Fire as a Removal Mechanism of Pyrogenic Carbon in Soils: Effects of Fire Characteristics and Pyrogenic Carbon Properties

Pyrogenic carbon (PyC) produced during vegetation fires represents one of the most degradation resistant organic carbon pools and has important implications for the global carbon cycle. Its long-term fate in the environment and the processes leading to its degradation are the subject of much debate. Its consumption in subsequent fires is usually highlighted in the literature as a possible major abiotic loss mechanism of PyC in soils. However, the only two studies that have empirically tested this hypothesis found only minor losses of existing PyC, suggesting that subsequent fire is not a major cause of PyC loss (Santin et al. 2013 median mass losses <15% in an experimental boreal forest fire and Saiz et al. 2014 average mass losses <8% in a prescribed fire in an open savannah woodland). Here we present new empirical data obtained in i) a high-intensity crown fire; ii) a surface low-intensity fire, and iii) a smouldering wildfire in boreal forests and show that the actual PyC combustion during subsequent fires is very variable and depends on both the characteristics of the fire and on the properties of the PyC. References- Saiz G, Goodrick I, Wurster C, Zimmermann MPN, Bird MI (2014) Charcoal recombustion efficiency in tropical savannas. Geoderma, 219, 40-45. - Santin C, Doerr SH, Preston C, Bryant R (2013) Consumption of residual pyrogenic carbon by wildfire. International Journal of Wildland Fire, 22, 1072-1077.