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林业科学 ›› 2016, Vol. 52 ›› Issue (10): 10-21.doi: 10.11707/j.1001-7488.20161002

• 论文与研究报告 • 上一篇    下一篇

亚热带4种林分类型枯落物层和土壤层的碳氮磷化学计量特征

喻林华1, 方晰1,2, 项文化1,2, 石俊1, 刘兆丹1, 李雷达1   

  1. 1. 中南林业科技大学生命科学与技术学院 长沙 410004;
    2. 南方林业生态应用技术国家工程实验室 长沙 410004
  • 收稿日期:2015-09-10 修回日期:2016-09-01 出版日期:2016-10-25 发布日期:2016-11-09
  • 通讯作者: 方晰
  • 基金资助:
    国家林业局林业公益性行业科研专项项目(201504411);教育部高等学校博士学科点专项科研基金项目(20124321110006);中南林业科技大学引进高层次人才科研启动基金项目(2014YJ019)。

Stoichiometry of Carbon, Nitrogen, and Phosphorus in Litter and Soil of Four Types of Subtropical Stand

Yu Linhua1, Fang Xi1,2, Xiang Wenhua1,2, Shi Jun1, Liu Zhaodan1, Li Leida1   

  1. 1. Faculty of Life Science and Technology, Central South University of Forestry and Technology Changsha 410004;
    2. National Engineering Laboratory for Applied Technology of Forest & Ecology in South China Changsha 410004
  • Received:2015-09-10 Revised:2016-09-01 Online:2016-10-25 Published:2016-11-09

摘要: [目的] 探讨亚热带森林恢复过程中枯落物层和土壤层的C,N,P含量及其化学计量比的变化规律,为阐明亚热带次生林恢复对土壤养分的影响及森林恢复提供科学依据。[方法] 采用空间代替时间的方法,以湘中丘陵区杉木人工纯林、马尾松+石栎针阔混交林、南酸枣落叶阔叶林和石栎+青冈常绿阔叶林作为1个恢复系列,分别在其1 hm2的长期定位观测样地内,沿着坡面选择6块10 m×10 m小样地,每块小样地随机设置2个1.0 m×1.0 m样方,采集地表未分解层、半分解层、已分解层枯落物和0~10,10~20和20~30 cm土层土壤样品,测定C,N,P含量并计算C,N,P的化学计量比。[结果] 随着森林恢复和阔叶树比例增大,同一分解层枯落物C含量呈下降趋势,而N和P(除已分解层外)含量大体呈增加趋势;C含量随枯落物分解而下降;马尾松+石栎针阔混交林N含量表现为半分解层 > 已分解层 > 未分解层,杉木人工林、南酸枣落叶阔叶林、石栎+青冈常绿阔叶林表现为半分解层 > 未分解层 > 已分解层;南酸枣落叶阔叶林P含量表现为未分解层 > 半分解层 > 已分解层,杉木人工林、马尾松+石栎针阔混交林和石栎+青冈常绿阔叶林均表现为半分解层最高,已分解层最低(除马尾松+石栎针阔混交林外);同一分解层枯落物C:N、C:P和N:P比值随森林恢复而下降;C:N、C:P比值随枯落物分解而下降,N:P比值无明显变化规律;同一土层C,N,P含量随森林恢复而增加;4种林分0~30 cm土壤层C:N和C:P平均比值变化趋势基本一致,石栎+青冈常绿阔叶林最高,其次是马尾松+石栎针阔混交林,杉木人工林最低;4种林分0~30 cm土壤层N:P平均比值无显著差异;未分解层枯落物C含量与0~10和0~30 cm土层C,N,P含量显著负相关,而N,P含量与0~10和0~30 cm土壤层C,N(除N外),P含量显著正相关;未分解层枯落物C:N、C:P和N:P比值与0~10和0~30 cm土壤层C(除N:P比值外),N,P含量显著负相关;枯落物层C:N、C:P和N:P比值与土壤层C:N、C:P和N:P比值相关性不显著。[结论] 随着森林恢复,阔叶树比例增大,枯落物层C:N、C:P和N:P比值逐渐下降,土壤层C,N,P含量增加,未分解层枯落物C,N,P含量及其化学计量比对土壤层C,N,P含量影响显著。在森林恢复和森林经营过程中,如何调整林分树种组成,改变枯落物层的质量显得十分关键。

