青海高寒沼泽湿地红色沉积物的物质组成及其自燃引火机制
收稿日期: 2025-09-09
修回日期: 2026-01-25
网络出版日期: 2026-08-07
基金资助
省部共建三江源生态与高原农牧业国家重点试验室自主课题“火干扰对高寒草甸冻土和植被的影响”(2024-ZZ-09)
Material composition and spontaneous ignition mechanism of red sediments in Qinghai alpine swamp wetlands
Received date: 2025-09-09
Revised date: 2026-01-25
Online published: 2026-08-07
青海高寒沼泽湿地春季野火频发,其自燃机制尚不明确。采集青海省天峻县木里镇阿子沟野火频发区湿地坑底0~0.2 cm红色沉积物,应用场发射扫描电镜-能谱(FE-SEM-EDS)、同步热分析(STA)和X射线光电子能谱(XPS),分析其微观形貌、元素组成、热稳定性及铁化学态,从铁氧化物化学特性角度,揭示湿地坑底红色沉积物的燃烧属性及其自燃引火的可能性。结果表明:1)研究区沉积物主要由羟基氧化铁(FeOOH)和有机质(OM)组成,呈多孔蜂窝状结构;2)实验室表观燃点约213 ℃,有机质燃烧是主要放热过程;3)铁元素能谱精细结构证实铁以FeOOH形态为主;4)FeOOH本身不可燃,但其凭借高比表面积和表面羟基特性,可作为“光热转化介质”吸附富集有机质。青海高寒沼泽湿地红色沉积物具备在特定条件下(如冰透镜聚焦阳光)将光能转化为热能并引发有机质阴燃的潜力,其引火机制是季节性冻融、微地形、太阳辐射与特殊物质属性耦合的结果,为高寒湿地自然火灾成因的研究提供了科学依据。
全小龙 , 陈梦词 , 乔有明 . 青海高寒沼泽湿地红色沉积物的物质组成及其自燃引火机制[J]. 林草资源研究, 2026 , 0(1) : 58 -66 . DOI: 10.13466/j.cnki.lczyyj.2026.01.006
Spring wildfires frequently occur in the alpine swamp wetlands of the Qinghai-Tibet Plateau,yet their spontaneous ignition mechanism remains unclear.This study reveal the combustion properties of red sediments at the bottom of wetland pits and their potential as a spontaneous ignition source from the perspective of the chemical characteristics of iron oxides.Red sediment samples(at a depth from 0 to 0.2 cm)were collected from the pit bottom in the fire-prone area of Azigou,Muli Town,Tianjun County,Qinghai Province.Their micromorphology,elemental composition,thermal stability,and iron chemical states were analyzed using field emission scanning electron microscopy coupled with energy-dispersive spectroscopy(FE-SEM-EDS),simultaneous thermal analysis(STA),and X-ray photoelectron spectroscopy(XPS).The results showed that:1)The sediments are mainly composed of iron oxyhydroxide(FeOOH),and organic matter(OM),exhibiting a porous honeycomb structure;2)The laboratory apparent ignition point is approximately 213 ℃,the combustion of organic matter is the main exothermic process;3)The fine structure of energy-dispersive X-ray spectroscopy confirms that iron mainly exists in the form of FeOOH;4)FeOOH is non-combustible however,owing to its high specific surface area and surface hydroxyl properties,it can act as a “photothermal conversion medium” to adsorb and enrich organic matter.The red sediments in the Qinghai alpine swamp wetlands have the potential to convert light energy into heat under specific conditions(e.g.,sunlight focused by ice lenses)and trigger the smoldering of organic matter.The ignition mechanism results from the coupling of seasonal freeze-thaws,micro-topography,solar radiation,and the special material attributes.This study provides a new perspective for understanding the causes of natural fires in alpine wetlands from a material basis standpoint.
Key words: natural wildfire; red sediment; FeOOH; photothermal conversion; ignition mechanism
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