Geostatistical Interpretation of Water Quality and Hydrogeochemistry of Shallow Groundwater in the Uljin Area, Korea
전체 글
(2)
(3) . . . . . .
(4) . . . . . . Geostatistical Interpretation of Water Quality and Hydrogeochemistry of Shallow Groundwater in the Uljin Area, Korea Nam-Jin Kim1, Seong-Taek Yun1*, Hyoung-Soo Kim2, Kyung-Moon Jung3 and Gyoo-Bum Kim2 1. Department of Earth and Environ. Sci., Korea University, Seoul 136-701, Korea Korea Water Resources Corporation, Daejon 3 Dohwa Consulting Engineers Co., Seoul 2. We have collected hydrogeochemical data of shallow groundwaters in the Uljin area located at eastern coastal area of Korea. Geostatistical analysis (ANOVA test, cluster analysis, and factor analysis) of the collected data sets was performed, in order to evaluate both the spatial and/or temporal variation of water quality data and the groundwater contamination, as well as the principal reactions occurring in the aquifer. Results of the ANOVA test show that regional water chemistry are not significantly changed spatially in eight watersheds. However, some ions such as Ca2+, HCO3− and SO42− show a meaningful watershed variation. Water chemistry variation according to sampling time (season) is not shown, except for SO42−. The cluster analysis shows that significant water chemistry variation is explained by the distance from the coast. Factor analysis indicates that the water chemistry is changed according to various factors as follows: in the order of decreasing importance, water-rock interaction (mainly, carbonate dissolution), sea-salt spraying, and then contamination by fertilizers and agrochemicals.. Uljin, shallow groundwater, water quality and hydrogeochemistry, geostatistics, sea-salt spray.
(5) !" # $%&'( ) * +, -.
(6) /012301 4 56# 78 9 :; <=>? @! A B# 9C DE FG H1 ) -.I J K LM N
(7) O 301 4K P@ QR&> S < TUI V'
(8) W X? 4K >YZ[E / \]/^ L_ ` 4? K ab 9? "c QRE de> FG -.
(9) 4? &' f
(10) g LM h@ i j8k Xl# / DE !" FG m
(11) -. I E5O !"
(12) n# o" DE p! q;' d !"# >r s t u AB @' v, Ht
(13) w xE; ^O ,
(14) yz {* |U } ~
(15) O +,&' E ) , yz . . . . . . . . . . . . . . . . . . .
(16) . . . . . . . . . 2 45 60 789 : ;< ="> 0 ?@ AB *C-12 =" 78 9 DE012 FG6: HI< JK0,L3 MN OP Q M, <R '@ # # SC@ T U 78 -9 : V W0XYW0 # U9 Z[ <. . !" # $ % &' ()* +,- ./012 3.
(17) . . *Corresponding author: [email protected]. . . .
(18) \% ]N H'^ _ `a0,< YXW01 Ê
(19) ÂÄ% Rz9 8< ,$ z f 2 <R ()b # V M9 @ ¸0 u *K v iË9 Ì c 012 de f! g
(20) @3 hi Í12 Î y0z, SÏ <
(21) ÐVÑ` ¿*z% #Ò0Ä123 K ÀO@ ?9 jk : jlN mno `da2 >Ó>^ ÃÄ _ Ä12 o ;1> p
(22) 6@3 =" q: r Àz Áz, , D12 Ô ;< ½ ¾ Õ7f zu ÂÃÄ% :Ö Jf s< MN t<@ u5 K vO V M SÏ >Ó×< Å« +ÂÄ% Ì O * % w x V y0z {0 K ÃÄ ØK@ Ì SÏ < M | ,k }~ g@ *12O B K 3´ @ Y 7 CÙÄ, `da2 @ t< U@ ! &' ()b # SÏ ;< m K |R SÏ VR| < @3 t<@ u5 m K vO V| Ú | ¹| @ ! JK0u V M9 Z[ L0¸ Û <
(23) |RÑÜ " V M W0 i0 # R79 ¡3O Ä #Ò 12 vO V M@
(24) U9 !" u9 de < , f 0Ä Ä SÏ Ý@ 2 0~Þ9 ß Äà ! 0 ?9 ,k *C12O vO | .O Ò0|: SÏ! ¬/012 |R Q z 6@3 !" / # U : Rá< O * Aâ@ y0|: 'ã {V : 9 + ,Q ä ,$% å vO « SÏ ; SSC SC uSC Ú, ; aæV9 ß ;H ¸0 Q : Rá <#E hi ?9 0k12 vO < m K |R Q % 3¡O À3O V@ U9 # $ , 789 .O [K9 Îg ç2 Rá \12 Ñ
(25) 012 *C! V M # u9 DE01 oè<
(26) |RÑÜ 2 de< m K JK0u w éi 3 ¨ ¨ M ê ë« da Ñ@ ! Q . o \12 ìDo ä 6 ,7 Ö9 íU, 'ã f * @ u5 ¡ Û Ñ m K ¿î Â E m K L0 ,< m K <
(27) 23 ¬
(28) ¿î +< ï1 3¢% £¤¥ ¦§ ¨9 ,© ;1^ , % ª@3 l v$% 3¡¢@3 *2 o ^ ð@ Â'E, Ìo ¬¨0u /  ;< «3 ¬¨012 3 ¨ ¨ M®9 ' ñò9 +, ;< 2 y0z9 « Øo vO +u< *2 o v ¯ y0@ Y _ °± ²: l³< | ,k ´L 712 ów@ m K y0z@ @3 +L µ¶ ² v , ! ãN ô < m K Î y OS9 · < JK012 ¸¹1 0z% 6õ 7 _ O * « SÏ^ 2 aæ Ú ¹|2 oH ;< 2 º ; ² », ¼,
(29) m K OS v% ö · ;<
(30) m K V % &' () <R< ÷v ¿* Àv ¡L Àv9 Îg O ½¾ ¿*z Àz Áz  S KL0, ² 2 Ö, ø% ¸0 `da «3 OS 7 : ù ÃÄ, /Ä9 ,© ;1^ ,$9 Y 7 v,^ ÂÃÄ Å« +ÂÄ, 8< , ! ú Y ú E, .Y@ *2 Øo U, z$ 7f@ Rzu z :Æ z, O ;< y0z ûü ./012 v ¯2 Uý D _ Çz 5È 8i2 É! ;1^ ¤[ þ ûÿm< = ûü +L ö÷v . 1.
(31)
(32)
(33) . . . . 32. . .
(34)
(35)
(36) .
(37)
(38) !. . ". . . . .
(39) 4%. ,3 !0. , !0. 1 !0. /0. 50. . . . -. 5. . . . . . . . #$#% &'()&
(40) . . . . 5. . . . *
(41) + . . . ,, ,! -. . . . . '1$3. . 1! --. . . 2 -. '+$'!*. !51 --. 36,. . . ,/ 0. , 10. ! 20. 1. 1/ 320. . . /1 20. . . . . . . . . . . . . . . 2 361 -.
(42)
(43) ¿* Àv ¯ ¡L Àv ¯ ³, 7012 <
(44) 9 « l³ y0z% ¸0 ûÿ ä ¸! > v >Ëv O
(45) v ¯ Jv ¯ & v ¯ v ¯ ~ 7 vO V # i012 +v 7v % y0z l f! u ð ð . . 3 261 5 -. . . . . 3 /62! - . . . 3 /6!1 / -. 2 56!5 -. / /6! -. . 16, -. . . ! 6 -. . ! 62 -. 6!1 -. Major watersheds and sampling sites of the Uljin area.. . 5. !. ,. 1. .
