Calculation of the coefficient of thermal conductivity of snow cover

Aleksandr Galkin, Nikolay Afanasievich Plotnikov
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Abstract

The aim of the work is to obtain generalized simple formulas for calculating the coefficient of thermal conductivity of snow cover when calculating its thermal resistance. To achieve the goal, a comparison was made of the parabolic formula of N.I. Osokin, obtained on the basis of generalization and correlation analysis of existing dependencies for calculating the coefficient of thermal conductivity having fractional coefficients, with its simplified version with integer coefficients. Based on the linearization of the base Simple linear formulas for determining the coefficient of thermal conductivity depending on the density of snow for two characteristic density ranges (200-300) and (300-400) kg/m3 were also obtained. The percentage errors in the calculations of the coefficient of thermal conductivity of snow, which are possible with the simplification of the coefficients and linearization of the basic parabolic dependence of the coefficient of thermal conductivity on the density of the snow cover, are determined. It is established that the errors arising from the linearization of the basic function do not exceed 5%, which is quite acceptable in engineering calculations. The discrepancy between the results of calculations according to the basic and simplified formula (with coefficients rounded to integer values of the first order) does not exceed 1.5% in the entire considered range of changes in snow density. The results of numerical calculations are presented in the form of graphs that allow you to visually assess the impact of simplifying the calculation formula and its linearization on the accuracy of determining the coefficient of thermal conductivity of snow cover.
积雪热导系数的计算
本文的目的是在计算积雪热阻时,得到计算积雪导热系数的广义简单公式。为了实现这一目标,将N.I. Osokin在对现有分数系数导热系数计算依赖项进行概化和关联分析的基础上得到的抛物式公式与整数系数的简化公式进行了比较。在基础线性化的基础上,还得到了两个特征密度范围(200-300)和(300-400)kg/m3下,根据雪密度确定导热系数的简单线性公式。确定了计算积雪热导系数的百分比误差,这些误差可以通过系数的简化和热导系数与积雪密度的基本抛物线关系的线性化来实现。结果表明,基本函数线性化引起的误差不超过5%,在工程计算中是完全可以接受的。在整个考虑的雪密度变化范围内,根据基本公式和简化公式(系数四舍五入为一阶整数值)计算结果的差异不超过1.5%。数值计算的结果以图表的形式呈现,使您可以直观地评估简化计算公式及其线性化对确定积雪导热系数精度的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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