Climate controls on nitrate dynamics and gross nitrogen cycling response to nitrogen deposition in global forest soils

Faculty Agriculture Year: 2024
Type of Publication: ZU Hosted Pages:
Authors:
Journal: Science of the Total Environment Elsevier Volume:
Keywords : Climate controls , nitrate dynamics , gross nitrogen    
Abstract:
response to N enrichment is critical to re-evaluating soil N limitation or availability and its environmental consequences. Nevertheless, how climatic conditions affect nitrate dynamics and the response of gross N cycling rates to N enrichment in forest soils is still only rudimentarily known. Through collecting and analyzing 4426-single and 769-paired observations from 231 15N labeling studies, we found that nitrifcation capacity [the ratio of gross autotrophic nitrifcation (GAN) to gross N mineralization (GNM)] was signifcantly lower in tropical/subtropical (19%) than intemperate (68%) forest soils, mainly due to the higher GNM and lower GAN in tropical/subtropical regions resulting from low C/N ratio and high precipitation, respectively. However, nitrate retention capacity [the ratio of dissimilatory nitrate reduction to ammonium (DNRA) plus gross nitrate immobilization (INO3) to gross nitrifcation] was signifcantly higher in tropical/subtropical (86%) than in temperate (54%) forest soils, mainly due to the higher precipitation and GNM of tropical/subtropical regions, which stimulated DNRA and INO3. As a result, the ratio of GAN to ammonium immobilization (INH4) was signifcantly higher in temperate than in tropical/subtropical soils. Climatic rather than edaphic factors control heterotrophic nitrifcation rate (GHN) in forest soils. GHN signifcantly increased with increasing temperature in temperate regions and with decreasing precipitation in tropical/subtropical regions. In temperate forest soils, gross N transformation rates were insensitive to N enrichment. In tropical/subtropical forests, however, N enrichment signifcantly stimulated GNM, GAN and GAN to INH4 ratio, but inhibited INH4 and INO3 due to reduced microbial biomass and pH. We propose that temperate forest soils have higher nitrifcation capacity and lower nitrate retention capacity, implying a higher potential risk of N losses. However, tropical/subtropical forest systems shift from a conservative to a leaky N-cycling system in response to N enrichmen
   
     
 
       

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