2015
DOI: 10.1016/j.soilbio.2014.10.006
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Effect of temperature on biochar priming effects and its stability in soils

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Cited by 177 publications
(103 citation statements)
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References 65 publications
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“…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.…”
Section: Quantification Of Pyrogenic Cmentioning
confidence: 99%
“…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.…”
Section: Quantification Of Pyrogenic Cmentioning
confidence: 99%
“…The anomalous behavior of biochar towards SOC mineralization primarily depends on characteristics of the biochar and soil properties (Cely et al, 2014;Singh and Cowei, 2014). In general, enhanced microbial and enzymatic activities due to the breakdown of labile organic C of biochar and the supply of nutrients from biochar result in increased SOC mineralization (Fang et al, 2015), a phenomenon commonly known as the positive priming effect. On the other hand, SOC mineralization can be suppressed by the sorption of labile organic C onto the surface or into the pore network of biochar (Lehmann et al, 2011), a phenomenon commonly known as the negative priming effect.…”
Section: Introductionmentioning
confidence: 99%
“…The stable properties of biochar also possess some instability. Nguyen [3] indicated that with the increasing of soil temperature, the loss rate of biological carbon increased, more incubation experiment showed that biochar character changes in its physical and chemical properties under different conditions [4]. The chemical and biological oxidation constantly changing the functional groups and chemical properties when biochar applied into soil [5].…”
Section: Introductionmentioning
confidence: 99%