Soil potential labile but not occluded phosphorus forms increase with forest succession
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- 作者：Hongzhi Zhang ; Leilei Shi ; Dazhi Wen ; Kailiang Yu
- 关键词：Soil P fractions ; Soil organic P ; Soil microbial properties ; Forest succession ; Tropical forest
- 刊名：Biology and Fertility of Soils
- 出版年：2016
- 出版时间：January 2016
- 年：2016
- 卷：52
- 期：1
- 页码：41-51
- 全文大小：736 KB
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Leilei Shi (1) (2)
Dazhi Wen (1)
Kailiang Yu (3)
1. Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, 723 Xingke Road, Tianhe District, Guangzhou, 510650, China
2. University of Chinese Academy of Sciences, Beijing, 100049, China
3. Department of Environmental Sciences, University of Virginia, Charlottesville, VA, 22904, USA - 刊物类别：Earth and Environmental Science
- 刊物主题：Life Sciences
Agriculture
Soil Science and Conservation - 出版者：Springer Berlin / Heidelberg
- ISSN：1432-0789
文摘
Quantifying soil P fractions is essential for understanding soil P cycling because these fractions are potential sources of bioavailable P. Here, we investigated whether soil P fractions (i.e., labile inorganic P [Pi], intermediately available Pi, organic P, occluded P, and apatite P) differed among three tropical forests at different stages of succession (early, middle, and late) in the Dinghushan Biosphere Reserve (DBR), Southern China. We also determined which soil P fractions was closely related to soil microbial and chemical properties in these forests. Soil microbial biomass and chemical properties (except pH, exchangeable Ca, and Mn) were higher in the late successional forest than those in the other two forests. We found that soil organic and occluded P were the dominant fraction in all three forests and together accounted for 78.9, 84.2, and 78.6 % of total P in the early, middle, and late successional forests, respectively. Soil P fractions and acid phosphomonoesterase activity differed significantly among forest successional stages; intermediately available Pi and organic P (potential sources of labile Pi) were highest in the late successional forest, occluded P was highest in the middle successional forest, and acid phosphomonoesterase activity significantly increased in middle and late successional forest. Soil labile Pi fraction and its potential sources (i.e., intermediately available Pi and soil organic P) were both positively correlated with soil microbial and chemical properties, suggesting that these properties may play critical roles in maintaining high levels of available or potentially available P fractions during this forest succession. Overall, our study indicates that succession in tropical forest ecosystems may not always lead to lower soil P availability.