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韩国不同林龄赤松人工林的碳氮储量。

Carbon and nitrogen storage in an age-sequence of Pinus densiflora stands in Korea.

机构信息

Division of Environmental Science and Ecological Engineering, Korea University, Seoul 136-713, Korea.

出版信息

Sci China Life Sci. 2010 Jul;53(7):822-30. doi: 10.1007/s11427-010-4018-0. Epub 2010 Aug 10.

DOI:10.1007/s11427-010-4018-0
PMID:20697871
Abstract

The carbon (C) and nitrogen (N) storage capabilities of Pinus densiflora in six different stand ages (10, 27, 30, 32, 44, and 71 years old) were investigated in Korea. Thirty sample trees were destructively harvested and 12 were excavated. Samples from the above and belowground tree components, coarse woody debris (CWD), forest floor, and mineral soil (0-30 cm) were collected. Tree biomass was highest in the 71-year-old stand (202.8 t ha(-1)) and lowest in the 10-year-old stand (18.4 t ha(-1)). C and N storage in the mineral soil was higher in the 71-year-old stand than in the other stands, mainly due to higher soil C and N concentrations. Consequently, the total ecosystem C and N storage (tree+forest floor+CWD+soil) was positively correlated with stand age: increasing from a minimum in the 10 year old stand (18.8 t C ha(-1) and 1.3 t N ha(-1)) to a maximum in the 71-year-old stand (201.4 t C ha(-1) and 8.5 t N ha(-1)). The total ecosystem C storage showed a similar sigmoidal pattern to that of tree C storage as a function of the age-sequence, while N storage in the CWD, forest floor and mineral soil showed no significant temporal trends. Our results provide important insights that will increase our understanding of C and N storage in P. densiflora stands and our ability to predict changes according to stand age in the region.

摘要

本研究在韩国调查了不同林龄(10、27、30、32、44 和 71 年)的赤松(Pinus densiflora)的碳(C)和氮(N)储量。破坏性收获了 30 棵标准树,并挖掘了 12 棵。收集了地上和地下树木组成部分、粗木质残体(CWD)、林分底层和矿质土壤(0-30cm)的样本。71 年生林分的树木生物量最高(202.8 t ha(-1)),而 10 年生林分的树木生物量最低(18.4 t ha(-1))。矿质土壤中的 C 和 N 储量在 71 年生林分中高于其他林分,主要是由于土壤中 C 和 N 浓度较高。因此,总生态系统 C 和 N 储量(树木+林分底层+CWD+土壤)与林龄呈正相关:从 10 年生林分的最小值(18.8 t C ha(-1)和 1.3 t N ha(-1))增加到 71 年生林分的最大值(201.4 t C ha(-1)和 8.5 t N ha(-1))。总生态系统 C 储量随林龄序列呈类似的 S 形模式,而 CWD、林分底层和矿质土壤中的 N 储量没有明显的时间趋势。我们的研究结果提供了重要的见解,将提高我们对赤松林分中 C 和 N 储量的理解,并提高我们根据该地区林龄预测变化的能力。

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