Post-fire recovery of temperate and mediterranean ecosystems: An interplay between fire severity, soil nutrients, and vegetation from early-stage to decadal-scale dynamics

IF 5.7 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Jhenkhar Mallikarjun , Anna Gorbushina , Yakov Kuzyakov , Moritz Koester , Rodrigo Castro , Anna Yudina , Khaled Abdallah , Francisco J. Matus , Michaela A. Dippold
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Abstract

Wildfires strongly alter soil properties, which in turn affect ecosystem recovery over extended periods, though long-term impacts are less certain. This study investigated a 14-year post-fire chronosequence in Chile’s mediterranean and temperate humid forests, revealing ecosystem-specific soil properties and nutrient recovery mechanisms. By analysing sites at successional stages, the chronosequence approach assessed temporal changes and ecosystem recovery, revealing long-term wildfire effects on soil dynamics and nutrients recovery.
Wildfires raised soil bulk density to 0.9 g cm−3 in humid temperate and 1.2 g cm−3 in mediterranean ecosystems. Mediterranean soils experienced greater compaction from organic matter loss, soil aggregate destruction, ash-clogged pores, and topsoil erosion. Soil texture shifts were ecosystem-dependent: mediterranean soils increased 10–12 % in clay and silt through ash redistribution and aggregation, while temperate soils saw sand content rise by 0.74 % and 0.32 % yearly at 0–5 and 5–10 cm depths from thermal disaggregation and erosion. Ground vegetation recovers quickly, but physical soil properties like bulk density require over 14 years to return to pre-fire conditions.
In humid temperate forests, ash input initially increased soil pH (4.8 to 5.8), reducing acidity, mitigating aluminium toxicity, while increasing nutrient availability. Base cation stocks increased in mediterranean woodlands (e.g., Ca: up to 0.41 Mg ha−1 y−1) due to ash retention, lower leaching, and ash infiltration into subsoil. Nutrient stocks in humid forests recovered slowly (Ca: 0.087–0.13 Mg ha−1 y−1) due to rainfall-driven leaching and low subsoil reserves. Carbon and N losses were restricted to the litter horizon in temperate forests, recovering via fire-resistant tree inputs, whereas mediterranean soils suffered severe C and N depletion from vegetation loss, erosion, and low N fixation.
Fire effects and recovery are ecosystem-specific, shaped by landscape, geology, hydrology, and vegetation resilience. Understanding how fire regimes affect soil and nutrient recovery is vital for improving projections in fire-prone regions.
温带和地中海生态系统火灾后的恢复:从早期到十年尺度的火灾严重程度、土壤养分和植被之间的相互作用
野火强烈地改变了土壤性质,这反过来又影响了长期的生态系统恢复,尽管长期影响不太确定。本研究调查了智利地中海和温带湿润森林火灾后14年的时间序列,揭示了生态系统特有的土壤特性和养分恢复机制。通过对不同演替阶段的样地进行时序分析,揭示了野火对土壤动态和养分恢复的长期影响。野火使湿润温带和地中海生态系统的土壤容重分别提高到0.9 g cm - 3和1.2 g cm - 3。地中海土壤由于有机质流失、土壤团聚体破坏、灰尘堵塞的孔隙和表土侵蚀而经历了更大的压实。土壤质地变化依赖于生态系统:地中海土壤通过灰分再分配和团聚增加了10 - 12%的粘土和粉砂,而温带土壤在0-5和5-10 cm深度由于热分解和侵蚀,砂含量每年增加0.74%和0.32%。地面植被恢复得很快,但土壤的物理性质,如体积密度,需要超过14年才能恢复到火灾前的状态。在湿润温带森林中,灰输入最初增加了土壤pH值(4.8至5.8),降低了酸度,减轻了铝毒性,同时增加了养分有效性。地中海林地的碱性阳离子储量增加(例如,Ca:高达0.41 Mg ha - 1 y - 1),原因是灰分滞留、较低的淋滤和灰分渗入底土。湿润森林的养分储量恢复缓慢(Ca: 0.087 ~ 0.13 Mg ha−1 y−1),主要原因是降雨驱动淋滤和底土储量低。温带森林的碳和氮损失仅限于凋落物层,通过抗火树木的输入恢复,而地中海土壤则因植被损失、侵蚀和低氮固定而遭受严重的碳和氮消耗。火灾的影响和恢复是生态系统特有的,受景观、地质、水文和植被恢复能力的影响。了解火灾制度如何影响土壤和养分恢复对于改善火灾易发地区的预测至关重要。
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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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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