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引用本文:孙筱璐, 唐佐芯, 尤业明, 曹元帅, 赵海雷.气候和林分类型对土壤团聚体有机碳的影响[J].广西植物,2018,38(3):341-351.[点击复制]
SUN Xiaolu, TANG Zuoxin, YOU Yeming, CAO Yuanshuai, ZHAO Hailei.Effects of climate and forest types on soil aggregation organic carbon[J].Guihaia,2018,38(3):341-351.[点击复制]
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气候和林分类型对土壤团聚体有机碳的影响
孙筱璐1, 唐佐芯1, 尤业明1, 2*, 曹元帅1, 赵海雷1
1. 北京林业大学 森林培育与保护教育部重点实验室, 北京 100083;2. 广西大学 林学院, 南宁 530004
摘要:
该研究选择我国分布于亚热带、暖温带和寒温带的三个样点8种林分(包括阔叶林、混交林和针叶林)下表层0~20 cm的土壤为研究对象,利用干筛法进行大团聚体和微团聚体分级,测定了各团聚体组分的有机碳量和有机碳百分比,并分析他们与气候、植被和土壤环境变量之间的关系。结果表明:土壤大团聚体和微团聚体有机碳量都受到气候的显著影响,表现为土壤大团聚体和微团聚体有机碳量随年均温的增高而降低,经分析这与低温抑制土壤微生物分解活动有关。土壤团聚体有机碳百分比受到林分类型的影响显著,表现为阔叶林土壤团聚体有机碳百分比高于针叶林,这与林分凋落物的质量有关。此外,土壤pH值和土壤质地也影响土壤团聚体有机碳百分比。这表明气温上升和人为干扰导致的林分类型改变都可能引起土壤团聚体有机碳的下降,加剧气候变化。该研究结果有助于了解土壤团聚体有机碳的变异规律,为预测全球变化下土壤有机碳响应提供数据支持。
关键词:  大团聚体, 微团聚体, 土壤有机碳, 气候, 林分类型
DOI:10.11931/guihaia.gxzw201703013
分类号:Q948
文章编号:1000-3142(2018)03-0341-11
基金项目:国家重点基础研究发展计划项目(2011CB403205)[Supported by the National Basic Research Program of China(2011CB403205)]。
Effects of climate and forest types on soil aggregation organic carbon
SUN Xiaolu1, TANG Zuoxin1, YOU Yeming1,2*, CAO Yuanshuai1, ZHAO Hailei1
1. Ministry of Education Key Laboratory for Silviculture and Conservation, Beijing Forestry University, Beijing 100083, China;2. College of Forestry, Guangxi University, Nanning 530004, China
Abstract:
Study on effects of climate and forest types on soil organic carbon(SOC)in aggregation would attribute much to a better understanding of the variation pattern of soil aggregation organic carbon(OC), and provide researchers with data support for better predicting SOC response to global climate change. We sampled 0-20 cm surface soil layers from eight forests(including broad-leaved, mingled and coniferous forests)in three climate zones, subtropical, warm temperate and cool temperate zone. We also classified macro-aggregation and micro-aggregation with dry sieve method, measured their OC contents and percentages, and analyzed the relationship between aggregation OC and environmental variables. The results showed that both macro-aggregation and micro-aggregation OC contents were significantly affected by climate, and the OC contents of both macro-aggregation and micro-aggregation decreased with the increasing mean annual temperature(MAT). We suggested that this results were caused by the inhibited microbial decomposition activity by the low temperature in the higher latitude area. Aggregation OC percentage was significantly affected by forest types: higher in broad-leaved forests and lower in coniferous forests, resulting from different litter qualities and quantities between various forest types. In addition, soil pH and texture could also affect soil aggregation OC. The aforementioned results indicated that temperature rise and forest structure variation by human disturbance might cause soil aggregation OC content decrease, and lead exacerbate global climate change.
Key words:  macro-aggregation, micro-aggregation, soil organic carbon, climate, forest types
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