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Çѱ¹ÀܵðÇÐȸ / v.23, no.1, 2009³â, pp.143-150
°ñÇÁÄÚ½º¸¦ Á¶¼ºÇÒ Æó¿°Àü ¸Å¸³ÁöÀÇ ÁöÇϼöÀ§¿¡ µû¸¥ Åä¾ç»êµµ ¹× Àü±âÀüµµµµ º¯È­
( Changes of Salt Concentration by the Height of Ground Water Table on Disused Saltpan for Golf Course Construction Site )
À̵¿ÀÍ;±è±âµ¿;ÁÖ¿µ±Ô; ºí·¢½ºÅæ°ñÇÁÀå;¿¬¼¼´ëÇб³ °úÇбâ¼ú´ëÇÐ »ý¸í°úÇбâ¼úÇкΠ»ý¹°ÀÚ¿ø°øÇÐ;¿¬¼¼´ëÇб³ °úÇбâ¼ú´ëÇÐ »ý¸í°úÇбâ¼úÇкΠ»ý¹°ÀÚ¿ø°øÇÐ;
 
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Æó ¿°Àü ¸Å¸³Áö¸¦ Ȱ¿ëÇÑ °ñÇÁÄÚ½º Á¶¼º¿¡ À־ Áß¿äÇÑ °ÍÀº °í³óµµÀÇ ¿°ÀÌ ½Ä¹° »ýÀ°ÀÇ Á¦ÇÑ ¿äÀÎÀ¸·Î ÀÛ¿ëÇÑ´Ù´Â °ÍÀÌ´Ù. ³ôÀº ³óµµÀÇ ¿°·ù¸¦ Á¶ÀýÇÏ´Â °ÍÀÌ ÇʼöÀûÀ̸ç, °Ç¼³ ºÎÁöÀÇ Åä¾çÀ» °³·®Çϱâ À§Çؼ­´Â Åä¾ç ¹× ÁöÇϼö ³» ¿° ³óµµ¿¡ ´ëÇÑ Ã¼°èÀûÀÎ ÁöÇ¥¸¦ ÇÊ¿ä·Î ÇÑ´Ù. ÀÌ¿¡ º» ¿¬±¸´Â ÁöÇϼöÀ§¿¡ µû¸¥ pH ¹× ¿° ³óµµÀÇ º¯È­¸¦ Á¶»çÇÏ¿´´Ù. ÀÌ´Â °ñÇÁÄÚ½º Á¶¼º ½Ã Áö¹Ý°ø»ç¸¦ À§ÇÑ ±âÃÊÀÚ·á°¡ µÉ »Ó¸¸ ¾Æ´Ï¶ó °ø»ç ÈÄ ½ÄÀçÁö¹ÝÀÇ È¿À²ÀûÀ̰í ÇÕ¸®ÀûÀÎ °ü¸®¿¡µµ À¯ÀÍÇÑ ÀÚ·á°¡ µÉ °ÍÀ¸·Î »ç·áµÈ´Ù. ´ë»óÁö¿ªÀÇ Åä¾ç ¹°¸® È­Çмº ºÐ¼® °á°ú, °Ç¼³ºÎÁö ³» Åä¾çÀÇ ´ëºÎºÐÀº ¿°ºÐ ÇÔ·®ÀÌ ³ô°í ¾à ¾ËÄ®¸®¼ºÀÇ ½ÄÅä(clay soil)·Î ºÐ·ùµÇ¾ú´Ù. ÁöÇϼö ¼öÀ§º¯È­´Â °¥¼ö±â(6¿ù Áß Çϼø), À帶±â(2006³â 7¿ù ÃÊ Áß¼ø), À帶Èıâ(7¿ù ¸»)·Î ÃøÁ¤ ½Ã±â¸¦ ±¸ºÐÇÑ °á°ú 1.3m, 3.3m ¹× 2.8m·Î À帶±â ÁöÇϼöÀ§´Â Æò±Õ Áö¸é³ôÀÌ 2.9m¿¡ ºñÇØ ¾à 0.4m ³ôÀº °ÍÀ¸·Î ÃøÁ¤µÇ¾ú´Ù. Àü±âÀüµµµµÀÇ º¯È­¸¦ ÃøÁ¤ÇÑ °á°ú °¥¼ö±â¿¡´Â Àüü ÃøÁ¤Áö¿ª¿¡¼­ $4.0dS{cdot}m^{-1}$ ÀÌ»óÀ¸·Î ÃøÁ¤µÇ¾ú°í, Áö¿ª¿¡ µû¶ó¼­ $20dS{cdot}m^{-1}$ ÀÌ»óÀ¸·Î ³ªÅ¸³µ´Ù. À帶±â ECe ÃøÁ¤°£Àº $1.2{sim}15.0dS{cdot}m^{-1}$·Î °¥¼ö±â¿¡ ºñÇØ »ó´ëÀûÀ¸·Î ³·Àº EC°ªÀ» ³ªÅ¸³Â´Ù. µû¶ó¼­ Æó ¿°Àü ¸Å¸³Áö¸¦ ÀÌ¿ëÇÑ °ñÇÁÄÚ½º Á¶¼º¿¡ ÀÖ¾î °í³óµµÀÇ ¿°À» ÇÔÀ¯ÇÑ ÁöÇϼö¿Í ½ÄÀçÁö¹Ý°úÀÇ ¸ð¼¼°ü ¿¬°áÀ» Â÷´Ü½ÃŰ´Â °ÍÀÌ Áß¿äÇÏ´Ù. À̸¦ ½ÇÇöÇϱâ À§ÇÏ¿©´Â ÃÖ°í ÁöÇϼöÀ§ º¸´Ù ³ôÀº ÁöÁ¡¿¡ Â÷´ÜÃþ(ÀÚ°¥Ãþ)À» Æ÷¼³ÇÑ ÈÄ ½ÄÀçÃþÀ» Æ÷¼³ÇÏ¿© Åä¾ç ³» ¸ð¼¼°ü ÀÛ¿ëÀ» Â÷´ÜÇÔÀ¸·Î½á ¿°¼ººÐÀÇ ½ÄÀçÁö¹ÝÀ¸·Î À̵¿À» Â÷´ÜÇÑ´Ù¸é ¿°ÇØ¿¡ ÀÇÇÑ ½Ä¹°»ýÀ°ÀÇ Àå¾Ö¸¦ ¹æÁöÇÒ ¼ö ÀÖÀ» °ÍÀ¸·Î »ç·áµÈ´Ù.
