RESUMEN
Introducing N2 -fixing tree species into Eucalyptus plantations could replace nitrogen (N) fertilization to maintain high levels of N consumption and productivity. However, N enrichment may exacerbate phosphorus (P) limitation as Eucalyptus robusta Smith is extensively planted in P-poor tropical and subtropical soils. We conducted a field experiment in a pure plantation of Eucalyptus urophylla × grandis to investigate the impacts of N fertilization and introduced an N2 -fixing tree of Dalbergia odorifera T. Chen on soil P transformation. Nitrogen fertilization significantly enhanced soil occluded P pool and reduced the other P pools due to acidification-induced pH-sensitive geochemical processes, lowering Eucalyptus leaf P concentration with higher N : P ratio. By contrast, introduced N2 -fixing tree species did not change soil pH, labile inorganic P pool, and Eucalyptus leaf N : P ratio, even enhanced organic P pools and reduced occluded P pool probably due to altering microbial community composition particularly stimulating arbuscular mycorrhiza fungal abundance. Our results revealed differential responses and mechanistic controls of soil P transformation in Eucalyptus plantations with N fertilization and introduced N2 -fixing tree species. The dissolution of occluded P pool along with organic P accumulation observed in the mixed plantations may represent a promising future to better manage soil P availability.
Asunto(s)
Eucalyptus , Árboles , Árboles/fisiología , Suelo/química , Eucalyptus/fisiología , Fósforo , Nitrógeno/análisis , FertilizaciónRESUMEN
BACKGROUND: The mixing of Eucalyptus with N2-fixing trees species (NFTs) is a frequently successful and sustainable cropping practice. In this study, we evaluated nitrogen (N) transfer and conducted a proteomic analysis of the seedlings of Eucalyptus urophylla × E. grandis (Eucalyptus) and an NFT, Dalbergia (D.) odorifera, from intercropping and monocropping systems to elucidate the physiological effects and molecular mechanisms of N transfer in mixed Eucalyptus and D. odorifera systems. RESULTS: N transfer occurred from D. odorifera to Eucalyptus at a rate of 14.61% in the intercropping system, which increased N uptake and growth in Eucalyptus but inhibited growth in D. odorifera. There were 285 and 288 differentially expressed proteins by greater than 1.5-fold in Eucalyptus and D. odorifera roots with intercropping vs monoculture, respectively. Introduction of D. odorifera increased the stress resistance ability of Eucalyptus, while D. odorifera stress resistance was increased by increasing levels of jasmonic acid (JA). Additionally, the differentially expressed proteins of N metabolism, such as glutamine synthetase nodule isozyme (GS), were upregulated to enhance N competition in Eucalyptus. Importantly, more proteins were involved in synthetic pathways than in metabolic pathways in Eucalyptus because of the benefit of N transfer, and the two groups of N compound transporters were found in Eucalyptus; however, more functional proteins were involved in metabolic degradation in D. odorifera; specifically, the molecular mechanism of the transfer of N from D. odorifera to Eucalyptus was explained by proteomics. CONCLUSIONS: Our study suggests that N transfer occurred from D. odorifera to Eucalyptus and was affected by the variations in the differentially expressed proteins. We anticipate that these results can be verified in field experiments for the sustainable development of Eucalyptus plantations.
Asunto(s)
Dalbergia/metabolismo , Eucalyptus/metabolismo , Nitrógeno/metabolismo , Proteínas de Plantas/metabolismo , Raíces de Plantas/metabolismo , Proteoma/metabolismo , Producción de Cultivos/métodos , ProteómicaRESUMEN
It has long been assumed that soil acidification increases reactive iron and/or aluminum (Fe/Al) oxides and promotes Pi sorption onto mineral surfaces, resulting in a decrease in Pi. However, this assumption has seldom been tested in long-term field experiments. Using a 12-year acid addition experiment in a tropical forest, we demonstrated that soil acidification increased the content of noncrystalline Fe and Al oxides by 16.3 % and 27.7 %, respectively; whereas it did not alter the absorbed Pi pool and Pi sorption capacity. Furthermore, soil acidification increased the Fe/Al-bound organic matter content by 82.5 %, causing a 54.9 % reduction in Pi desorption, a 42.3 % decrease in soluble Pi content, and a 9.2 % increase in occluded Pi content. Our findings demonstrate that soil acidification reduces Pi bioavailability by repressing Pi desorption rather than enhancing Pi sorption. These results could be attributed to the enhanced organomineral association, which competes for sorption sites with Pi and promotes the Pi occlusion. However, the interactions between organomineral-Pi have not been incorporated into global land models, which may overestimate ecosystem productivity under future acid rain scenarios.