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JOURNAL OF NEW MEDICAL TECHNOLOGIES - 2016 - V. 23, № 3 - P. 230-237
Раздел VII РЕДАКЦИОННЫЙ ПОРТФЕЛЬ
УДК: 614.64
ПРИРОДНЫЕ УСЛОВИЯ И ЗАПАСЫ ПИТЬЕВОЙ И МИНЕРАЛЬНОЙ ВОДЫ В СЕВЕРНОЙ
ОСЕТИИ
М.Э. ДЗОДЗИКОВА
Северо-Осетинский государственный природный заповедник, ул. ЧабаханБасиевой, д.1, г. Алагир, РСО-Алания, 363000, Россия, e-mail: [email protected]@osetia.ru
Аннотация. По данным Федерального государственного учреждения "Центр водных ресурсов" Республики Северная Осетия-Алания, территориального отдела водных ресурсов Республики Северная Осетия-Алания и результатам наших полевых исследований,проведен комплексный анализ природных условий и влагообеспеченности в республике Северная Осетия Алания.
Выявлено, что ресурсы пресных вод достаточны для обеспечения потребности населения и хозяйственных объектов республики в хозяйственно-питьевой воде.Впечатляют запасы питьевой и минеральной воды в Алагирском районе (46,4% от всех запасов в республике), а именно на территориях имеющих отношение к заповеднику, и это при том, что территории СОГПЗ составляет лишь 12,86 % всей площади РСО-А.
Ключевые слова: природные условия, влагообеспеченность, пресная вода, запасы, питьевая и минеральная вода, заповедник, Алагир, Северная Осетия, Кавказ.
THE CLIMATIC CONDITIONS AND DRINKING AND MINERAL WATER IN NORTH OSSETIA
MARGARITA E. DZODZIKOVA
North Ossetian State Nature Reserve, d.1, ChabahanBasiev St., Alagir, North Ossetia-Alania, 363000, Russia,
e-mail: [email protected]
Abstract. According to the Federal State Institution "Water Centre" Republic of North Ossetia-Alania, Territorial Division of Water Resources of the Republic of North Ossetia-Alania and the results of our field research conducted a comprehensive analysis of moisture in the Republic of North Ossetia Alania. Revealed that the freshwater sufficient to ensure the needs of the population of and commercial facilities in the Republic of household drinking water. Impressive reserves of drinking and mineral water Alagir area (46.4% of all stocks in the country), namely the territories relevant to the reserve, and this despite the fact that the territory of North Ossetian State Nature Reserve is only 12.86 % of the area of North Ossetia.
Key words: North Ossetian State Nature Reserve, drinking and mineral water reserve, Kaukaz, Alagir.
Introduction. The Republic of North Ossetia-Alania is situated on the northern depression of the Main Caucasian ridge and is part of the Central Caucasus and Eastern Ciscaucasia between 42° 38' - 43° 50' northern latitude and 43° 25'- 44° 57' east longitude. Its length from north to south is 125 km and from west to east is 120 km. Its area is 7971 km2, of which 4121 sq. km are on the plane. The population of the Republic, according to the State statistics Committee of Russia, is 678.2 thou-
sand people (data as of 2014), and the capital city of Vladikavkaz - 350 thousand people. The Republic of North Ossetia-Alania is one of the most densely populated regions of the Russian Federation and takes on this indicator 5th place (after Moscow, St. Petersburg, Moscow region and Ingushetia). The real density of population in places of residence of the main part is over 140 people/km2. More than half - 56% of the population lives in Vladikavkaz [1].
JOURNAL OF NEW MEDICAL TECHNOLOGIES - 2016 - V. 23, № 3 - P. 230-237
North Ossetia is on the same parallel with Bulgaria, Central Italy and southern France. To the north it borders with the Stavropol region, in the west with the Kabardino-Balkar Republic, on the east with the Chechen and Ingush republics, south of the border goes along the watershed of the Main Caucasian range and borders with the Republic of South Ossetia and with Georgia. The main Caucasian ridge delays the entry to the Republic of North Ossetia-Alania warm and moist air masses from the Black Sea. The impact on the thermal regime of the water balance of the basin of the Caspian Sea, due to its great distance, slightly. The weak impact of the seas caused continental climate with moderately hot and long summer. The vegetation period lasts from may to October inclusive [2].
