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Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

机译:探索大气强迫对蒸发的影响:大气边界层和浅层地下的实验整合

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摘要

Evaporation is directly influenced by the interactions between the atmosphere, land surface and soil subsurface. This work aims to experimentally study evaporation under various surface boundary conditions to improve our current understanding and characterization of this multiphase phenomenon as well as to validate numerical heat and mass transfer theories that couple Navier-Stokes flow in the atmosphere and Darcian flow in the porous media. Experimental data were collected using a unique soil tank apparatus interfaced with a small climate controlled wind tunnel. The experimental apparatus was instrumented with a suite of state of the art sensor technologies for the continuous and autonomous collection of soil moisture, soil thermal properties, soil and air temperature, relative humidity, and wind speed. This experimental apparatus can be used to generate data under well controlled boundary conditions, allowing for better control and gathering of accurate data at scales of interest not feasible in the field. Induced airflow at several distinct wind speeds over the soil surface resulted in unique behavior of heat and mass transfer during the different evaporative stages.
机译:蒸发直接受到大气,陆地表面和土壤地下之间相互作用的影响。这项工作旨在通过实验研究各种表面边界条件下的蒸发,以提高我们目前对这种多相现象的理解和表征,并验证将大气中的Navier-Stokes流与多孔介质中的Darcian流耦合的数值传热和传质理论。 。使用与小型气候控制风洞连接的独特土壤箱设备收集实验数据。实验设备配备了一套最先进的传感器技术,用于连续和自主收集土壤水分,土壤热特性,土壤和空气温度,相对湿度和风速。该实验设备可用于在边界条件得到很好控制的情况下生成数据,从而可以在现场无法实现的感兴趣范围内更好地控制和收集准确的数据。在土壤表面上以几种不同的风速引起的气流在不同的蒸发阶段导致了传热和传质的独特行为。

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