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<br />C:\). <br />~r, <br />. <br /> <br />29 <br /> <br />computations made in the subroutine due to the fact that the salt flows <br /> <br />depend entirely upon the water trows. An exception to this is the <br /> <br />quantity of salt obtained from the area. This is determined as the <br /> <br />difference between the quantity of salt outflow which must occur to <br /> <br />maintain an annual salt ba~ance and the quantity of salt which is <br /> <br />indicated from ground water outflows and salinity concentrations <br /> <br />measured. The problem of leaching the deposited salts from the root <br /> <br />zone due to evapotranspiration is handled by comparing the water <br /> <br />added to the ground water with the quantity .esti~<l:ted to be the_ leacJ:1- <br />ing require~~~t, c!e <br />'--- ,------------ <br /> <br />Subroutines PCUO, BUDO, CGSC, SABU, GWMOP <br /> <br />These subroutines are tl1e output functions for the computational <br /> <br />subroutines. Their operation is fairly straight forward and examples <br /> <br />of their operation, which represent the study results, will be presented <br /> <br />in a subsequent section. <br /> <br />,-0' <br />