|
|
|
Çѱ¹ÇÏõȣ¼öÇÐȸ / v.37, no.4, 2004³â, pp.431-435
|
ÀϺ» Ã÷²ÙÀÌ ¼±»óÁö ÁöÇϼöÀÇ Áú»ê¼º Áú¼Ò ¿À¿°¿¡ ´ëÇÑ ¼ö¹®Áö±¸ÈÇÐÀû ¿¬±¸
( Hydrogeochemical Environmental Research in Nitrate Contamination in Alluvial Fan Area Groundwater in Tsukui, Central Japan ) |
| ;; ;;
|
|
|
 |
|
| |
| ÃÊ ·Ï |
| ÀÌ ¿¬±¸´Â ÀϺ»ÀÇ Ä«³ª°¡¿ÍÇö Ã÷²ÙÀÌ¿¡ À§Ä¡Çϰí ÀÖ´Â ¼±»óÁö¿¡¼ ÁöÇϼö ¼öÁúÀ» Á¶ÀýÇÏ´Â ¿äÀεéÀ» Æò°¡Çϱâ À§ÇØ Áú»ê¼º Áú¼Ò¿¡ ÀÇÇØ ¿À¿°µÈ ÁöÇϼö¸¦ ¼ö¹®Áö±¸ÈÇÐÀûÀ¸·Î Á¶»çÇÏ¿´´Ù. 2003³â ¿ùº° ÁöÇϼöÀÇ ¼öÀ§´Â °¿ì¿¡ ÀÇÇØ Å©°Ô Áõ°¨ÇÏ¿´Áö¸¸, ÁöÇϼö ³»ÀÇ Áú»ê¼º Áú¼Ò ³óµµ´Â ¾à°£ÀÇ º¯È¸¸À» º¸¿©ÁÖ¾ú´Ù. »Ó¸¸¾Æ´Ï¶ó ³âÁß ´ëºÎºÐ ÁöÇϼö ¼öÁú ±âÁØÀÇ ÃÖ°í ¿À¿° ¼öÁØ $10mgL^{-1}$À» ÃʰúÇÏ¿´´Ù. 2003³â 1³â°£ ÁöÇϼöÀÇ ÀçÃæÀü·®Àº 1,730mm(ÁöÇϼö ¼öÀ§ÀÇ ÀÏ Áõ°¡ÀÇ ³â°£ ÃÑÇÕÀÎ 20,056mm¿Í ÀϺ° °¨¼Ò·®ÀÇ ³â°£ ÃÑÇÕÀÎ 18,326mmÀÇ Â÷ÀÌ)·Î ³ªÅ¸³µ´Ù. ±×·¯³ª ÁöÇϼö ¼öÀ§ÀÇ ÀϺ° Áõ°¡·®ÀÇ ³â°£ ÃÑÇÕ(20,056mm)Àº ³â°£ °¿ì·®º¸´Ù ¾à 10¹è ÀÌ»ó ³ô¾Ò´Ù. ´õ¿íÀÌ ÀϺ° °¨¼Ò·®ÀÇ ³â°£ ÃÑÇÕ(18,326mm)Àº ¸¹Àº ¾çÀÇ ÁöÇϼö°¡ Áú»ê¼º Áú¼Ò ¿À¿°°ú ÇÔ²² ¹æÃâµÇ¾úÀ½À» º¸¿©ÁÖ¾ú´Ù. »ó´çÈ÷ ³ôÀº Áú»ê¼º Áú¼Ò¸¦ º¸À¯ÇÑ °¿ì°¡ ÀÖÀº ÈÄ, ¼±»óÁö¸¦ ÅëÇØ ¸¹Àº ¾çÀÇ ÁöÇϼö À¯ÃâÀÔÀÌ °üÂûµÇ¾ú´Ù. °á°úÀûÀ¸·Î, »ê¸²Áö´ë¸¦ Æ÷ÇÔÇÑ ÀÌ ¼±»óÁö¿¡¼´Â 'Áú¼Ò °úÀ×' ¶Ç´Â 'Áú¼Ò Æ÷È' ¶ó°í ÇÏ´Â »óŸ¦ ¹Ý¿µÇϰí ÀÖ´Ù. ¸¹Àº ¾çÀÇ ÁöÇϼö ¹æÃâÀº ÁöÇ¥¼ö¿¡¼ Áú»ê¼º Áú¼ÒÀÇ ¿À¿°°ú °°Àº ȯ°æ¹®Á¦¸¦ ¾ß±âÇÒ ¼ö ÀÖÀ¸¸ç, º» ¿¬±¸¸¦ ÅëÇØ ¼ö¹®Áö±¸ÈÇÐÀû ÀÚ·á°¡ ¼öÁú°ü¸®¿¡ À¯¿ëÇÏ±æ ±â´ëÇÑ´Ù. |
|
| A nitrate-contaminated groundwater was hydrogeochemically investigated to estimate the factors controlling groundwater quality in an alluvial fan area. Even though monthly groundwater levels increased with monthly rainfalls, the monthly $NO_3^--N$ concentrations in groundwater showed a small variation, mostly exceeding a maximum contaminant level of 10 mg $L^{-1}$ in environmental quality standards for groundwater during 2003. The 2003 annual groundwater recharge was 1,730 mm =20,056 mm-18,326 mm. Where 20,056 mm and 18,326 mm are annual sum of daily increase and decrease in ground water level. However, the annual sum of increase in ground water level (20,056 mm) was approximately 10 times higher than annual rainfall. Moreover, the annual sum of daily ground water level decrease (-18,326mm) showed that a large amount of groundwater was discharged with $NO_3^-$-contamination. Hydrogeochemically, a large amount of groundwater input and output through the alluvial fan area were observed after rainfall with a considerably high concentration of $NO_3^-$. Consequently, this alluvial fan area including forest area reflects on the evidence under the condition of 'nitrogen excess' or 'nitrogen saturation'. In addition, such a large amount of groundwater outflow can cause environmental damage in surface water, associated with $NO_3^-$- contamination. This study also expects that this hydrogeochemical data will be useful for water management. |
| |
| Ű¿öµå |
| nitrate-contaminated groundwater;groundwater recharge;rainfall; |
| |
|
|
 |
|
Çѱ¹ÇÏõȣ¼öÇÐȸÁö / v.37, no.4, 2004³â, pp.431-435
Çѱ¹ÇÏõȣ¼öÇÐȸ
ISSN : 1976-8087
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200418317183521)
¾ð¾î : ¿µ¾î |
|
| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
|
|
|
|
|
|