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喀斯特峰丛洼地不同森林类型植物和土壤C、N、P化学计量特征
引用本文:俞月凤,彭晚霞,宋同清,曾馥平,王克林,文丽,范夫静,. 喀斯特峰丛洼地不同森林类型植物和土壤C、N、P化学计量特征[J]. 生态学杂志, 2014, 25(4): 947-954
作者姓名:俞月凤  彭晚霞  宋同清  曾馥平  王克林  文丽  范夫静  
作者单位:(;1.中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室, 长沙 410125; ;中国科学院环江喀斯特生态系统观测研究站, 广西环江 547100; ;中国科学院大学, 北京 100049; ;4.江西农业大学, 南昌 330045)
摘    要:研究西南喀斯特峰丛洼地人工林、次生林、原生林3个不同森林类型的6个代表性植物群落C、N、P化学计量特征及其与土壤的关系.结果表明: 不同森林类型植物和土壤C、N、P含量均存在显著差异.土壤C和N含量均为次生林最高,人工林最低,土壤P含量为人工林最高,原生林最低;植物C和P含量变化趋势为人工林>原生林>次生林,植物N含量为次生林最高,原生林最低.土壤C∶P、N∶P以及植物C∶P均为原生林显著高于次生林和人工林,土壤C∶N在不同森林类型间差异不显著;植物N∶P为次生林最高,人工林最低,植物C∶N为原生林>人工林>次生林.在不同森林类型中,乔木叶片N含量与P含量、C∶N与C∶P以及C∶P与N∶P之间均呈显著线性正相关,除了植物叶片C∶N与N∶P以及土壤C∶N与N∶P之间呈显著线性负相关外,植物和土壤的C、N、P、C∶P均无显著相关性,说明土壤C、N、P供应量对乔木叶片C、N、P含量影响不大.

关 键 词:化学计量  相关分析  森林类型  喀斯特峰丛洼地

Stoichiometric characteristics of plant and soil C,N and P in different forest types in depressions between karst hills,southwest China.
YU Yue-feng,PENG Wan-xia,SONG Tong-qing,ZENG Fu-ping,WANG Ke-lin,WEN Li,FAN Fu-jing,. Stoichiometric characteristics of plant and soil C,N and P in different forest types in depressions between karst hills,southwest China.[J]. Chinese Journal of Ecology, 2014, 25(4): 947-954
Authors:YU Yue-feng  PENG Wan-xia  SONG Tong-qing  ZENG Fu-ping  WANG Ke-lin  WEN Li  FAN Fu-jing  
Affiliation:(;1.Key Laboratory of Agro ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China; ;2.Huanjiang Observation and Research Station of Karst Ecosystem, Chinese Academy of Sciences, Huanjiang 547100, Guangxi, China; ;3.University of Chinese Academy of Sciences, Beijing 100049, China; ;4.Jiangxi Agricultural University, Nanchang 330045, China)
Abstract:The stoichiometric properties of plant carbon (C), nitrogen (N) and phosphorus (P) and their relationships with soil were studied in six dominant plant communities in three forest types, i.e., plantation forest, secondary forest and primary forest in depressions between karst hills, southwest China. The C, N and P contents of both plant and soil had significant differences among the different forest types. Soil C and N contents were the highest in the secondary forest and the lowest in the plantation forest. Soil P content was the highest in the plantation forest and the lowest in the primary forest. Plant C and P contents were in the order of plantation forest > primary forest >secondary forest, and plant N content was the highest in the plantation forest and the lowest in the primary forest. Soil N:P,C:P and plant C:P ratios were significantly higher in the primary forest than in the other two forest types. There were no significant difference for the soil C:N ratio among the three forest types. Plant N:P ratio was the highest in the secondary forest and the lowest in the plantation forest. Plant C:N ratio was in the order of primary forest > plantation forest > secondary forest. There were significantly positive linear correlations between N and P contents, C:N and C:P ratios, C:P and N:P ratios of arbor leaves in the different forest types, and significant negative linear correlations between plant C:N and N:P ratios, and between soil C:N and N:P ratios. There were no significant correlations between plant and soil C, N, P contents and C:P ratio, suggesting that the supply of C, N and P from soil had little influence on plant C, N and P contents.
Keywords:stoichiometry   correlation analysis   forest type   depression between karst hills.
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