(46) . . Sample no.. Physicochemical data of shallow groundwaters from the Uljin area (sampling date: December 1997) Surface geology. Distance1) Drilling G.W.L.2) Temp. (km) depth (m) (m) (oC). pH. EC3). TDS4). (µS/cm) (mg/l). Dissolved constituents (mg/l) Na. K. Mg. Ca. SiO2. Cl. SO4. HCO3. NO3. 3.8. F. B112. granitic gneiss. 2.4. 2.5. 0.54. 14.0. 7.21. 80. 122.2. 14.2. 1.4. 1.7. 5.2. 38.0. 14.4. 39.7. 3.8. 0.04. G108. granitic gneiss. 5.6. 100.0. artesian. 15.0. 7.20. 200. 226.9. 15.3. 1.9. 4.7. 24.2. 55.4. 8.1. 6.9 109.8. 0.3. 0.36. G121. granitic gneiss. 1.5. 80.0. 7.60. 15.0. 6.72. 120. 104.0. 7.0. 2.1. 3.8. 14.8. 13.6. 6.9. 9.8. 42.0. 4.1. 0.04. G122. limestone. 3.3. 70.0. 22.50. 16.0. 7.21. 400. 383.6. 16.9. 1.9. 13.4. 74.8. 15.8. 48.9. 13.4 177.0. 21.4. 0.08. G151. granitic gneiss. 6.0. 15.7. 5.02. 14.0. 6.89. 220. 116.2. 9.2. 2.4. 4.0. 11.6. 21.4. 9.4. 9.4. 39.7. 9.0. 0.03. G59. biotite granite. 0.4. 3.0. 1.80. 14.0. 7.05. 180. 231.4. 32.4. 1.1. 5.9. 20.4. 30.1. 52.4. 12.7. 70.2. 6.1. 0.12. H53. biotite-hornblende granite. 2.7. 4.8. 1.00. 10.0. 7.32. 150. 197.7. 19.3. 3.5. 7.1. 28.9. 17.0. 31.3. 25.9. 39.7. 24.9. 0.05. H65. biotite-hornblende granite. 1.1. 5.5. 2.55. 12.0. 7.21. 200. 227.8. 14.0. 3.4. 7.1. 41.1. 20.5. 14.1. 39.6. 75.0. 10.8. 2.23. K102. granitic gneiss. 3.3. 1.07. 16.0. 7.39. 140. 112.7. 7.4. 1.8. 5.4. 12.2. 13.5. 10.5. 14.6. 35.1. 12.0. 0.10. 2.3. 5.0. 0.92. 14.0. 7.20. 130. 134.9. 9.8. 1.9. 5.5. 16.3. 15.7. 10.7. 10.7. 58.0. 6.2. 0.09. K164-1 granitic gneiss. 1.0. 3.1. 2.00. 13.0. 7.05. 180. 160.5. 17.1. 3.0. 7.6. 14.2. 16.2. 28.1. 15.7. 42.7. 15.8. 0.05. K176. banded biotite gneiss. 2.8. 3.4. 0.08. 15.0. 7.15. 80. 104.1. 8.0. 1.6. 4.4. 10.1. 16.5. 7.9. 12.5. 36.6. 6.4. 0.06. K41. banded biotite gneiss. 5.2. 3.4. 0.12. 14.0. 6.46. 250. 198.7. 10.6. 2.1. 12.1. 27.2. 13.8. 19.5. 24.9. 54.9. 33.4. 0.29. O48-1. biotite-hornblende granite. 10.9. 1.2. 0.80. 10.0. 7.10. 170. 194.8. 16.0. 2.8. 5.1. 21.3. 38.3. 14.2. 9.0. 36.6. 51.5. 0.10. O60. banded biotite gneiss. 7.9. 6.6. 2.31. 9.0. 6.89. 110. 116.1. 8.6. 1.5. 2.9. 15.0. 14.0. 8.9. 13.4. 45.8. 6.0. 0.15. P107. clastic sed. rock. 4.0. 7.3. 0.80. 13.0. 7.31. 120. 141.1. 9.0. 2.4. 4.3. 19.0. 15.6. 11.5. 14.7. 42.7. 21.7. 0.04. P44. granitic gneiss. 1.0. 11.5. 1.69. 12.0. 6.12. 180. 185.0. 15.2. 2.6. 5.1. 24.0. 20.5. 18.0. 22.2. 76.3. 1.0. 0.08. UL118 granitic gneiss. 0.0. 3.0. 0.55. 13.0. 6.92. 350. 366.9. 49.7. 1.0. 12.4. 37.1. 29.1. 74.9. 32.4. 58.0. 72.3. 0.04. UL81. granitic gneiss. 2.3. 1.9. 0.28. 17.0. 6.50. 110. 119.9. 10.9. 2.3. 5.4. 10.9. 17.8. 14.1. 8.4. 45.8. 4.4. 0.04. UP96. granitic gneiss. 2.3. 5.3. 2.20. 15.0. 6.74. 100. 94.0. 8.0. 2.0. 2.5. 8.1. 12.0. 8.3. 11.0. 36.6. 5.4. 0.17. W124. granitic gneiss. 0.3. 2.7. 0.95. 10.0. 7.10. 250. 232.9. 38.8. 4.6. 9.6. 25.7. 14.4. 65.3. 23.0. W40. limestone. 3.2. 9.6. 0.05. 13.0. 6.61. 220. 313.0. 20.5. 2.5. 9.6. 41.4. 32.8. 24.0. W54 granitic gneiss 6.4 3.7 2.00 8.0 7.25 60 78.9 6.2 1) distance from the coast, 2) ground water level, 3) electrical conductivity, 4) total dissloved solids. 1.1. 2.7. 8.2. 11.4. 5.3. 44.0. 7.3. 0.14. 4.2 177.0. 0.6. 0.36. 7.9. 2.4. 0.09. 33.6. . 2.0. K150-1 banded biotite gneiss.
