Effects of physical, chemical, and biological ageing on the mineralization of pine wood biochar by a Streptomyces isolate.

If biochar is to be used for carbon (C) management, we must understand how weathering or ageing affects biochar C mineralization. Here, we incubated aged and unaged eastern white pine wood biochar produced at 350 and 550°C with a Streptomyces isolate, a putative biochar-decomposing microbe. Ageing w...

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Main Authors: Nayela Zeba, Timothy D Berry, Kevin Panke-Buisse, Thea Whitman
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2022-01-01
Series:PLoS ONE
Online Access:https://doi.org/10.1371/journal.pone.0265663
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author Nayela Zeba
Timothy D Berry
Kevin Panke-Buisse
Thea Whitman
author_facet Nayela Zeba
Timothy D Berry
Kevin Panke-Buisse
Thea Whitman
author_sort Nayela Zeba
collection DOAJ
description If biochar is to be used for carbon (C) management, we must understand how weathering or ageing affects biochar C mineralization. Here, we incubated aged and unaged eastern white pine wood biochar produced at 350 and 550°C with a Streptomyces isolate, a putative biochar-decomposing microbe. Ageing was accelerated via three different processes, namely, (a) physical ageing-subjecting biochar to alternating freeze-thaw and wet-dry cycles, (b) chemical ageing-treating biochar with concentrated hydrogen peroxide and (c) biological ageing-incubating biochar in the presence of nutrients and microorganisms. Elemental composition and surface chemistry (Fourier Transform Infrared spectroscopy) of biochar samples were compared before and after ageing. Biochar C mineralization between ageing treatments was significantly different in the case of 350°C biochar (p value = 0.03). Among the 350°C biochars, physical ageing resulted in the greatest increase (by 103%) in biochar C mineralization (p value = 0.05). However, in the case of 550°C biochar, ageing did not result in a significant change in biochar C mineralization (p value = 0.40). Biochar C mineralization was positively correlated with an increase in O/C ratio post-ageing (rs = 0.86, p value = 0.01). In the case of 350°C biochar, surface oxidation during ageing enhanced biochar degradation by the isolate. For 550°C biochar, however, ageing did not significantly increase biochar C mineralization, likely due to high condensed aromatic C content and lower surface oxidation during ageing. The results from our study suggest that low temperature aged biochar is more susceptible to biological degradation by soil microbes. These findings have implications for the use of biochar for long term C storage in soils.
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spelling doaj.art-e1f0dba82984486d9193f079140f066e2022-12-22T02:37:08ZengPublic Library of Science (PLoS)PLoS ONE1932-62032022-01-01174e026566310.1371/journal.pone.0265663Effects of physical, chemical, and biological ageing on the mineralization of pine wood biochar by a Streptomyces isolate.Nayela ZebaTimothy D BerryKevin Panke-BuisseThea WhitmanIf biochar is to be used for carbon (C) management, we must understand how weathering or ageing affects biochar C mineralization. Here, we incubated aged and unaged eastern white pine wood biochar produced at 350 and 550°C with a Streptomyces isolate, a putative biochar-decomposing microbe. Ageing was accelerated via three different processes, namely, (a) physical ageing-subjecting biochar to alternating freeze-thaw and wet-dry cycles, (b) chemical ageing-treating biochar with concentrated hydrogen peroxide and (c) biological ageing-incubating biochar in the presence of nutrients and microorganisms. Elemental composition and surface chemistry (Fourier Transform Infrared spectroscopy) of biochar samples were compared before and after ageing. Biochar C mineralization between ageing treatments was significantly different in the case of 350°C biochar (p value = 0.03). Among the 350°C biochars, physical ageing resulted in the greatest increase (by 103%) in biochar C mineralization (p value = 0.05). However, in the case of 550°C biochar, ageing did not result in a significant change in biochar C mineralization (p value = 0.40). Biochar C mineralization was positively correlated with an increase in O/C ratio post-ageing (rs = 0.86, p value = 0.01). In the case of 350°C biochar, surface oxidation during ageing enhanced biochar degradation by the isolate. For 550°C biochar, however, ageing did not significantly increase biochar C mineralization, likely due to high condensed aromatic C content and lower surface oxidation during ageing. The results from our study suggest that low temperature aged biochar is more susceptible to biological degradation by soil microbes. These findings have implications for the use of biochar for long term C storage in soils.https://doi.org/10.1371/journal.pone.0265663
spellingShingle Nayela Zeba
Timothy D Berry
Kevin Panke-Buisse
Thea Whitman
Effects of physical, chemical, and biological ageing on the mineralization of pine wood biochar by a Streptomyces isolate.
PLoS ONE
title Effects of physical, chemical, and biological ageing on the mineralization of pine wood biochar by a Streptomyces isolate.
title_full Effects of physical, chemical, and biological ageing on the mineralization of pine wood biochar by a Streptomyces isolate.
title_fullStr Effects of physical, chemical, and biological ageing on the mineralization of pine wood biochar by a Streptomyces isolate.
title_full_unstemmed Effects of physical, chemical, and biological ageing on the mineralization of pine wood biochar by a Streptomyces isolate.
title_short Effects of physical, chemical, and biological ageing on the mineralization of pine wood biochar by a Streptomyces isolate.
title_sort effects of physical chemical and biological ageing on the mineralization of pine wood biochar by a streptomyces isolate
url https://doi.org/10.1371/journal.pone.0265663
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