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Dolerite Fines Used as a Calcium Source for Microbially Induced Calcite Precipitation Reduce the Environmental Carbon Cost in Sandy Soil

Microbial-Induced Calcite Precipitation (MICP) stimulates soil microbiota to induce a cementation of the soil matrix. Urea, calcium and simple carbon nutrients are supplied to produce carbonates via urea hydrolysis and induce the precipitation of the mineral calcite. Calcium chloride (CaCl(2)) is ty...

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Autores principales: Casas, Carla C., Graf, Alexander, Brüggemann, Nicolas, Schaschke, Carl J., Jorat, M. Ehsan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7505998/
https://www.ncbi.nlm.nih.gov/pubmed/33013787
http://dx.doi.org/10.3389/fmicb.2020.557119
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author Casas, Carla C.
Graf, Alexander
Brüggemann, Nicolas
Schaschke, Carl J.
Jorat, M. Ehsan
author_facet Casas, Carla C.
Graf, Alexander
Brüggemann, Nicolas
Schaschke, Carl J.
Jorat, M. Ehsan
author_sort Casas, Carla C.
collection PubMed
description Microbial-Induced Calcite Precipitation (MICP) stimulates soil microbiota to induce a cementation of the soil matrix. Urea, calcium and simple carbon nutrients are supplied to produce carbonates via urea hydrolysis and induce the precipitation of the mineral calcite. Calcium chloride (CaCl(2)) is typically used as a source for calcium, but basic silicate rocks and other materials have been investigated as alternatives. Weathering of calcium-rich silicate rocks (e.g., basalt and dolerite) releases calcium, magnesium and iron; this process is associated with sequestration of atmospheric CO(2) and formation of pedogenic carbonates. We investigated atmospheric carbon fluxes of a MICP treated sandy soil using CaCl(2) and dolerite fines applied on the soil surface as sources for calcium. Soil-atmosphere carbon fluxes were monitored over 2 months and determined with an infrared gas analyser connected to a soil chamber. Soil inorganic carbon content and isotopic composition were determined with isotope-ratio mass spectrometry. In addition, soil-atmosphere CO(2) fluxes during chemical weathering of dolerite fines were investigated in incubation experiments with gas chromatography. Larger CO(2) emissions resulted from the application of dolerite fines (116 g CO(2)-C m(–2)) compared to CaCl(2) (79 g CO(2)-C m(–2)) but larger inorganic carbon precipitation also occurred (172.8 and 76.9 g C m(–2), respectively). Normalising to the emitted carbon to precipitated carbon, the environmental carbon cost was reduced with dolerite fines (0.67) compared to the traditional MICP treatment (1.01). The carbon isotopic signature indicated pedogenic carbonates (δ(13)C(av) = −8.2 ± 5.0‰) formed when dolerite was applied and carbon originating from urea (δ(13)C(av) = −46.4 ± 1.0‰) precipitated when CaCl(2) was used. Dolerite fines had a large but short-lived (<2 d) carbon sequestration potential, and results indicated peak CO(2) emissions during MICP could be balanced optimising the application of dolerite fines.
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spelling pubmed-75059982020-10-02 Dolerite Fines Used as a Calcium Source for Microbially Induced Calcite Precipitation Reduce the Environmental Carbon Cost in Sandy Soil Casas, Carla C. Graf, Alexander Brüggemann, Nicolas Schaschke, Carl J. Jorat, M. Ehsan Front Microbiol Microbiology Microbial-Induced Calcite Precipitation (MICP) stimulates soil microbiota to induce a cementation of the soil matrix. Urea, calcium and simple carbon nutrients are supplied to produce carbonates via urea hydrolysis and induce the precipitation of the mineral calcite. Calcium chloride (CaCl(2)) is typically used as a source for calcium, but basic silicate rocks and other materials have been investigated as alternatives. Weathering of calcium-rich silicate rocks (e.g., basalt and dolerite) releases calcium, magnesium and iron; this process is associated with sequestration of atmospheric CO(2) and formation of pedogenic carbonates. We investigated atmospheric carbon fluxes of a MICP treated sandy soil using CaCl(2) and dolerite fines applied on the soil surface as sources for calcium. Soil-atmosphere carbon fluxes were monitored over 2 months and determined with an infrared gas analyser connected to a soil chamber. Soil inorganic carbon content and isotopic composition were determined with isotope-ratio mass spectrometry. In addition, soil-atmosphere CO(2) fluxes during chemical weathering of dolerite fines were investigated in incubation experiments with gas chromatography. Larger CO(2) emissions resulted from the application of dolerite fines (116 g CO(2)-C m(–2)) compared to CaCl(2) (79 g CO(2)-C m(–2)) but larger inorganic carbon precipitation also occurred (172.8 and 76.9 g C m(–2), respectively). Normalising to the emitted carbon to precipitated carbon, the environmental carbon cost was reduced with dolerite fines (0.67) compared to the traditional MICP treatment (1.01). The carbon isotopic signature indicated pedogenic carbonates (δ(13)C(av) = −8.2 ± 5.0‰) formed when dolerite was applied and carbon originating from urea (δ(13)C(av) = −46.4 ± 1.0‰) precipitated when CaCl(2) was used. Dolerite fines had a large but short-lived (<2 d) carbon sequestration potential, and results indicated peak CO(2) emissions during MICP could be balanced optimising the application of dolerite fines. Frontiers Media S.A. 2020-09-08 /pmc/articles/PMC7505998/ /pubmed/33013787 http://dx.doi.org/10.3389/fmicb.2020.557119 Text en Copyright © 2020 Casas, Graf, Brüggemann, Schaschke and Jorat. http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
spellingShingle Microbiology
Casas, Carla C.
Graf, Alexander
Brüggemann, Nicolas
Schaschke, Carl J.
Jorat, M. Ehsan
Dolerite Fines Used as a Calcium Source for Microbially Induced Calcite Precipitation Reduce the Environmental Carbon Cost in Sandy Soil
title Dolerite Fines Used as a Calcium Source for Microbially Induced Calcite Precipitation Reduce the Environmental Carbon Cost in Sandy Soil
title_full Dolerite Fines Used as a Calcium Source for Microbially Induced Calcite Precipitation Reduce the Environmental Carbon Cost in Sandy Soil
title_fullStr Dolerite Fines Used as a Calcium Source for Microbially Induced Calcite Precipitation Reduce the Environmental Carbon Cost in Sandy Soil
title_full_unstemmed Dolerite Fines Used as a Calcium Source for Microbially Induced Calcite Precipitation Reduce the Environmental Carbon Cost in Sandy Soil
title_short Dolerite Fines Used as a Calcium Source for Microbially Induced Calcite Precipitation Reduce the Environmental Carbon Cost in Sandy Soil
title_sort dolerite fines used as a calcium source for microbially induced calcite precipitation reduce the environmental carbon cost in sandy soil
topic Microbiology
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7505998/
https://www.ncbi.nlm.nih.gov/pubmed/33013787
http://dx.doi.org/10.3389/fmicb.2020.557119
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