Soil pH and Soluble Organic Matter Shifts Exerted by Heating Affect Microbial Response

Gael Bárcenas-Moreno (), Elizabeth Jiménez-Compán, Layla M. San Emeterio, Nicasio T. Jiménez-Morillo and José A. González-Pérez
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Gael Bárcenas-Moreno: MED Soil Research Group, Departmento de Cristalografía, Mineralogía y Química Agrícola, Facultad de Química, Universidad de Sevilla, C/Prof Garcia Gonzalez 1, 41012 Sevilla, Spain
Elizabeth Jiménez-Compán: MED Soil Research Group, Departmento de Cristalografía, Mineralogía y Química Agrícola, Facultad de Química, Universidad de Sevilla, C/Prof Garcia Gonzalez 1, 41012 Sevilla, Spain
Layla M. San Emeterio: MED Soil Research Group, Departmento de Cristalografía, Mineralogía y Química Agrícola, Facultad de Química, Universidad de Sevilla, C/Prof Garcia Gonzalez 1, 41012 Sevilla, Spain
Nicasio T. Jiménez-Morillo: Instituto de Recursos Naturales y Agrobiología de Sevilla, Consejo Superior de Investigaciones Científicas (IRNAS-CSIC), Av. Reina Mercedes 10, 41012 Sevilla, Spain
José A. González-Pérez: Instituto de Recursos Naturales y Agrobiología de Sevilla, Consejo Superior de Investigaciones Científicas (IRNAS-CSIC), Av. Reina Mercedes 10, 41012 Sevilla, Spain

IJERPH, 2022, vol. 19, issue 23, 1-22

Abstract: Fire-induced alterations to soil pH and organic matter play an important role in the post-fire microbial response. However, the magnitude of which each parameter affects this response is still unclear. The main objective of this work was to determine the magnitude in which soil pH and organic matter fire-induced alterations condition the response of viable and cultivable micro-organisms using laboratory heating, mimicking a range of fire intensities. Four heating treatments were applied to unaltered forest soil: unheated, 300, 450, and 500 °C. In order to isolate the effect of nutrient or pH heating-induced changes, different culture media were prepared using soil:water extracts from the different heated soils, nutrient, and pH amendments. Each medium was inoculated with different dilutions of a microbial suspension from the same original, unaltered soil, and microbial abundance was estimated. Concurrently, freeze-dry aliquots from each soil:water extract were analyzed by pyrolysis-gas chromatography/mass spectrometry. The microbial abundance in media prepared with heated soil was lower than that in media prepared with unheated soil. Nutrient addition and pH compensation appear to promote microbial proliferation in unaltered and low-intensity heated treatments, but not in those heated at the highest temperatures. Soil organic matter characterization showed a reduction in the number of organic compounds in soil-heated treatments and a marked increase in aromatic compounds, which could be related to the observed low microbial proliferation.

Keywords: laboratory heating; soil pH; soil organic matter (SOM); pyrolysis–gas chromatography–mass spectrometry (Py-GC/MS); soil micro-organisms; colony forming units (CFU) (search for similar items in EconPapers)
JEL-codes: I I1 I3 Q Q5 (search for similar items in EconPapers)
Date: 2022
References: View complete reference list from CitEc
Citations: View citations in EconPapers (1)

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