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Comparative measurements of ambient atmospheric concentrations of ice nucleating particles using multiple immersion freezing methods and a continuous flow diffusion chamber

机译:使用多种浸入冷冻法和连续流动扩散室对冰核颗粒的周围大气浓度进行比较测量

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摘要

A number of new measurement methods for ice nucleating particles (INPs) havebeen introduced in recent years, and it is important to address how thesemethods compare. Laboratory comparisons of instruments sampling major INPtypes are common, but few comparisons have occurred for ambient aerosolmeasurements exploring the utility, consistency and complementarity ofdifferent methods to cover the large dynamic range of INP concentrations thatexists in the atmosphere. In this study, we assess the comparability of fouroffline immersion freezing measurement methods (Colorado State University icespectrometer, IS; North Carolina State University cold stage, CS; NationalInstitute for Polar Research Cryogenic Refrigerator Applied to Freezing Test,CRAFT; University of British Columbia micro-orifice uniform depositimpactor–droplet freezing technique, MOUDI-DFT)and an online method (continuous flow diffusion chamber, CFDC) used in a manner deemed to promote/maximizeimmersion freezing, for the detection of INPs in ambient aerosols at differentlocations and in different sampling scenarios. We also investigated thecomparability of different aerosol collection methods used with offlineimmersion freezing instruments. Excellent agreement between all methods couldbe obtained for several cases of co-sampling with perfect temporal overlap.Even for sampling periods that were not fully equivalent, the deviationsbetween atmospheric INP number concentrations measured with different methodswere mostly less than 1 order of magnitude. In some cases, however, thedeviations were larger and not explicable without sampling and measurementartifacts. Overall, the immersion freezing methods seem to effectivelycapture INPs that activate as single particles in the modestly supercooledtemperature regime ( −20 °C), although more comparisons areneeded in this temperature regime that is difficult to access with onlinemethods. Relative to the CFDC method, three immersion freezing methods thatdisperse particles into a bulk liquid (IS, CS, CRAFT) exhibit a positive biasin measured INP number concentrations below −20 °C, increasingwith decreasing temperature. This bias was present but much less pronouncedfor a method that condenses separate water droplets onto limited numbers ofparticles prior to cooling and freezing (MOUDI-DFT). Potential reasons forthe observed differences are discussed, and further investigations proposedto elucidate the role of all factors involved.
机译:近年来已经引入了许多新的测量冰核颗粒(INP)的方法,解决这些方法之间的比较非常重要。实验室对主要INP类型进行采样的仪器比较是很常见的,但是对于环境气溶胶测量,很少有比较会探索各种方法的效用,一致性和互补性,以覆盖大气中存在的INP浓度的大动态范围。在这项研究中,我们评估了四种离线浸入式冷冻测量方法(科罗拉多州立大学冰光谱仪,IS;北卡罗来纳州立大学冷台,CS;美国极地研究低温冷冻技术研究所用于冷冻测试的技术; CRAFT;不列颠哥伦比亚大学孔口均匀沉积物-液滴冻结技术,MOUDI-DFT)和在线方法(连续流扩散室,CFDC)以促进/最大程度地浸没冻结的方式使用,用于检测不同位置和不同采样场景下环境气溶胶中的INP 。我们还研究了离线浸没冷冻仪器使用不同气溶胶收集方法的可比性。对于几种具有完美时间重叠的共同采样情况,所有方法之间都可以取得极好的一致性。即使在采样时间不完全相等的情况下,使用不同方法测得的大气INP数量浓度之间的偏差也大多小于1个数量级。但是,在某些情况下,如果没有采样和测量伪像,则偏差会更大且无法解释。总体而言,浸入冷冻方法似乎可以有效捕获在中等过冷温度范围(> -20°C)中作为单个颗粒激活的INP,尽管在这种温度范围内需要进行更多的比较,而在线方法很难对此进行比较。相对于CFDC方法,将颗粒分散到散装液体(IS,CS,CRAFT)中的三种浸没冷冻方法在-20°C以下时测得的INP数浓度呈正偏差,随温度降低而增加。存在这种偏差,但是对于在冷却和冷冻之前将单独的水滴凝结成有限数量的颗粒的方法(MOUDI-DFT)而言,这种偏差就不那么明显了。讨论了观察到的差异的潜在原因,并提出了进一步的研究以阐明所有相关因素的作用。

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