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Çѱ¹ÀܵðÇÐȸ / v.10, no.1, 1996³â, pp.49-59
Åä¾çÀÇ Ä§½Ä°ú º¸Á¸¿¡ °üÇÑ ÀÌ·ÐÀû ºÐ¼® 4. »ï¸²Åä¾çÀÇ Ä§½Ä°ú À¯½Ç±â±¸
( The Theoretical Analyses of the Soil Erosion and Conservation 4. Erosion and Leaching Mechanism of the Forest Soils )
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This report is researched on the cause and mechanism of soil erosion in comparison among Kwangnung, Mt. Kaya, Mt. Chili, and Mt. Soorak by physical and chemical analyses of their for- est soils. Clay, silt, and fine sand of Mt. Soorak are far less than those of Mt. Chili, Mt. Kaya, and Kwangnung area while coarse sand is very high level. The clay ratio of soil at Mt. Soorak is the most high level in comparison with that of other area. Denudation at Mt. Soorak, therefore, is cause of erosion by the result of transportation of soil particles. The eroding velocity increase for larger particle size and stronger cohesion between soil particles. Very fine sand, silt, and clay can be present in suspension near the bottom and the size of the particles in suspension depends upon the velocity of the current near the bottom and the roughness of the bottom. Key words: Theoretical analyses, Soil erosion and conservation, Forest soils.
 
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Çѱ¹ÀܵðÇÐȸÁö / v.10, no.1, 1996³â, pp.49-59
Çѱ¹ÀܵðÇÐȸ
ISSN : 1229-3253
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199611920302115)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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