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Natural Radioactivity of Water in Slovakia
LADISLAV LU&#268;IVJANSKÝ lucivjansky@uranpres.sk

Introduction

Natural radioactivity of waters is caused by the content of dissolved solid and gaseous natural radioactive substances. Major natural radionuclides in ground and surface waters comprise 40K, 238U, 234U, 232Th, 226Ra and 222Rn, all of which pass into waters from a rock environment. Of these radionuclides, those of the uranium decay series (a mixture of 238U and 234U referred, to as Unat, 226Ra and 222Rn) are most abundant in water. Mapping of natural radioactivity of Slovakia&#8216;s waters was compiled from some studies completed in 1991 &#8211; 1997. The first of these studies was aimed at producing the reportant map &#8222;Radiohydrochemical sampling of Slovakia&#8221; at a scale of 1:200,000. Second study was part of the geological factors of the environment map of Slovakia compiled on regional geological maps at a scale of 1:50,000. This study also included the compilation of radiohydrochemical maps in the areas of the Upper Nitra river, Malá Fatra Mts. and surrounding basins, Nízke Tatry Mts., Starohorské vrchy Mts., Hornád river Basin and the Eastern Slovak Ore Mts., Ko&#353;ice Basin and Slanské vrchy, (1991-1993), the Jel&#353;ava-Lubeník-Hnú&#353;&#357;a region (1994-1997), Tatry Mts. and the Liptov Basin (1996-1997).

Methods of Sampling and Radiochemical Analyses

Throughout the Slovak Republic 5818 water samples were collected from springs, mineral springs, fresh, mineral and thermal waters from artesian wells, from wells, water sources, pumped wells, mine effluent, streams, lakes and tailing dumps. The sampling density at the survey scale of 1:200,000 averaged sample per 10 km2 and in some areas (Upper Nitra river, Malá Fatra Mts. and surrounding basins, Nízke Tatry Mts., Starohorské vrchy Mts., Hornád river Basin and the Eastern Slovak Ore Mts., Ko&#353;ice Basin and Slanské vrchy, Jel&#353;ava-Lubeník-Hnú&#353;&#357;a region, Tatry Mts., Liptov Basin), surveyed at scale 1:50,000, one sample per 5 km2. Unat contents, as well as 226Ra and 222Rn volume activities, were determined in laboratories. Unat contents were measured through colorimetric method on instrument whose sensitivity range was 0.002 &#8211; 0.40 mg.l-1. 226Ra volume activity was determined on the instrument having sensitivity range is 0.002 &#8211; 400 Bq.l-1. The apparatus with lucastype scintillation chambers measured 222Rn volume activity with sensitivity range is 0.05 &#8211; 10 000 Bq.l-1.

Natural radioactivity of groundwaters in major geological units of Slovakia

Paleogene

Flysch Belt

Groundwaters in the Flysch Belt of northwestern Slovakia have relatively stable values of uranium concentrations, as well as radium and radon volume activities. Average values of uranium concentrations are typical of flysch facies (0.003 mg.l-1). An increased number of samples with increased uranium contents were noted only in the Javorníky Mts. The values of radium volume activities are also low (arithmetic mean &#8222;x&#8221; - 0.033 &#8211; 0.039 Bq.l-1, geometric mean &#8222;GM&#8221; &#8211; 0.018 &#8211; 0.024 Bq.l-1). The lowest values were found in the Javorníky Mts. (mostly below 0.03 Bq.l-1). The values of radon volume activities are increased only locally. Uranium concentrations in waters of the eastern Slovakia Flysch Belt (mostly 0.002 &#8211; 0.003 mg.l-1) reflect the variation of lithological types of underlying rocks. Radium and radon volume activities are increased only in waters having a deeper circulation.

Inner Carpathian Paleogene

Ground waters with increased radium concentrations occur in the rocks of the Inner Carpathian Paleogene. In many springs, mainly in the Hornád basin, the concentration of Ra is higher than 0.1 Bq.l-1. The source of radium is probably in the underlying mesozoic carbonate rocks. Hypoallogene radon (from 20 to 30 Bq.l-1) occurs in the spring waters with deeper circulation. The average concentration of uranium varies from 0.002 mg.l-1 (in the Huty formation, mainly claystones) to 0.004 mg.l-1 (in the sandstone-dominated Biely Potok formation).

Core Mountains

Malé Karpaty Mts.

