We compared analogous healthy topsoils and ones burned by fires of different temperatures for their elemental and isotopic Pb content. The fires only affected the top 5 cm of the soil. We found that soils affected by low-temperature fires had increased Pb compared to healthy soils. The accumulation of Pb was not observed in the soils exposed to higher temperatures. The same results were found in ash. Lead isotopic ratios were affected by the fires. These increased in soils affected by higher temperatures but didn’t change with the low temperatures. We proposed that the temperature dependence is due to anthropogenic Pb (206Pb/207Pb < 1.16) volatilizing at lower temperatures than geogenic Pb (206Pb/207Pb > 1.19). This work suggests that it may be possible to determine the temperature of a forest fire from the Pb isotopic signatures of the burned materials.
Baieta R., Vieira A.M.D, Vaňková M., Mihaljevič M. (2022): Effects of forest fires on soil lead elemental contents and isotopic ratios. Geoderma 414, 115760. (DOI)