野火燃烧严重程度和野火后时间对森林土壤机械和水力特性的影响

IF 3.1 2区 农林科学 Q2 SOIL SCIENCE
Ryan A. Ramirez , Woojae Jang , Tae-Hyuk Kwon
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引用次数: 0

摘要

植被有助于提高斜坡的整体稳定性,是公认的环保型自然解决方案。野火会烧毁和毁坏植被,从而增加浅层滑坡和泥石流的风险。然而,人们很少注意评估野火燃烧的严重程度和野火燃烧后的时间对烧毁斜坡的水文地质力学特性的影响。本研究进行了一系列标准实验室测试,以评估从中度低烧(ML)、中度高烧(MH)和未烧(UB)试验小区采集的森林土壤的剪切强度和饱和导流系数(ksat)。在韩国蔚珍郡 2022 年 3 月野火发生后的 1 个月、4 个月和 6 个月对这些地块进行了取样。结果表明,根系的持续退化在很大程度上取决于燃烧的严重程度。ML和MH烧毁土壤的根生物量一直低于UB土壤。根系退化在时间上降低了土壤的抗剪强度。野火后六个月,烧毁土壤的内聚力截距是未烧毁土壤的 1.80-2.30 倍,摩擦角未受影响。野火后 1 个月和 4 个月,烧毁土壤的 ksat 比未烧土壤低 1.22-3.15 倍。ksat降低的原因是细灰堵塞了土壤表层下的孔隙和疏水层。然而,野火后六个月,由于根系贫化形成的大孔隙水流通道,烧毁土壤的 ksat 比野火前增加了约两倍。随着时间的推移,砂分的增加、细粒含量的减少以及疏水性的减弱也凸显了它们在 ML 和 MH 烧毁土壤性质的时间变化中所起的作用。本文记录的结果可用于受野火影响斜坡的降雨渗透和稳定性分析、滑坡易发性绘图以及缓解措施设计。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Wildfire burn severity and post-wildfire time impact mechanical and hydraulic properties of forest soils

Vegetation contributes to the overall slope stability and is recognized as an environmentally friendly nature-based solution. Wildfires burn and denude vegetated slopes, thus increasing the risk of shallow landslides and debris flows. However, little attention has been given to assessing the effects of burn severity and the time elapsed since a wildfire on the hydro-geomechanical properties of burned slopes. This study performed a series of standard laboratory tests to evaluate the shear strength and saturated hydraulic conductivity (ksat) of forest soils collected from moderate-low (ML) burned, moderate-high (MH) burned, and unburned (UB) test plots. The plots were sampled one, four, and six months after the March 2022 wildfire in Uljin County, South Korea. The results show that the continuous deterioration of roots highly depended on the burn severity. The root biomass of ML- and MH-burned soils was consistently lower than those of the UB soils. The root deterioration reduced the shear strength of the soils temporally. The burned soil's cohesion intercept was 1.80–2.30 times lower than that of the UB soil six months post-wildfire, with the friction angle unaffected. One- and four-months post-wildfire, ksat of the burned soils was 1.22–3.15 times lower than the UB soil. Such lowered ksat was due to the fine ash-clogged pores and hydrophobic layers beneath the soil surface. However, six months post-wildfire, the burned soils' ksat increased by approximately twice that of the pre-wildfire condition because of macropore flow passages formed by impoverished roots. The appreciation of sand fraction, depreciation of fines content, and weakening of hydrophobicity over time have also emphasized their role in the temporal shifts in the properties of the ML- and MH-burned soils. The documented results herein can be incorporated into rainfall infiltration and stability analyses of wildfire-affected slopes, landslide susceptibility mapping, and mitigation measures design.

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来源期刊
Geoderma Regional
Geoderma Regional Agricultural and Biological Sciences-Soil Science
CiteScore
6.10
自引率
7.30%
发文量
122
审稿时长
76 days
期刊介绍: Global issues require studies and solutions on national and regional levels. Geoderma Regional focuses on studies that increase understanding and advance our scientific knowledge of soils in all regions of the world. The journal embraces every aspect of soil science and welcomes reviews of regional progress.
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