Effects of burn severity on organic nitrogen and carbon chemistry in high-elevation forest soils

Holly K. Roth , Amy M. McKenna , Myrna J. Simpson , Huan Chen , Nivetha Srikanthan , Timothy S. Fegel , Amelia R. Nelson , Charles C. Rhoades , Michael J. Wilkins , Thomas Borch
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Abstract

Fire frequency and severity have increased in recent decades in the western United States, with direct implications for the quantity and composition of soil organic matter (SOM). While the effects of wildfire on soil carbon (C) and inorganic nitrogen (N) have been well studied, little is known about its impacts on soil organic N. Since organic N is the most abundant form of soil N in conifer forests and dominant source of plant N facilitated by symbiotic mycorrhizae and mineralization, better understanding of post-fire organic N chemistry will help address a critical gap in our understanding of fire effects on SOM. Here, we characterized changes to organic N chemistry across fire severity gradients resulting from two wildfires that burned lodgepole pine (Pinus contorta) forest along the Colorado/Wyoming border, USA. One representative gradient was selected for high-resolution analysis based on results from bulk data (total C and N, and pH). Mineral soils were collected from two depths in low, moderate, and high severity burned areas and adjacent, unburned locations one year following the Ryan and Badger Creek fires. Nuclear magnetic resonance spectroscopy and 21 tesla ultrahigh-resolution Fourier transform ion cyclotron resonance mass spectrometry analysis showed that N content and aromaticity of water-extractable SOM (0–5 ​cm depth) increased with burn severity, while minimal changes to 5–10 ​cm depth were observed. Heterocyclic N species are generally higher in toxicity compared to their non-nitrogenated counterparts, which prompted soil toxicity measurements. Complementary Microtox® analysis revealed a positive relationship between increased fire severity and increased soil toxicity to Aliivibrio fischeri (microbial test species). These findings add to our molecular-level understanding of organic C and N responses to wildfire severity, with likely implications for nutrient cycling, forest recovery and water quality following severe wildfire.

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烧伤严重程度对高海拔森林土壤有机氮和碳化学的影响
近几十年来,美国西部的火灾频率和严重程度有所增加,对土壤有机质(SOM)的数量和组成产生了直接影响。虽然野火对土壤碳(C)和无机氮(N)的影响已经得到了很好的研究,但对其对土壤有机氮的影响知之甚少。由于有机氮是针叶树林中最丰富的土壤氮形式,也是共生菌根和矿化促进的植物氮的主要来源,更好地理解火灾后的有机氮化学将有助于解决我们对火灾对SOM影响的理解中的一个关键差距。在这里,我们描述了美国科罗拉多州/怀俄明州边境两场烧毁洛奇波尔松(Pinus contorta)森林的野火导致的不同火灾严重程度梯度的有机氮化学变化。根据大量数据(总碳、氮和pH)的结果,选择了一个具有代表性的梯度进行高分辨率分析。Ryan和Badger Creek火灾发生一年后,从低、中、高严重程度燃烧区域和邻近未燃烧位置的两个深度采集了矿物土。核磁共振波谱和21特斯拉超高分辨率傅立叶变换离子回旋共振质谱分析表明,水萃取SOM(0–5​cm深度)随着烧伤严重程度的增加而增加,而最小变化为5-10​cm深度。与非含氮物种相比,杂环氮物种的毒性通常更高,这促使进行了土壤毒性测量。Microtox®补充分析显示,火灾严重程度的增加与土壤对费氏Aliivibrio fischeri(微生物试验物种)毒性的增加之间存在正相关关系。这些发现增加了我们对有机碳和氮对野火严重程度反应的分子水平理解,可能对严重野火后的营养循环、森林恢复和水质产生影响。
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