Small variations in soil properties control fire-induced water repellency.

  1. Mataix Solera, Jorge
  2. Arcenegui Baldo, Victoria
  3. Martínez Zavala, Lorena M.
  4. Jordán López, Antonio
  5. Morugán Coronado, Alicia
  6. Bárcenas Moreno, G.
  7. Jiménez Pinilla, Patricia
  8. Lozano Guardiola, Elena
  9. Pascual Granged, Arturo
  10. Gil Torres, Juan
Journal:
Spanish Journal of Soil Science: SJSS

ISSN: 2253-6574

Year of publication: 2014

Volume: 4

Issue: 1

Pages: 51-60

Type: Article

DOI: 10.3232/SJSS.2014.V4.N1.03 DIALNET GOOGLE SCHOLAR lock_openDialnet editor

More publications in: Spanish Journal of Soil Science: SJSS

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Abstract

Fire induced soil water repellency (WR) is controlled by many different factors (temperature reached, amount and type of fuel, etc.). Soil properties may determine the occurrence and intensity of this property in burned soils. The objectives of this paper are to make advances in the study of soil properties as key factors controlling the behaviour of fire-induced WR, and to study the impact of pre-fire SOM content and SOM quality in fire-induced soil WR. In this research, experimental laboratory burnings were carried out using soil samples from different sites with different lithologies, soil types and plant species. Soil samples from the same site differ only in quantity and quality of soil organic matter, as they were collected from under different plant species. All soil samples were heated in a muffle furnace at 200, 250, 300 and 350 ºC without the addition of any fuel load. WR was measured using the water drop penetration time test (WDPT). The results showed significant differences between soil types and plant species, indicating that small differences in soil properties may act as key factors controlling the development and persistence of WR reached, with burned soil samples ranging from wettable to extremely water repellent. The main soil property controlling the response was texture, specifically sand content. The quality of organic matter was also observed to have an effect, since soil samples from the same site with similar organic matter contents, but collected from beneath different plant species, showed different WR values after burning.