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The 2009 Smouldering Peat Fire in Las Tablas de Daimiel National Park (Spain)

机译:Las Tablas de Daimiel国家公园(西班牙)的2009年阴燃泥炭火

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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.
机译:Las Tablas de Daimiel国家公园(TDNP)被联合国教科文组织和拉姆萨尔遗址公认为是生物圈保护区,是伊比利亚地中海湿地半岛与地下水动态相关的最后代表之一。它构成了杰出的动植物保护区。支持该系统的地下水资源的不当农业管理导致湿地从2004年到2009年干drying。结果,2009年8月TDNP内部开始发生闷燃的泥炭大火。支持生态系统的物理结构及其下面的地下水质量。 9月,当公园东边界(距第一个地下座位3.5公里)的地面火灾传播到地下土壤时,情况进一步恶化,在公园外引发了第二次闷烧的泥炭大火。对在不同深度的TDNP多个位置中监测的关键参数(例如土壤湿度,温度和有机质含量)进行分析,结果表明,以前有足够的证据可以预见泥炭自燃以及可能传播任何表面火的风险到地下。公园的面积相对较小,有关泥炭团块的空间分布的知识,以及有关土壤和渗流带结构的详细知识,可以设计并执行紧急计划来阻止火灾。经验使我们能够检查所实施的警戒和警报系统的优缺点,确认用于消防的措施的有效性,并提出短期和长期的行动,以防止将来发生火灾。

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