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Development of Analyzing Model of Groundwater Table Fluctuation(II): Characteristics of Recharge

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(1)

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)

 ǣŠ––’ǣȀȀ†šǤ†‘‹Ǥ‘”‰ȀͳͲǤͳʹ͸ͷʹȀ•…‡ǤʹͲͳ͵Ǥ͵͵Ǥ͸Ǥʹʹͺͷ ™™™Ǥ•…‡Œ‘—”ƒŽǤ‘”Ǥ”

⽾㬖⟖Ⳃ#≾ᦗ#㬲⛛⁦ᤶⴖ#ᇚ⇚(II): 㬦⭏#㡷⛯

׌ْ଀ ȵ׌ଗ୨ ȵ୨ଵࢂ

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 520.4904.0mm (32.761.8%) and 447.4633.4mm (24.045.1%), 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 ḡᱱᮡ520.4904.0mm (32.761.8%), JW Ŗ⧎ḡᱱᮡ447.4633.4mm (24.045.1%) 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

ⓑḡᩎᯝᙹಾ޵ᬒᵲ᫵⦽᮹ၙෝw۵݅. ✚⯩ᱽᵝࠥᨱ۵ྜྷᔑᨦᯕ⪽ᖒ⪵ࡹᨕḡ⦹ᙹ᮹ᙹ᫵a᷾a⦹ᩍḡ⦹ᙹ᮹ᦩᱶᱢᯙŖɪŝ

ᙹప ⪶ᅕෝ ᭥⦽ šญa ᫵Ǎࡽ݅.

Cho and Park (2008)ᨱ঑෕໕ 1990֥ݡ ᯕ⬥ ḡ⦹ᙹ᮹⧉᧲పᮥ ᗱᛞí ᨜ʑ ᭥⧕ ᱥℕ vᬑపᵲ ⧉᧲పᯕ ₉ḡ⦹۵ እᮉᮥ

ƒ–‡”‰‹‡‡”‹‰ սėॡ

(2)

ḡ⦹ᙹ⧉᧲ᮉ’ᯕ௝⦹ᩍ⪽ᬊࡹŁᯩ݅. K-water (2003)ᨱ঑෕

໕ᱽᵝࠥ᮹⧉᧲పᮥⅾvᙹప᮹46.1%ಽaᱶ⦹ᩍᱢᬊ⦹ᩡ݅.

ə్ӹḡ⦹ᙹ⧉᧲ᮡๅḩ᮹ᙹญḡḩ⦺ᱢᩢ⨆ᮥၼʑভྙᨱ

᜽Ŗeᱢaᄡᖒᮥaḥ݅. ঑௝ᕽzᮡḡᩎᯕ௝ࠥǎḡᱢᮝಽ

݅᧲⦽sᮥaḡအಽḡ⦹ᙹ⧉᧲పᮥᔑᱶ⦹ʑ᭥⧕ᕽ۵݉᭥᜽

eᄥ ⧉᧲పᮥ ᔑᱶ⦹ᩍ Ƚ໦ࡹᨕ᧝ ⦽݅.

⩥ᰍ⧉᧲పᔑᱶᮥ᭥⧕ᱢᬊ⦹۵ႊჶᮝಽ۵ᙹྙᖒᇥᇥญჶ, ʑᱡᮁ⇽ᇥญჶ, ḡ⦹ᙹ᭥ᄡ࠺ჶ, ḡ⦹ᙹ᭥ᄡ࠺༉ߙ॒ᱢᬊࡹ۵

}ֱᨱ ঑௝ ݅᧲⦹í ᇥඹࡹŁ ᯩ݅. b ⇵ᱶႊჶॅᮡ ᵝᨕḥ

⪹Ğᨱ঑௝Ⓧíᩢ⨆ᮥၼᮝ໑, ᩑǍᯱӹᩑǍ}ֱᨱ঑௝ᔢݡᱢ ᯙ ᪅₉᪡ ᰆ݉ᱱᯕ ᳕ᰍ⦹ʑࠥ ⦽݅(Yun et al., 2009).

ḡ⦹ᙹ᭥ ᄡ࠺ᯱഭෝ ᯕᬊ⦽ ႊჶ᮹ ݡ⢽ᱢᯙ ᮁ⩶ᮝಽ۵

Healy and Cook (2002)ᨱ᮹⧕ᱽᦩࡽvᙹ᜽ၽᔾ⦹۵ḡ⦹ᙹ᭥

᮹ᄡ⪵పᨱݡᙹ⊖᮹እᔑ⇽ශᮥŒ⦹ᩍḡ⦹ᙹ⧉᧲పᮥᔑ⇽⦹

۵ ḡ⦹ᙹ᭥ ᄡ࠺ჶᯕ ᯩ݅. ᯕ᫙ᨱࠥ }ֱ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).

