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<br />The links to the groundwater nodes represent reservoir <br />seepage, channel losses, deep percolation from irrigated lands <br />and river depletions from groundwater pumping. The link <br />lower bounds are zero and the upper bounds, except the <br />pumping links, are calculated iteratively. <br /> <br />For the pumping links, the lower bounds are zero, and the <br />upper bounds are set equal to the actual pumping or <br />specified pumping capacities of the corresponding demand <br />areas. Calculations defining the bounds on the stream- <br />aquifer interaction links are based on work by Glover (1974) <br />using the concept of diserete kemal functions. <br /> <br />23 <br /> <br />'C, <br /> <br />: . <br />