(47)
(48) Physicochemical. surface geology. Distance1) Drilling G.W.L.2) Temp. (km) depth (m) (m) (oC). pH. Eh EC3) TDS4) (mV) (µS/cm) (mg/l). Dissolved constituents (mg/l) Na. K. Mg. Ca. SiO2. Cl. SO4 HCO3 NO3. F. B112. granitic gneiss. 2.4. 2.5. 0.64. 11.5. 7.23. 82.5. 113.1. 93.6. 11.0. 1.4. 1.7. 4.9. 35.9. 8.4. 1.5. 28.7. 0.0. 0.01. B117. granitic gneiss. 0.5. 3.0. 0.85. 11.4. 6.40. 31.0. 119.0. 83.3. 11.1. 1.5. 2.6. 5.4. 10.4. 10.5. 5.2. 33.1. 3.3. 0.27. B57-1. banded biotite gneiss. 8.0. 1.0. 0.05. 11.4. 5.70. 70.1. 75.6. 62.9. 5.4. 0.6. 1.3. 5.8. 17.8. 6.5. 8.2. 16.3. 1.0. 0.03. H53. biotite-hornblende granite. 2.7. 4.8. 1.16. 12.3. 5.29. 207.0. 387.0. 252.9. 23.8. 2.1. 9.1. 35.6. 14.7. 22.4. 17.0 100.7 27.4. 0.01. H65. biotite-hornblende granite. 1.1. 5.5. 3.25. 12.4. 6.35. 273.3. 189.0. 154.1. 7.4. 1.9. 3.6. 23.8. 12.7. 6.9. 16.8. 2.9. 0.56. J66. granitic gneiss. 4.0. 4.9. 0.64. 13.4. 5.59. 77.5. 300.0. 211.1. 18.5. 1.4. 8.2. 20.6. 47.6. 26.4. 2.6. 65.6 20.1. 0.05. K102. granitic gneiss. 2.0. 3.3. 1.28. 12.0. 6.26. 40.5. 143.0. 98.0. 6.7. 2.0. 5.1. 12.0. 12.2. 8.7. 10.2. 31.4. 9.5. 0.15. K164-1 granitic gneiss. 1.0. 3.1. 2.30. 10.5. 5.57. 80.4. 245.0. 184.4. 21.6. 1.0. 4.5. 11.4. 33.3. 39.6. 13.5. 29.0 30.3. 0.17. K41. banded biotite gneiss. 5.2. 3.4. 0.20. 13.2. 5.57. 80.4. 230.0. 174.3. 11.7. 8.4. 7.7. 13.0. 18.1. 8.4. 5.3. 82.0 19.7. 0.03. O300. clastic sed. rock. 5.8. 8.7. 3.63. 8.5. 6.54. 24.5. 118.7. 84.6. 5.7. 1.0. 2.2. 10.8. 11.1. 6.5. 5.0. 38.9. 3.4. 0.06. O48-1 biotite-hornblende granite. 10.9. 1.2. 0.40. 13.6. 6.24. 41.4. 225.0. 174.2. 11.7. 1.6. 4.9. 21.2. 35.1. 11.3. 7.0. 33.5 47.9. 0.09. 51.9. 2.3. 0.17. 77.5. O60. banded biotite gneiss. 7.9. 6.6. 3.02. 9.0. 6.57. 23.1. 101.2. 86.3. 5.8. 1.1. 1.7. 10.5. 8.6. 0.0. 4.1. P107. clastic sed. rock. 4.0. 7.3. 1.36. 13.0. 5.87. 49.4. 171.4. 145.0. 8.1. 2.9. 3.8. 17.7. 14.5. 17.5. 14.2. 42.7 23.6. 0.02. W124. granitic gneiss. 0.3. 2.7. 1.59. 9.1. 6.11. 49.2. 226.0. 153.6. 21.6. 2.4. 5.7. 13.4. 12.1. 23.1. 9.6. 52.8 12.7. 0.07. W54. granitic gneiss. 6.4. 3.7. 2.14. 11.5. 5.39. 89.0. 125.9. 94.2. 4.3. 1.4. 3.5. 14.1. 10.3. 6.6. 9.0. 38.8. 0.02. 6.1.
(49) . Sample no.. data of shallow groundwaters from the Uljin area (sampling date: April 1998).. 1) distance from the coast, 2) ground water level, 3) electrical conductivity, 4) total dissloved solids. .
(50) . . Sample no.. Physicochemical data of shallow groundwaters from the Uljin area (sampling date: July 1998). Surface geology. Distance1) Drilling G.W.L.2) Temp. (km) depth (m) (m) (oC). pH. EC3) TDS4) (µS/cm) (mg/l). Dissolved constituents (mg/l) Na. K. Mg. Ca. SiO2. Cl. SO4. HCO3. NO3. F. granitic gneiss. 2.4. 2.5. 0.43. 16.4. 6.17. 200. 59.1. 5.4. 2.3. 1.2. 3.3. 17.3. 7.2. 4.5. 15.3. 2.4. 0.15. B117. granitic gneiss. 0.5. 3.0. 0.40. 17.8. 7.13. 160. 67.2. 14.2. 1.8. 3.0. 6.1. 11.2. 13.9. 6.2. 6.1. 4.4. 0.31. B42. granitic gneiss. 3.8. 5.7. 3.05. 17.5. 6.62. 130. 137.6. 9.9. 2.3. 4.4. 18.2. 15.5. 11.0. 27.7. 36.6. 11.7. 0.30. B57-1. banded biotite gneiss. 8.0. 1.0. 0.05. 18.0. 6.99. 90. 54.6. 5.5. 0.7. 1.2. 4.9. 18.8. 6.8. 5.9. 9.8. 0.8. 0.27. G151. granitic gneiss. 6.0. 15.7. 5.23. 15.0. 6.66. 150. 121.5. 6.0. 1.1. 4.4. 12.5. 19.0. 8.6. 7.2. 61.0. 1.6. 0.13. G59. biotite granite. 0.4. 3.0. 1.61. 17.5. 6.67. 250. 346.5. 42.0. 2.0. 14.7. 31.5. 26.5. 68.1. 23.6. 48.8. 89.1. 0.16. H53. biotite-hornblende granite. 2.7. 4.8. 0.90. 19.1. 6.91. 370. 140.0. 9.8. 1.8. 4.6. 17.3. 13.0. 17.8. 12.0. 48.8. 14.8. 0.05. H65. biotite-hornblende granite. 1.1. 5.5. 2.17. 18.7. 6.77. 290. 154.4. 7.9. 1.4. 4.6. 19.5. 14.7. 16.6. 10.8. 70.2. 8.8. 0.05. J66. granitic gneiss. 4.0. 4.9. 0.74. 18.5. 6.94. 280. 247.2. 22.8. 1.7. 8.9. 21.8. 46.1. 43.7. 4.5. 58.0. 39.5. 0.11. K102. granitic gneiss. 2.0. 3.3. 1.15. 19.8. 6.71. 150. 120.1. 7.9. 1.6. 5.6. 12.5. 14.6. 14.2. 12.9. 39.7. 11.1. 0.07. K150-1 banded biotite gneiss. 2.3. 5.0. 0.99. 18.0. 6.36. 130. 116.9. 10.3. 2.2. 4.2. 12.3. 16.5. 19.4. 6.9. 42.7. 2.4. 0.06. K164-1 biotite-hornblende granite. 1.0. 3.1. 1.69. 17.5. 6.53. 230. 189.0. 12.5. 1.6. 5.2. 21.3. 34.2. 16.5. 9.8. 36.6. 51.1. 0.14. K176. banded biotite gneiss. 2.8. 3.4. 0.06. 18.4. 6.46. 90. 85.4. 6.7. 1.1. 2.8. 7.4. 13.2. 10.7. 12.1. 15.3. 15.9. 0.11. K41. banded biotite gneiss. 5.2. 3.4. 0.07. 16.5. 6.93. 280. 151.5. 9.1. 5.3. 6.6. 14.0. 15.3. 26.0. 15.3. 30.5. 29.1. 0.19. O300. clastic sed. rock. 5.8. 8.7. 3.32. 18.8. 6.96. 200. 208.5. 11.0. 1.5. 7.1. 26.8. 16.5. 20.3. 11.8. 83.0. 30.5. 0.09. O48-1. biotite-hornblende granite 10.9. 1.2. 0.42. 17.0. 6.47. 230. 160.6. 21.5. 1.1. 4.1. 9.2. 34.2. 29.8. 9.9. 39.7. 10.9. 0.26. O60. banded biotite gneiss. 7.9. 6.6. 2.70. 19.7. 7.32. 110. 112.0. 7.1. 1.2. 2.7. 14.0. 14.9. 8.4. 7.7. 48.8. 7.1. 0.16. P107. clastic sed. rock. 4.0. 7.3. 1.07. 18.9. 7.26. 150. 162.9. 8.4. 1.8. 4.9. 20.6. 13.5. 16.8. 11.9. 58.0. 27.0. 0.04. P44. granitic gneiss. 1.0. 11.5. N.D.. N.D.. N.D.. N.D.. 139.4. 7.8. 1.3. 4.2. 18.1. 14.1. 13.7. 9.9. 61.0. 9.1. 0.07. UL118 granitic gneiss. 0.0. 3.0. 0.45. 18.2. 6.72. 440. 362.4. 49.7. 1.1. 10.7. 27.5. 31.1. 57.2. 22.0. 85.4. 77.6. 0.05. UP96. granitic gneiss. 2.3. 5.3. 2.20. 17.5. 6.34. 170. 234.3. 27.6. 5.3. 8.2. 17.4. 33.1. 42.1. 7.3. 43.9. 49.2. 0.20. W124. granitic gneiss. 0.3. 2.7. 1.59. 22.0. 6.87. 190. 181.3. 13.0. 1.6. 5.6. 23.5. 14.8. 21.1. 9.3. 73.2. 19.0. 0.20. W40. limestone. 3.2. 9.6. 0.10. 18.4. 6.87. 240. 150.6. 9.9. 1.1. 5.5. 20.4. 13.1. 17.7. 6.0. 73.2. 3.5. 0.21. W54. granitic gneiss. 6.4. 3.7. 2.25. 18.4. 6.20. 200. 110.5. 6.1. 2.1. 5.5. 19.7. 11.8. 10.7. 11.9. 22.9. 19.9. 0.05. 1) distance from the coast, 2) ground water level, 3) electrical conductivity, 4) total dissloved solids. . B112.
