Characterization of atmospheric bulk phosphorus deposition in China

Atmospheric phosphorus (P) deposition is an important environmental nutrient which has significant implications for terrestrial and aquatic ecosystems due to regulating the ratio of nitrogen (N) and P. Here, P bulk deposition and its spatial and temporal variation characteristics were monitored in China from June 2019 to May 2021, and the concentrations and fluxes of different P species were further investigated. The annual mean concentrations in precipitation were 0.14 +/- 0.02 mg L-1 for total P (TP), 0.06 +/- 0.01 mg L-1 for dissolved inorganic P (DIP), 0.05 +/- 0.007 mg L-1 for dissolved organic P (DOP), and 0.03 +/- 0.003 mg L-1 for particulate P (PP). Annual bulk deposition fluxes of TP, DIP, DOP and PP were 1.08 +/- 0.12, 0.46 +/- 0.07, 0.36 +/- 0.05, and 0.26 +/- 0.03 kg ha(-1) yr(-1) on average, respectively. Atmospheric bulk P concentration showed a negative correlation with precipitation. PP, DIP and DOP contributed 24%, 43% and 33% of TP, respectively. DIP and DOP accounted for 56% and 44% of total dissolved P (TDP). According to analysis of PCA source identification, TP in the bulk deposition most likely originated from anthropogenic sources of combustion in China. The N:P ratios (by mass) in deposition (precipitation) were 32.1 +/- 3.88 higher than the Redfield ratio (16.0), which may lead to P limitation and eutrophication of the water body, and may affect the structure, diversity, and function of ecosystems.

Automated summary

Atmospheric phosphorus (P) deposition in China exhibits significant spatial and temporal variations. Dissolved inorganic P (DIP) and dissolved organic P (DOP) are important components of total P, with anthropogenic sources of combustion in China being the primary contributor to atmospheric P deposition. The N:P ratios in deposition are higher than the Redfield ratio, potentially leading to P limitation, eutrophication, and impacts on the structure, diversity, and function of ecosystems.