Hidrológiai Közlöny 1931 (11. évfolyam)

Gedeon Tihamér: Hidrológiai megfigyelések a Vértes-hegység délkeleti részéből

124 S. S. de Finály SrSOí Ca(B0 2) 2 Ca(HC0 3) 2 Mg(HCOs) 2 Fe(HC0 3) 2 H2SÍO3 0.0004 g 0.0397 „ 0.0570 „ 0.0343 „ 0.0022 „ 0.0620 „ Total: 5.7457 g Temperature of the water at the outflow: 77.0 C°, temperature of the air at the same time: 23.5 C°. Specific gravity of the water at 20 C: 1.00464. Lowering of freezing point: 0.371°. Osmotic pressure of the dissolved salts: 4.49 atm. Electric conductivity: 86.6.10" 4 £2 _ 1 cm-i 1 liter of the water contains 0.10.10-" millicurie Radium emanation. The earth gas consists of 91.4 vol. % CH4 0.5 „ „ C nH m 7.6 „ „ C0 2 0.5 „ „ O2 Too.o „ „ It is interesting to compare the chemical composition of this alkaline salt water with other waters of deep borings of that part of the Hungarian Great Plain. The following table shows the data of their chemical analysis in aequivalent percents: Water of Cations: Hajdúszoboszló: Boring I. B. II. Karcag: Tiszaörs: Debrecen: K + : Na+ : Ca++ : Sr++ : Mg++ : Fe++ : A1+++ 0.79 98.06 0.90 0.22 0.03 0.89 97.05 1.51 0.01 0.51 0.03 1.19 93.64 2.83 0.41 99.44 0.05 1.08 94.50 3.97 0.44 0.14 1.74 0.10 0.40 0.05 100.00 100.00 100.00 100.00 100.00 Anions: CI— : 70.82 82.70 46.45 64.25 94.74 Br—: 0.37 0.37 0.15 0.27 0.03 J— : 0.07 0.06 0.04 0.05 traces B0 2 — : 0.65 0.68 SŰ4 : 0.02 0.08 0.79 0.82 HCOs— : 12.51 53.37 29.99 4.41 COs : 28.07 3.60 4.63 100.00 100.00 100.00 100.00 100.00 Amount of salts dissolved in 1 000 g: 4.5074 5.7457 2.9990 4.2357 13.6654 Analyst: Emszt Finály Straub Szelényi Finály Date: 1925. 1931. 1929. 1931. 1931.

Next

/
Oldalképek
Tartalom