¹ßÇ¥³â¿ù |
2016 ³â 06 ¿ù
|
°ü·ÃºÐ¾ß |
Çؾçȯ°æ
|
ISSN CODE |
ISSN - 2288 - 0089
|
³í¹®±¸ºÐ |
KCI
|
¹ßÇà±â°ü |
Çѱ¹Çؾçȯ°æ¿¡³ÊÁöÇÐȸ
|
¹ß°£ÁÖ±â |
ºÐ±âº°
|
¹ßÇ¥Áö¸í(ÇÑ) |
Çѱ¹Çؾçȯ°æ¿¡³ÊÁöÇÐȸÁö
|
¹ßÇ¥Áö¸í(¿µ) |
Journal of The Korean Society of Marine Environmental Engineers
|
Á¦1ÀúÀÚ |
˱ȗ̦
|
Á¦2ÀúÀÚ |
À±ÀÌ¿ë
|
Á¦3ÀúÀÚ |
|
±³½ÅÀúÀÚ |
|
°øµ¿ÀúÀÚ |
|
±â¿©À² |
100
|
¹ß°£ÀÚ È£¼ö |
19(2) ȣ
87 -
98 ÂÊ
|
»öÀξî(ÇÑ) |
¿µ¾ç¿°, ¿±·Ï¼Ò, µ¿ÇØ, ¿¬¾È¿ë½Â, ³¼ö¿ª, ³Ã¼ö¿ª
|
»öÀξî(¿µ) |
¿µ¾ç¿°, ¿±·Ï¼Ò, µ¿ÇØ, ¿¬¾È¿ë½Â, ³¼ö¿ª, ³Ã¼ö¿ª
|
´ë¿Ü¹ßÇ¥½ÂÀο©ºÎ |
°ø¹®¹øÈ£ : ±âÈĺ¯È¿¬±¸°ú-1889
°á Á¦ ÀÏ : 2016.05.16
|
ȨÆäÀÌÁö°ø°³ |
|
³»¿ë¿ä¾à(ÇÑ) |
2009³â 7¿ù 3ÀϺÎÅÍ 7¿ù 27ÀϱîÁö ·¯½Ã¾Æ Á¶»ç¼± R/V Lavrentyev¸¦ ÀÌ¿ëÇÏ¿© ·¯½Ã¾Æ ¿¬¾ÈÀ¸·ÎºÎÅÍ 4°³ÀÇ Line(D, R, E, A)À» µû¶ó Ç¥Ãþ 30 m ¼ö½ÉÀÇ ½Ã·á¸¦ 26°³ÀÇ Á¤Á¡(¿ï¸ªºÐÁö¿Í ÀϺ»ºÐÁö¸¦ Æ÷ÇÔÇÑ µ¿ÇØÀÇ Àü ¼ö¿ª)¿¡¼ ä¼öÇÏ¿© ¿µ¾ç¿° ¹× ¿±·Ï¼Ò-aÀÇ ³óµµ¸¦ ºÐ¼®ÇÏ¿´´Ù. ³Ã¼ö¿ªº¸´Ù ³¼ö¿ª¿¡¼ 1.4¹è ³ôÀº Áú»ê¿°À» Á¦¿ÜÇÑ ³ª¸ÓÁö Ç׸ñµéÀº ¸ðµÎ ³¼ö¿ªº¸´Ù ³Ã¼ö¿ª¿¡¼ ³ô°Ô ³ªÅ¸³µ´Ù(NH4, PO4 °¢ 1.8¹è, Si(OH)4 1.2¹è, ¿±·Ï¼Ò-a 1.9¹è). ¾Ï¸ð´Ï¾Æ¿Í Àλ꿰, ¿±·Ï¼Ò-aÀÇ ¼öÆòºÐÆ÷´Â ¸Å¿ì À¯»çÇÑ ºÐÆ÷¸¦ º¸À̸ç, ÇÑ·ù¿Í ÀúÃþ¼öÀÇ ¿ë½Â ¿µÇâ±Ç¿¡ ÀÖ´Â ·¯½Ã¾Æ ±ÙÇØ¿¡¼ ÃÖ´ëÄ¡¸¦ º¸ÀÌ°í, ¿ï¸ªºÐÁö¿¡¼ ºñ±³Àû ³·Àº ºÐÆ÷¸¦ º¸ÀδÙ. ¹Ý¸é, Áú»ê¿°Àº ´ë¸¶³·ù¼öÀÇ Á÷Á¢ÀûÀÎ ¿µÇâ±Ç¿¡ ÀÖ´Â ¿ï¸ªºÐÁö¿¡¼ ÃÖ´ëÄ¡¸¦ º¸À̸ç, Á¡Â÷ ºÏ»óÇÒ¼ö·Ï °¨¼ÒÇÑ´Ù. N/P ºñ´Â ÇÑ·ù¼ö°èº¸´Ù ´ë¸¶³·ù ÁßÃþ¼ö¿¡¼ °¡Àå ³ôÀº °ªÀ» º¸À̸ç, ´ë¸¶³·ù¼ö´Â µ¿ÇØ·Î À¯ÀԵǴ Áú»ê¿°ÀÇ ÁÖ¿ä °ø±Þ¿øÀ¸·Î ÀÛ¿ëÇÏ°í ÀÖ´Ù. ±×·¯³ª ³¼ö¿ª¿¡¼ Àλ꿰ÀÇ Æò±Õ ³óµµ´Â 0.2 ¥ìM ÀÌÇÏ·Î ½Ä¹°ÇöûÅ©Åæ ¼ºÀåÀÇ Á¦ÇÑ ¿äÀÎÀ¸·Î ÀÛ¿ëÇÒ ¼ö ÀÖ´Â ¹Ý¸é, ³Ã¼ö¿ª¿¡¼ÀÇ ³ôÀº ³óµµ´Â ¿±·Ï¼Ò-a¿Í Á÷Á¢ÀûÀÎ »ó°ü¼ºÀ» º¸ÀÌ°í ÀÖ´Ù. Çؾçȯ°æ¿¡ ¿µÇâÀ» ¹ÌÄ¡´Â ÁÖ¿äÀÎÀ» ºÐ¼®Çϱâ À§ÇÑ ÁÖ¼ººÐ ºÐ¼®°á°ú ÁÖ¼ººÐ IÀº ¼ö¿Â¿¡ ÀÇÇØ µ¿ÇØÀÇ Çؾçȯ°æÀÌ ÁÖ·Î ¿µÇâÀ» ¹ÞÀ¸¸ç, ÁÖ¼ººÐ II´Â ¿µ¾ç¿°°ú ¿±·Ï¼Ò-a °¡ ÁÖ¿äÀÎÀ¸·Î ÀÛ¿ëÇÑ´Ù. µû¶ó¼ ¿¬±¸ÇØ¿ªÀÇ Çؾçȯ°æÀº ¼ö¿Â¿¡ Áö¹èµÇ¸ç, ±×¿¡ µû¶ó ³Ã¼ö¿ª°ú ¿Â¼ö¿ªÀ¸·Î ±¸ºÐµÇ´Â Ư¼ºÀ» º¸¿´´Ù.
|
³»¿ë¿ä¾à(¿µ) |
