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水热平衡联系方程为苏联学者布德科所提出,国内曾有人用来计算地表迳流。本文提出用它计算地下迳流有一定的精度,这样就为调动我国大量的水文气象资料,为地下水资源评价服务开辟了一条途径。同时,用水热平衡联系方程又能方便地算出多年地下水资料,从而给地下迳流量保证率计算创造了条件。 (一)水量平衡方程水量平衡方程通常是有下列形式: (1)其中: (2)所以: (3)则地下水补给量ω_地: (4)
Water-heat balance equation for the Soviet scholar Bude Ke proposed that some people used to calculate the surface doldrums. In this paper, it is proposed to calculate the underground flow with a certain accuracy, so as to mobilize a large number of hydrological meteorological data in China, groundwater resources assessment services for the development of a way. At the same time, using the equation of heat and water balance can easily calculate the groundwater data for many years, thus creating the conditions for the calculation of the underground flow rate guarantee. (1) Water Balance Equation The water balance equation usually has the following form: (1) Including: (2) So: (3) Groundwater recharge ω_: (4)