(51) . Sample no.. Physicochemical data of shallow groundwaters from the Uljin area (sampling date: September 1998). Surface geology. Distance1) Drilling G.W.L.2) (km) depth (m) (m) 2.5. 0.60. pH. 18.0. 6.52. EC3) TDS4) (µS/cm) (mg/l) 230. 98.9. Dissolved constituents (mg/l) Na. K. Mg. 19.5. 1.2. 2.2. Ca. SiO2. Cl. 5.2. 27.0. 25.1. SO4. HCO3 NO3. F. 1.8. 0.07. 58.0. 8.9. 0.48. 39.7. 11.5. 0.31. 3.9. 9.2. 0.3. 0.04. 6.0. 58.0. 1.2. 0.13. B112. granitic gneiss. 4.6. 12.2. B117. granitic gneiss. 0.5. 3.0. 0.11. 19.0. 7.11. 140. 132.5. 22.9. 3.2. 3.8. 7.9. 11.4. B42. granitic gneiss. 3.8. 5.7. 3.88. 18.0. 6.32. 220. 131.6. 12.0. 2.6. 4.1. 17.5. 15.0. 11.3. 4.8. 10.3. 18.7. B57-1. banded biotite gneiss. 8.0. 1.0. 0.05. 18.0. 6.73. 80. 44.9. 5.3. 0.7. 0.6. 2.5. 18.0. 4.3. G151. granitic gneiss. 6.0. 15.7. 5.48. 18.0. 6.58. 120. 115.9. 6.6. 1.1. 4.5. 13.5. 18.1. 6.8. G59. biotite granite. 0.4. 3.0. 2.03. 18.0. 6.51. 290. 300.1. 47.5. 2.2. 14.1. 30.0. 25.5. 71.6. 23.0. 36.6. 49.5. 0.16. H53. biotite-hornblende granite. 2.7. 4.8. 1.01. 19.0. 6.35. 610. 162.1. 12.3. 2.5. 5.4. 21.5. 13.9. 13.7. 10.8. 67.1. 14.8. 0.06. H65. biotite-hornblende granite. 1.1. 5.5. 2.82. 18.0. 6.57. 410. 136.2. 9.5. 1.4. 4.1. 18.0. 14.9. 12.0. 8.8. 61.0. 6.4. 0.05. J66. granitic gneiss. 4.0. 4.9. 0.63. 19.0. 6.78. 200. 242.1. 24.4. 2.0. 9.1. 23.6. 44.0. 40.1. 4.3. 54.9. 39.6. 0.10. K102. granitic gneiss. 2.0. 3.3. 1.20. 19.0. 6.57. 130. 124.8. 9.5. 1.8. 5.5. 13.0. 14.4. 10.5. 9.8. 48.8. 11.5. 0.05. K150-1. banded biotite gneiss. 2.3. 5.0. 1.08. 18.0. 6.98. 110. 104.4. 7.8. 1.4. 3.8. 11.7. 13.2. 8.4. 5.4. 48.8. 3.7. 0.21. K164-1. granitic gneiss. 1.0. 3.1. 1.96. 18.0. 6.34. 240. 199.3. 26.1. 1.3. 4.8. 11.5. 33.5. 23.8. 13.6. 64.1. 20.4. 0.22. K176. banded biotite gneiss. 2.8. 3.4. 0.15. 19.0. 6.72. 110. 69.0. 8.1. 1.1. 2.1. 5.7. 14.1. 7.3. 8.1. 19.5. 2.9. 0.08. K41. banded biotite gneiss. 5.2. 3.4. 0.27. 17.0. 6.59. 470. 126.2. 14.3. 7.3. 5.1. 3.5. 25.7. 10.8. 14.5. 30.5. 14.4. 0.06. O48-1. biotite-hornblende granite. 10.9. 1.2. 0.41. 18.0. 6.63. 250. 207.8. 17.5. 2.5. 5.9. 23.2. 30.4. 15.9. 9.5. 39.7. 63.0. 0.11. O60. banded biotite gneiss. 7.9. 6.6. 3.81. 20.0. 7.11. 140. 69.6. 7.9. 0.9. 1.0. 4.0. 26.8. 5.5. 4.3. 18.3. 0.8. 0.15. P107. clastic sed. rock. 4.0. 7.3. 1.23. 20.0. 7.02. 140. 137.6. 9.5. 2.2. 4.0. 17.3. 14.9. 8.3. 8.4. 54.9. 17.9. 0.02. P44. granitic gneiss. 1.0. 11.5. N.D.. N.D.. N.D.. N.D.. 119.6. 8.4. 1.3. 3.5. 15.3. 14.5. 8.9. 7.1. 54.9. 5.6. 0.06. UL118. granitic gneiss. 0.0. 3.0. 0.70. 19.0. 6.81. 470. 321.2. 58.6. 1.2. 12.7. 23.5. 32.5. 49.0. 21.8. 39.7. 82.3. 0.05. UL81. granitic gneiss. 2.3. 1.9. 0.33. 21.0. 6.81. 130. 97.7. 9.4. 2.0. 3.4. 7.3. 14.9. 10.3. 4.8. 42.7. 2.8. 0.06. UP96. granitic gneiss. 2.3. 5.3. 2.66. 19.0. 6.52. 130. 217.7. 28.0. 5.6. 7.6. 16.5. 31.0. 38.4. 6.3. 36.6. 47.5. 0.21. W124. granitic gneiss. 0.3. 2.7. 0.61. 20.0. 6.71. 150. 178.2. 14.6. 1.9. 5.1. 22.0. 22.9. 15.3. 8.4. 64.1. 23.7. 0.19. W40. limestone. 3.2. 9.6. 0.22. 19.0. 6.83. 290. 172.0. 14.9. 1.5. 5.7. 21.5. 15.1. 10.2. 6.2. 88.5. 8.2. 0.24. W54. granitic gneiss. 6.4. 3.7. 2.34. 17.0. 6.65. 130. 83.8. 5.2. 1.5. 2.1. 7.8. 14.7. 3.6. 4.0. 39.7. 5.1. 0.03.
(52) . 2.4. Temp. (oC). 1) distance from the coast, 2) ground water level, 3) electrical conductivity, 4) total dissloved solids. .
(53) @3 SC' \,< i)
(54) Y }Ö´ 'u ð ð Ù@ }Ö Ñ Y
(55) noè< 2 y0z SÏ K@ D SC * A
(56) 61@ D< D Y
(57) ¹ @3 v O Y <
(58) Í aû x2O ,6,^
(59) ,k yS R @ x§ í?