During the period between July 3 and 27 of 2009, water samples were collected from the Russian coast at a depth of 30m from 26 stations (including Ulleung and Japan basins) onboard the Russian survey vessel R/V Lavrentyev following 4 lines (D, R, E, and A). The samples were analyzed for nutrients and chlorophyll a contents. All parameters exhibited higher values in warm waters than in cold waters (NH4:1.8-fold, PO4:1.8-fold, SiO2:1.2-fold, and chlorophyll-a: 1.9-fold), except nitrates, which was 1.4-fold higher in cold waters than in warm waters. The horizontal distribution of ammonia, phosphate, and chlorophyll-a was very similar to each other and showed the highest values in the waters near Russia, where a upwelling influence of cold current and bottom water prevails, while relatively low distribution was observed at the Ulleung Basin. On the other hand, nitrates showed the highest concentration at the Ulleung Basin, which is under the direct influence of the Tsushima warm water, and showed a gradual decrease northward. The N/P
ratio showed the highest value in the Tsushima middle water, rather than in the North Korean Cold Water, the Tsushima Warm Water was the primary source of nitrate flow into the East Sea. However, the average concentration of phosphate in the warm waters was < 0.2 ¥ìM, thereby limiting phytoplankton growth, while a high concentration of phosphate in cold waters showed a direct correlation with chlorophyll-a. The results of principal component analysis for the identification of primary factors that influence the marine environment showed that principal component I as water temperature and principal component II was influenced chlorophyll-a and nutrients. Therefore, Study area has greatest influenced by water temperature, and clearly distinct cold and warm water regions were observed in the East Sea.
|
¿¬±¸ÀÚ·á Áö½ÄºÐ·ù |
±ÙÇØ Á¶»ç/
|