Fig. 3: Partitioning between atmospheric deposition and GCN into TF nitrate fluxes and its ecological relevance. | Nature Geoscience

Fig. 3: Partitioning between atmospheric deposition and GCN into TF nitrate fluxes and its ecological relevance.

From: Substantial contribution of tree canopy nitrifiers to nitrogen fluxes in European forests

Fig. 3: Partitioning between atmospheric deposition and GCN into TF nitrate fluxes and its ecological relevance.

a, Partitioning of the NO3–N TF fluxes into the two main sources (atmosphere and GCN, mean and s.d., n = 19) obtained using fBio from Fig. 2 (more details are provided in the Methods). b, Difference between TF and BD for NO3–N fluxes as measured (without GCN) and after accounting for GCN (with GCN). The grey line in a indicates the mean NO3–N flux in TF across all sites, that is, 5.03 kg N ha−1 yr−1. Each point is the mean calculated over two or three sampling dates (n = 19; see Extended Data Table 4 for data). The orange and green rectangles to the right indicate the range of apparent release (source) and apparent retention (sink) of NO3–N by forest canopies, respectively.

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