In the southwestern part of the mountain range, crystalline complex rocks prevail, which is reflected by the presence of waters with increased concentrations of radioactive elements, mainly radon. These are the waters, mainly of shallow circulation, connected to the weathering zone of granites and granodiorites, where exist good conditions for the formation of hypergene radon in the waters. Uranium concentrations are slightly increased, values of radium volume activity are fairly high (x 0.070 Bq.l-1, GM 0.053 Bq.l-1) and the values of volume activity of radon are high (x 33.31 Bq.l-1, GM 17.00 Bq.l-1). The water from the spring &#8222;Zbojnícka stud&#328;a&#8221; near Ra&#269;a (volume activity 222Rn 303.69 Bq.l-1) and from the spring near Kuchy&#328;a (volume activity 222Rn 261.48 Bq.l-1) are classified as low-radon water (Lu&#269;ivjanský, 1996).

Pova&#382;ský Inovec Mts.

In the crystalline complex of the eastern part of the mountain range, waters with increased uranium and radon concentrations are present. These waters occur for instance near Podhradie (Unat 0.195 mg.l-1, 226Ra 0.447 Bq.l-1) and Duchonka (222Ra 315.79 Bq.l-1). Water with increased concentrations of radionuclides flows from the uranium exploration adit no. 60 in Kálnica. Its uranium concentration is 0.063 mg.l-1, the volume activity 226Ra is 0.464 Bq.l-1, and the volume activity of radon is 61.11 Bq.l-1.

Strá&#382;ovske vrchy Mts.

Slightly increased values of uranium concentrations (0.004 &#8211; 0.008 mg.l-1) are present in waters from the Middle to Upper Triassic dolomites of the Cho&#269; nappe in the southern part of Strá&#382;ovske vrchy. These waters are also slightly enriched in radon, probably from the underlying crystalline complex. Higher concentrations of radon are present in waters of the crystalline complex, which is underlain by banded migmatites and migmatitized paragneisses in the Kanianka area (the maximum value of radon volume activity is 173.36 Bq.l-1).

Tríbe&#269; Mts.

In the southwestern (Zobor) part of the mountain range, where the granitoids prevail over Mesozoic complexes, occur waters with increased concentrations of uranium (more than 0.004 mg.l-1) and radon (more than 30 Bq.l-1). In the northeastern (Razdiel) part, where crystalline complex rocks (migmatites, paragneisses) and Mesozoic (envelope as well as nappe types) are present fairly equally, no waters had increased radioactivity values.

Malá Fatra Mts.

Waters from the weathered zone of crust crystalline complex commonly contain increased concentrations of uranium and radon. In the Lú&#269;anská Malá Fatra Mts. these waters are connected to two-micas and biotite paragneisses and in the Krivánska Malá Fatra Mts. to biotite quartz diorites to granodiorites. The water from the spring near Tur&#269;ianske K&#318;a&#269;any is classified as radioactive &#8211; low-uranium water (uranium concentration is 0.035 mg.l-1). In waters from dolomites of the Cho&#269; nappe of the Lú&#269;anska Malá Fatra Mts., slightly increased uranium concentrations are present (more than 0.004 mg.l-1).

Ve&#318;ká Fatra Mts.

Slightly increased values of uranium concentrations (x 0.0041 mg.l-1, GM 0.0033 mg.l-1) are present in waters from Middle Triassic dolomites of the Cho&#269; nappe. Some samples have an increased volume activity 226Ra. These are the waters draining Lower Triassic and Cretaceous pelitic rocks in the northern part of the Ve&#318;ká Fatra Mts.

Tatry Mts.

Waters from the crystalline units of the Západné Tatry and Vysoké Tatry are isolated occurrences of increased values uranium, radium and radon. They are controlled by altitude and consequently by the speed and length of groundwater circulation. The summit sectors of the highest mountain ranges of Tatry are without springs. In the southern mountain ranges are waters having slightly increased values of radionuclids, mainly radon. These are the waters from the weathering zone of acid igneous rocks.

Nízke Tatry Mts. (part &#270;umbierske Tatry)

Increased uranium concentrations occur mainly in waters of Cho&#269; nappe dolomites (average value of uranium is 0.004 mg.l-1). Moderately increased uranium concentrations are also present from the crystalline complex, such at waters from leucocratic granites south Partizánska &#317;up&#269;a and of waters from migmatites in the Jasenie and Dolná Lehota regions (max. 0.026 mg.l-1). Radium volume activity is increased only rarely. In this region, waters with increased values of radon volume activity are present. These increased values can be divided into two groups: -	Waters connected to the weathering zone of leucocratic granites and migmatites of the crystalline complex in the surroundings of Brusno (293.45 Bq.l-1 &#8211; low-radon water, Pohronský Bukovec 108.53 Bq.l-1, Jasenie 159.78 Bq.l-1) -	Deeply circulated waters associated with tectonic faults, e. g. near the Partizánska Lup&#269;a (increased volume activities of radium are also typical).

