Nitrogen Deposition and Responses of Forest Structure to Nitrogen Deposition in a Cool-Temperate Deciduous Forest

Autor: Shinpei Yoshitake, Ruoming Cao, Toshiyuki Ohtsuka, Siyu Chen
Rok vydání: 2019
Předmět:
Zdroj: Forests
Volume 10
Issue 8
Forests, Vol 10, Iss 8, p 631 (2019)
ISSN: 1999-4907
DOI: 10.3390/f10080631
Popis: Few studies have reported the estimation of nitrogen (N) deposition, including dissolved organic N (DON) fluxes, through water flows and the contribution of snowfall in Asia. In this study, the concentrations and fluxes of DON and dissolved inorganic N (DIN) in bulk precipitation (BP), the throughfall (TF) of trees and understory dwarf bamboo, and stemflow (SF) were evaluated in a cool-temperate forest over three years to clarify N fluxes via precipitation and responses of trees and understory canopies to N deposition. The input of N to the study site in BP was 11.1 ±
1.71 kg N ha&minus
1 year&minus
1, with a significant contribution from DON (78%). Snowfall fluxes contributed up to 46% of the total N input, with variations related to the amount of snowfall (2.08&ndash
5.52 kg N ha&minus
1). The forest canopy enriched DON (2.11 ±
0.42 kg N ha&minus
1) but consumed NO3 + NO2&ndash
N (&minus
0.73 ±
0.19 kg N ha&minus
1). In contrast, through the understory bamboo canopy, DON (&minus
1.02 ±
0.55 kg N ha&minus
1) decreased while DIN (0.35 ±
0.44 kg N ha&minus
1) increased. This study indicates that DON and snowfall should not be neglected when evaluating total N deposition into forest ecosystems, especially in remote regions. The canopy processes related to the dissolved N in the presence of understory plants might have significant implications for the internal N cycle in forest ecosystems.
Databáze: OpenAIRE