Abstract
Las Tablas de Daimiel National Park (TDNP), recognized as both Biosphere reserve by UNESCO and Ramsar site, is one of the last representatives in the Iberian Peninsula of Mediterranean wetlands linked to groundwater dynamics. It constitutes an outstanding flora and fauna reserve. The inappropriate agricultural management of the groundwater resources that support the system has caused the drying up of the wetland from 2004 to 2009. As a consequence, a smouldering peat fire started inside the TDNP in August 2009. This fire poses an enormous risk for both the physical structure supporting the ecosystem and the quality of groundwater beneath it. The situation got worse in September when a surface fire in the eastern limit of the Park, 3.5 km away from the first underground seat, transmitted to the subsoil giving rise to a second smouldering peat fire outside the Park. The analysis of key parameters monitored in several locations of the TDNP at different depths, such as soil moisture, temperature and organic matter content, shows there was enough previous evidence to foresee the peat self-combustion and the risk that any surface fire could be transmitted to the subsoil. The relatively small size of the Park, the knowledge of the spatial distribution of peat masses, together with the detailed knowledge about soil and vadose zone structure, have allowed to design and execute an emergency plan to hold the fire back. The experience has allowed to check for strong and weak points in the vigilance and alert system implemented, to confirm the effectiveness of the measures applied for the fire control and to propose short and long term actions for preventing fires from starting in the future.
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References
Mitsch WJ and Gosselink JG (1993) Wetlands. Van Nostrand Reinhold, New York, p 722
Phillips JD (1989) Fluvial sediment storage in wetlands. Water Resources Bulletin. 25:867-873
Costanza R, d’Arge R, de Groot R, Farber S, Grasso M, Hannon B, Limburg K, Naeem S, O’Neill RV, Paruelo J, Raskin RG, Sutton P and Van den Belt M (1997) The value of the world’s ecosystem services and natural capital. Nature, 387:253-260
Joosten H, Clark D (2002) Wise use of mires and peatlands. Background and Principles Including a Framework for Decision Making. International Mire Conservation Group and International Peat Society (Ed), Saarijärvi, Finland
Parish F, Sirin A, Charman D, Joosten H, Minaeva T, Silvius M (eds) (2008) Assessment on peatlands, biodiversity and climate change. Global Environment Centre, Kuala Lumpur & Weatlands International, Wageningen
Rein G, Cleaver N, Ashton C, Pironi P, Torero JL (2008) The severity of smouldering peat fires and damage to the forest soil. Catena 74:304–309
Page SE, Siegert F, Rieley JO, Boehm HDV, Jaya A, Limin S (2002) The amount of carbon released from peat and forest fires in Indonesia during 1997. Nature 420:61–65
Stracher GB, Taylor TP (2004) Coal fires burning out of control around the world: thermodynamic recipe for environmental catastrophe. Int J Coal Geol 59:7–17
Rein G, (2009) Smouldering Combustion Phenomena in Science and Technology. International Review of Chemical Engineering, 1: 3-18
Frandsen WH (1987) The influence of moisture and mineral soil on the combustion limits of smoldering forest duff. Can. J. For. Res. 17:1540-1544
Moreno L, Castaño S, Jiménez ME, Aguilera H, De la Losa A (2007) Control del efecto de la inversión del flujo vertical (descarga a recarga) sobre la composición química del agua subterránea en el Parque Nacional de Las Tablas de Daimiel. Resúmenes del I Congreso Nacional sobre Cambio Global, Getafe, p 30
DeBano LF (1981) Water repellent soils: a state-of-the-art. United States Department of Agriculture, Forest Service, General Technical Report PSW-46. Berkeley, California, p 21
