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Soil Functional Responses to Natural Ecosystem Restoration of a Pine Forest Peucedano-Pinetum after a Fire

机译:火灾后杉木森林天然生态系统恢复的土壤功能性反应

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摘要

Progressing climate change increases the frequency of droughts and the risk of the occurrence of forest fires with an increasing range and a dramatic course. The availability of water and its movement within an ecosystem is a fundamental control of biological activity and physical properties, influencing many climatic processes, whereas soil water repellency (SWR) is a key phenomenon affecting water infiltration into the soil system. Focusing on wide-spectrum effects of fire on the soil system, the research was conducted on a pine stand (Peucedano-Pinetum W. Mat. (1962) 1973) in Kampinos National Park located in central Poland, affected by severe and weak fires, as well as control plots. The main aim of the study was to examine the regeneration of the ecosystem 28 months after the occurrence of a fire. The effect of SWR and soil moisture content, total organic carbon, nitrogen and pH, and gain an understanding of the environmental conditions and processes that shaped the evolution of the species structure of soil microorganism communities (fungal vs. bacterial) have been examined. The Water Drop Penetration Time (WDPT) test was used to assess spatial variability of SWR in 28 plots. Soil bacterial and fungal communities were analysed by Illumina’MISeq using 16S rRNA and Internal Transcribed Spacers 1 (ITS1) regions in six selected plots. After a relatively wet summer, elevated hydrophobicity occurred in areas affected by a weak fire as much as 20 cm into the soil depth. The severe fire and subsequent increase in the richness of the succession of non-forest species contributed to the elimination of hydrophobicity. SWR was more closely linked to the structure and diversity of soil microbial communities than soil physicochemical properties that took place in response to the fire. A statistically significant relationship between the relative occurrence of microorganisms (≥ 1.0% in at least one of the samples) and SWR was established for the following fungi and bacteria species: Archaeorhizomyces sp., Leotiomycetes sp., Byssonectria fusispora, Russula vesca, Geminibasidium sp., family Isosphaeraceae and Cyanobacteria (class 4C0d-2, order MLE1-12). Insight into the functional roles of the individual identified microbial taxa that may be responsible for the occurrence of hydrophobicity was also presented.
机译:正在进行的气候变化会增加干旱的频率和森林火灾的发生具有增加范围和戏剧性的过程中的风险。水的生态系统中的可用性和其运动是生物活性和物理性质,影响许多气候过程的基本控制,而土壤斥水性(SWR)是一个关键的现象影响水渗透到土壤中的系统。着眼于火土系统上的宽谱的影响,这项研究是在马尾松位于波兰中部坎皮诺斯国家公园进行(Peucedano-松树园W.垫。(1962)1973),受严重和弱火,以及控制地块。该研究的主要目的是火灾发生后的28个月的考察生态系统的再生。已经检验SWR和土壤水分含量,总的有机碳,氮和pH值,并获得的环境条件和过程形土壤微生物群落的物种结构(真菌对细菌)的演变的理解的效果。水滴渗透时间(WDPT)试验来评估28个样SWR的空间变异。土壤细菌和真菌社区通过使用16S rRNA和内转录间隔区在六个选定图1(ITS1)区Illumina'MISeq进行分析。相对多雨的夏季后,疏水性升高,发生在受弱火多达20厘米的土层地区。发生严重火灾和非森林物种继承的丰富随后增加有助于消除疏水性。 SWR更紧密联系在一起的土壤微生物群落比发生在响应火土壤理化性质的结构和多样性。 。Archaeorhizomyces属,Leotiomycetes属,Byssonectria fusispora,菇vesca,Geminibasidium SP:微生物和SWR,建立了下面的真菌和细菌物种(在样本中的至少一个≥1.0%)的相对发生次数之间的统计学显著关系。,家庭Isosphaeraceae和蓝藻(类4C0d-2,顺序MLE1-12)。洞察个体识别的微生物类群的功能角色可能是负责疏水性的发生,还介绍。

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