논문 상세보기
To understand functional changes of forest ecosystems due to climate change, correlation between decomposition rate of leaf litter, an important function of forest ecosystems, and microclimatic factors was analyzed. After 48 months elapsed, percent remaining weight of Quercus mongolica leaf litter was 27.1% in the east aspect and 37.0% in the west aspects. Decay constant of Q. mongolica leaf litter was 0.33 in the east aspect and 0.25 in the west aspect after 48 months elapsed. Initial C/N ratio of Q. mongolica leaf litter was 38.5. After 48 months elapsed, C/N ratio of decomposing Q. mongolica leaf litter decreased to 13.43 in the east aspect and 16.72 in the west aspect. Average air temperature and soil temperature during the investigation period of the research site were 8.2±9.0 and 9.1±9.3 in the east and 8.5±7.4 and 9.3±7.3°C in the west aspect, respectively, with the west aspect showing higher air and soil temperatures. Soil moisture showed no significant difference between east and west aspects (average soil moisture: 19.4±11.0% vs. 20.5±5.7%). However, as a result of analyzing the correlation between decomposition rate and microclimatic factors, it was found that the decomposition rate and soil moisture has a positive correlation (r=0.426) in the east aspect but not in the west aspect. Our study shows that the correlation between decomposition rate and microclimatic factors can be significantly different depending on the direction of the aspect.
서 론
재료 및 방법
1. 조사지 개황
2. 미기상 자료 수집
3. 낙엽주머니 제작 및 설치
4. 낙엽주머니 수거 및 처리
5. 낙엽의 영양염류 분석
6. 통계분석
결과 및 고찰
1. 연구지역의 사면별 미기상 자료 분석
2. 분해율과 분해상수
3. 분해과정에 따른 낙엽의 탄소, 질소 함량 및 C/N비의변화
4. 낙엽분해율과 미기상요인과의 상관관계 분석
적 요
사 사
REFERENCES
