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APPLICATION OF NATURAL ISOTOPES AND WATER CHEMICAL STUDY IN DETERMINING THE ORIGIN OF WATER IN KARSTIC SPRINGS

APPLICATION OF NATURAL ISOTOPES AND WATER CHEMICAL STUDY IN DEFERMINING THE ORIGIN OF WATER IN KARSTIC SPRINGS
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摘要 In attempt to determine the originity of water in several springs Biljana spring, St. Naum. St. Zaum and others) located along the coast of Ohrid lake (south-western part of Macedonia. Yugoslavia) the distribution of environmental isotopes (δ<sup>1δ</sup>O,δ<sup>2</sup>H and <sup>3</sup>H) in the local waters of interest (precipitation, surface accumulations and underground) has been observed. In attempt to determine the originity of water in several springs (Biljana spring, St. Naum, St. Zaun and others) located along the coast of Ohrid lake (south - western part of Macedonia, Yugoslavia) the distribution of environmental isotopes (δ 18O, δ 2H and 3H in the local waters of interest (precipitation, surface accumulations and underground) has been observed. On the basis of the obtained so far results and by application of one-cell mixing model, the participation of the upper lake Prespa (by drainage through karstificated Galicica Mountain) in the observed spring's discharges was calculated. The performed water chemical studies has confirmed previously differentiated spring waters based on their environmental' isotope content.
出处 《中国岩溶》 CAS CSCD 北大核心 1992年第S1期78-83,共6页 Carsologica Sinica
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