ᯕ౑ႊჶॅᮡ✚ᱶᔢ᜚ੱ۵⦹vǍeᨱݡ⦹ᩍ⧉᧲ᮉᮥᔑᱶ⦹

ᩍᱥǍeᨱᱢᬊ⦹အಽ⧉᧲పᯕŝ⇵ᱶࡹÑӹ݉ʑe᮹⧉᧲ప

ᮥᔑᱶ⧁ᙹᨧ݅۵⦽ĥaᯩ݅. ᯕ᫙ᨱࠥCho and Park (2008)ᨱ

᮹⧕ ᱽ᜽ࡽ ∊ḥŖɚᮉᮥ ᯕᬊ⦽ ḡ⦹ᙹ᭥ ᄡ࠺ ༉ߙᯕ ᯩ݅.

ᱽᦩ⦽ ᜾ᮡ ᯕುᱢ ɝÑෝ ᱽ᜽⦹Ł ᯩᮝӹ ๅ}ᄡᙹ ᔑᱶ᜽

ᇡᙹᱢᯙ᳑ᔍၰᝅ⨹ᯕ᫵Ǎࡽ݅. ᔢʑᨱʑᚁ⦽ၵ᪡zᯕ⧉᧲ప

⇵ᱶᨱݡ⦽ฯᮡᩑǍaḥ⧪ࡹŁᯩᮝӹbᔑᱶჶॅᮡᙹ᜾ᔢ᮹

᪅ඹ᪡ᱢᬊᔢ᮹⦽ĥෝḡܭ݅. ə్ӹḡ⦹ᙹ᭥ᄡ࠺ᯱഭෝᯕᬊ

⦹۵ႊჶᮡᙹྙᖒᇥᇥญჶ᮹᷾ÑᯱഭᯕŁʑᱡᮁ⇽ჶŝࠥᯝš ᖒᮥᮁḡ⦹໑޵ᬒᯕš⊂ᯱഭᨱ᯦b⦽ႊჶᯕ௝۵ᱱᨱᕽ∊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 àΌŸ—ãà ķƒäâ ćÕ×׳ķ

«ƒÞÎ à ŒŸ—ãà ķƒäß

(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 ŒŸ—ãà ķƒäŒŸ—ãà ķƒäæZ 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 ࢱଦծ৤ॺ୨

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⇽ࢉᨱ঑௝ḡ⦹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)

(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┡ԕ۵ᵝ᫵ᯙᯱᯕ݅. Eq. (1)ᮥእᔑ⇽ᮉ ᨱ ݡ⧕ ᱶญ⦹໕ Eq. (4)ŝ zᯕ ⢽⩥⧁ ᙹ ᯩ݅.

ł á ćÕ××ķÞƆƇà ƆƇ àΌŸ—ãà ķƒäß

«ƒÞÎ àŒŸ—ãàķƒäß

(4)

ə్ӹEq. (4)᮹እᔑ⇽ᮉᮡၹ᮲ĥᙹ᪡⧉᧲పᮥၙญ᦭ᦥ᧝

⦹ʑভྙᨱḢᱲᔑᱶ⧁ᙹᨧ݅. ʑ᳕ᩑǍᨱᕽ۵⧉᧲పݡᝁᨱ

vᙹపᮥᱲ༊⦹ӹᅙᩑǍᨱᕽ۵ḡ⦹ᙹ᮹⧉᧲ᨱ᮹⦽ၽᔾ⦹۵

ḡ⦹ᙹ᭥ᔢ᜚Ǎeᨱݡ⧕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⪵a᯹ӹ┡ӹ۵∊ᱢ⊖ᨱš⊂ḡᱱᮥ

ᖁᱶ⦹ᩡ݅(Kim et al., 2013).

ᱽᵝࠥ᮹ᇢ἞ᵲᦺ⧕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᭥

ᔢ᜚ၹ᮲ᯕ዁ෙäᮝಽӹ┡ԍ݅. ੱ⦽ḡ⦹ᙹ᭥qᙹ᪡ᔢ᜚Ǎe 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

ᔢ᜚ᇡa℉ࢱ⩶┽ಽๅᬑɪĞᔍෝᯕ൉Łᯩ۵ߑᯕ۵݉ʑeᨱ

ԕฑ݅ప᮹vᙹಽᯙ⧕ၽᔾ⦽ḡ⦹ᙹ᭥ᔢ᜚ŝš⊂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}

(4)

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⧉᧲ᯕᯝᨕӹŁᯩ۵äᮥ᦭ᙹᯩ݅.

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⊂ᯱഭᨱᕽࠥ᦭ᙹᯩ۵ä⃹ౝḡ⦹ᙹ᭥ᄡ࠺᧲ᔢᯕ

እ᜘⦽ࢱḡᱱᯕအಽ⧉᧲ࡹ۵ŝᱶࠥᮁᔍ⦹݅۵äᮥӹ┡ԙ݅.

ə్ӹFig. 3᮹(d)᪡zᯕᯕᄅ✙vᬑᨱ঑ෙ݉ʑe᮹⧉᧲

᧲ᔢᮡ ݅ᗭ₉ᯕෝ ᅕᯕ۵ߑ ᯕ۵⋉⚍ࡽ ᧲ᯕ ☁᧲⊖ᮥ☖⧕

ᯕ࠺⦹۵ŝᱶᨱ঑௝⧉᧲ŝ႑⇽᮹⩶┽aݍ௝ḡʑভྙᯕ݅.

