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首页> 美国政府科技报告 >Evaluation of the Operation of Yermasoyia Surface and Groundwater Reservoirs. Final Report for the Period December 1984 - September 1987.
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Evaluation of the Operation of Yermasoyia Surface and Groundwater Reservoirs. Final Report for the Period December 1984 - September 1987.

机译：Yermasoyia地表水和地下水库运行评价。 1984年12月至1987年9月期间的最终报告。

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The environmental isotope technique has been used in conjunction with hydrochemical methods to study the conjunctive use of surface and groundwater in the Yermasoyia area of Cyprus. The isotopes used in this study are (sup 18)O, (sup 2)H and (sup 3)H. The isotopically enriched water in the Yermasoyia dam is released periodically in order to study the movement of the released water. From the stable isotopes and tritium data, it became evident that two regions can be distinguished in the aquifer, the Upper part and the Delta area. The secondary aquifer on either side of the river valley does not appear to receive any water from the seepage of the dam. The overall tracer average velocity in the aquifer was computed to be 16+-3m per day and this is equivalent to a permeability of 160m per day. Water bodies originating from low frequency spills have been identified at the coast on the basis of oxygen-18 and tritium. A successful simulation of the reservoir for 1985 increased the confidence in the water balance and was used to verify the quantities estimated for evaporation and seepage. Refs, figs and tabs. (Atomindex citation 19:092156)

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