Hydrogeological investigations of the locality "Mitev Most" for water supply to Kumanovo with ground water
Abstract
This paper shows the results from detailed hydrogeological investigations on locality Mitev Most for water supply to Kumanovo with ground water. In the first stage of investigations were conducted detailed hydrogeological and geophysical explorations and were made six exploration boreholes. In the second phase, in the alluvial Quaternary sediments and in the Paleozoic marbles were made three exploration – exploitation wells EB-MM–1 with depth of 42 m, EB-MM–2 with depth 33 m and EB-MM–3 with depth of 46 m. Based on the individual and grouped testing of the wells and conducted graphical analysis on the results from pumping, exploitation yielding of each well was determined and they amount to 20 l/s for EB-MM–1, 12 l/s for EB-MM–2 and 18 l/s for EB-MM–3.Downloads
References
Alekin A. O.: Principles of Hydrochemistry, Gidrometeoizdat, Leningrad (1970).
Arsovski М.: Tectonics of Macedonia, RGF – Štip (1997).
Gjuzelkovski D.: Groundwater (well) for solving the water supplying in the Republic of Macedonia and their protection. Institute Geohydroproekt. Skopje, 1997.
Karajovanović et al.: Interpreter of Basic Geological Map of SFRJ. 1:100 000, sheet Kumanovo. Geological Institute, Skopje, 1972.
Peševska S.: Preliminary report for performed hydrogeological exploration works on locality Mitev Most and village Proevce – Municipality of Kumanovo, Civil Engineering Institute "Macedonia", Skopje, 2003.
Peševska S.: Report for performed exploitation wells on locality Mitev Most and village Proevce – Municipality of Kumanovo, Civil Engineering Institute "Macedonia", Skopje, 2004.
Cooper, H. H. and Jacob, C. E.: A generalized graphical method for evaluating formation constants and summarizing well field history, Am. Geophys. Union Trans., vol. 27, pp. 526–534 (1946).
Jacob, C. E.: Notes on Determining Permeability by Pumping Tests Under Water Table Conditions. U.S. Geological Survey. Open file report, 1944.
