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杉木与木荷混交23 a后土壤碳氮剖面特征

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研究23 a生杉木纯林、木荷纯林和杉木木荷混交林的土壤碳、氮、碳氮比(C/N)之间的剖面分布差异。结果表明:杉木纯林、木荷纯林和杉木木荷混交林地的表层土壤(0~10 cm)碳、氮元素含量最高并逐层递减,且杉木木荷混交林碳、氮元素含量明显高于木荷纯林和杉木纯林(P<0。05);在向下3个土层中3类林分的碳、氮元素含量差异较小(P>0。05),杉木木荷混交林的优势并不明显,低于木荷纯林和杉木纯林。与纯林相比,杉木木荷混交林在表层土壤中对土壤碳、氮含量有显著提高,可能是因为杉木与木荷混交改变了林冠结构,有利于落叶分解。
Profiles of Soil Carbon,Nitrogen of 23 a Mixed Plantation of Schima superba and Chinese Fir
The distribution profiles of soil carbon,nitrogen characteristics of 23 a Chinese fir pure stand(CS), Schima superba pure stand( SS) and the mixed plantation of Schima superba and Chinese fir ( MS) were explored. Results show that:in the upper soil (0~10 cm) ,N content of CS,SS,MS are the highest and CS>SS>MS,and C,N of MS are significantly higher than those of CS and SS(P<0. 05);but in the deep layer soil,there was no significant difference among 3 types of stands (P>0. 05). Compared with pure forest,Chinese fir and Schima superba mixed forest in surface soil on soil carbon, nitrogen content has a significantly improved. This may be mixed forest of Chinese fir and Schima superba has changed the structure of canopy, which is favorable to decomposition of leaves.

Chinese firSchimas uperbamixed standsoil

杨起帆、孙敏、郑莹莹、孟晓蕊、黄猛、黄玉梅、丁国昌

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福建农林大学林学院,福建 福州 350002

福建农林大学艺术与园林学院,福建 福州 350002

国家林业局森林公园工程技术研究中心,福建 福州 350002

杉木 木荷 混交林 土壤

福建省产学研重大专项

2012N5003

2017

北华大学学报(自然科学版)
北华大学

北华大学学报(自然科学版)

CSTPCD
影响因子:0.609
ISSN:1009-4822
年,卷(期):2017.18(3)
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