(60) @ « mn< m K vO V 2 }Ö@3 gO 5È9 ÷ f! O V ¨ V 0 m R79 ¬ M β 6@3 ¬f /012 + f! Z,+ <,=,9 Y ¬¬ ´D1^ 0D9 h < ¹Y' . ¹@3 i ! ´D< 9 h )2
(61) ' Y OS ¿î( * > { Y t2 µ 2 V 9 t-12 * ,< h Y O{V9 ÎB1^ R, V ¨ # R79 +L ç012 9$ SCk Y@ *3 â ì:< } 89( ¨12O '$9 ¨@ ¸0 .b Ö@3 SCk Y " Y Ì( SÏ9 ;< ," #
(62) Y §¸1^ a Y +8@3 ¹$ W0 SÏ 8H +L ¨ !«,, ,k! "Ö 7£ < @ A5 Y OS% K O *@ kP , SC% ¬#J{ u5 Yµ9 /uý ;< 0, $ 6 ‘ |R SC%’ Ì E, ¸0 1122 E9 E@ 3! <,=,9 Y! +L ,k! n< â D@ '´ =4 0, @ ;H 3 &' , E ´D( ô} ´D 7 E, 5:* U, 67< MN i ¬î¨ 9 ãÍ 8@ A5! ¹Yo Y$% OS . ,. 5. . @9. 1. !/. . . ,2. . 1 -. . &78&. /. . ". ". # . *. 8. *9. . !. . . # . %. 1/. -. 1. - . . - . . . . . !. . 4 . . '$9. :97$&*+7 * - ;4 < 2. ;4 !. :9= >. . A
(63) 61 '(. '(. 9. . !. . 9 B'(. .?. 1. @&". . 9 B'(.
(64) Piper diagram showing the chemistry of alluvium groundwaters in the Uljin area. Each plot represents the mean value of four seasonal samples from each sampling site..
(65)
(66) . . Major ions versus TDS concentration diagrams of alluvium groundwaters in the Uljin area. Each plot represents the mean value of four seasonal samples from each sampling site.. v K Ì ¯ O _ À O @ f < 9 @3 ô t :, ," ¯ K% ²: Ì SÏ u: 4' * K@ *; < «3 * K@ :<V þ vO 2 , ¹5 ;09 ìý ;< 7¯2O ¯ U Ì@ V &ç ÄC _ y0z { ÄC /, /'< ," / D 70u ç¯YW9 c 012 / V # u kP , E , 8i 0 788i 3ÊH @ Y< @3 Ã=:2 ¹$%
(67) ¹) i > ¿î(12 Y< 9 +L E 5: 3ÊH >: Rá 78 8i +!§< MN 1% E@ * 1% E9 . . . . 9. '(. . . $. A=+ 4
(68)
(69) 4.
(70) 4
(71) . . 2. . !. 1. . 2. A=+. '. 9. . '. 9. A=+. +, Y$% *@ :<, f^ «3 , $% ?- t< U9 Âb Y < R , Ì > E @% 78 9 +!- : 1% ¢@3 = > 5: : Ao U, ;< ," U% @ Y t :, : 1L3 BJ{@ ! Ï Ñ@ :<C 8Do \12 EÇ'< y0z M@ « vO V M, 7, F|! +G< 93 ô t :, y0z l³, 2 Ö y0z ûü ´L@3 Rá # ² L0, 7 012 .% ö÷v ¡L Àv ¿* Àv K9 > =H12 I y0z l³, <` > Ëv Ov Jv &v v ~+v 7v K9 _ < =H12 >JH *. :< >@ kP , SÏ . 9. ;. A=+. A=+. . 1. A=+. . ". . . . . . . . . . . /. A=+.
(72) 7 E¸ y0z M)2 67 ·,: >Ó> s < «3 y0z ûü ² L012 )! x}' y0z M% m K vO @ K U9 s \12 EÇ'< . .
(73) . 0 u MN V &ç ÄC _ |R { /% V ¨@ ;H 012 Ì ^ «3 , Z[!¶- uf0 u @ V # D c 012 Z[ý ;< <R V &ç@ Pô B J{ MN í* C % MN 1% k*12 u! MN vO V ¨@ 0u U9 \1 2 L M ;< m K vO '@ = V M% y0z V . . . $. . . . . . . .
(74) . C
(75) . ,. The relationship between TDS concentration and the saturation index (S.I.) of calcite and dolomite for shallow groundwaters in the Uljin area.. . Major cations versus TDS concentration diagrams of alluvium groundwaters in the Uljin area, showing the variation of water quality in terms of different watersheds. Each plot represents the mean value of four seasonal samples from each sampling site..
(76)
(77) &ç @ 78N, .·012 B k*/ * '( E% &' ï *: Ì @ * Ño ;0% Se< MN @H2W '( E KY &' ï122 ¨ @ ;H3 1% 788i +, m K ¯ K @3 .O OS% @3 Y lXo 1% '( E% t< U Y8 t :, B J{ k* * 2 *C'< \12 EÇ'< «3 ¯@ Ì' >Üj m K v y0z Ì da@ ;H x9 Bj 3ÊH ` ¸ Û _ 7¯ ymK 2O ¯ Q K @ _ Z : i2 oH ' * 2 U !" Y:
(78) XSC' ¿* Àv K y '< 0z @ ! kP , E W0 # ! +G< % *12O B 7¯ A5 @ «
(79) ' 7 E9 5:Y[ ; i) V M # >Ó6 ;< O u >u , 12 V&ç y S ' R, Ì@ : 0, Ì@ 0z Ä/ 6 dJ{ 2 ÖC k : R012 :Ö 'ã ,12 >Ó> ;H * t< U9 Uý ;< ="> 78, &' ï% \ 12 ¬/012 B J{ k*: V M9 Q E. ;09 e/N Y < _ ,$ û ,% + dJ{ k* > 5:Y[ W0 i012 :Ö K E # >Ó6è u123 Ì s% \12 EÇ'< /L , * < " D'
(80) ¹@3 V M , 1% > 78 >¸ m K V # i)2 +L &' ÊdO # + (@ A5 µ9 ;< à ," ÊdO # y ¨@ ;H t< U, \9 Y*§< 0z 1% & ¸0 P% Í 8D! " , E W0 # +L * Â' Q& ym Q : &' RSb .H> 12O ] B: ,6@ ; Y@ ów. \,< y0z 6@3 ç¯ YW 3 1% E9 +,^ B: 5:@ « 70 , ø% '@ ¿¨@ ³ý D yS V 12 ï% > +, ;< &ç { /% H'^ «3 K V@ t< U * V M% B J{ { / g@ S , >Ó> u12 ^_ TC 5l {V !" () u k@ « z12 * : ]5 o } $@ ! ÊdOb # \12 EÇ'< 7 `f ‘* Q&’ `_ ta{ 5l _ Z@ {0 b h! c{ _ * ¨£2 o }712 >JH º uf0u 9 M®012 Y \12 ;<. k12 u K * Q& m '( ,% A=+: 1% .O ¹@3 >: g
(81) @3 !" @ * ' t ;< p <` 1 U , ;< SC' ," '@ '( E 9
(82) 6 V§ Uj E% * ( £¿R ¡f Aâ@3 k >Ük Ük @ A5b '< V { V §. ¸ 7 '@ P% 8D Í , ! +L SC Y Ì Y @3 V { V §9 T 1^ ,$ O 6 Û ów@ ÇéN d i W0 SÏ9 * +L S% MN @
(83) '< p z9 h ]50u * Q& H \,< M ð@
(84) Y N ' vO ( µ >Ük 2 0 s% 1% '( E E % * Q& * 2 + 9 >Ó6è< E, V§9 T Y 9 Îg OS *@ A5 @ eY ï% ($,< 3> * Q&: .H> ' * d i ¯ K \$,< . 9$89(. 9. . . A=+. ;. 2. 4 . 5. . 1. . . '8+(. . . . '8'(. . . 3. . . A=+. . '. 9. . 89(. . . '. . . . A=+. . +(G. D 3. '. . 9. . D 5. '"9. . '. . . '. 9. . -. . . 5& H. $. . ". . $. . . . . . . . .
