Baloh Philipp, Els Nora, David Robert O, Larose Catherine, Whitmore Karin, Sattler Birgit, Grothe Hinrich
Institute for Materials Chemistry, TU Wien, Vienna, Austria.
Lake and Glacier Research Group, Institute of Ecology, University of Innsbruck, Innsbruck, Austria.
Front Microbiol. 2019 Oct 4;10:2278. doi: 10.3389/fmicb.2019.02278. eCollection 2019.
Artificial snow production is a crucial part of modern skiing resorts in Austria and globally, and will develop even more so with changing precipitation patterns and a warming climate trend. Producing artificial snow requires major investments in energy, water, infrastructure and manpower for skiing resorts. In addition to appropriate meteorological conditions, the efficiency of artificial snow production depends on heterogeneous ice-nucleation, which can occur at temperatures as high as -2°C when induced by specific bacterial ice nucleating particles (INPs). We aimed to investigate the presence, source and ice nucleating properties of these particles in the water cycle of an alpine ski resort in Obergurgl, Tyrol, Austria. We sampled artificial snow, river water, water pumped from a storage pond and compared it to samples collected from fresh natural snow and aged piste snow from the area. Particles from each sampled system were characterized in order to determine their transport mechanisms at a ski resort. We applied a physical droplet freezing assay [DRoplet Ice Nuclei Counter Zurich (DRINCZ)] to heated and unheated samples to characterize the biological and non-biological component of IN-activity. Bacterial abundance and community structure of the samples was obtained using quantitative PCR and Illumina Mi-Seq Amplicon Sequencing, and their chemical properties were determined by liquid ion-chromatography, energy dispersive X-ray spectroscopy (EDX) and scanning electron microscopy (SEM). The results show the flow of biological and inorganic material from the river to the slopes, an uptake of new microorganisms through the air and the piping, and possible proliferation or introduction of ice nucleation active biological particles in aged piste snow. Natural snow, as the first stage in this system, had the lowest amount of ice nucleation active particles and the least amount of biological and mineral particles in general, yet shares some microbial characteristics with fresh artificial snow.
人工造雪是奥地利及全球现代滑雪胜地的关键组成部分,随着降水模式的变化和气候变暖趋势,其重要性将进一步提升。滑雪胜地进行人工造雪需要在能源、水、基础设施和人力方面进行大量投资。除了适宜的气象条件外,人工造雪的效率还取决于异质冰核形成,当由特定的细菌冰核粒子(INPs)诱导时,在高达-2°C的温度下也可能发生异质冰核形成。我们旨在调查奥地利蒂罗尔州奥贝古尔格一个高山滑雪胜地水循环中这些粒子的存在、来源和冰核形成特性。我们采集了人工雪、河水、从蓄水池抽取的水样本,并将其与从该地区新鲜天然雪和老化雪道雪采集的样本进行比较。对每个采样系统中的粒子进行表征,以确定它们在滑雪胜地的传输机制。我们对加热和未加热的样本应用了物理液滴冷冻分析[苏黎世液滴冰核计数器(DRINCZ)],以表征冰核活性的生物和非生物成分。使用定量PCR和Illumina Mi-Seq扩增子测序获得样本的细菌丰度和群落结构,并通过液相离子色谱、能量色散X射线光谱(EDX)和扫描电子显微镜(SEM)确定其化学性质。结果显示了生物和无机物质从河流到雪道的流动,通过空气和管道吸收新的微生物,以及老化雪道雪中冰核活性生物粒子可能的增殖或引入。天然雪作为该系统的第一阶段,冰核活性粒子数量最少,生物和矿物粒子总体数量也最少,但与新鲜人工雪具有一些微生物特征。