Hidrológiai Közlöny 1946 (26. évfolyam)

Földvári Aladár dr.: A kassai Lajos forrás hidrogeológiája

7f er formations along planes of the Hernád valley fault-system. These Dissur

es may conduct the gases occluded in the Pliocene beds to the surface. For this reason the salts and gases dissolved in the Lajos-spring water are of different origin and become mixed only just before isueinjg. That is why the C0

2 is not in molecular solution but only loosely bound in coarse bubbles. The chemical characteristics of the spring-water compared with the river-water, show marked differences. The actual outlet of the spring does not exclude the possibility of the mingling of spring and river-waters. By a thorough regulation of the outlet tapping only the dolomite underground, this disadvantageous circumstance should be avoided.