Global distribution of oxygenated polycyclic aromatic hydrocarbons in mineral topsoils

Wilcke, Wolfgang ORCIDiD
Bigalke, Moritz
Wei, Chong
Han, Yongming
Musa Bandowe, Benjamin A.

DOI: https://doi.org/10.1002/jeq2.20224
Persistent URL: http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9615
Wilcke, Wolfgang; Bigalke, Moritz; Wei, Chong; Han, Yongming; Musa Bandowe, Benjamin A., 2021: Global distribution of oxygenated polycyclic aromatic hydrocarbons in mineral topsoils. In: Journal of Environmental Quality, 50, 3, 717-729, DOI: https://doi.org/10.1002/jeq2.20224. 
 
Bigalke, Moritz; 2 Institute of Geography Univ. of Bern Hallerstrasse 12, 3012 Bern Switzerland
Wei, Chong; 3 Shanghai Carbon Data Research Center, Key Lab. of Low‐carbon Conversion Science and Engineering, Shanghai Advanced Research Institute Chinese Academy of Sciences Shanghai 201210 China
Han, Yongming; 4 State Key Lab. of Loess and Quaternary Geology, Institute of Earth Environment Chinese Academy of Sciences Xi'an 710061 China
Musa Bandowe, Benjamin A.; 6 Dep. of Multiphase Chemistry Max Planck Institute for Chemistry Hahn‐Meitner‐Weg 1, 55128 Mainz Germany

Abstract

Hazardous oxygenated polycyclic aromatic hydrocarbons (OPAHs) originate from combustion (primary sources) or postemission conversion of polycyclic aromatic hydrocarbons (PAHs) (secondary sources). We evaluated the global distribution of up to 15 OPAHs in 195 mineral topsoils from 33 study sites (covering 52° N–47° S, 71° W–118 °E) to identify indications of primary or secondary sources of OPAHs. The sums of the (frequently measured 7 and 15) OPAH concentrations correlated with those of the Σ16EPA‐PAHs. The relationship of the Σ16EPA‐PAH concentrations with the Σ7OPAH/Σ16EPA‐PAH concentration ratios (a measure of the variable OPAH sources) could be described by a power function with a negative exponent <1, leveling off at a Σ16EPA‐PAH concentration of approximately 400 ng g–1. We suggest that below this value, secondary sources contributed more to the OPAH burden in soil than above this value, where primary sources dominated the OPAH mixture. This was supported by a negative correlation of the Σ16EPA‐PAH concentrations with the contribution of the more readily biologically produced highly polar OPAHs (log octanol‐water partition coefficient <3) to the Σ7OPAH concentrations. We identified mean annual precipitation (Spearman ρ = .33, p < .001, n = 143) and clay concentrations (ρ = .55, p < .001, n = 33) as important drivers of the Σ7OPAH/Σ16EPA‐PAH concentration ratios. Our results indicate that at low PAH contamination levels, secondary sources contribute considerably and to a variable extent to total OPAH concentrations, whereas at Σ16EPA‐PAH contamination levels >400 ng g–1, there was a nearly constant Σ7OPAH/Σ16EPA‐PAH ratio (0.08 ± 0.005 [SE], n = 80) determined by their combustion sources.


Core Ideas:

Some oxygenated PAHs are more hazardous to the environment and human health than PAHs. OPAHs can originate from combustion or postemission conversion from PAHs. At low PAH concentrations, secondary OPAHs dominate the OPAHs mixture. The concentration ratio of combustion‐derived OPAHs to PAHs appears to be almost constant. The OPAH/PAH concentration ratios in topsoils at low PAH concentrations correlate with rainfall and clay content.