The mountainous part of North Ossetia-Alania consists of five ridges stretching from north-west to south-east parallel to each other: Woody, Pasturable, Rocky, Lateral and Main. To the north lie the North-Ossetian sloping plain. Its height above sea level decreases in the direction from south to north from 700 up to 400 m. The northern part of the Republic is the Terek-Kuma lowland, which is separated from the southern part of the Sunzha and Terek ranges. There are large differences in climate and moisture mountain and lowland parts of North Ossetia-Alania. In the north of the Republic of features of the continental climate are manifested most strongly. Here is the biggest absolute annual amplitude of temperatures (76°C), absolute lowest winter temperature (-34°C) and maximum summer (+42°C). The area is characterized by a small number of annual rainfall, frequent dry winds and drought. However, the low temperature in the area is rare in the winter, as a rule, is soft, the summer is hot and long [3].
The mild climatetypical for the North-Ossetian sloping plain. Average temperature of January is -4.5°C, in July +20.1°C. Rainfall for the year 600-700 mm. In the mountains cool summer, long and cold winter, less amplitude of fluctuations of temperatures, abundant rainfall [4].
For historical, orographic, soil and climatic conditions of the territory of North Ossetia-Alania is divided into two distinct areas: the mountainous and flat. In turn, these districts are divided into sub-districts. Today plain and Ossetian artesian pool was formed in after Jurassic period (approximately 25-30 thousand years ago) on the basis of Vladikavkaz depression (deflection). Boulder-
pebble deposits fluvioglacial origin were covered by sediments of the Terek river and its many tributaries, river bed gradually moved [5].
The purpose of the study was the analysis of security of the Republic of North Ossetia-Alania drinking and mineral (medicinal and table) water and water for domestic purposes.
Materials and methodology. Apart from literary data [6] were used operational reports of the Centre of water resources of the Republic of North Ossetia-Alania («Center for the study, use and protection of water resources of the Republic of North Ossetia-Alania - URL: http://comready.ru/ company/4534140), Territorial Department of water resources of the Republic of North Ossetia-Alania (Territorial Department of water resources of the West-Caspian basin water management in the Republic of North Ossetia-Alania, abbreviated -TDWR RNO-Alania) and the results of their own field research.
Results and discussion. Within Ossetian artesian basin in the thickness of Quaternary deposits, lies a powerful horizon of underground waters. The power of this horizon occurs mainly in the southern part of the plain, at the expense infiltrate from river beds of the waters. Nutrition also participate rain falling within this plain. The unloading of the horizon is in the northern part of her within tracts Becan and Tuaca.
The depth of groundwater in the area of the cities of Vladikavkaz and Alagir is from 70 to 110 m in the area, Beslan - 50 m, to the north from the village Humalag reduced to zero. The capacity of the aquifer in the southern part of the plain of about 100 m, and in the district, Beslan exceed 180 m. Consumption spring water in the discharge zone is estimated at 20-25 m3/sec. (Becan 15 m3/sec.; Tuaca 5-10 m3/sec). Deposits and lots of fresh underground waters in territory RNO-Alania with approved reserves are shown in table 1.
The number of freshwater springs and their total output in the fourth hydrogeological area are shown in Table 2.
Arrangement of freshwater springs on the territory of North Ossetia-Alania Republic is represented on the map in Figure 1.
List of natural mineral springs of North Osse-tia-Alania shown in Table 3.
