“…Aside from these methods, a very interesting technique, not usually cited in quantification studies and reviews (Glaser et al, 1998;Schmidt et al, 2001;Masiello, 2004;Simpson and Hatcher, 2004;Brodowski et al, 2005;Hammes et al, 2007;Koide et al, 2011;Wiedemeier et al, 2015), is the C stable isotopic ratio (δ 13 C) (Bird and Ascough, 2012), which is widely used in studies on biochar mineralization and priming (Hamer et al, 2004;Cross and Sohi, 2011;Keith et al, 2011;Luo et al, 2011;Fang et al, 2015;Rittl et al, 2015b), but still uncommon for pyrogenic C quantification. The application of biochar with isotopically distinct δ 13 C values of the native soil organic matter (distinct photosynthetic pathway) would provide a powerful tool, aside from tracing the fate of pyrogenic C in the environment, as reference method to study quantification and stability (e.g.…”