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METHOD OF REMOTE DETERMINATION OF SPATIAL DISTRIBUTION OF THERMAL PHYSICAL PARAMETERS OF EARTH SURFACE

机译:远程确定地球表面热物理参数空间分布的方法

摘要

FIELD: measuring equipment.;SUBSTANCE: measurement of radiation temperature of earth surface under study (2) by means of equipment mounted on an unmanned flying vehicle (1) of helicopter type. The heat and temperature conductivity of the earth surface is calculated (2). The spatial distribution of the obtained parameters is constructed. In this case, reference materials (3) are set on earth surface (2) under study with known values of thermophysical parameters. These materials are subjected (3) to solar radiation from the sunrise to the sunset. Simultaneously with given interval, the total and reflected solar radiation delivered to the earth surface (2) under study is recorded, and radiation balance of earth surface under study is measured (2). Then ambient and soil temperature, wind speed, radiation temperature on the surface of the reference material (3) and the earth surface (2) under study are measured from the sunset up to the sunrise. The averaged energy luminance of the reference materials (3) is determined using the obtained measurement results. The heat and temperature conductivity of the earth surface under study (2) is clarified.;EFFECT: increased accuracy for determining spatial distribution of the thermophysical parameters of the earth surface.;1 dwg
机译:领域:测量设备;物质:通过安装在直升机类型的无人飞行器(1)上的设备测量被研究地面(2)的辐射温度。计算出了地表的热传导率和温度传导率(2)。构造获得的参数的空间分布。在这种情况下,参考材料(3)被放置在正在研究的地球表面(2)上,具有已知的热物理参数值。这些材料从日出到日落都会受到(3)的太阳辐射的影响。在给定间隔的同时,记录传输到被研究地表(2)的总和反射太阳辐射,并测量被研究地表的辐射平衡(2)。然后,从日落到日出,测量环境温度和土壤温度,风速,所研究的参考物质(3)和地球表面(2)的温度。使用获得的测量结果确定参考材料(3)的平均能量亮度。澄清了研究中的地表(2)的导热性和温度传导性;效果:确定地表热物理参数的空间分布的精度提高了; 1 dwg

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