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Çѱ¹ÀܵðÇÐȸ / v.10, no.1, 1996³â, pp.41-47
Åä¾çÀÇ Ä§½Ä°ú º¸Á¸¿¡ °üÇÑ ÀÌ·ÐÀû ºÐ¼® 3. »ç¸é Åä¾çÀÇ Ä§½Ä¿¡ °üÇÑ ÀÌ·Ð
( The Theoretical Analyses of the Soil Erosion and Conservation 3. Analytical Theory of Slope Erosion )
Àå³²±â; ¼­¿ï´ëÇб³ »ý¹°±³À°°ú;
 
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The theory of slope erosion is developed along similar lines to the theory of heat flow in solid added to the correcting factor. if slope erosion in the forest and grassland proceeds according to the hypothesis, it is $delta$y $delta^2$y = k $delta^2$y $delta$$X^2$+f(s b. t) where 5 is internal properties of slope soil and b is biota on slope. When the variables of the equation of slope erosion are x = -¥ë the initial elevation=-f(¥ë), x=¥ë, x==a, the steady value of the initial elevation=y, and dy dx x=0> =O(t>o), respectively, the houndary condition due to the solution of the equation of slope erosion is y= 2 ¡î$pi$kt [¡òa o ¥ëe $(X-¥ë)^2$4kt d¥ë- ¡òao- $(x+¥ë)^2$4kt d¥ë] + ¡ò¡ò¡ò f (s.b. t)dtdbds Key words: Theoretical analyses, Soil erosion and conservation, Slope erosion
 
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Theoretical analyses;Soil erosion and conservation;Slope erosion;
 
Çѱ¹ÀܵðÇÐȸÁö / v.10, no.1, 1996³â, pp.41-47
Çѱ¹ÀܵðÇÐȸ
ISSN : 1229-3253
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199611920302106)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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