Table l
Table 2
Fields of fresh underground waters in the territory RNO-Alania, according to Territorial department of water resources RNO-Alania
Freshwater springs and their total production rate (according to the Territorial Department of Water Resources North Ossetia-Alania)
Waterutility Name fields and sectors of fresh groundwater The reserves, thousand m3/day Yearofapproval stocks
HDW Ordzhonikidzevsky (total) includingsites: 527.в0 1985
Redant 1 210,0 1985
Balta 140,0 1985
Redant 2 13,8 1985
Dlinnodolinsky 14,8 1985
Chmiysky 80,0 1985
IW Yuzgny 70,0 1985
HDW Alagirskoye 25,0 198в
HDW Tamiskskoe 4,1 1972
Gizeldonskaya 30,8 1989
HDW Abstractionborehole 25,0 1989
3 Capturingandsprings 5,8 1989
HDW Ardon 50,0 1973
Beslan (total) includingsites: 73,7 2008
Municipal Unitary Enterprise "Production management of water and sanitation " 20,00 2008
Open Joint Stock Company "Salute" 5,99 2008
HDW+ IW Fayur-Union 8,5 2008
Limited Liability Company "Vladikavkazsky Food Plant of North Ossetia Consumer Union" 0,061 2008
Closed Joint Stock Company "Ariana" 0,085 2008
Company Limited Responsibility "Forward-S" 0,060 2008
HDW Michurinskoe 4,446 2007
IP Iraf (total) includingsites: 0.98 1981
Tagar-totors 0,37 1981
Hoskharanrag-Habal 0,12 1981
IP Gachina 0,22 1981
Regah 0,27 1981
WFI Mikhailovskoe 9.в 1987
WFI Humallag-Zilginskoe (total) including sites: 19.2 1987
Humalagsky 6,4 1987
Zilginsky 12,8 1987
WFI Levoberegnoye 154.1 1979
WFI Veselovskoye 80.2 1979
WFI Kizlyarskoye 25.0 1974
WFI Kievskoye в1.4 1987
WFI Vinogradnenskoe 112.2 1970
HDW NorthChermensky 0.0009 2008
HDW Koban 0.0105 2008
HDW Lots 1 and 2 in the Suburb area RSO-A 28.1 2007
HDW+IW Mozdok 0.140в 2008
Administrative region Number springs Nonsprin gs Total flow rate, l / s Non-springs used for water supply
Alagirsky 83 31-92, 111,11в-118, 119124, 12913в, 147 837 30, 32, 34, 54, 56, 92, 111
Ardonsky 8 103-110 3733 -
Digorsky 2 29-30 45 -
Irafsky 30 1-28, а, б 1014 1,2,14
Kirovsky 4 99-102 7 -
Pravoberegny в 93-98 7 93,95,96
Prigorodny 37 112115,125128,137-1в0,170-174 527 112,113,125,1 26,173
Vladikavkaz 9 1в1-1в9 852 161,163,166,1 68
Total 179 - 7022
Note. Direct deposits are water font, italics - areas of these deposits. HDW - household and drinking water purposes, WFI - water for irrigation (watering), IW - water for industrial purposes, IP - water for irrigation of pastures
Figure 1. Schematic freshwater springs on the territory of North Ossetia-Alania. Scale 1:570 000 (according to the
Territorial Division Water North Ossetia-Alania) Symbols: 1). 2-4 - group of springs, 2). P - Redantskie springs, 3).® - spring Fanykdon, 4). Discharge zone of fresh groundwater basin Ossetianatrezianskogo
Table 3
Natural mineral waters North Ossetia-Alania (according to the Territorial Division Water North Ossetia-Alania)
Names of mineral springs Type of water salt composition Mineralization (M g I l) Output (Q l I s)
