意大利地中海森林集水区的火后侵蚀和沉积物产量

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC ACS Applied Electronic Materials Pub Date : 2024-03-29 DOI:10.1016/j.ijsrc.2024.03.008
Giovanni Mastrolonardo , Giulio Castelli , Giacomo Certini , Melanie Maxwald , Paolo Trucchi , Cristiano Foderi , Alessandro Errico , Elena Marra , Federico Preti
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引用次数: 0

摘要

野火是一种日益令人担忧的现象,它影响着森林和农业生态系统,产生多种连锁效应,其中土壤侵蚀是最具破坏性的效应之一。因此,需要大量基于数据的证据来证明火灾后流域范围内的土壤侵蚀和沉积物产量,尤其是在处理野火特别频繁的地区(如地中海盆地)时。本研究分析了一场大型野火后的第一场降雨对意大利中部皮桑山脉这一地中海地区流域尺度的土壤侵蚀和沉积物产量的影响。这里约有 1000 公顷的橄榄树林、灌木丛、海洋松和栗树林,全部位于陡峭的山坡上,于 2018 年被烧毁。火灾(或焚烧)严重程度由遥感技术绘制,并通过实地调查进行检查。通过对研究流域出口处拦水坝上游沉积的土质进行取样,对泥沙产量进行了评估。最后,在水文工程中心-水文模拟系统(HEC-HMS)环境中开发了一个水文模型,以探索在流域中观察到的侵蚀沉积事件与降雨引起的水文过程之间的关系。火灾后的前两场降雨转移了大量沉积物,这些沉积物大多为非有机物,颜色较浅,可能在火灾前就已经存在于溪流中,而随后的四场降雨则沉积了富含热成有机物的物质。总体而言,这六场大雨造成的土壤侵蚀--其中较大的一场的恢复时间为一年--估计达到 7.85 吨/公顷(流域内为 0.26 毫米),相当于未燃烧条件下流域年平均潜在侵蚀率的 42%。这一数值低于预期,如果与其他地中海案例研究相比,总体上属于中等水平,这可能是因为该流域土壤的性质,即浅层土壤和石质土壤,因此细粒较少,容易受到侵蚀。
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Post-fire erosion and sediment yield in a Mediterranean forest catchment in Italy

Wildfires are an increasingly alarming phenomenon that affects forests and agroecosystems, generating several cascade effects among which soil erosion is one of the most deleterious. A robust body of data-based evidence on post-fire soil erosion and sediment yield at the watershed scale is, thus, required, especially when dealing with areas where wildfires are particularly frequent, such as the Mediterranean basin. This study analyzes the impact of the first rains after a large wildfire in terms of soil erosion and sediment yield at the watershed scale in a Mediterranean area, the Pisan Mountains, central Italy. Here about 1,000 ha of olive groves, maquis, maritime pine, and chestnut forests, all on steep slopes, burned in 2018. Fire (or burn) severity was mapped by remote sensing and checked by a field survey. Sediment yield was assessed by sampling earthy materials deposited upstream of a check dam at the outlet of the studied watershed. Finally, a hydrological model was developed in the hydrologic engineering center–hydrological modelling system (HEC–HMS) environment to explore the relationship between the erosion–deposition events observed in the watershed and the rainfall-induced hydrological processes. The first two post-fire rainy events relocated a high mass of sediment, mostly non-organic and characterized by light color, perhaps already in the stream before fire, while the subsequent four rain showers deposited materials rich in pyrogenic organic matter. Overall, the soil erosion caused by these six major rainfall events–the larger of which had a return time of one year–was estimated to amount to 7.85 t/ha (0.26 mm in the watershed), corresponding to 42% of the watershed average annual potential erosion rate in unburned conditions. This value is lower than expected, and, overall, moderate if compared to other Mediterranean case studies, possibly because of the nature of soils in the watershed, i.e., shallow and stony, thus, poor in fines prone to erosion.

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