Veporic Zone

Increased uranium concentrations are found mainly in waters from Permian sediments in the Kozie chrbty Mts. (average uranium content 0.004 mg.l-1). The increased contents in Permian sediments are associated with the occurrences of U minerals in sandstones, for example a spring south of the village Východná in Chmelinec Valley, which was explored for uranium, the water containing 0.027 mg.l-1. Further examples of such waters come from the Vikartovce, Kravany and Primovce areas. These waters have increased radon volume activity, too. The average values of radon volume activity in waters in the crystalline units of the Veporské vrchy Mts. and Stolické vrchy Mts. rank among the highest in Slovakia (x 57.47 and 56.82 Bq.l-1, GM 29.94 and 30.11 Bq.l-1). As much as 40 % of the waters show values above 50 Bq.l-1. These are waters of shallow circulation in the weathered zone of crystalline rocks of the Krá&#318;ova ho&#318;a and Kohút unit, notably biotite granodiorites to quartz diorites and light-coloured granites. Major occurrences of such waters are situated in the area between Detvianska Huta, Sihla and Klenovec and northwest of Revúca in the Kohút and Stolica areas.

Gemeric zone

The average uranium concentrations in waters of the Volovské vrchy Mts. Paleozoic are not substantially different from those in groundwaters. In some areas (near &#352;vedlár, Nálepkovo, Henclová and Smolník), the values are 0.004 &#8211; 0.008 mg.l-1. These scattered anomalies are bound to minor occurrences of uranium or uranium-bearing minerals. The area underlain by Paleozoic rocks is characterized by highly variable values of radon's volume activity values in groundwaters (5 &#8211; 500 Bq.l-1). Increased values occur in shallow-circulation waters associated with Silurian metarhyolite tuffs of the Gelnica Group (in waters near Henclová, Stará Voda, Smolnícka píla, Prakovce) and to the Gemeric granites (near Popro&#269; and Rudník). These values often exceed 200 Bq.l-1 and therefore the waters fall into the category of slightly radon waters. The maximum value was measured in water from a spring near Dob&#353;iná (518.86 Bq.l-1). The abandoned uranium deposit Novoveská Huta lies in the northern sector of the Volovské vrchy. Of the several mine-water discharges, only that from adit No. 2 displays increased values of radionuclids. Average monitored values are Unat 0.185 mg.l-1, 226Ra 0.185 Bq.l-1 and 222Rn 205.00 Bq.l-1. Slightly increased radon volume activities were noted in waters from the vicinity of uranium occurrences at Pelc near Dob&#353;iná and at Jahodná near Ko&#353;ice. Groundwaters in Mesozoic complexes of the Slovenský raj Mts., Slovak Karst Mts. and Galmus Mts. display increased values of radium volume activity. These waters are largely associated with to Lower Triassic shales interlayered with evaporites. Uranium concentrations are low. Radon volume activity is locally increased through emanations of hypoallogenic radon from the Paleozoic substratum.

Intramontane Basins

Danube Basin (Danube Lowland and Podunajská pahorkatina Upland)

Natural radioactivity of groundwaters in the Danube Lowland and that in the Podunajská pahorkatina Upland are almost identical, except for the radon volume activity. The average uranium concentration (0.0053 mg.l-1) is among the highest in Slovakia. These concentrations are associated mostly with waters whose T.D.S. (Total Disolved Solids) is 750 &#8211; 1,000 mg.l-1 (Rapant et al., 1997). This agrees with Lisicin&#8217;s (1975) data that waters with such T. D. S. in arid areas most intensively dissolve uranium from rocks. Radium volume activity is increased only in western sector (between Dunajská Streda and Bratislava) which, like the Záhorie Basin, is rich in waters whose T.D.S. is 500 &#8211; 750 mg.l-1. More strongly mineralized waters mostly have a radium volume activity range from 6.55 Bq.l-1 in the Danube Lowland to 11.73 Bq.l-1 in the Podunajská pahorkatina Upland. Greatest activities in the Podunajská pahorkatina probably result from the presence of thickness of Tertiary sediments.

