Burn effects on soil properties associated to heat transfer under contrasting moisture content

•High soil moisture content attenuates the heat transmission within burned topsoil.•Soil thickness affected by burning is mainly limited to the first cm, either wet or dry.•Fire leads to a C loss of 50% in dry soil and 25% in wet soil for up to the 1st cm.•SWR is tightly linked with fire, soil moist...

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Veröffentlicht in:The Science of the total environment 2017-12, Vol.601-602, p.1119-1128
Hauptverfasser: Badía, David, López-García, Sergio, Martí, Clara, Ortíz-Perpiñá, Oriol, Girona-García, Antonio, Casanova-Gascón, José
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Sprache:eng
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Zusammenfassung:•High soil moisture content attenuates the heat transmission within burned topsoil.•Soil thickness affected by burning is mainly limited to the first cm, either wet or dry.•Fire leads to a C loss of 50% in dry soil and 25% in wet soil for up to the 1st cm.•SWR is tightly linked with fire, soil moisture content and soil depth. [Display omitted] The aim of this work is to investigate the topsoil thickness affected by burning under contrasting soil moisture content (field capacity versus air-dried conditions). A mollic horizon of an Aleppo pine forest was sampled and burned in the laboratory, recording the temperature continuously at the topsoil surface and at soil depths of 1, 2, and 3cm. Changes in soil properties were measured at 0–1, 1–2, 2–3, and 3–4cm. Both the maximum temperature and the charring intensities were significantly lower in wet soils than in air-dried soils up to 3cm in depth. Moreover, soil heating was slower and cooling faster in wet soils as compared to dry soils. Therefore, the heat capacity increase of the soil moistened at field capacity plays a more important role than the thermal conductivity increase on heat transfer on burned soils. Burning did not significantly modify the pH, the carbonate content and the chroma, for either wet or dry soil. Fire caused an immediate and significant decrease in water repellency in the air-dried soil, even at 3cm depth, whereas the wet soil remained hydrophilic throughout its thickness, without being affected by burning. Burning depleted 50% of the soil organic C (OC) content in the air-dried soil and 25% in the wet soil at the upper centimeter, which was blackened. Burning significantly decreased the total N (TN) content only in the dry soil (to one-third of the original value) through the first centimeter of soil depth. Soluble ions, measured by electrical conductivity (EC), increased after burning, although only significantly in the first centimeter of air-dried soils. Below 2cm, burning had no significant effects on the brightness, OC, TN, or EC, for either wet or dry soil.
ISSN:0048-9697
1879-1026
DOI:10.1016/j.scitotenv.2017.05.254