FOREST LITTER DECOMPOSITION IN RELATION TO SOIL-NITROGEN DYNAMICS AND LITTER QUALITY
FOREST LITTER DECOMPOSITION IN RELATION TO SOIL-NITROGEN DYNAMICS AND LITTER QUALITY
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DOI:
10.2307/1941327
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发表时间:
1985-01-01
期刊:
影响因子:
4.8
通讯作者:
MELILLO, JM
中科院分区:
文献类型:
--
作者:
MCCLAUGHERTY, CA;PASTOR, J;MELILLO, JM
Decomposition and changes in N and organic-chemical content of 6 types of forest litter were studied for 2 yr in 5 adjacent Wisconsin [USA] forests. The 5 forests were floristically dissimilar, being dominated, respectively, by sugar maple(Acer saccharum), white oak (Quercus alba), bigtooth aspen (Populus grandidentata), white pine (Pinus strobus), and hemlock (Tsuga canadensis). N mineralization rates in the 5 stands ranged 29-125 kg.ha-1.yr-1. Decomposition rates of transplanted sugar maple leaves and red maple (A. rubrum) wood were not correlated with N mineralization rates in all 5 stands, indicating that N mineralization rates do not affect initial decomposition rates. However, mineralization rates were correlated with decomposition rates of the native dominant foliage litter. N first accumulated in all litters, but by the end of the 2-yr incubation period N release had begun in all foliage litters. N concentrations increased approximately linearly with cumulative mass loss but eventually declined in some foliage litters. Neither maximum amount of N accumulated nor amount accumulated per gram of litter mass loss was related to the rate of soil N mineralization. Chemical composition of litter affected decomposition rates and patterns. Soluble substances and litters relatively rich in solubles disappeared rapidly during early stages of decomposition. Eventually, slowly disappearing acid-soluble and acid-insoluble substances dominated the pattern of mass loss in all litters.