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Çѱ¹ÀܵðÇÐȸ / v.4, no.1, 1990³â, pp.42-48
°­¿øµµÁö¿ªÀÇ Åä¾çµ¿°á½É ¹× »ó·Ï½Ä¹°ÀÇ ÇÔ¼ö·® ÃßÀÌ¿¡ °üÇÑ¿¬±¸ (1)
( Studies on the soil freezing depth and change of moisture contents in evergreen plants upon subzero temperature in )
È«Á¾¿î;Çã¹ü¾ç;¿ø°æ¿­;ÀÓº´Ãá;À̱âö;ÇÏ»ó°Ç; Ãáõ±³À°´ëÇÐ;°­¿øµµ ³óÃÌÁøÈï¿ø;Ãáõ±³À°´ëÇÐ;Ãáõ±³À°´ëÇÐ;Ãáõ±³À°´ëÇÐ;°­¿øµµ ³óÃÌÁøÈï¿ø;
 
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Experiments were conducted to investigate the soil freezing depth and pattern with freezing measuring instruments during 1988-l989 winter season in Kangwon province. Freezing measuring instrument was made with acrylic pipes which were consisted of inner and outer parts. Inner pipe was filled with 0.01 % methylene blue solution and rubber hose to protect pipe breakdown by solution freezing. Freezing measurements were carried out by observing discoloration of methylene blue solution. Moisture content of evergreen trees and ground cover plants was also examined in the winter season. The observed results are as follows: 1.In the land of I OOM above sea level, soil freezing depth became deeper as the sum of Accumulated degree-days of temperature below 0¢ªC(0¢ªC . day) increased: Soil freezing depth was 30-40cm at l00¢ªC, 42-43cm at 150¢ªC, and 47cm at 200¢ªC day 2.Soil freezing with vinyl mulching was less developed by l3cm at l00¢ªC with sum of subzero temperature, by l7cm at 200¢ªC than that of the bare ground. Soil of rich hulls mulching with 4Ocm was not frozen until soil freezing at the bare ground was developed to 25cm depth. 3.Cashmeron mulching was more effective than felt mulching in the heat insulation of soil. 4.Thawing of soil was done from the lowest part of the frozen in the ground to upward in the beginning and after that it was done from the surface of frozen soil to downward. Finally thawing was completed at the middle of frozen soil.
 
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Çѱ¹ÀܵðÇÐȸÁö / v.4, no.1, 1990³â, pp.42-48
Çѱ¹ÀܵðÇÐȸ
ISSN : 1229-3253
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199011920301232)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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