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蒸發에 의한 土壤 落葉層의 含水率 變化에 關한 硏究(Ⅱ) : with Larix leptolepis litter layer 落葉松 落葉層을 中心으로
李賢揆 尙志大學校 1996 論文集 Vol.17 No.-
This study was carried out to investigate the change of moisture content in forest soil litter layer by evaporation with Larix leptolepis litter layer during of April-August 1995. It devide forest soil litter layer into F layer(partly decomposed organic materials), litter layer, soil layer. The results were as follows. 1. After the precipitation have been 34mm on April, moisture content of F layer changed from 60% into 67%. Moisture content of litter layer changed from 22% into 40-50%, and after 2-3 days it went down mean moisture. Moisture content of soil layer kept 16%. 2. As May is the dry season, moisture content of F layer falls 27% and moisture content of soil layer falls 6%. After the precipitation have been 10mm, moisture content of F layer go up 60% rapidly. Moisture content of litter layer go up 50% and after one days it went down 20%. 3. After the torrential rain(129mm) visited the stand on july, it rains during 10days. Then moistur content of litter, F, soil layers are in saturation, moisture content of F layer is 69%, moisture content of litter layer is 70% and moisture content of soil layer keep 22%. 4. After the torrential rain (100mm) visited the stand on sugust, moisture content of F layer is 66%, moisture content of litter layer is 70% and moisture content of soil layer keep 22%. 5. The highest, the lowest of moisture content by layers shows that heigh is 74%. low is 6% in litter layer and heigh is 69%, low is 25% in F layer and heigh is 23%, low is 12%.
李賢揆 漢陽大學校 基礎科學硏究所 1981 基礎科學論文集 Vol.1 No.-
파티·살람이론에 의한 파톤 분포함수의 에너지 변화에 따른 변화 형태는 색자문지방 아래나 위의 영역에서 같은 방식이라는 것을 밝혔다. 또한 그 변화 형태는 보통의 색자게이지 이론에 의한 분포함수의 변화와도 그 방식이 같다는 것을 밝혔다.