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Evaluation of Composite Burn Index and Land Surface Temperature for Assessing Soil Burn Severity in Mediterranean Fire-Prone Pine Ecosystems

机译:评估地中海火棘松生态系统土壤燃烧强度的复合燃烧指数和地表温度评估

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摘要

We analysed the relationship between burn severity indicators, from remote sensing and field observations, and soil properties after a wildfire in a fire-prone Mediterranean ecosystem. Our study area was a large wildfire in a Pinus pinaster forest. Burn severity from remote sensing was identified by studying immediate post-fire Land Surface Temperature (LST). We also evaluated burn severity in the field applying the Composite Burn Index (CBI) in a total of 84 plots (30 m diameter). In each plot we evaluated litter consumption, ash colour and char depth as visual indicators. We collected soil samples and pH, soil organic carbon, dry aggregate size distribution (MWD), aggregate stability and water repellency were analysed. A controlled heating of soil was also carried out in the laboratory, with soil from the control plots, to compare with the changes produced in soils affected by different severity levels in the field. Our results shown that changes in soil properties affected by wildfire were only observed in soil aggregation in the high severity situation. The laboratory-controlled heating showed that temperatures of about 300 °C result in a significant reduction in soil organic carbon and MWD. Furthermore, soil organic carbon showed a significant decrease when LST values increased. Char depth was the best visual indicator to show changes in soil properties (mainly physical properties) in large fires that occur in Mediterranean pine forests. We conclude that CBI and post-fire LST can be considered good indicators of soil burn severity since both indicate the impact of fire on soil properties.
机译:我们分析了在火灾多发的地中海生态系统中发生野火后,来自遥感和现场观察的烧伤严重性指标与土壤性质之间的关系。我们的研究区域是Pinus pinaster森林中的一场大火。通过研究火灾后的立即着陆表面温度(LST),可以确定遥感造成的烧伤严重程度。我们还在总共84个地块(直径30 m)中应用复合燃烧指数(CBI)在现场评估了燃烧严重程度。在每个样地中,我们评估了垫料消耗,灰分颜色和炭黑深度作为视觉指标。我们收集了土壤样品并分析了pH,土壤有机碳,干骨料粒度分布(MWD),骨料稳定性和憎水性。在实验室中,还对土壤进行了控制加热,对照地块中的土壤与田间受到不同严重程度影响的土壤中产生的变化进行了比较。我们的结果表明,仅在高严重度情况下,仅在土壤聚集中观察到受野火影响的土壤性质的变化。实验室控制的加热表明,约300°C的温度导致土壤有机碳和MWD的显着降低。此外,当LST值增加时,土壤有机碳显着减少。炭深是显示地中海松林大火中土壤性质(主要是物理性质)变化的最佳视觉指示。我们得出的结论是,CBI和火灾后的LST可被视为土壤燃烧严重程度的良好指标,因为两者都表明火灾对土壤特性的影响。

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