摘要
以杉木林采伐迹地为对象,比较上坡、中坡和下坡的土壤碳分配以及0—20cm、20~40cm和40~60cm土层的土壤碳垂直分布,研究了不同坡位和土层对固碳功能的影响。结果表明,采伐迹地各土层的有机碳含量均为下坡〉中坡〉上坡,各坡位的土壤有机碳含量均随土层深度的增加而减少。土壤有机碳密度为下坡〉中坡〉上坡,随土层加深而减少,0—20cm土层有机碳密度分别为20~40cm和40~60cm土层的1.37倍和1.78倍。
Taken cutover land of a Cunninghamia Lanceolata stand as the research object, soil organic carbon in upper, middle and lower slope positions, 0-20 cm, 20-40 cm and 40-60 cm soil layers was studied. The resuits showed that soil organic carbon content in all soil layers was in the order of lower slope 〉 middle slope 〉 upper slope, and it decreased with increasing soil depth at each slope. The order of the soil organic carbon density was lower slope 〉 middle slope〉 upper slope, and it decreased with increasing soil depth at each slope. The soil organic carbon density of 0-20 cm soil layer was 1.37 times and 1.78 times of 20-40 cm and 40-60 cm soil layers, respectively.
出处
《安徽农业大学学报》
CAS
CSCD
北大核心
2014年第1期126-129,共4页
Journal of Anhui Agricultural University
基金
广东省林业局资助项目"财政支持公益林森林生态效益补偿机制问题研究"资助
关键词
土层
坡位
土壤有机碳
杉木林
采伐迹地
soil layer
slope position
soil organic carbon
Cunninghamia lanceolata stand
cutover land