(85)
(86) . . . D 1!. A
(87) 61. . . D! -". . . . 2. '($'. -". . ,2. . . F31$. E73. 5. . '(. A=+. . 1. 1 -. 20. . E. ,. /. $. 8 ? . % $. . . /. . -". 2. 223 -" 9
(88) 4 ,5. '($'. . (1,$. . D1 -". '($'. , ,. . *9. A=+. +"-. 363. 11 62,1 1 -". (1,$. . . . $.
(89) . . Temporal/spatial hydrochemical changes of alluvium groundwaters sampled along the Pyeonghae Namdae stream.. ¬ÇO @3 fN ,, V &ç {V@ ghoB> , ,L3 = > i` >¸ 5: b '< p . '. 9. . '4 . . . 9"'. ,. . . ;?. . ,/. . = . ="> @3 + L *@ u5 K@3 >¸: 5: R79 º N1^ «3 , U% K '@ ]50u * Q& U, N< _ < 5B2 º ;< «3 m K vO @3 uo * S % , 2O * U, « º ;< * _ *Y kj 7£ ã í _ 5l' ¨£2 , oH * u5 K |R _ M@ U9 \12 M ;< % *@3 kHm , K@3 B9 Ï |Rz Ì R, @ n ä .l *Y ¨£. ,,. . . 2. . .. 59. 9"'. . .
(90)
(91) %. %. / -. . +. 9. !. *R @H2W2O , < +< mnb! c{ E@ 8 @ SL * , c{@ op @ « * u5K Â'@3 , kHm K@3 ! -" , >Ó>b o^ = E% B 5:@ « 012 i` < +' t ;< 0 ¨ £2 * U r% »w@3 +' t ; ä @ SL * K Ì O Ì@ 2 o *@ Ñ, ¬ç ·^ = <012 '( : !20 0 < < ÕA , qr ÀO@3 Ù Js `> Y t@ Ò0' , E9 * +L t <2O ,6@3 Õ 1 -"- ' , Ò0o^ B: 5:ý þ , ,20. !"2. 9. .
(92) . #
(93) .
(94) . . 2 -". . !61 -. . 44 . & . . 7
(95) -. 1. 5,. 4
(96) . !. 9 . . '. 4%. 9. 9.
(97)
(98) 4 4.
(99) . A+7. 9. 30. +(. .? !. .
(100)
(101)
(102) . . . -. . !3 -"-. 9. .
(103)
(104) . . Results of two-way ANOVA test. Spatial factor represents the variation in relation to different watersheds, and the temporal factor represents the seasonal variation.. ! ,Q SSC9 n< = {0% ^ _ V M, hi0 8¹@ 3 YW0
(105) Y i) _ W0
(106) ¹ iS) 12 ; # F| `_ = #R7 , <L MN H| ,@ ! =" # +, Z[ \,< , f! Y W0 Ç% i)
(107) : ,©Hm Ç12 W0 Ç% iS 2 >Jè< YW0 Ç@ 8 uY:}% ‘1i YÇ, hi012 H| #R79 +, s aû . <’ :},^ Ð:}% ‘0H > i Ç% 7, M9 +u<’ \,< W0 Ç@ 8*3 ¸~ uY:} Ð:}9 }D < ," :}9 t-12 SSC9 %Y! { 0 @ ! YW W Ç #@ ( 9 Ø1^ YW0 # W0 #@ 8 9 »ý ; µi(% ,k! §@3 12 Øoè< SC * +L YW W012 aû # +u \% ,,^ i Ç@ ! W0 #-9 +u \% 89( 9 , ,è< > OS ,% YW W01 2 ÊdO # Û \12 Z[oè< 9: i) @ « W01 MN 2 ; # +u< %% 9@3 ô. . ". .. . . . Ò0{ E% 2= Ùuv9 +,^ ùwN i` < < m K vO MN t<@ :< K @3 h! , *, tx@ 0 _ @HW2O yv0 ¨£2 ÂL3 V@ U9 ; \12 U'< ,@ *3 z OS@3 <Y »ý \,<. . # . 4
(108) . ! "# $% 9 @3 2 @ 0 9 h! V M <R u :9 ! +G< @3 , " u$9 DE012 * + hi 0 *C p 9 Y< &'() *+* m K vO Y {0 @ . . ". . I. . !.
(109) ,2. . .
(110) . . . Spatial changes of Na and Cl concentrations and Ca/ Na ionic ratio in alluvium groundwaters in the Uljin area, in terms of distance from the coast.. .
(111) $. . . . 1. ,. . #
(112) 4
(113) . . ,. .. . .. .
(114) . . /0. .D! 5!. .
(115) D! 2. . ,. . +(. ,. . 89(. .
(116) . . Surface geology of watersheds in the Uljin area. Watershed. Lithology. Nagok stream Bugu stream Bukmyon Namdae stream Goang, Wangpi, & Maehwa streams. Precambrian metamorphic rocks (Wonnam Formation) Precambrian granitic gneiss Precambrian granitic gneiss Precambrian granitic gneiss, Jurassic granite Precambrian metamorphic rocks (Wonnam Formation), Precambrian granitic gneiss Precambrian metamorphic rocks (Wonnam Formation), Precambrian granitic gneiss Precambrian metamorphic rocks (Pyeonghae Formation), Cretaceous sedimentary rocks, limestone, Jurassic granite Cretaceous sedimentary rocks, Jurassic granite. Chucksan stream Hwangbo stream Pyeonghae Namdae stream Sangyul stream. ý pD,< ,7@3 t :, W0 V #@ ; H i) S, K : N122 < §@ « Y = M®9 <Y +2 < ,-* < §@ ! Y Çý @ « ,$ > # @ ! YW ·, Î! B ív9 t -12 Y$9 <Y Ç< 93 t :, Y$, 5:@ « Ço U9 +,22 Çf @ ! + D {0 M # ,k! Y@ ! ÇW ¿î*ív 9 ,k SC9 %Y < SC * 12 S¯oè ä ^ _ =H@ û _ =H@ ã _ =H@ Y: *;oè< , Ì r!2=, 7@3 6 YW u5: . t :, vO V% .·012 B J{ k*/@ * r% U9 09 < m K ' i)2 i V M, Ñ 7, ä ," V Q ·, B J{ PôE. k* ·, 8i: ;9 \12 U'< OS , >: i Ç # @ « #R79 +, .·0u , 23 V &ç 6@3 vO ç¯Y W, ø ów@ B J{ g < J{ MN d J{ yS k* « 3 i) V M9 ySN / ó w12 EÇ'< " K% i)2 V , Çé s () ów, ý \ ,< 2
(117) ¹ Ì@ ½¾ ÂÃÄ K@ Ö`: ÌoH ; Ó Å« ÂÄ K ` ¤[ Ò0į ½¾ #į K, ` CÙÄ K `: SÏ < U@ V V M 78@ ! +< DE0Xçi0u 9 Y. . . #
(118) 4. . . ,. %. A. /. . . .
