|
|
|
Çѱ¹¼öÀÚ¿øÇÐȸ / v.26, no.4, 1993³â, pp.47-60
|
À׿ï¾Ï°ñÁÖº¯ Æí¸¶¾Ï¿¡¼ÀÇ ÁöÇϼöÀ¯µ¿Æ¯¼º ºÐ¼®
( An Analysis on Groundwater Flow Properties in the Gneiss of the Ingulam Valley ) |
| ±è°è³²;±èÀçÇÑ; Çѱ¹¿øÀÚ·Â ¿¬±¸¼Ò ¼ö¹®±â¼ú½Ç ¿¬±¸¿ø;Ãæ³²´ëÇб³ Åä¸ñ°øÇаú ±³¼ö, Çѱ¹°úÇбâ¼ú¿ø Åä¸ñ°øÇаú ±³¼ö, Çѱ¹¿øÀÚ·Â ¿¬±¸¼Ò ¼ö¹®±â¼ú½Ç ½ÇÀå;
|
|
|
 |
|
| |
| ÃÊ ·Ï |
| »ï±¤±¤»ê ÁÖº¯ÀÇ À׿ï¾Ï°ñÀ» Áß½ÉÀ¸·Î ¼ö°è¸¦ Çü¼ºÇÏ´Â À¯¿ª³»¿¡¼ÀÇ ÁöÇϼö À¯µ¿Æ¯¼ºÀ» ºÐ¼®ÇÏ¿´´Ù. À̸¦ À§ÇØ ÇöÀå¼ö¸®½ÃÇèÀ» ½Ç½ÃÇϰí, ÁöÇϼö À¯Ãâ·®À» ÃøÁ¤Çϰí MODFLOW¸ðÇüÀ» ÀÌ¿ëÇÏ¿´´Ù. ºÐ¼®°á°ú ¿¬±¸Áö¿ª³»ÀÇ ÁöÇϼö¸éÀ¸·Î À¯ÀÔµÈ °¼ö´Â ÇØ¼ö¸é ¼±»ó EL(+)100m ÀÌÇÏÀÇ Æí¸¶¾Ï ½ÉºÎ·Î´Â °ÅÀÇ Ä§ÅõÇÏÁö ¸øÇß´Ù. ¼ö°è°æ°è ºÎ±ÙÀ¸·Î À¯ÀÔµÈ °¼ö´Â °³¿ï ÁÖº¯À¸·Î À¯ÃâµÇ¾ú°í, À¯ÀÔ°¼öÀÇ ÁöÇϼö À¯µ¿½Ã°£Àº 15³â¿¡¼ 263³â »çÀÌÀÇ °ªÀ¸·Î °è»êµÇ¾ú´Ù. ¶ÇÇÑ ¿¬±¸Áö¿ª³»¿¡¼ÀÇ ÃÑ ÁöÇϼö À¯Ãâ·®Àº 307§©/day·Î »êÁ¤µÇ¾ú´Ù. |
|
| The evaluation of grounwater flow in the Ingulam valley catchment area in the vicinity of SamKwang mine was studied. In this study, field hydraulic tests, groundwater flow measurement, and MODFLOW model application were carried out. The results of analysis are described as follows. The rainrate infiltrated into the ground in the study area, hardly reached the gneiss region deeper than EL.(+)100m above the surface of seawater. The rainwater infiltrated into the ground near the water system boundary, flowed out into the vicinity of streams and the travel time was between 15 and 263 years. Also, the estimated total flow rate of the groundwater in the study area was 307§©/day |
| |
| Ű¿öµå |
|
| |
|
|
 |
|
Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.26, no.4, 1993³â, pp.47-60
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199311920094645)
¾ð¾î : Çѱ¹¾î |
|
| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
|
|
|
|
|
|