuation and unsaturate zone soil water content model.” Journal of the Korean Society of Groundwater Environment, Vol. 13, No. 1, pp. 67-76 (in Korean).
Choi, B. S. and Ahn, J. G. (1998). “A study on the estimation of regional groundwater recharge ra.” Journal of the Korean Society of Groundwater Environment, Vol. 5, No. 2, pp. 57-65 (in Korean).
Choi, H. M. and Lee, J. Y. (2010). “Groundwater level distribution and rainfall response characteristics in haean basin of Yangu.”
Journal of the Korean Society of Groundwater Environment, Vol.
15, No. 6, pp. 1-8 (in Korean).
Chung, I. M., Lee, J. W., Kim. J. T., Na, H. N. and Kim, N. W.
(2011). “Development of threshold runoff simulation method for runoff analysis of Jeju island.” Journal of the environmental sciences, Vol. 20, No. 10 pp. 305-312 (in Korean).
De Zeeuw, J. and Hellinga, W. F. (1958). “Precipitation and drain.”
Agricultural Magazine, Vol. 70, pp. 405-421 (in Dutch).
Healy, R. W. and Cook, P. G. (2002). “Using groundwater levels to estimate recharge.” Hydrogeology Journal, Vol. 10, No. 1, pp.
91-109.
Kim, G. B., Choi, D. H. and Jeong, J. H. (2010). “Considerations on the specific yield estimation using the relationship between rainfall and groundwater level variations.” Journal of Engineering Geology, Vol. 20, No. 1, pp. 61-70 (in Korean).
Kim, N. W., Kim, Y. J. and Chung. I. M. (2013). “Development of analyzing model of groundwater table fluctuation (i) : Theory of model.” Journal of the Korean Society of Civil Engineers, Vol.
33, No. 6, pp. 2277-2284.
K-Water (2003). Comprehensive Investigation report on Hydrgeologic and groundwater in Jeju island (ⳓ) (in Korean).
Moon, S. K. and Woo, N. C. (2001). “Estimation of groundwater recharge ratio using cumulative precipitation and water-level change.” Journal of the Korean Society of Groundwater Environment, Vol. 6, No. 1, pp. 33-43 (in Korean).
Yun, S. W., Jo, Y. J. and Lee, J. Y. (2009). “Comparison of groundwater recharges estimated by waterlevel fluctuation and hydrograph separation in haean basin of yanggu.” Journal of the Geological Society of Korea, Vol. 45, No. 4, pp. 391-404 (in Korean).