Southern Slovakia Basin

This region is characterized by increased uranium concentrations, notably in areas underlain by Neogene sediments (average 0.004 &#8211; 0.005 mg.l-1). Concentrations between 0.002 &#8211; 0.003 mg.l-1 are typical of volcanoclastic rocks. Waters in the volcanic complexes of the Cerová vrchovina upland display slightly increased radon volume activities (x 28.38 Bq.l-1, GM 22.72 Bq.l-1).

Eastern Slovakia Basin (Ko&#353;ice Basin, Eastern Slovakia Lowland)

In the Ko&#353;ice Basin, uranium concentrations and radium volume activity do not exceed average values of Slovakia&#8217;s groundwaters. Slightly increased values have been noted only in wells in Quaternary sediments in the vicinity of the Hornád River. These higher values, such as those at Haniska and Se&#328;a, are presumably caused by fragments of Gemeric rocks of Paleozoic age in poorly consolidated Quaternary sediments. In places, increased values of radon volume activity (up to 50 Bq.l-1) are associated with N or NE-trending tectonic lines. Unlike waters in the Danube Lowland, those in Neogene sediments of the Eastern Slovakia Lowland are devoid of increased uranium concentrations (average Unat content is 0.003 mg.l-1). The latter have a T. D. S. above 1 000 mg.l-1 and therefore their ability to dissolve uranium from rocks is reduced (Lisicin, l. c.).

Neovolcanic rocks (Central Slovakia Neovolcanic Rocks, Slanské Vrchy Mts. and Vihorlatské vrchy Mts.) The groundwater radioactivity in neovolcanic mountain ranges is extremely low. Uranium concentrations in groundwaters from the neovolcanic rocks are typical for the shallow groundwater circulation in disturbed upper parts of the volcanic rocks. Radium volume activity of waters in the Central Slovakia Neovolcanic Rocks differs from that in the Slanské vrchy Mts. and Vihorlatské vrchy Mts. neovolcanic rocks. Waters in acid rock varieties of the Central Slovakia Neovolcanic Rocks have very low radium values (x 0.031 Bq.l-1, GM 0.017 Bq.l-1) in comparison with more mafic neovolcanic rocks in the Slanské vrchy Mts. (x 0.052 Bq.l-1, GM 0.049 Bq.l-1) and Vihorlatské vrchy Mts. (x 0.047 Bq.l-1, GM 0.039 Bq.l-1). Radon volume activity is highest in the Central Slovakia Neovolcanic Rocks (x 15.32 Bq.l-1, GM 9.10 Bq.l-1) and lowest in the Slanské vrchy Mts. neovolcanic rocks (x 6.40 Bq.l-1, GM 3.40 Bq.l-1). The radon here is of hypallogenic origin associated with faults and hyperallogenic origin from upper parts of weathering crusts.

Radioactivity of Slovakia&#8217;s Mineral and Thermal Waters

In comparison with fresh waters, cold mineral waters are enriched in some radionuclides, notably radium and radon. Radium volume activity of some thermal waters is 100 x high than that of fresh waters. These mineral and thermal waters fall into the category of low-radium or low-radon waters. On the basis of natural radioactivity of 243 of Slovakia&#8217;s sampled mineral water occurrences, they are divided into several types:

-	mineral waters bound to Triassic carbonates, mostly in the Kri&#382;na and Cho&#269; nappes Uranium concentrations in these waters are low, averaging 0.003 mg.l-1. Radium volume activity usually is 0.2 to 0.9 Bq.l-1. Such mineral water occurs at such as Be&#353;e&#328;ová, Sivá Brada near Spi&#353;ské Podhradie, Sobrance and Oravice. Many of them (e.g. the springs &#8222;Sv. Ondrej&#8221; and &#8222;Sv. Krí&#382;a&#8221; at Sivá Brada, and the spring &#8222;O&#269;ný prame&#328;&#8221; at Sobrance) are classified as low-radium waters. Radon volume activities largely are 20 &#8211; 50 Bq.l-1, but in some waters they are much higher. For example the spring &#8222;Sv. Ondrej&#8221; at Sivá Brada yields 170.5 Bq.l-1. Vicinity of these springs is commonly covered with travertine. The highest radon volume activity occurs in water from spring &#8222;Uhli&#269;itý&#8221; at Oravice &#8211; 1,293.2 Bq.l-1.

