Analyzing fire-induced water repellency and runoff in forest soil from beech forest: A controlled laboratory experiment

P. Šurda, J. Vitková, Anton Zvala, Ľ. Lichner
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Abstract

Forest fires are a common ecological disturbance affecting soil properties and hydrological processes. In this study, we investigated the impact of fire on surface runoff and soil water repellency (SWR) in beech forest through a laboratory experiment. Our main goals were to quantify the severity of SWR caused by low-intensity fires (simulated at 300°C in a muffle furnace) using contact angle measurements with an optical goniometer and to analyze the relationship between heat-induced alterations in SWR and subsequent surface runoff generated by a rainfall simulator in laboratory conditions. The secondary goal of this study was to propose an innovative laboratory approach as an alternative for fire experiments in real forest environments. We collected six monoliths, each with a forest soil surface layer measuring 20 cm x 15 cm x 10 cm, from the Zvolen-Budča site. These monoliths were heated at 300°C for 20 minutes in a muffle furnace to simulate the impact of low-intensity wildfires. Subsequently, the burnt monoliths and the Control were exposed to artificial rain from a rainfall simulator, and surface runoff was measured. The results showed a significant increase in surface runoff from the burnt monoliths compared to the Control, indicating the impact of fire-induced changes in soil structure and SWR. Additionally, contact angle measurements using an optical goniometer showed increased SWR in the burnt disturbed samples. The findings of our study underscore the significance of the interplay between fire-induced alterations in SWR and surface runoff. They offer valuable insights into the post-fire hydrological responses and erosion risks in forest ecosystems. These insights could help develop effective strategies to mitigate the environmental impacts of forest fires.
分析山毛榉林火灾引起的森林土壤憎水性和径流:受控实验室实验
森林火灾是一种常见的生态干扰,会影响土壤性质和水文过程。在本研究中,我们通过实验室实验研究了火灾对山毛榉林地表径流和土壤斥水性(SWR)的影响。我们的主要目标是利用光学测角仪测量接触角,量化低强度火灾(在马弗炉中以 300°C 模拟)造成的 SWR 的严重程度,并分析热引起的 SWR 变化与随后在实验室条件下由降雨模拟器产生的地表径流之间的关系。本研究的第二个目标是提出一种创新的实验室方法,作为在真实森林环境中进行火灾实验的替代方法。我们从兹沃伦-布德查(Zvolen-Budča)采集了六块石碑,每块石碑的森林土壤表层尺寸为 20 厘米 x 15 厘米 x 10 厘米。这些石碑在马弗炉中以 300°C 的温度加热 20 分钟,以模拟低强度野火的影响。随后,将烧毁的石碑和对照组暴露在降雨模拟器的人工降雨中,并测量地表径流。结果表明,与对照组相比,烧毁的单块石碑的地表径流明显增加,这表明火灾引起的土壤结构变化和 SWR 产生了影响。此外,使用光学测角仪进行的接触角测量显示,被烧毁的扰动样本的 SWR 增加了。我们的研究结果凸显了火灾引起的 SWR 变化与地表径流之间相互作用的重要性。它们为了解森林生态系统的火后水文响应和侵蚀风险提供了宝贵的见解。这些见解有助于制定有效的战略,减轻森林火灾对环境的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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