Kartasuar Zgil KalakKalak Kamskho Dvuhgolovi Lisri Carbonic с заглавием графы 1.2 - 2.8 0.3-2.5
Bicarbonate-calcium
Sodium
Sodium
Sodium Sodium
Halatsa Carbonate-calcium-sodium 1.8-2.0 0.1-0.5
Abana Carbonic hydro-carbonate-sodium-iron-magnesium 1.8-2.0 0.3-0.5
Tib 1 Carbonic hydro-carbonate -calcium-magnesium 1.0-1.6 0.1-0.5
Bubu Carbonate-hydro-carbonatecalcium 1.2-1.8 0.2-0.4
Kaliat Carbonate-hydro-carbonatecalcium 0.9-1.4 0.1-0.2
Kudzahta Carbonate-hydro-carbonatecalcium 1,4-1,6 0.5-l .5
Zaramag Carbonate-hydro-carbonatecalcium 5-6.5 0.5-1.0
Lyakau Carbonate-hydro-carbonatecalcium 3.2-3.8 0.1-0.2
Tapankau Carbonate-hydro-carbonatecalcium 2.8-3.1 0.05-00.1
Gurkumta Carbonate-hydro-carbonatecalcium 1.8-2.8 0.01-0.05
Narski Carbonate-hydro-carbonatecalcium 2-2.2 0,01-0.05
Hasievsky (Zrug) Carbonate-hydro-carbonate calcium, magnesium 9.4 0.6-1.2
Ginat (Zrug) Carbonate-hydro-carbonate calcium, magnesium 6.8-8.2 0.01-0.02
Zacka Carbonate-hydro-carbonatecalcium 5-5.5 60.1-0.2
Zintsar Chloride-sulphate 7.6-8.8 0.01-0.02
Kalotikau (Hilak) Carbonate-chloride-bicarbonate-sodium, iron, boron, silicon 5-6.0 0.5-0.6
Suar1 Sodiumchloride 11.7 0,005
Zilahar Sodiumchloride 14.6 0.005
Tamisk Hydrogen sulfide-sulfide-calcium-magnesium 0.5-2.5 7.5-20.0
Humesidon Carbonate-bicarbonate-chloride-sodium 1.5 0.05
Tanadon Hydro-bromo-iodine 4.5 0.3
Koltasuar Carbonate-bicarbonate-chloride-sodium 2.7 0.01-0.03
Haznidon Sodiumchloride 4.6-6.1 0.01
Karidon Chloride-sodium-sulphate-calcium 8-12.0 8-9.0
Skottat Chloride-sodium-sulphate-calcium 6.5-6.8 0.05
Masota Carbonate-bicarbonate-chloride-calcium 1.2-1.3 0.1
UpperKarmadon Carbonate-chloride-sodium 0.6- S.5 t=10-60 С0 6.0
Unalsky Sodiumchloride 2.1 0.1
Suargom Sulphate-bicarbonate 1.9 0.2
Chmi Sulphate-bicarbonate 2.5 0.05-0.1
Kesatikau Carbonate-bicarbonate 4.5-4.8 0.1-0.6
Abaytikau Carbonate-bicarbonate 2.8-3.2 0.2-0.3
Dzinaga Carbonate-bicarbonate 1.8-2.4 0.05-0.06
Deposits of mineral waters used are shown in Table 4.
Table 4
Deposits used mineral water (according to the Territorial Department of Water Resources North Ossetia-Alania)
Number Inventories m3/day
map Fig. 2 Namefield (plot) Useofwater
1 Lower-Karmadon 2200 watertreatment
2 UpperKarmadon 178 watertreatment
3 Tamisskoe 492 watertreatment
4 Zaramagskiye 55 watertreatment
5а Tibskoe - Tib-1 97 watertreatment
56 Tibskoe - Tib-2 84 watertreatment, industrialbottling
6 Redantskoe 704 watertreatment
7 Korinskoe 630 watertreatment
S Zamankulskoe, wells 2-3 and 8-3 34 industrialbottling
9 Zamankulskoenewwells in 1991 250 industrialbottling
10 Razdolnoeplot, well 1-M 1081 watertreatment
11 PlotBiragzang (well 1 BT) 484 watertreatment
12 Tsemzavodplot, well 3-T 1080 industrialbottling
13 PlotTibsource 7-56, "Fatima" 250 industrialbottling
Arrangement of sources of mineral water North Ossetia-Alania Republic is represented on the map (Figure 2).
