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作 者:宋庆妮[1] 杨清培[1] 刘骏[1] 余定坤[1] 方楷[1] 徐佩[1] 何宇娟[1]
机构地区:[1]江西农业大学/江西省竹子种质资源与利用重点实验室,南昌330045
出 处:《应用生态学报》2013年第2期338-344,共7页Chinese Journal of Applied Ecology
基 金:国家自然科学基金项目(31260120;31170306);江西省自然科学基金项目(20122BAB204019);江西省教育厅科学技术研究项目(GJJ08192);大岗山生态站基金项目资助
摘 要:采用时空替代法和PVC顶盖原位培养法,分析了江西大岗山毛竹扩张形成的竹-阔混交林与邻近常绿阔叶林土壤中的无机氮含量、氮矿化速率和吸收速率等指标.结果表明:两种林分土壤总无机氮含量时空变化趋势相同;竹-阔混交林年均矿化速率低于常绿阔叶林,前者以氨化作用为主,后者氨化作用与硝化作用相当,但生长季硝化作用明显占优势.两林分全年都以吸收NH4+-N为主,但生长季常绿阔叶林对NO3--N的吸收明显占优势.说明毛竹向常绿阔叶林扩张会增强土壤氮素氨化作用、减弱硝化作用和总矿化作用,同时也会增加对NH4+-N的吸收,减少对NO3--N和总无机氮的吸收.By the methods of space-time substitution and PVC tube closed-top in situ incubation,this paper studied the soil mineralized-N content,N mineralization rate,and N uptake rate in Phyllostachys edulis-broadleaf mixed forest(PBMF) formed by P.edulis expansion and its adjacent evergreen broadleaf forest(EBF) in Dagangshan Mountain of Jiangxi Province,China.There existed the same spatiotemporal variation trend of soil total mineralized-N(TMN) content between the two forests.The annual average N mineralization rate was slightly lower in PBMF than in EBF.In PBMF,soil N mineralization was dominated by ammonification;while in EBF,soil ammonification and nitrification were well-matched in rate,and soil nitrification was dominated in growth season(from April to October).The N uptake by the plants in PBMF and EBF in a year was mainly in the form of NH4+-N,but that in EBF in growth season was mainly in the form of NO3--N.These findings indicated that the expansion of P.edulis into EBF could promote the ammonification of soil N,weakened soil nitrification and total N mineralization,and also,increased the NH4+-N uptake but decreased the NO3--N and TMN uptake by the plants.
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