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Çѱ¹¼öÀÚ¿øÇÐȸ / v.28, no.5, 1995³â, pp.129-140
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ÁöÇ¥Æ÷ÈÁö¿ª-Áß°£·ùÀ¯Ãâ-Èë¼öºÐÀú·ù·® °ü°è: I. Á¤»ó·ù ºÐ¼®
( Surface Saturation Area-Subsurface Outflow-Soil Moisture Storage Relationships: I. Steady-State Analysis ) |
| À̵µÈÆ;ÀÌÀºÅÂ; °æÈñ´ëÇб³ Åä¸ñ°øÇаú;°æÈñ´ëÇб³ Åä¸ñ°øÇаú;
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| ´Ù°ø¼º ¸ÅÁú¿¡¼ÀÇ ºÒÆ÷È-Æ÷È È帧À» ¹¦»çÇÏ´Â Richards ¹æÁ¤½ÄÀ» ÀÌ¿ëÇÑ ¼öÄ¡½ÇÇèÀ» ÅëÇÏ¿© °æ»ç¸é¿¡¼ ÁöÇ¥Æ÷ÈÁö¿ª-Áß°£·ùÀ¯Ãâ Á¤»ó·ù °ü°è ¹× ÁöÇ¥Æ÷ÈÁö¿ª-Èë¼öºÐÀú·ù·® Á¤»ó·ù °ü°è¸¦ À¯µµÇÏ¿´´Ù. ¼öÄ¡½ÇÇè¿¡¼´Â ÁöÇüÀÎÀÚ ¹× Åä¾ç ¼ö¸®Æ¯¼ºÀÇ º¯È°¡ ÁöÇ¥Æ÷ÈÁö¿ª-Áß°£·ùÀ¯Ãâ °ü°è¿¡ ¹ÌÄ¡´Â ¹Î°¨µµ¸¦ ºÐ¼®Çϰí, ÁöÇ¥Æ÷ÈÁö¿ªÀ» Áß°£·ùÀ¯Ãâ ¶Ç´Â Èë¼öºÐÀú·ù·®ÀÇ ÇÔ¼ö·Î Ç¥½ÃÇÏ´Â ¸è¹ýÄ¢À» °áÁ¤ÇÏ¿´´Ù. |
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| In this study we derived steady-state relationships between surface saturation area and subsurface outflow, and between surface saturation area and soil moisture storage through numerical experiments with Richards equation on a hillslope. Numerical experiments analyzed the sensitivity of topographic and soil hydraulic properties on steady-state relationships between surface saturation area and subsurface outflow. And the power law for the extent of surface saturation area was determined as a function of subsurface outflow or soil moisture storage. |
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.28, no.5, 1995³â, pp.129-140
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199511920096221)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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