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Prva stran - WBC-INCO Net

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On the territory of the RM the most important convective<br />

hydro geothermal systems are: Skopje's Valley, Kocani's<br />

Valley, Strumica's Valley, Gevgelija's Valley, Kezovica,<br />

Toplik - Topli Dol on the Kozuf Mountain, Toplec near<br />

Dojran, Proevci near Kumanovo, Strnovec, Zdravevci on<br />

the Povisnica River near Kratovo, Sabotna Voda near Veles,<br />

as well as dry systems in western Macedonia - Kosovraska<br />

and Debarska's spas and Banice on the Pena River near Tetovo.<br />

In the following text there will be given details of data<br />

and parameters for more important hydro geothermal systems<br />

in the RM. The location of the main geothermal fields<br />

and their hydro geothermal systems which are at current<br />

exploitation shown on this photo.<br />

Fig. 1. Main geothermal fields in Macedonia (K. Popovski, E. Micevski,<br />

2001)<br />

III. ENERGETIC POTENTIAL OF THE RESOURCES<br />

Total balance-sheet of geothermal exploitation reserves<br />

in RM (state 2004) is 1.473 l/sec, registered on 17 more<br />

important locations and complexes (Table 1 and Fig. 1).<br />

Quantity of geothermal energy contained in hydro geothermal<br />

systems is determined by many methods for determination<br />

of geothermal potential. There are viewed more hydrogeoloic,<br />

geologic and geothermal sizes that are more or less<br />

defined or taken with certain proximities.<br />

In the table below valorization is made of available hit<br />

power of all exploitation geothermal resources in RM. The<br />

total maximum available power of 173 MW is gained or<br />

annual production capacity of 1.515.480 MWh/year/ effective<br />

valorization of one geothermal resource is possible only<br />

if there are available data for composition of its users.<br />

Each one separately is causes temperature area for use<br />

and possibilities to compose cascade chain for optimal use<br />

of available temperature level. According to Lindal's diagram<br />

which gives the areas used for proved technology and<br />

direct application of geothermal energy recommends low<br />

usage limit from 20, however, it has been proved that limit<br />

from 15 is a real base for aquaculture (K. Popovski, 1995).<br />

The quality influence is an illustrative technical solution<br />

for heating capacity of concrete geothermal source. To reach<br />

maximum use of one hydro geothermal system the normal<br />

outlet temperature should be 15.<br />

Unfortunately, applied technical solution by users in RM<br />

give results with outlet temperatures in winter conditions<br />

between 30 and 45, which automatically lowers heating ca-<br />

pacity of geothermal resource to 30-50%.<br />

TABLE 1<br />

BALANCE-SHEET OF HYDROGEOTHERMICAL RESOURCES IN RM<br />

(STATE 2004)<br />

Hydro<br />

geothermal<br />

system<br />

Locality<br />

Temp.<br />

(C°)<br />

Yield<br />

(l/sec.)<br />

Exploitationreserves<br />

(l/sec.)<br />

IV. VALORIZATION OF GEOTHERMAL RESOURCES<br />

A. Use of geothermal energy<br />

Use of geothermal energy in RM is long centuries tradition<br />

in the domain of balneology, and there is 40-year old<br />

tradition worming greenhouses complexes. So-called energetic<br />

crisis in the 70 and 80's from the previous century<br />

started the researches in the area of geology in order to find<br />

out potential energetic resources as well as systems development<br />

of low temperature geothermal water. There have<br />

been performed many projects for heating greenhouses<br />

complexes, drying agriculture products, heating administrative<br />

and industrial objects, basins, preparing sanitary hot<br />

water, industry use etc. In RM there are current7 geothermal<br />

projects and 6 spa complexes where geothermal water is<br />

used. All these geothermal projects started in the 80's in the<br />

previous century, and spa complexes are dating from earlier<br />

period. There are valid documents for the geothermal systems<br />

(Kocani), Podlog Spa, Istibanja (Vinica), Bansko,<br />

Gevgelija Valley etc.<br />

B. Economic aspects (Comparative geothermal potential)<br />

Macedonia use sources of energy like coal and river hydro<br />

energy from domestic origin and important oil. Use of<br />

sun energy is insignificant compared to the needs and possibilities<br />

and use of natural gas in preparation phase, but it has<br />

2<br />

Heat<br />

power<br />

(MWt)<br />

Skopje<br />

Valley<br />

Volkovo 25 60 20 2.10<br />

Skopje<br />

Valley<br />

Katlanovo 50 20 15 10.45<br />

Kumanovo<br />

spa<br />

Dupnatina 31 6 4 0.52<br />

Strnovec ST-5, PEB 47 50 46 9.05<br />

Zdravevci ZD-3,4,5,6 48 22 20 4.02<br />

Dobrevo Borehole 28 12 8 0.94<br />

Podlog<br />

Kocani<br />

Borehole 75 650 300 94.14<br />

Istibanja-<br />

Vinica<br />

ID-3,4,5 68 73 73 20.78<br />

Strumica<br />

Valley<br />

Bansko 70 82 50 14.65<br />

Gevgelija<br />

Valley<br />

Negorci 50 100 80 16.74<br />

Gevgelija<br />

Valley<br />

Smokvica 65 180 120 32.65<br />

Dojran Toplec 28 28 10 1.17<br />

Kozuf Toplik 21 2 2 0.18<br />

Rakles Dupnatina 26 5 2 0.22<br />

Veles Sabota v. 21 5 5 0.44<br />

Stip Kezovica 57 8 7 1.67<br />

Tetovo-<br />

Pena R.<br />

Baniche 30 10 10 1.26<br />

Debar spa Baniste 50 120 100 16.74<br />

Kosovraska<br />

spa<br />

Kosovrasti 48 100 60 12.05<br />

Total ∑ 1473 933 239.92

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