High salt concentration is one of the most important limit factor on plant growth at a disused saltpan for golf course construction site. The control of salt in soil is definitely required and the monitoring of salt concentration in soil and ground water also required to amend soil physiochemical properties. This research was carried out to monitor the pH and salt concentration changes by the height of ground water. By the physiochemical analysis test, the soil contains a high salt concentration and classified as a slight alkaline clay soil. The height of ground water table changed to 1.3m, 3.3m and 2.8m at dry season(mid-late June, 2005), monsoon season(early-mid July) and after monsoon(late July), respectively. Compare to the average ground level of 2.9m, the ground water was over flooded about OAm at monsoon season. The electrical conductivity(ECe) was measured above $4.0dS{cdot}m^{-1}$ over all areas and however, some areas showed over $20dS{cdot}m^{-1}$. During a monsoon season, ECe was lowered to $1.2{sim}15.0dS{cdot}m^{-1}$, compared with those of the dry season. Therefore, the interception of the capillary connection between planting layer and ground water which contains high salt concentration should be adapted when golf courses are constructed on disused saltpan. The phytotoxicity caused by salt damage may be controled by the interception of capillary fringe of salt flow to the topsoil profile at the upper layer of the ground water table.
 
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Çѱ¹ÀܵðÇÐȸÁö / v.23, no.1, 2009³â, pp.143-150
Çѱ¹ÀܵðÇÐȸ
ISSN : 1229-3253
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200924733173381)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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