Acceleration of soil N2O flux and nitrogen transformation during tropical secondary forest succession after slash-and-burn agriculture
Acceleration of soil N2O flux and nitrogen transformation during tropical secondary forest succession after slash-and-burn agriculture
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刀耕火种农业后热带次生林演替过程中土壤 N2O 通量和氮转化的加速
DOI:
10.1016/j.still.2020.104868
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发表时间:
2021-04
影响因子:
6.5
通讯作者:
Minkun Chen
中科院分区:
文献类型:
--
作者:
Shaojun Wang (王邵军);Qianqian Zuo;Qianqian Zuo;Ping Wang;Bo Yang;Shuang Zhao;Run Cao;Minkun Chen
The responses of soil nitrous oxide (N2O) fluxes to tropical forest development are not well documented. We linked the characteristics of N2O fluxes with community composition, N cycling, inorganic nitrogen (N) pools, as well as other soil variables during tropical secondary forest succession after slash-and-burn agriculture in Xishuangbanna, Yunnan, China. During succession, fromMallotus paniculatustoSyzygium oblatumcommunities, N2O emissions increased from 390.8 ug N m−2h−1to 671.6 ug N m−2h−1, where the greatest value occurred during the wet season. The increased soil water content following forest succession explained 71–90 % of the N2O emissions, while decreased soil temperature only contributed 66–70 % to the emissions. Net N mineralization and nitrification increased along the secondary succession of tropical forests, which was positively and nonlinearly correlated with variations in the inorganic nitrogen pool. The variations in N2O fluxes were positively correlated with net N mineralization and nitrification, ammonia and nitrate N, and microbial biomass, but negatively associated with bulk density of soils and C:N ratio of the litter and soil. Our data suggested that a substantial acceleration of soil N2O flux was mainly determined by the increasing availability of inorganic N stimulated by the improved litter quality (low C:N ratio), as well as elevated gravimetric water content, and net N mineralization and nitrification during the spontaneous succession of secondary tropical forests after slash-and-burn agriculture.
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