Abstract
Background and aims: Plants take up and use silicon (Si) as a beneficial nutrient for growth or survival, which can affect terrestrial Si biogeochemistry and its links with the carbon cycle. While nitrogen (N) deposition can impact many processes in terrestrial ecosystems (soil biogeochemical processes, plant productivity, etc.), how it affects plant Si cycling in subtropical forests remains unknown.Methods:We performed a field experiment in a subtropical forest to explore the effects of nine − years of canopy and understory N addition at three rates (0, 25 and 50 kg N ha−1 yr−1) on Si biogeochemical cycling. We quantified different soil Si pools, and phytolith concentrations in the vegetation.Results: In topsoil, soil pH decreased in all N − addition treatments. In CN50 and UN50, concentrations of CaCl2 − Si (mobile Si) and NaOH − Si (amorphous Si) increased and decreased, respectively. H2O2 − Si (fragile phytoliths associated with SOM) concentrations increased following N addition. The rates of carboxylate exudation were significantly enhanced, especially under high − rate N addition. Leaf phytolith concentrations significantly increased in all N − addition treatments, except CN25. Concentrations of CaCl2 − Si were negatively correlated with those of NaOH − Si and positively correlated with those of H2O2 − Si in topsoil. Rhizosheath organic acids, soil pH and CaCl2 − Si were dominant factors affecting leaf phytoliths.Conclusions: Nitrogen addition decreased soil pH, increased the soil H2O2 − Si pool, and stimulated carboxylate release of fine roots which, together, enhanced Si availability and plant phytolith accumulation. Our results show that atmospheric N deposition affects Si dynamics in plant-soil systems in subtropical forests.