Zhu Feifei, Lu Xiankai, Liu Lei, Mo Jiangming
1] Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China [2] Forest and Soil Ecology, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110164, China.
Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China.
Sci Rep. 2015 Jan 21;5:7923. doi: 10.1038/srep07923.
Elevated nitrogen (N) deposition may constrain soil phosphorus (P) and base cation availability in tropical forests, for which limited evidence have yet been available. In this study, we reported responses of soil inorganic nutrients to full factorial N and P treatments in three tropical forests different in initial soil N status (N-saturated old-growth forest and two less-N-rich younger forests). Responses of microbial biomass, annual litterfall production and nutrient input were also monitored. Results showed that N treatments decreased soil inorganic nutrients (except N) in all three forests, but the underlying mechanisms varied depending on forests: through inhibition on litter decomposition in the old-growth forest and through Al(3+) replacement of Ca(2+) in the two younger forests. In contrast, besides great elevation in soil available P, P treatments induced 60%, 50%, 26% increases in sum of exchangeable (K(+)+Ca(2+)+Mg(2+)) in the old-growth and the two younger forests, respectively. These positive effects of P were closely related to P-stimulated microbial biomass and litter nutrient input, implying possible stimulation of nutrient return. Our results suggest that N deposition may result in decreases in soil inorganic nutrients (except N) and that P addition can enhance soil inorganic nutrients to support ecosystem processes in these tropical forests.
氮(N)沉降增加可能会限制热带森林土壤中磷(P)和碱金属阳离子的有效性,而目前关于这方面的证据还很有限。在本研究中,我们报告了在三种初始土壤氮状况不同的热带森林(氮饱和的老龄林和两种氮含量较低的幼龄林)中,土壤无机养分对全因子氮和磷处理的响应。同时还监测了微生物生物量、年凋落物产量和养分输入的响应。结果表明,氮处理降低了所有三种森林的土壤无机养分(除氮外),但其潜在机制因森林而异:在老龄林中是通过抑制凋落物分解,在两种幼龄林中是通过铝(3+)替代钙(2+)。相反,除了土壤有效磷大幅增加外,磷处理分别使老龄林和两种幼龄林中可交换离子(钾(+)+钙(2+)+镁(2+))总量增加了60%、50%、26%。磷的这些积极作用与磷刺激的微生物生物量和凋落物养分输入密切相关,这意味着可能刺激了养分归还。我们的结果表明,氮沉降可能导致土壤无机养分(除氮外)减少,而添加磷可以增强土壤无机养分,以支持这些热带森林中的生态系统过程。