Hydrophysical Properties of Peat in Undisturbed and Smelter-Impacted Peatlands: Implications for Moss Recovery, Drought and Wildfire

IF 2.9 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-12-25 DOI:10.1002/hyp.70034
Colin P. R. McCarter, Emma Tutt, Paul A. Moore, Alex K. Furukawa, Gregory J. Verkaik, Sophie L. Wilkinson, Pete Whittington, James M. Waddington
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Abstract

Peatlands are critical for global climate regulation storing approximately 500 Gt of carbon and accounting for 33% of global soil organic carbon. Regionally, these ecosystems provide essential wildfire resilience and are important pollutant sinks but degradation puts these key ecosystem services at risk. Smelting operations in Sudbury, ON, Canada, released approximately 12 000 t of particulate copper and nickel into the atmosphere between 1883 and 1969. Toxic metal and sulphur deposition on peatlands from smelting activities caused the widespread decline of keystone peatland moss species (i.e., Sphagnum) and altered peat properties. The changes in peat hydrophysical properties due to historical metal contamination likely reduce peatland resilience to drought and wildfires, thereby increasing the potential for toxic heavy metal remobilisation; however, these peat properties changes have yet to be quantified. We determine 1) how historical smelter pollution impacts peat hydrophysical properties by measuring bulk density, saturated hydraulic conductivity and soil water retention in the upper 40 cm of both undisturbed (located ~160 km outside the deposition region) and smelter-impacted peatlands, 2) use these data to explore the vulnerability of these peatlands to wildfires and drought and 3) assess the potential for natural Sphagnum moss recovery. Smelter-impacted peat had a significantly higher bulk density, lower macroporosity and saturated hydraulic conductivity that drove large differences in modelled soil water tension profiles during simulated drying events. These differences in soil water tension and retention profiles resulted in the smelter-impacted peat having a far greater proportion of the peat profile that would be susceptible to smouldering combustion than the undisturbed peat. Additionally, the smelter-impacted peat properties likely contributed to the limited Sphagnum moss recovery, while concurrently increasing drought and wildfire risk. As such, we argue that contaminated peatland restoration is necessary to enhance Sphagnum moss recovery to mitigate toxic metal remobilisation risk from drought and wildfire.

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未受干扰和受冶炼影响泥炭地泥炭的水物理性质:对苔藓恢复、干旱和野火的影响
泥炭地对全球气候调节至关重要,储存约500亿吨碳,占全球土壤有机碳的33%。从区域来看,这些生态系统提供了必要的野火恢复能力,是重要的污染物汇,但退化使这些关键的生态系统服务处于危险之中。1883年至1969年间,加拿大萨德伯里的冶炼作业向大气中释放了大约12000吨铜和镍微粒。冶炼活动产生的有毒金属和硫在泥炭地的沉积导致泥炭地关键苔藓物种(即泥炭藓)的广泛减少和泥炭性质的改变。由于历史上的金属污染,泥炭水物理性质的变化可能会降低泥炭地对干旱和野火的抵御能力,从而增加有毒重金属再活化的可能性;然而,这些泥炭性质的变化尚未被量化。我们通过测量未受干扰的泥炭地(位于沉积区域外约160公里处)和受冶炼影响的泥炭地的容积密度、饱和水力电导率和土壤保水率,确定1)历史冶炼污染对泥炭水物理特性的影响;2)利用这些数据探索这些泥炭地对野火和干旱的脆弱性;3)评估天然泥炭藓恢复的潜力。冶炼厂冲击泥炭具有显著更高的容重、更低的宏观孔隙率和饱和导电性,这导致了模拟干燥过程中模拟土壤水张力曲线的巨大差异。这些土壤水张力和保持剖面的差异导致受冶炼厂影响的泥炭比未受干扰的泥炭具有更大比例的泥炭剖面容易阴燃。此外,冶炼厂影响的泥炭特性可能导致泥炭藓恢复有限,同时增加了干旱和野火的风险。因此,我们认为受污染的泥炭地恢复是必要的,以加强泥炭藓的恢复,以减轻干旱和野火造成的有毒金属再动员风险。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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