Mip legend: '> Mirer» weter V:::
Mineral waters [»male weals) ». winereE waren Inenrrel sources]
Figure 2. Layout sources deposits mineral waters North Ossetia-Alania. Scale 1:570 000 (According to the regional department of water resources North Ossetia-Alania). Symbols: 1 - mineral water, 2 - single wells, which revealed mineral water, 3 - natural mineral waters
JOURNAL OF NEW MEDICAL TECHNOLOGIES - 2016 - V. 23, № 3 - P. 230-237
The complex analysis of data on security with water resources of all settlements RNO-Alania showed that expected operational resources of underground fresh waters are sufficient for providing both current, and perspective requirement of the population, economic and technical objects for economic drinking water that doesn't contradict earlier published data [7,8].
The total amount of expected operational resources on the republic is estimated at 803 million m3/year. Needs for economic drinking water make about 240 million m3/year. The specified requirement is satisfied due to water selection on fields of underground fresh waters with explored reserves (about 63 % of the general water selection) and on sites of water intakes with unconfirmed stocks.
In the territory of North Ossetia operational stocks on 29 fields of drinking water of 1678.94 thousand m3/days are reconnoitered and approved, from them 13 fields are intended for economic and drinking water supply. In total for economic and drinking water supply it is reconnoi-tered stocks in number of 1086.08 thousand m3/days, for production water supply - 129 thousand m3/days. Other stocks are intended for an irrigation of lands and flood of pastures.
Besides the reconnoitered fields in the republic for economic and drinking water supply and other purposes the borehole water intakes located on sites with not explored reserves are used. The general water selection in the republic in 2011 made 503.35 thousand m3/days or 183.7 million m3/year that makes about 23 % of the total amount of operational resources of the territory RNO-Alania.
The North Ossetian National Natural Park is located in the Alagirsky area RNO-Alania on a northern slope of Big Caucasian ridge within heights of 650-4646 m above sea level. From the North to the south the reserve in whole or in part includes the ridges of the Caucasus: Foothill, Woody, Pasturable, Rocky, Lateral and Main. To NONNP territory, 592 rivers, with a general extent of 831.5 km are related, 76 glaciers with a total area about 37 sq.km are registered. The Tseysky glacier, the largest in the reserve, has the area of 9.7 sq.km and length of 8.6 km. It comes to an end at the height of 2 300 m, in a forest zone. From glaciers the reserve rivers - Ardon (biggest), Arkhondon, Baddon, Bugultydon, Sadon, Fiagdon, Tsazhiudon, and others originate. There are also some lakes -Tsazhiutsad and others. There is a small mineral
lake at the settlement Zgil [9].
In the territory of NONNP there is a large number a little studied, but springs used by the population (Figures 3 and 4).
Figure 3. Springs drinking water on the left - on the left
bank of the Ardon, before entering the first tunnelTranskam (about town Chyramad); Right - on the
left bank of the river Fiagdon, just above her left tributary of the river Tsazhiudon. (Photo Dzod-zikovoy M.E.)
Figure 4.Tsazhiudon Left River - a tributary of the left Fiagdon. Right - a spring of fresh water, 5 meters left of the river Tsazhiudon. (Photo Dzodzikovoy M.E.)
List of mineral springs territories Alagirsky region studied with healing properties is shown in Table 5.
List of mineral springs territories Alagirsky region with poorly known healing properties is shown in Table 6.
Thus, from 179 springs of fresh water registered in the territory RNO-Alania (see. Table 2), the most part - 83 springs, that is 46.4% are on territories of the Alagirsky area, goes further Suburban - 37 (20,7%), Irafsky - 30 (16,8%), Vladikavkaz - 9 (5,02%), the Ar-donsky area - 8 (4,5%), Right-bank - 6 (3,4%), Ki-rovski - 4 (2,2%) and least of all in the Digor area -2 (1,1%).
