1. Interactive priming of soil N transformations from combining biochar and urea inputs: A 15N isotope tracer study.
- Author
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Fiorentino, N., Sánchez-Monedero, M.A., Lehmann, J., Enders, A., Fagnano, M., and Cayuela, M.L.
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BIOCHAR , *NITROGEN in soils , *INORGANIC compounds , *SOIL amendments , *UREA , *ISOTOPES - Abstract
Abstract Biochar has been found to interact with N transformations in soil but the mechanisms remain largely unknown. In this study we investigated the priming effect of combined biochar and urea inputs on soil inorganic N pools through an isotope tracer approach. Biochar was applied in combination with urea in two complementary laboratory experiments: (i) in the first one, three 15N-labeled organic amendments (wheat straw (WS)), its biochars produced at 350 °C (B350) and at 550 °C (B550) were added to soil in combination with unlabeled urea; (ii) in the second experiment the three same, but unlabeled, amendments were added to soil in combination with 15N labeled urea. This system allowed partitioning between three N sources: native soil N, biochar-derived N and urea-derived N. In addition, CO 2 fluxes were measured to follow total C mineralization in soil and N 2 O emissions were monitored. The proportion of N that mineralized from biochar was always below 0.5% of the added N. The co-addition of urea increased the concentration of NH 4 + derived from B350, but not from B550, demonstrating the lower mineralization of N in biochars produced at 550 °C. Whereas the addition of WS led to a rapid immobilization of N, we found that despite their high C:N, none of the biochars, applied at a rate of 1.5%, immobilized inorganic N in soil. On the contrary, significantly higher NH 4 +concentrations derived from native soil organic N (SON) and urea were found throughout the incubation when B550 was added. This effect can be attributed to an apparent priming effect since a net decrease in CO 2 fluxes was recorded when biochar was added to the soil. The addition of glucose (a low molecular weight carbon source) stimulated an increase in CO 2 fluxes in all treatments along with a net N immobilization in soil. However, both biochars significantly reduced C readily available to microbes, as proved by lower soil CO 2 fluxes, and limited the immobilization of NH 4 + induced by glucose addition. Our results suggest that biochar may partially offset the mineralization of easily available organic C, buffering the immobilization of inorganic N in soil when labile organic compounds (e.g. root exudates, fresh manure, etc.) are incorporated. Highlights • Less than 0.3% of the biochar-N mineralized in soil after 42 days. • Urea addition did not favor the mineralization of high temperature biochar-N. • Biochar at 550 °C increased soil native NH 4 +, most likely due to apparent priming. • Biochar increased the NH 4 +/NO 3 − ratio of urea-derived inorganic N. • Biochar offset the N immobilization in soil caused by glucose addition. [ABSTRACT FROM AUTHOR]
- Published
- 2019
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