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Methods for Measuring Snow Moisture and Density

机译:测量雪中水分和密度的方法

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The manual measurement of snow density through sample collection and liquid water content by calorimetry can be cumbersome and time consuming, while electronic methods are considerably faster. Field and laboratory experiments were conducted to compare several techniques for measuring snow density and moisture content. Two methods for the measurement of snow moisture were used in both field and laboratory settings: the Denoth meter capacitance plate and the Toikka Oy 'Snow Fork' microwave resonance technique. Snow density was measured using three techniques: a direct sample measurement (rectangular snow scoop); snow fork; and, in the lab setting, the Bruker Sky-Scan 1173 Micro CT-X-ray scanner using image analysis techniques. Results show that the snow fork densities are generally reliable in dry snow but become inaccurate (low) in wet snow. Density from direct sampling was on average 0.037 g/cc greater than the snow fork density. Densities measured by the Micro-CT were inaccurate once the snow began to melt, primarily due to sample collection and processing technique. For moisture measurements, we found the Snow Fork to be a reliable tool for measuring the moisture content and density of snow. The Denoth moisture values are on average 0.054% by volume higher than the snow fork moisture. All Denoths tested, report similar moisture values, which was encouraging as these devices are over 20 years old and there is no other source for calibration.
机译:通过样品收集手动测量雪密度和通过量热法测量液态水含量既麻烦又费时,而电子方法要快得多。进行了野外和实验室实验,以比较几种测量雪密度和水分含量的技术。在野外和实验室环境中都使用了两种测量雪中水分的方法:Denoth计电容板和Toikka Oy“雪叉”微波共振技术。使用三种技术测量雪密度:直接采样测量(矩形雪铲);以及雪叉;在实验室环境中,使用图像分析技术的Bruker Sky-Scan 1173 Micro CT-X射线扫描仪。结果表明,雪叉密度在干雪中通常是​​可靠的,但在湿雪中会变得不准确(低)。直接采样的密度平均比雪叉密度大0.037 g / cc。一旦积雪开始融化,Micro-CT测量的密度是不准确的,这主要是由于样品收集和处理技术的缘故。对于水分测量,我们发现Snow Fork是测量水分和雪密度的可靠工具。 Denoth的水分含量平均比雪叉的水分含量高0.054%。所有经过测试的Denoths都报告了相似的水分值,这令人鼓舞,因为这些设备已有20多年的历史,并且没有其他校准来源。

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