݅᜽ั⧕, ᯙɝḡᩎᯕ௝⦹޵௝ࠥݡᙹ⊖᮹ᙹญḡḩ⦺ᱢ✚ᖒᨱ

঑௝ ๅ}ᄡᙹa ݍ௝Კ ၽᔾ⦹۵ äᯕ݅.

ᅙᩑǍᨱᕽᱽ᜽⦽༉ߙᮥᯕᬊ⦹ᩍᔑᱶ⦽⧉᧲పᵲᯝᇡa

ᮭᙹੱ۵0᮹sᮝಽӹ┡ӹFig. 3᮹(c)᪡zᯕ݅ప᮹vᬑ

⬥⧉᧲ᮥ⇵ᱶ⦹ḡ༜⦹۵Ğᬑaၽᔾ⦹ʑࠥ⦽݅. ᯕᨱݡ⧕

⩥ᰍಽᕽ۵םญᱢᯙᖅ໦ᯕᨕಅᬑ໑༉ߙᯱℕ᮹᪅₉ᯕÑӹv ᙹ᪡ḡ⦹ᙹ᭥š⊂ᯱഭ᮹᪅ඹੱ۵⧉᧲పᅕ݅႑⇽ࡹ۵᧲ᯕ

ฯᦥӹ┡ӹ۵⩥ᔢᮝಽ⇵ᱶ⧁ᙹᯩᮝӹᯕ౑⩥ᔢᨱݡ⧕ᕽ۵

⇵aᱢᯙ ᩑǍa ޵ ᯕ൉ᨕᲙ᧝ ⧁ 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

(5)

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⧉᧲ࡹᨩᮝ໑ᯕ᜽ʑ᮹vᙹప

ᩎ᜽ԏíӹ┡ԍ݅. 2006֥ŝ2007֥᮹vᙹ᪡⧉᧲పᮥእƱ⧕

ᅕ໕, vᙹపᮡ2006֥ᯕ2,139mmಽ޵ฯᮝӹ⧉᧲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

ᯝᇡ᜽ʑ۵100%ෝⅩŝ⦹ᩍӹ┡ӹʑࠥ⦹۵ߑᯕ۵ĉᬙ℁

vᙹపᮡ ԏᦥḡŁ ᯕᱥ 7~9ᬵ ࠺ᦩ ԕฑ vᬑᨱ ᮹⦽ ḡℕࡽ

(6)

(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┡ӹŁ݅᜽ĉᬙ℁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࠺

⩶┽aݍ௝ӹ┡ӹ۵⩥ᔢᮝಽ❱݉ࡽ݅. JW Ŗ⧎ḡᱱ᮹vᬑݡ እ⧉᧲ప᮹እෝᔕ⠕ᅕ໕ᩑᄥ⧉᧲እ۵24.0ⴇ45.1(%)ᔍᯕಽ, ᱥၹᱢᮝಽ JD ᬊݕ1ḡᱱᅕ݅ ԏí ӹ┡ԍ݅.

4.3 ෌ઑ൉ন

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┡ԉᮥ᦭ᙹᯩ݅. ੱFigs. 4 and 5᮹

(c)᪡(d)ᨱᕽ᦭ᙹᯩॐ, vᙹప᮹᷾aa⧉᧲ప᮹᷾aಽḢđࡹ

ḡᦫ۵äᮥ᦭ᙹᯩ݅. vᙹపᯕ☁᧲⊖᮹⋉⚍܆ᮥⅩŝ⦹໕

ḡ⢽⦹ಽ⋉⚍⦹ḡ༜⦹ŁḢᱲᮁ⇽॒ᮝಽᯙ⧕⮹్ӹaʑভྙ

ᨱ⧉᧲పᯕ᷾a⦹۵ߑ⦽ĥaᯩ݅. ঑௝ᕽvᙹప᮹ᯝᱶእᮉᮥ

⧉᧲పᮝಽaᱶ⦹ᩍ⧉᧲ᮥᖅ໦⦹۵äᮡฯᮡ᪅₉ෝ⡍⧉⦹í

ࡹအಽ⧉᧲పᔑᱶ᜽݉᭥᜽eᄥᨱ঑ෙ ⧉᧲పᮥᱢᬊ⦹ᩍ᧝

ᝁ഑ᖒᮥ ׳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

(7)

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).

(8)

수치

Fig. 1. Location of Groundwater Monitoring Wells in Jeju Island  (Figure from Kim et al
Fig. 3. Observed Groundwater Level and Simulated Recharge at  JD Yongdam1(a) and JW Konghang(b)
Fig. 4. Comparison of Rainfall and Simulated Recharge at JD  Yongdam 1 :(a) Daily, (b) Monthly, (c) Quarterly, (d) Annual
Fig. 5. Comparison of Rainfall and Simulated Recharge at JW Konghang :(a) Daily, (b) Monthly, (c) Quarterly, (d) Annual

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