Doerr SH, Shakesby RA, Walsh RPD (2000) Soil water repellency: its causes, characteristics and hydro-geomorphological significance. Earth-Science Reviews 51:33–65
Tucker KA, Karnok KJ, Radcliffe DE, Landry GJr, Roncadori RW and Tan KH (1990) Localized dry spots as caused by hydrophobic sands on bentgrass greens. Agronomy Journal, 82:549-555
Ritsema CJ and Dekker LW (1996) Water repellency and its role in forming preferred flow paths in soils. Australian Journal of Soil Research, 34:475-487
Fox DM, Darboux F and Carrega P (2007) Effects of fire-induced water repellency on soil aggregate stability, splash erosion, and saturated hydraulic conductivity for different size fractions. Hydrol. Process. 21:2377–2384
Domínguez-Castro F, Santisteban JI, Mediavilla R, Dean WE, López-Pamo E, Gil-García MJ and Ruiz-Zapata MB (2006) Environmental and geochemical record of human-induced changes in C storage during the last millennium in a temperate wetland (Las Tablas de Daimiel National Park, central Spain). Tellus. 58:573-585
Sánchez-Carrillo S, Angeler DG, Sánchez-Andrés R, Álvarez-Cobelas M and Garatuza Payán J (2004) Evapotranspiration in semi-arid wetlands: relationships between inundation and the macrophyte cover:open-water ratio. Advances in Water Resources. 27:643-655
Aguilera H, Moreno L, Jiménez ME, De la Losa A, Castaño S (2009) Propiedades físicas e hidráulicas de la ZNS en el Parque Nacional de las Tablas de Daimiel. In: Silva O et al (eds) Estudios en la Zona no Saturada del Suelo, vol IX. Barcelona. http://congress.cimne.com/zns09/frontal/papers.asp
Holden J, Burt TP (2002) Piping and pipeflow in a deep peat catchment. Catena 48 163–199
García M (1996) Hidrogeología de las Tablas de Daimiel y de los Ojos del Guadiana. Bases hidrogeológicas para una clasificación funcional de humedales ribereños. Ph Thesis, Universidad Complutense de Madrid. Madrid. http://eprints.ucm.es/3104/
Cirujano S (1996) Bentos vegetal, flora y vegetación superior. In: Alvarez-Cobelas M & Cirujano S (ed) Las Tablas de Daimiel. Ecología acuática y sociedad. Organismo Autónomo Parques Nacionales. Ministerio Español de Medio Ambiente, Madrid, 129-139
Van Reeuwijk LP (ed) (2002) Procedures for soil analysis, 6th edn. Tech. Pap. 9, ISRIC, Wageningen
Bisdom EBA, Dekker LW, Schoute JFT (1993) Water repellency of size fractions from sandy soils and relationships with organic material and soil structure. Geoderma 56:105–118
Aguilera H, Moreno L, Castaño S, Jiménez ME, De la Losa A (2009) Contenido y distribución espacial de nutrientes móviles en la zona no saturada en el Parque Nacional de las Tablas de Daimiel (Nutrient content and its spatial distribution in the unsaturated zone at the Las Tabla de Daimiel National Park). Boletín Geológico y Minero de España 120(3):393–408. http://www.igme.es/internet/default.asp
Garcia MGJ, Zapata MBR, Santisteban JI, Mediavilla R, Lopez-Pamo E, Dabrio CJ (2007) Late holocene environments in Las Tablas de Daimiel (south central Iberian peninsula, Spain). Veg Hist Archaeobot 16(4):241–250
Frandsen WH (1997) Ignition probability of organic soils. Can. J. For. Res. 27(9):1471-1477
Acknowledgements
The presented data have been obtained thanks to the Spanish Ministry of Science and Innovation financing through the CICYT project CGL2005-06458-C02-01. Analytical determinations have been carried out at the Edaphology Department of the Complutense University of Madrid. Special thanks must be given to Las Tablas de Daimiel National Park Direction for all the facilities and support for access and sampling.
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Moreno, L., Jiménez, ME., Aguilera, H. et al. The 2009 Smouldering Peat Fire in Las Tablas de Daimiel National Park (Spain). Fire Technol 47, 519–538 (2011). https://doi.org/10.1007/s10694-010-0172-y
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DOI: https://doi.org/10.1007/s10694-010-0172-y