CAJ | 학술논문

本文对大气环境下的土壤蒸发作用进行数值模拟，分析了蒸发作用中土壤的水分运移规律，其中包括将饱和土的蒸发过程分为三个相互联系的阶段；并对土壤的供水能力等影响因素做出了分析。结果表明，地下水供水能力越强，蒸发作用越不明显。
본문대대기배경하적토양증발작용진행수치모의，분석료증발작용중토양적수분운이규률，기중포괄장포화토적증발과정분위삼개상호련계적계단；병대토양적공수능력등영향인소주출료분석。결과표명，지하수공수능력월강，증발작용월불명현。
A soil evaporation model under atmosphere condition was established .The regularity of soil moisture movement under evapora-tion effect have been analyzed .The time effect of soil evaporation can be separated into three connected parts;the influences of water sup-ply ability for the evaporation model have been analyzed .As the result, the evaporation effect is more unremarkable when water supply a-bility is better.