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. 2018 Dec 3;53(1):20–28. doi: 10.1021/acs.est.8b05079

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Volatilization, mineralization, and NER formation of tetralin (left) and decane (right) in four different soils (see section 2.2). Volatilization, mineralization, and NER were calculated as a percentage of the initial applied radioactivity (%aR). The figure shows that volatilization is higher for low OC content soils (01-A and 02-A) in comparison with the high OC soils (03-G and 04-A). In contrast, fastest mineralization and NER formation was observed in 03-G soil with the highest OC content.