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Çѱ¹¼öÀÚ¿øÇÐȸ / v.44, no.5, 2011³â, pp.351-362
¼³¸¶Ãµ ¹ü·û»ç »ç¸é À¯Ãâ°úÁ¤ÀÇ ÀÌÇØ¸¦ À§ÇÑ ½ÇÃøÅä¾ç¼öºÐ »ó°üµµ ºÐ¼®
( Soil Moisture Measurements and Correlation Analysis to Understand the Runoff Generation Process for a Bumrunsa Hillslope of Sulmachun Watershed )
±è»óÇö;°­¹ÌÁ¤;°û¿ë¼®; ºÎ»ê´ëÇб³ °ø°ú´ëÇРȯ°æ°øÇаú;ºÎ»ê´ëÇб³ ´ëÇпø ȯ°æ°øÇаú;ºÎ»ê´ëÇб³ ´ëÇпø ȯ°æ°øÇаú;
 
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ÀÌ¿¬±¸¿¡¼­´Â»êÁö»ç¸é¿¡¼­ÃøÁ¤µÈÅä¾ç¼öºÐÀÇ»ó°ü°ü°èºÐ¼®À»¼öÇàÇϰí, À̸¦ ÅëÇÏ¿© »ç¸é¿¡¼­ ¹ß»ýµÇ´Â ¼ö¹®°úÁ¤ÀÇ ÀÌÇØ¸¦ µµ¸ðÇÏ¿´´Ù. Åä¾ç¼öºÐÀ» º¯È­½ÃŰ´Â °øÅëµÈ ÁÖ¿ä ¼ö¹®±â»óÀÎÀÚÀÎ °­¿ìÀÇ Ãß°èÇÐÀûÀΠƯ¼ºÀ» Åä¾ç¼öºÐÀÇ ½Ã°è¿­·ÎºÎÅÍ Á¦°ÅÇϰí, »ó°ü¼º ºÐ¼®À» ¼öÇàÇÏ¿´´Ù. °æ±âµµ ÆÄÁÖ ¼³¸¶Ãµ ¹ü·û»ç¿¡ À§Ä¡Çϰí ÀÖ´Â »ç¸é¿¡¼­ 2007³â 8¿ù 1ÀÏ¿¡¼­ 27ÀÏ »çÀÌÀÇ ±â°£°ú µ¿³â 9¿ù 18ÀÏ¿¡¼­ 10¿ù 8Àϰ£ÀÇ ±â°£¿¡ Åä¾ç¼öºÐ ÀڷḦ »ç¿ëÇÏ¿© ºÐ¼®À» ¼öÇàÇÏ¿´°í, ¼öÇàµÈ ºÐ¼®Àº ´ë»ó»ç¸éÀÇ ¿¬Á÷È帧, ¼öÆòÈ帧, ÃæÀüÈ帧, º¹·ù¼ö È帧ÀÇ Å©±â¿Í ºÐÆ÷¿¡ ´ëÇØ¼­ °¢°¢ 8°÷, 14°÷, 7°÷, 7°÷ÀÇ °ü°è¸¦ º¸¿©ÁÖ°í ÀÖ´Ù. µµÃâµÈ Åä¾ç¼öºÐÀÇ »ó°ü°ü°è´Â °ø°£ÀûÀ¸·Î´Â »óºÎ»ç¸é¿¡¼­ ÇϴܺηΠÁøÇàµÇ´Â »ç¸é¿¡¼­ÀÇ ¼ö¹®°úÁ¤ÀÇ º¯È­ ¾ç»óÀ» º¸¿©ÁÖ°í ÀÖ°í, ½Ã°£ÀûÀ¸·Î´Â, À帶öÀÇ °æ¿ì´Â Åä¾ç±¸Á¶Ã¼¿Í ´ë°ø±Ø È帧ÀÌ ¸ðµÎ Áß¿äÇÑ Áö¹èÀÎÀÚÀÌÁö¸¸, °¡À»Ã¶ÀÇ °æ¿ì´Â Åä¾ç±¸Á¶Ã¼ÀÇ È帧ÀÌ ÁÖ¿äÇÑ ¿ªÇÒÀ» ÇÏ´Â °ÍÀ¸·Î ÆÇ´ÜµÈ´Ù.
The soil moisture measurements and correlation analysis are presented to improve understanding the hydrological process at the hillslope scale. The rainfall events is a main driver of soil moisture variation, and its stochastic characteristic need to be properly treated prior to the correlation analysis between soil moisture measurements. Using field measurements for two designated periods during the late summer and autumn seasons in 2007 obtained from the Bumrunsa hillslope located at the Sulmachun watershed, prewhitened correlation analysis were performed for 8, 14, 7 and 7 relationships representing the vertical, lateral, recharge and return flows, for two designated periods, respectively. The analysis indicated both temporal and spatial variation patterns of hydrological processes, which can be explained by the relative contribution of matrix and macropore flows and the impact of transect topography, respectively.
 
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Åä¾ç¼öºÐ;»ç¸é¼ö¹®ÇÐ;»ó°üºÐ¼®;¼±¹é»öÈ­ 󸮱â¹ý;soil moisture;hillslope hydrology;correlation analysis;prewhitening method;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.44, no.5, 2011³â, pp.351-362
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201118834665881)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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