Increased nitrogen (N) inputs are widely recognised to reduce soil respiration (Rs), but how
N deposition affects the temporal dynamics of Rs remains unclear. Using a decade‐long …

Increasing anthropogenic nitrogen (N) deposition will affect the global carbon (C) cycle,
although the mechanisms and magnitudes of its effects are not yet fully understood. Soil …

Little is known about the effects of nitrogen (N) additions on soil respiration (Rs) in tropical
and subtropical forests. We therefore conducted an N-fertilization experiment in a …

We investigated how soil respiration (Rs), heterotrophic respiration (Rh) and rhizosphere
respiration (Rr) respond to nitrogen addition in a 21-yr-old larch (Larix principis-rupprechtii) …

The response of soil respiration (Rs) to nitrogen (N) addition is one of the uncertainties in
modelling ecosystem carbon (C). We reported on a long-term nitrogen (N) addition …

Soil respiration is the second largest terrestrial carbon (C) flux; the responses of soil
respiration to nitrogen (N) deposition have far-reaching influences on the global C cycle. N …

Background and aims Increasing global atmospheric nitrogen (N) deposition has a
considerable impact on soil respiration. Due to different carbon dioxide (CO 2) resources of …

Abstract Knowledge of the impact of N enrichment on soil respiration components is critical
for understanding carbon (C) cycling and its feedback processes with climate change. We …

How precipitation mediates the responses of soil respiration (Rs) and its components, ie,
heterotrophic respiration (Rh) and autotrophic respiration (Ra), to N addition remains …

Nitrogen (N) deposition has been steadily increasing for decades, with consequences for
soil respiration. However, we have a limited understanding of how soil respiration responds …