-	mineral waters of the crystalline unit These are mostly cold acidic water, with increased values of uranium and radium, but mainly of radon. The increased contents result from aggressive CO2 affecting crystalline rocks and from the hypallochtonous origin of the radon. Such waters include those of the Nízke Tatry Mts. crystalline unit (near Bacúch, in Jasenie and near Braväcovo) and Veporské vrchy (springs near &#268;ierny Balog, e.g. water from mineral spring &#8222;Zuzka&#8221; has a 222Rn volume activity as much as 817.89 Bq.l-1) and others. The group partly comprises also the mineral waters of the Tatry Mts. crystalline unit associated with the Subtatric fault (e.g. at Starý Smokovec). The mineral waters of the crystalline units have uranium contents of 0.005 &#8211; 0.015 mg.l-1, 226Ra volume activity mostly 0.1 &#8211; 0.5 Bq.l-1 and 222Rn volume activity commonly greater than 200 Bq.l-1, and consequently are classified as radon waters.

-	mineral waters of the Flysch belt These are sodium-bicarbonate waters with hydrogensulphide or acidulous water. The waters are linked to tectonic lines in all partial-flysch units. They are characterized by slightly increased uranium concentrations (0.004 &#8211; 0.005 mg.l-1), average 226Ra volume activity (0.02 &#8211; 0.08 Bq.l-1, only rarely above 0.1 Bq.l-1). The 222Rn volume activity is 10 &#8211; 20 Bq.l-1, and only in waters enriched in CO2 is above 20 Bq.l-1.

-	mineral waters of the neovolcanic rocks The are characterized mostly by low uranium (average 0.002 mg.l-1) and radium contents (as much as 0.05 Bq.l-1) and mildly increased 222Rn volume activity (20-40 Bq.l-1).

Slovakia&#8217;s thermal waters are divided into two groups reflecting their associated rocks:

-	thermal waters of pre-Tertiary units Are characterized by a high 226Ra volume activity. They comprise waters at Be&#353;e&#328;ová &#8211; well ZGL-1 (226Ra volume activity 9.7 Bq.l-1), Pie&#353;&#357;any (3.068 Bq.l-1), Oravice &#8211; well OZ-2 (3.209 Bq.l-1), Lú&#269;ka near Spi&#353;ské Podhradie &#8211; well B&#352;-1 (2.503 Bq.l-1), Poprad - well PP-1 (1.733 Bq.l-1), Ková&#269;ová &#8211; well K-1 (0.998 Bq.l-1), Lú&#269;ky &#8211; well BJ-101 (0.985 Bq.l-1), Tren&#269;ianske Teplice &#8211; well SBP-5 (0.784 Bq.l-1) and elsewhere. These waters have temperatures between 30 and 60 °C, and Ca-Mg-Na-SO4-HCO3 (well OZ-1), Ca-Mg-HCO3 (wells PP-1, B&#352;-1), Ca-Mg-SO4-HCO3 (well BJ-101) chemistries. The waters are associated primarily with Triassic rocks of the Krí&#382;na and Cho&#269; nappes. Waters of the Cho&#269; nappe in Poprad and Lu&#269;ka are enriched in uranium (e. g. in well B&#352;-1 as much as 0.111 mg.l-1).

-	thermal waters of Tertiary units These characterized by a low 226Ra volume activity (as much as 0.1 Bq.l-1). The group includes thermal waters from wells at Dunajský Klátov, Vl&#269;any, Tvrdo&#353;ovce, Sládkovi&#269;ovo, Diakovce, Nové Zámky and Topo&#318;níky.

Conclusion

Uranium - Unat

Uranium concentrations in groundwaters are increased in waters flowing from uranium mine workings (Novoveská Huta, Kálnica), in springs close to uranium occurrences, such as those near Vychodná and in some thermal waters (Oravice, Lú&#269;ka near Spi&#353;ské Podhradie). A locally increased uranium concentration also occur in waters of some core mountains composed of crystalline units, such as the Pova&#382;ský Inovec Mts., Malá Fatra Mts., Tríbe&#269; Mts., and in waters of Cho&#269; nappe dolomites, e.g. in the Nízke Tatry Mts. The largest area of slightly increased uranium content (averaging as much as 0.005 mg.l-1) is in found the waters of the Danube Basin, Southern Slovakia Basin and Vienna Basin. In flysch areas, waters from sandstone formations (average uranium content 0.003 mg.l-1) are a little different from those in claystone and claystone-sandstone formations (average uranium content 0.002 mg.l-1). Waters in neovolcanic rocks typically have low uranium concentrations (0.002 mg.l-1).

