傅抱璞. 1981: 土壤蒸发的计算. 气象学报, (2): 226-236. DOI: 10.11676/qxxb1981.024
引用本文: 傅抱璞. 1981: 土壤蒸发的计算. 气象学报, (2): 226-236. DOI: 10.11676/qxxb1981.024
Fu Bao-pu(Fuh Baw-puh). 1981: ON THE CALCULATION OF EVAPORATION FROM SOIL. Acta Meteorologica Sinica, (2): 226-236. DOI: 10.11676/qxxb1981.024
Citation: Fu Bao-pu(Fuh Baw-puh). 1981: ON THE CALCULATION OF EVAPORATION FROM SOIL. Acta Meteorologica Sinica, (2): 226-236. DOI: 10.11676/qxxb1981.024

土壤蒸发的计算

ON THE CALCULATION OF EVAPORATION FROM SOIL

  • 摘要: 本文根据对土壤蒸发过程的物理考虑和量纲分析,推导了适用于计算各阶段土壤蒸发的普遍公式.计算值与实际观测资料相比较,结果相当良好.

     

    Abstract: If E is the evaporation from soil,E0 the evaporative power and Q the possible maximum amount of water which may be supplied by soil for evaporation during given period,we may consider that ∂E/∂E0 and ∂E/∂Q are some founctions of Q,E0 and E viz ∂E/∂E0=F(Q,E0,E),∂E/∂Q=ФF(Q,E0,E).Assuming E=E1+E2,F(Q,E0,E)=F1(Q,E0,E1)+F2(Q,E0,E2)and Ф(Q,E0,E)=Ф1(Q,E0,E1)+Ф2(Q,E0,E2),we get Eqs.(9)and (10).By applying dimensional analysis and the theory of differential equation we have shown that the forms of Fi and Фi(i=1,2) are Eqs.(15),and hence derived formula (34).The relationship between E/E0 and w computed by formula(34) is shown in figure 2,it is in good agreement with the measurement by Popof-evaporation gauge.

     

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