关键词: 养分含量, 地表枯落物, 分解层, 生态化学计量比, 杉木, 人工林, 次生林

Abstract: [Objective] The objective was to investigate the stoichiometry of carbon (C), nitrogen (N) and phosphorus (P) in litter and soil in four forest types at different succession stages in subtropical region of China, in order to provide a scientific basis for understanding the mechanism of influence of restoration of subtropical secondary forest on soil nutrients and forest restoration. [Method] The study was conducted in a permanent observation plot in size of 1 hm2 at Dashanchong Forest Park in Changsha County, Hunan Province, China. The method of spatial sequence was used instead of time successional sequence, four types of subtropical forests:plantation of Cunninghamia lanceolata, mixed forest of Pinus massoniana+Lithocarpus glaber, deciduous broad leaved forest of Choerospondias axillaris, and evergreen broad-leaved forest of L. glaber+Cyclobalanopsis glauca were chosen to represent successional stages of forest restortation in the region. Based on the status of litter decomposition, the litter of forest ground was divided into layers of un-decomposed, semi-decomposed and decomposed. within the permanent observation plot, 6 small sample plots (10 m×10 m) were established along the slope, and each was set at random with 2 sample squares (1 m×1 m), Within each of the sample squares, soil samples were collected from the three soil layers respectively with 0-10 cm, 10-20 cm, and 20-30 cm depth. Concentrations of C, N and P in litter and soil samples were analyzed and the ratios of C/N, C/P, and N/P were estimated. [Result] At the same litter decomposition layer, concentrations of C was decreased, while N and P contents were increased with successional stages and the increases of proportion of broad-leaved trees in the studied sites, except at the decomposed layer. Contents of C was decreased with litter decomposition progress in the four forest types. Specifically, N content ranked in an order of semi-decomposed layer > decomposed layer > un-decomposed layer in the mixed fores of P. massoniana+L. glaber, and in an order as semi-decomposed layer >un-decomposed layer >decomposed layer in the plantation of C. lanceolata, deciduous broad leaved forest of C. axillaris, and the evergreen broad-leaved forest of L. glaber+C. glauca. The distribution of P content was in an order of un-decomposed layer>semi-decomposed layer>decomposed layer in the deciduous broad-leaved forest of C. axillaries, and semi-decomposed layer>un-decomposed layer>decomposed layers (except the mixed forest of P. massoniana+L. glaber) in the plantation of C. lanceolata, the mixed forest of P. massoniana+L. glaber, evergreen broad-leaved forest of L. glaber+C. glauca. At the similar decomposition conditions, the ratios of C/N, C/P and N/P of litter were decreased along with forest successional progress. The C/N and C/P ratios of litter were decreased, but the N/P ratios were not significantly changed with the litter decomposition progress. The contents of C, N and P were increased with successional stages. The ratios of C/N and C/P were similar in 0-30 cm soil layer in the four subtropical forest types. It was found that the ratios of C/N and C/P were the highest in the evergreen broad-leaved forest of L. glaber+C. glauca, followed by the mixed forest of P. massoniana+L. glaber, and the lowest in the plantation of C. lanceolata. No significant differences of N/P ratios were found among the studied forests. There were significant negative correlations between C concentration at un-decomposed layer and C, N and P contents in 0-10 cm, 0-30 cm soil layers, while significant positive correlations were founded between N and P contents at un-decomposed layer and C, N (except N) and P contents in 0-10 cm, 0-30 cm soil layers. Significant negative correlations were found between the C/N, C/P and N/P ratios and C (except N/P), N and P contents in 0-10 cm, 0-30 cm soil layers. There were no significant correlations of C/N, C/P and N/P ratios between litter and soil in all four forest types. [Conclusion] The ratios of C/N, C/P and N/P were decreased, but C, N and P were increased along with the successional stages and the increase of proportion of broad-leaved trees in forests. The C, N and P contents and the C/N, C/P and N/P ratios in undecomposed layers significantly affected the contents of C, N, P in soil. As a consequence, it is a critical during forest management process to adjust the species composition of the forests in order to change the quality of litter layer.

Key words: nutrient concentration, forest floor litter, decomposed layer, ecological stoichiometric ratio, Cunninghamia lanceolata, plantation, secondary forest

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