Radium &#8211; 226Ra

The radium volume activity values are more widely dispersed than are the uranium concentrations (from less than 0.001 to 9.7 Bq.l-1). The highest values are typical of mineral and thermal waters. Increased values also have been noted in fresh waters of the Záhorie Lowland and western part Danube Lowland, and in some core mountains (Malé Karpaty Mts., Pova&#382;ský Inovec Mts.), eastern sector of Nízke Tatry Mts., Hornád Basin, Poprad Basin, Galmus Mts. and western part Volovské vrchy Mts. From pre-Tertiary units, these waters are mostly associated with to Lower Triassic (Werfenian) rocks with gypsum and baryte occurrences. In Paleogene rocks, radium volume activity increases with the depth of groundwater circulation. Radium values in waters of the Central Slovakia Neovolcanics Rocks are half as large as those from the neovolcanic rocks of the Slanské vrchy Mts. and Vihorlat Mts., except for areas composed mostly of volcanic-sedimentary rocks, e.g. the Krupinská planina Plain.

Radon &#8211; 222Rn

Radon volume activity values are from less than 0.05 &#8211; 1,293.20 Bq.l-1. Radon occurrences in water depend on the presence of uranium minerals in rock, tectonic setting, mineralization and water temperature. The highest values of radon in groundwaters are from crystalline units of the Tatricum and Veporicum, also in some waters from acid neovolcanic rocks, in waters from the volcanic-sedimentary rocks of the Cerová vrchovina Upland, Zemplínske vrchy Mts.. The lowest values are from waters from sedimentary rocks of the Danube Basin, Southern Slovakia Basin, Vienna Basin, Eastern Slovakia Basin, and from waters of the Slovenský raj Mts., Slovak Karst Mts., northwestern part Flysch Belt (Magurský fly&#353;) and the inner carpathian Paleogene rocks in the Levo&#269;ské vrchy Mts..

Several kinds of radon waters are distinguished, according to Lange&#8217;s (1969) classification:

1.	Waters with increased to high radon volume activity occur from crystalline parts of core mountains (composed mostly of acid granitoids and migmatites). These waters are most common radon water of weathered zone of igneous rocks formed in the upper parts of fractured zones. Such waters are found in nearly all core mountains, notably the Malé Karpaty Mts., Pova&#382;ský Inovec Mts., Tríbe&#269; Mts., Malá Fatra Mts. and Nízke Tatry Mts.. They are most widespread in the crystalline units of Veporské and Stolické vrchy Mts. Waters from some acid rocks in the Central Slovakia Neovolcanic Rocks and the Cerová vrchovina Upland are also included in this category.

2.	The second type is made up of radon waters with increased radium values associated with clayey-travertine sediments. This type comprises mineral waters at Sivá Brada and Be&#353;e&#328;ová.

3.	The third type consists of radon waters from along deep tectonic faults of high discharge and increased temperature. Such waters include the mineral spring &#8222;Uhli&#269;itý&#8221; at Oravice. This spring has the highest radon volume activity in Slovakia &#8211; 1,293.2 Bq.l-1.

4.	Fairly widely distributed types of radon waters are radon waters on tectonic faults. These waters are mineralized to various degrees and they ascend from various depths along the faults. Many of them are enriched in radium and satured with CO2. Radon here originated at depth or from radium precipitated on the walls of faults. These waters are found near the Subtatric faults, on tectonic lines in the Hornád Basin and Ko&#353;ice Basin and, to a lesser extent, also in the neovolcanics rocks and other intramontane depressions.

5.	Radon waters of uranium deposits draining uranium deposits and present in springs near uranium occurrences. These waters are also characterized also by increased uranium concentrations and radium volume activity. Waters discharged from abandoned uranium deposits at Novoveská Huta and Kálnica best exemplify the type.

References

Daniel, J. &#8211; Lu&#269;ivjanský, L. &#8211; Stercz, M., 1996: Geochemical Atlas of Slovakia &#8211; Natural rock radioactivity.

Lange, O. K., 1969: Gidrogeologija. &#8222;Vy&#353;&#353;aja &#353;kola&#8221;, Moscow.

Lisicin, A. K., 1975: Uranonosnos&#357; podzemnych vod. Materialy pervogo vsesojuznogo radiogeochimi&#269;eskogo sove&#353;&#269;anija Radioaktivnyje elementy v gornych porodach. &#8222; Nauka&#8221; Novosibirsk.

Rapant, S., Vrana, K., Bodi&#353;, D., 1997: Geochemical Atlas of Slovakia, Part Groundwater. Slovak Geological Magazine. Volume 3 No 1., Geological Survey of Slovak Republic, Bratislava.