(119) G 4 * 4 4
(120) . . . . . . . . . . . 2. !2. . . . /. . . 4 4-. Mean and range of physicochemical data of two group waters divided by cluster analysis.. Group (Cluster). 1). . . 2. . #
(121) . !. 3. . ,2. !/. . A=+. A=+-- ". Distance1) (km). Concentration (mg/l) pH. Na. K. Ca. Mg. SiO2. Cl. SO4. HCO3. NO3. F. TDS. Mean I Min. Max.. 1.3 0.0 4.0. 6.5 5.6 7.1. 23.6 10.6 33.5. 1.2 0.3 2.8. 9.2 5.1 19.5. 5.6 3.5 7.7. 10.1 4.0 22.8. 19.2 3.5 30.7. 2.7 0.6 6.6. 20.1 7.9 50.1. 7.9 1.1 17.7. 0.3 0.0 1.0. 204.2 62.9 366.9. Mean II Min. Max.. 3.8 0.3 10.9. 6.4 5.3 7.4. 15.0 9.8 23.3. 1.7 0.9 4.1. 14.1 8.6 20.9. 6.8 4.8 11.9. 9.8 4.5 16.3. 12.6 6.1 22.4. 4.1 0.7 10.4. 28.4 14.0 44.1. 7.5 0.1 23.2. 0.2 0.0 0.6. 141.9 69.0 313.0. distance from the coast.
(122)
(123) S¯' ^ _ û _ Ç@ T hi E9 A 3@ D1^ @ =H)2 S' Y$
(124) ¹ SÏ 9 Y< , + L ^ _ Ç û _ Ç% ' *#12O B@ AB! 67, S9 ;< *#12O :< B ¿î @ f Y$2 o ^ _ Ç% û _ Ç@ ¸! ¿î ¿î >: }N 109 ;< ./* SC@ ! Ø' û Ç@ ! Ç V M@ U9 u, Yu f! u SC9 %Y< " uSC * 93 }e t ; 0 *C * 7á ¸12 <#E hi? 0k Ó;9 F5 < ' Y@ ! ' { # $, DdSÏ F5 1^ ,ó DdSÏ ,© s '@ 2= DdSÏ # 2 k < ,b â' # $9 ,k! 788in2 O S SC @ « u9 ìØ1^ , Ù¬ 9 k! Ù¬Y *C Distribution of two water groups in the Uljin area. < Ø' * ,< The grouping of water is based on cluster analysis. See also *@ u5 Y$2 o ^ _ Ç the text for detailed explanation. @ uSC * @ D< 788i n9 +L M s% YW ), Â! 788i: ï% N , E 8 < # $ 7 ã _ =H9 Îg ^ _ û _ =H@ 88i: T /L . % ¸0 1% 788i +µ9 .D SC9 n< . . . . . 61 -. '. 2 -. !2 3 -". 9 . ! -". . . ,2. . . - 4
(125) . . - ?. - %
(126)
(127) 79& . -> . . J /. !2. . A. 5. A. A 5. . . . F. ,. . .. '$9 '$A=+ 9 $A=+. 9;$A=+. Correlation matrix for group I waters.. logNa logK Mg logCa Cl logSiO2 logSO4 logNO3 logTDS logHCO3 logF pH. logNa. logK. Mg. logCa. Cl. 1.00 0.25 0.82 0.63 0.88 0.53 0.55 0.81 0.85 0.29 -0.20 0.40. 1.00 0.24 0.22 0.16 -0.10 -0.09 0.26 0.21 0.10 0.46 0.28. 1.00 0.86 0.89 0.49 0.56 0.85 0.89 0.38 -0.29 0.27. 1.00 0.77 0.44 0.56 0.73 0.90 0.65 -0.19 0.23. 1.00 0.53 0.66 0.74 0.86 0.27 -0.30 0.32. logSiO2 logSO4 logNO3 logTDS logHCO3. 1.00 0.06 0.64 0.64 0.25 -0.37 -0.15. 1.00 0.39 0.57 0.22 -0.11 0.19. 1.00 0.88 0.43 -0.15 0.14. 1.00 0.63 -0.20 0.22. 1.00 0.02 0.04. logF. pH. 1.00 0.25. 1.00.
(128) . Rotated. component matrix for group I waters.. . Rotated component matrix for group II waters.. Component. Component. 1. 2. 3. logNa logK Mg logCa Cl logSiO2 logSO4 logNO3 logTDS logHCO3 logF pH. 0.57 0.27 0.67 0.75 0.55 0.74 0.13 0.81 0.84 0.72 -0.16 -0.14. 0.72 0.06 0.66 0.50 0.78 0.04 0.78 0.42 0.53 -0.03 -0.16 0.63. 0.01 0.80 -0.04 0.05 -0.11 -0.40 -0.13 0.02 -0.01 0.18 0.83 0.49. eigen value % variance. 4.19 34.87. 3.32 27.66. 1.79 14.92. logNa logK Mg Cl logHCO3 logNO3 logSiO2 logSO4 logTDS logCa eigen value % variance. 1. 2. 3. 0.70 0.31 0.80 0.71 0.85 0.02 0.25 0.20 0.87 0.85. 0.30 0.69 0.34 0.48 -0.43 0.76 0.05 0.82 0.25 0.21. 0.46 0.18 0.03 0.09 0.01 0.27 0.92 -0.33 0.39 0.21. 4.05 40.49. 2.44 24.46. 1.49 14.86. >: 6 ¤ 2 ²122 KY * @ U, 'ã \12 U'< L * _ *Y2O 7;E @H2W% tx9 « 6õ12 , x Ò0 _ Â'@ Â9 h! vO MN *12O ¿î ,6@ f vO V M9 #Y[ ; \12 *C'< 6õ ¢ *12O B ¿î @ f û _ @ 8 788i n uSC * @ D< ìØ' u9 +L ¬çS }e9 ë u @3 5: 8D # 23 : 1% u¹ ,7 >Ó1 2 V &ç Ì BJ{ k*/, Ì V #uµ9 /u! è< ="> . "-. ;< Ù¬' u n9 +L ¬ ç S }e9 ë u @3 ü : 1% R u¹ >Ó6è < u¹ ¸0 b >1> , Î g V# $% 2 V &ç { / * 2 *C'< ^ _ Ç@ ! }e9 ë u @3 3ÊH MN : 1% u¹ ë ; ä , %% 93 }e t :, t<2O * _ *Y U9 Y \12 *C '< !3 '@ t<@3 ~ U .O /ý \12 U'< - t<@3 A ,. . -$. 21 ,50. . A=+. B. +(. 9. ;. 89(. 4. '(. . $. . !5 330. !. ;. '. +( 8. 9 . .
(129) .
(130) .
(131)
(132) % +(. 4- %.
(133) 4 . =;+. . =;+. . .- . . . . . 1 -. 2 -. A 3. 26 -. 2 ,. . - A 3. D/. A. A . . A . 1 10. - . A=+. ,. 9 ; 89(. . . '. Correlation matrix for group II waters.. logNa logK Mg Cl logHCO3 logNO3 logSiO2 logSO4 logTDS logCa. logNa. logK. Mg. Cl. logHCO3. logNO3. logSiO2. logSO4. logTDS. logCa. 1.00 0.53 0.62 0.70 0.46 0.29 0.58 0.26 0.83 0.67. 1.00 0.45 0.58 0.02 0.36 0.27 0.49 0.46 0.35. 1.00 0.71 0.47 0.29 0.27 0.37 0.77 0.70. 1.00 0.34 0.32 0.27 0.42 0.74 0.62. 1.00 -0.24 0.19 -0.17 0.66 0.65. 1.00 0.20 0.46 0.38 0.36. 1.00 -0.13 0.59 0.41. 1.00 0.27 0.31. 1.00 0.93. 1.00.
