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| DOI | 10.3390/SU132112061 | ||||
| Año | 2021 | ||||
| Tipo | artículo de investigación |
Citas Totales
Autores Afiliación Chile
Instituciones Chile
% Participación
Internacional
Autores
Afiliación Extranjera
Instituciones
Extranjeras
Wildfire induces soil alterations that have a long-term impact on soil organic matter (SOM) quality. We postulated that after different fire severities, the neutral sugars in soils can be used as an indicator of soil organic matter quality after fire. The aim of this study was to determine the contribution of neutral sugar, bulk and occluded particulate organic matter (oPOM) affected by wildfire, at different soil depths in an Araucaria–Nothofagus Forest, four years post-after fire. The concentration and composition of the neutral sugars in the soils clearly comprised the major fraction in the unburned soil. Medium-and high-severity fires caused a drastic reduction in soil sugars in the bulk soil as well as in the oPOM fractions. The13C-CPMAS NMR spectroscopy analysis revealed a high contribution of recalcitrant carbon to the decomposition such as aryl–C and aryl–O derived from charred material, whereas the abundance of O–alkyl C and alkyl C functional groups were decreased. The neutral sugars (Galactose+Mannose/Xilose+Arabinose) revealed a major microbial origin in fire affected areas as the ratio was >2. Therefore. Therefore, we suggest that the neutral sugar content of soil should be used for monitoring both short-and long-term changes in SOM altered by fires.
| Ord. | Autor | Género | Institución - País |
|---|---|---|---|
| 1 | Rivas, Yessica | - |
Universidad Adventista de Chile - Chile
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| 2 | RETAMAL-SALGADO, JORGE ANDRES | Hombre |
Instituto de Investigaciones Agropecuarias - Chile
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| 3 | Knicker, Heike | Mujer |
CSIC - Instituto de Recursos Naturales y Agrobiologia de Sevilla (IRNAS) - España
CSIC - España |
| 4 | MATUS-BAEZA, FRANCISCO JAVIER | Hombre |
Universidad de La Frontera - Chile
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| 5 | RIVERA-SALAZAR, DIEGO ANDRES | Hombre |
Universidad del Desarrollo - Chile
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| Fuente |
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| FONDECYT |
| Fondo Nacional de Desarrollo Científico y Tecnológico |
| Comisión Nacional de Investigación Científica y Tecnológica |
| Water Research Center For Agriculture and Mining, CRHIAM |
| Water Research Center For Agriculture and Mining |
| Agradecimiento |
|---|
| Alternatively, and more likely, this is due to a preferential input of PyOM from decaying charcoal residues into the soil organic matter fraction, leading to an increase of aryl C (Figures 1 and 2) [48]. The aging of charcoal leads to material which has numerous functional groups to interact with the mineral phase [48]. Subsequently, those interactions are likely to stabilize those partially degraded residues within the oPOM fractions. This explanation is supported by the concomitant increase of aryl C alongside the fire severities [48]. A fast oxidation of charcoal during post-fire humification has also been observed by others [55]. Skjemstad et al. [55] extracted aromatic clusters rich in aryl C groups from oxidized charred residues. |
| The first author also thanks CONICYT (National Commission for Scientific and Technological Research) and FONDECYT Postdoctoral Project # 3140161 (National Fund for Scientific and Technological Development). D.R. was funded by the Water Research Center for Agriculture and Mining, CRHIAM (ANID/FONDAP/15130015). |