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牛津怀瑟姆森林山毛榉林地的凋落物输入、凋落物分解及二氧化碳释放情况

Litter input, litter decomposition and the evolution of carbon dioxide in a beech woodland-Wytham woods, Oxford.

作者信息

Phillipson J, Putman R J, Steel J, Woodell S R J

机构信息

Animal Ecology Research Group, Oxford University, Oxford.

Botany School, Oxford University, Oxford.

出版信息

Oecologia. 1975 Sep;20(3):203-217. doi: 10.1007/BF00347473.

Abstract

Tree litter fall was measured from May 1969 to April 1973 and varied between 205 and 388 g ma. Peak standing crops of the ground flora were determined between September 1969 and October 1972 and fell in the range 17.3 to 20.9 g m a. Litter losses due to wind action had a net value of 8 g m a and the mean above ground litter input to the soil was 235 g m a.Between February 1971 and January 1973 above ground litter loss due to decomposition was calculated from litter standing crop depletions and litter turnover times. It was estimated to be 235.8 g m a. Steady state conditions were thus assumed for this woodland.The contribution to litter from dying roots was estimated at 92 g m a and hence the total input of dead organic matter to the site was 327 g m a.Soil metabolism, measured as carbon dioxide evolution, showed a significant correlation with temperature and during 1973-1974 had a dry matter equivalent of 342 g m a. The difference between the above ground litter input (235 g m a) and the dry matter equivalent of soil metabolism (342 g m a ) was attributed to the decomposition of root litter, root respiration and the respiratory activity of fungal mycorrhizae. Total organic matter decomposition accounted for 95% of total soil metabolism whilst the contributions by root and mycorrhizal respiration approximated 4 and 1%, respectively.

摘要

1969年5月至1973年4月对树木凋落物进行了测量,其变化范围在205至388克/平方米·年之间。1969年9月至1972年10月测定了地面植物群的峰值现存生物量,范围在17.3至20.9克/平方米·年之间。风蚀造成的凋落物损失净值为8克/平方米·年,土壤中地上凋落物的平均输入量为235克/平方米·年。1971年2月至1973年1月,根据凋落物现存生物量的减少和凋落物周转时间计算了由于分解造成的地上凋落物损失。估计为235.8克/平方米·年。因此,假定这片林地处于稳态条件。估计枯死根系对凋落物的贡献为92克/平方米·年,因此该场地死亡有机物质的总输入量为327克/平方米·年。以二氧化碳释放量衡量的土壤代谢与温度呈显著相关,在1973 - 1974年期间,其干物质当量为342克/平方米·年。地上凋落物输入量(235克/平方米·年)与土壤代谢干物质当量(342克/平方米·年)之间的差异归因于根系凋落物的分解、根系呼吸和真菌菌根的呼吸活动。总有机物质分解占土壤总代谢的95%,而根系和菌根呼吸的贡献分别约为4%和1%。

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