(134)
(135) § @3 { ,k , ¸0 1% E)¹ D >Ó6 \1 Q SSC9 n! JK0u V M # 2 + û _ 12 S¯' .O Y Ì@ F| *
(136) Y@ i # +! * U9 QÎý N09 Y*§< +( : § ,% ] +( 1^ iS)2 F|' }e9 >Ó× u @3 1% E)¹ Û ä ,$% >Ü Ó uWj W # +!§ V {% ê, @ uf0 U9 / \12 *C'< è< «3 K vO V M% i # iS@ « 67b # s 09 ;< YW W iS) u9 YY V m K@ OP Í ,6 vO hi0 8@ SC9 n * `@3 i)2 Y 7 *12O B E12 So Y , Øoè< *Y 12 V n< U, V =H9 >J ä Ì uµ9 ; * <0 :< ' @ 8 JK0, D0u *C è< û @ uSC 9 n 9 h! K V M% aû . ·012 B J{ MN í*C Ñ0 k*/ ! V # u9 +< ç012 F|< * Õ @ * Q9 /u< ,@ « *@ u @ :<'L3 ¿î ¿B ¸0 1% E ¿î 5 .O K9 Îg OS 12 Mo ^ _ Y * ¨ V M9 +!§< i) V M Çf S% V M ¨@ ]50, ; V M% B J{ k*@ · Ì U9 ; ä , : u S9 }e g@ * u R vO M ów@ B J{9 Îg }e 12 }eoè< /L *@3 @3
(137) oè ï% E ¿ Ó J{ MN d J{ yS k* B ¿î î ¿î 9 >Ó× û _ ów12 *C'< K V9 Q û _ V M% B J{ k* .O *Y u% 2 ²j 8D' \12 +! V U ²j @ u {V 12 }e ,< V % i Q oè< K ¯ @ *;o K12 Ú þ ¹· Í o U9 +!è ä , v y0z da L0 Í 5: 3ÊH ²j , 5:L3 OE, 5: ów12 U'< ," , »w%
(138) ¬#J{$ U% Z,+ <,=, 7@3 L >Ó> t 7 OS012 môÇ ¸ ¯@3 @ ! oè< »w9 Í ¨ ÌX¯2 :L 3 ¨12 ¹# M9 + * û Íf }0 ¸¿ Ñ@ i! < !è< 2 V M ¨ ã _ u123 t<2O * *Y , /uoè< , *12 A5ý þ ' E, 5:o }712 >Ó < ," # M®012 t<@ :< K@ ) O) 3 uo ä Y@3 67b >Ó> ,$ Y V ¨% ¬¨0u ¨ O 3 ^P9; . 4 ,è< «3 K V M *C@ O5^ J5 ;H3 0u { ÄC / U g@ * c ãÍN *¶ ý \,< 9. 5. . !. F '(. 1 /0. . !1 130. . . . . 9. 89( +(. . . /. . . 1 -. !/. ,2. . . '. 9. !. . . J /. 3. . . . . . 9$. 89(. 2 -. -. '. 9. . !2 3. ! -". ! 261 . !2. . . . . . . . 2/0. . . . '. 2 , -. / -". . !,0. 9 . ! 3 -". !. . . '(. . . . . . . F.$!$=7125. 9$89(. '$9 $'($89(. 9.
(139) . E. . . '$9.
(140) . . , !1 /.
(141) . .
(142)
(143) . . . . . . . $. !" # $% %&&' () !*) %+
(144) . ,"-+(+&( &. / +." 0++%+' & &%% +&(.
(145) . . +(1 ++0% (%'+ $(2+"&(-(% 3&%&1' 2. 3 .&( B$9 () ;"&( $ +% () -&"% &. 0%&"+) )&++&( +( & "( *)(.
(146)
(147) . 4 55 () 546
(148) ()") -&) .&" )"-+(+&( &. *" () * *"
(149) ) 4 %+0+&(. 5" +" () &+% 4&%% +&( 2
(150) B1"+C B&")08+ () ; C+" !$
(151) 5" "&08 +("0+&( () *" ."*" -+D+(1 ..0 +(. %& ! () 4&- ,
(152) 3&0-+"' 1"& ()*" () &%% +&( 7%8- 9&")- . . 0&%. ) (. / +.". &0&. 7'. "1&(. 3&0+-+0 &-&0+-+0 0 2
(153) . (1 :; ;- < ( ;= 5(1 > () (1. #)%" B1"+D B () BC" $
(154)
(155) -+0%. << -+0% 0"0"++0 &. "&&% . "0+&( &. *" *+ "&08 () ."*". 0&% +&( +( &(1 <&(1 &(% 2"++&( &.. D"+-(%. -?&" +&( %&1( () -+("% ) *(
(156) . *" +( "% 3&0+-+0 &-&0+-+0 0 2. ()
(157) -&"+0 $(2+"&(-( 2
(158) . .+%). &"2+&(. &(. "08+. 9+0" 7 <"+%" 5 () 7%)& 7$
(159) . &)+& $
(160) ')"&1&0-+"' () "0" ( &)+& $ $) 3"& ()*" "&%- +( 0&% ". (). )'. (). "&". +(. ')"&%&1'. (&. 3&0-+0% 0(+/ .&" +)(+.'+(1 & "0 &. 1"& ()*" %+(+C+&( < -&%' . . 9+))" >7
(161) ( 0-+"' &. "0+++&( +(. ,"2" !
(162) > 1&0-+' &. ( "% *". 9&( () !&(
(163) &("&% &( 0-+0%. @#$
(164) () ) 4"(+0 %% 6&"-(+ 4 4+8 ! () ((1"( !
(165) . , 0 9&'% B ( 9 0&-&++&( &. 1"& ()*" ."&- %% 2+% / +." +( 5(8 () 58+. +( ("% 1& #*. ,0+&( &. (&( % %. "&&% "-&. :%() ')"&1&%&1' !& "(% 2
(166) . 0&% + +( & ."+0 4A$ )' # 0%". 9& (+ () 508"(1%
(167) B %+2"+ 1&. (" -( () B&) +( 4'+0 9"0 7
(168) . ++0% "&0 & 0 +- ) (%'+ 5". . 9& "0 9"0 2
(169) . 6"+C !
(170) "2' &. 0"1 %(0 ""&" &(. 5+8' $ & 9 )*+08 () *". %+) (%' &. 1"& () () ".0 *". 75 > +-&"(0 &. "' & 0+&(. 3"& ()*" 2 . )1 &. 0&% *++( &+% "&(+ - +&&. 3&%)"1 $, 7"&08" 5 3"& B3 () > "8+(. "&0 -+0% 3&%&1' 2
(171) . <<
(172)
(173) B"+( 0-+"' ( 9)+&0+2+' +( . = ( > &+ 7= () ; 4< ,+"+ +&( &.. -"+( (2+"&(-( 5+(1&( , #+&(% 0). 2' -% " :( 4 ) +( "&)+) ). -' &. 0+(0
(174)
(175) . +-( & % -"&&%+( 0+' <&" $(2+"&(-(. 3 .&( B$9 () 6"(C( ;3 (%() "(&" &. -"+( "&&% +( & "( *)( -&"+0 $(2+"&(-( 2
(176) . % >0(&%&1' 2
(177)
(178) . < 9.
(179).
(180).
(181) . < ".
(182). . . .
(183)
관련 문서
A A A A Study Study Study Study Analysis Analysis Analysis Analysis of of of of the the the the J. Bach, a representative composer in Baroque period. Composed
Thirdly, it appeared that social support had meaningful effect on self-efficacy and the quality of life, and in the case of the difference analysis by
XRD analysis, surface roughness test, FE-SEM imaging, and biaxial flexural strength test were performed... Results: In the result of XRD analysis, an phase change occurred
Second, the analysis of differences by affiliation showed that the controlled coaching actions were perceived higher in order of the general, secondary, and
The torque analysis was performed acting on the joint of robot by modeling the kinematics and dynamics of the robot.. Load torque of the joint
For the analysis of the contents of the 'Energy and Transport Technology' section, the analysis frame was divided into 3 categories, including the ratio of
In order to conduct a more detailed and dense analysis of the overall operation of the Creation & Production Center, the case of the creation
t-test and analysis of variance were carried out to find out the differences along general characteristics and it was analyzed by setting correlation