Table 5
Mineral springs territories Alagirsky region (byDontsov V.I. and Tsogoev V.B. [6])
Table 6
Mineral springs territories Alagirsky region (by Dontsov V.I. and Tsogoev V.B. [6])
As officially used, it is registered 39 natural (see the Table 3) sources of mineral water, from them 25 (64,1%) fall on the territory of the Alagirsky area (seethe table 2). In the territory of NONNP, a security zone and border sites the chemistry of a surface water, dynamics of chemical seasonal changes, influence of waters of various genesis on the frequency of emergence of the induced tumors is comprehensively studied, radi-ometric measurements of the ruslovykh deposits along coast of the rivers and vicinities of mineral sources [10-12] are conducted. At the same time on lands of the Reserve there are more than 70 mineral sources (seethe Table 5) from which it is studied and only 10%, curative properties of 45 registered sources (are used see the Table 6) are insufficiently studied [13-15].
Conclusions. The comprehensive analysis of data on security with water of all settlements of the Republic Northern Ossetia-Alania showed:
1. Expected operational resources of fresh waters are sufficient for ensuring requirement of the population and economic objects of the republic in economic drinking water.
2. It is revealed that most of all stocks of drinking and mineral water it is registered in the Alagirsky area, namely in the territories concerning North Ossetian national natural park and this with the fact that the territory of the reserve makes only 12,86 % of all square RNO-Alania.
3. Profound studying of a chemical composition of water and its therapeutic effect of the North Ossetian national natural park could expand recreational opportunities of these territories significantly.
Mineral water with healing properties insufficiently studied
Name and chemical characteristics of the source Belonging to the River Basin Territorial identity, the name of the gorge Mineralization of water, Q g /1
Kalotikaudon 1 Fiagdon Fiagdonskaya
Hanikomdon2 Fiagdon Fiagdonskaya
Zaramagskiyemineralwater3 Ardon Alagirskoye 3.5-11.2
Nara (Hasievskie)4 Ardon Alagirskoye 0.5-0.7
Zakkinskie5 Ardon Alagirskoye 0.5-0.75
Gurkumta Ardon Alagirskoye
Tapankau Ardon Alagirskoye
Lyakau Ardon Alagirskoye
Ginat Ardon Alagirskoye
Kartasuar Mamyshondon Mamyshonskoe 2.0
Zgil (Kubaladzhy Suar) Mamyshondon Mamyshonskoe 1.1-1.2
Kalak Mamyshondon Mamyshonskoe 1.1-1.5
Kalak 2 Mamyshondon Mamyshonskoe 1.6-2.3
Kamskol Mamyshondon Mamyshonskoe 1.5-2.8
Kamskho 2 Mamyshondon Mamyshonskoe 1.6-3.0
Dvuhgolovi Mamyshondon Mamyshonskoe 1.6-2.5
Lisri Mamyshondon Mamyshonskoe 0.8-3.6
Halatsa contains boric acid (H3BO3) and 150 mg / l, and silicon (Si) 23,4 mg / l Mamyshondon Mamyshonskoe
Abana (2 sources)6 Mamyshondon Mamyshonskoe
Tibskie - 1, 2, 4 Mamyshondon Mamyshonskoe 8.7-6.4
Bubu Mamyshondon Mamyshonskoe 1.2-1.8
Kaliat, carbonic sodium-calcium bicarbonate. Mamyshondon Mamyshonskoe
Kudzahta Mamyshondon Mamyshonskoe 1.6.0
Zintsar, sulphate-sodiumchloride. Ardon Alagirskoye
Unalsky Ardon Alagirskoye 2.1
Healingmineralsprings
Name and chemical characteristics of the source Belonging to the River Basin Territorial identity, the name of the gorge Mineralization of water, Q g / l
"Tib-1", carbonate-bicarbonate-sodium-calcium medical-table water Ardon Alagirskoye 4.16
"Tib-2", bicarbonate, magnesium-calcium, medical-table water Ardon Alagirskoye 1.38
"Zaramag" chloride-bicarbonate-sodium, medical-table water Ardon Alagirskoye 5.98
"Tsey" sodium chloride, medical-table water Ardon Alagirskoye 5.52
"Hilak" medical-table, boric sredneuglekislaya, ferruginous water of low mineralization Ardon Alagirskoye 1.79
"Biragzang" medical-table water. GOST 13273-88 Ardon Alagirskoye 2.1
"Sadon" medical-table, sulphate-sodium bicarbonate water Ardon Alagirskoye 0.71
"Tamisk" medical-tablewater Ardon Alagirskoye 1.08
Note.1 has 2 outputs the river Bugultadon, 2 follows the northern outskirts of the village Dallagkau3 has 18 wells, 4 has 6 sources, 5 has 6 sources, 6 carbonated mineral water
Литература
1. Official portal of the Republic of North Ossetia -Alania / Administration of the Head of the Republic of North Ossetia-Alania and the Government of the Republic of North Ossetia-Alania. About Republic. Geographical Position. Mode of access: http://www.rso-a.ru/ (May 26, 2014).
2. Grigorovich S.F. The mountains and plains of North Ossetia: Satellite tourist, local historian and sightseers. 2nd edition, revised, Ordzhonikidze North Ossetian Book Publishers, 1960. 128 p.
3. Beroev B.M. North Osetii. Moscow: Physical Education and Sports, 1984. 144 p.
4. Amirkhanyan A.M. North Ossetian State Reserve. Ordzhonikidze. Ir., 1989. 104 p.
5. Kovalev P.V. Patterns of development of glaciation in the Greater Caucasus. / Abstract for the degree of Doctor of Science. Moscow, 1966. 95 p.
6. Dontcov V.I., Tsogoev V.B. Natural Resources of the Republic of North Ossetia-Alania. Water resources. Vladikavkaz: Projects Press, 2001. 367 p.
7. Phallagova D.M. Mineral waters of North Ossetia and their chemical characteristics. Vladikavkaz. Ir., 1992. 207 p.
8. Dzodzikova M.E. Mineral springs of North Ossetian State Natural Reserve. / Proceedings of the scientific -practical conference "The role of protected areas in the sustainable development of North Ossetia.". Vladikavkaz, 2011. P. 35-41.
9. Dzodzikova M.E. Water resources of North Ossetia Reserve, problems and improvement of the ecological situation. / Proceedings of the 10th International Congress "Environmental and children." - Anapa. Spa Association "Change", 2013. P. 303-305.
10. Dzodzikova M.E., Pogosyan A. Rivers and glaciers of the North Ossetian Nature Reserve. / Collection of scientific papers on the 75th anniversary of B.M.Beroeva "Mountain regions: XXI Century". Vladikavkaz. North Ossetian State University K.L. Khetagu-rov, 2011. P. 175-179.
11. Dzodzikova M.E., Pavlova, I.G., Gabaraeva V.M. Effect of treatment of various origins on the incidence of mammary tumors in rats induced by methyl-nitroso-urea. / Proceedings of the 7th International Conference "Sustainable development of mountain areas in the context of global change". Vladikavkaz. North-Caucasian Mining and Metallurgical Institute (State Technical University), 2010. P. 124-125.
12. Dzodzikova M.E., Tedeyev T.G. Radiometric measurements of channel deposits in the valley of the rivers and Zymagondon Mamyshondon. / Proceedings of the I-th International scientific conference "Regional Development in the 21st Century". Vladikavkaz. - North Ossetian State University K.L.Khetagurov, 2013. P. 170-172.
References
Official portal of the Republic of North Ossetia -Alania / Administration of the Head of the Republic of North Ossetia-Alania and the Government of the Republic of North Ossetia-Alania. About Republic. Geographical Position. Mode of access: http://www.rso-a.ru/ (May 26, 2014). Russian
Grigorovich SF. The mountains and plains of North Ossetia: Satellite tourist, local historian and sightseers. 2nd edition, revised, Ordzhonikidze North Ossetian Book Publishers; 1960. Russian.
Beroev BM. North Osetii. Moscow: Physical Education and Sports; 1984. Russian.
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