ANNUAL AND SEASONAL VARIATIONS OF INDOOR RADON CONCENTRATION

IN SKOPJE (REPUBLIC OF MACEDONIA)

Stojanovska Zdenka1,*, Boev Blazo2, Ristova Mimoza3, Žunić S. Zora4, Zoran Curguz5 Januseski Jovan6

1,* Faculty of Medical Sciences, Goce Delcev University, Stip, Republic of Macedonia2Faculty of Mining, Geology and Polytechnic, Goce Delcev University, Stip, Republic of Macedonia3 Institute of Physic, Faculty of Natural Sciences and Mathematics, University in Skopje, Republic of Macedonia4ECE Lab, Institute of nuclear sciences "Vinča", University of Belgrade, Serbia5Faculty of transport Doboj, University in East Sarajevo, Republic of Srpska6Institute for Public Health of RM, Laboratory for radioecology Skopje, Republic of Macedonia

Introduction The pathway for radon generation in rock and soil to its

indoors accumulation is controlled by a number of geogenic and anthropogenic factors, which leads to a large temporal and spatial variability.

The seasonal variability of the indoor radon on the territory of Republic of Macedonia, confirmed its regional distribution character. Furthermore, geological diversity of the Country contributes to the large scale of spatial variations.

In order to clarify variation and factors which enable to affecting the indoor radon concentration the results of indoor radon concentration, measured in Municipalities of Skopje, are analyzed observed and discussed.

Study area Skopje is the capital and largest city of the

Republic of Macedonia located in the northern part of the Country, in the center of the Balkan Peninsula, covering an area of 571.46 km2. According to State Statistical Office, the territory is organized into ten municipalities, with a total population of 506 926.

The center of Skopje is located at an elevation of 225 m with highest altitude of 1066 m above sea level.

The summers are hot and humid, while the winters are cold, wet, and often snowy.

Study area With respect to the geology, Skopje belongs to

the geotectonic Vardar zone, which is mainly composed of Neogene–Quaternary sediments.

Its surface is formed at the intersection between NW-SE and E-W trending deep Mesozoic magmatic structures.

Skopje lies over a weak, highly porous zone, also associated with high seismic activity in that region.

Methodology Skopje municipalities:

Aerodrom (1), Butel (2), Cair (3), Centar (4), Gazi Baba (5), Gjorce Petrov (6), Karpos (7), Kisela Voda (8), Saraj (9), Suto Orizari (10)

Indoor radon concentrations were measured in 124 randomly selected dwellings of 10 municipalities through the entire Skopje area.

In each dwelling, a detector was placed either in a bedroom or a living room, depending on where residents spent most of their time, at a height of 1 to 1.5 m above the floor, at a distance greater than 0.5 m from each wall, and at a minimum of 20 cm from any other object.

Detectors RSKS detector consisted of CR-39 chip placed in a

25mm x 40mm cylindrical diffusion chamber. The RADUET detector was used for simultaneous

detection of radon and thoron activity. It consisted of two detector chips CR 39, fixed in the pot section of two diffusion chambers (60mm x 30mm). The main chamber was sensitive to radon, whereas the secondary chamber was sensitive to both, radon and thoron. The detectors were exposed in the following periods:

• December 2008 - February 2009 (winter period), • March – May, 2009 (spring period); • June – August, 2009 (summer period) and • September – November, 2009 (autumn period).

Upon the exposition of the measuring time (3 mouths), the detectors were collect; the Cr-39 chips were etched in 25% NaOH solution at 92°C for 4-5h.

Results The results are ranged from 18 to 502 Bq m−3 of

which 112 dwellings revealed indoor radon concentrations lower than 200 Bq m−3.

0

10

20

30

40

50

60

1 2 3 4 5 6 7 8 9 1 11 12

Annual radon concentration (Bq m-3)

Frequency

0 100 200 300 400 500 600 Annual radon concentration (Bq m-3)

Histogram of annual indoor radon concentration

The municipalities geometric mean values are significantly different (ANOVA, p=0.021). The annual indoor radon concentration was found to be higher in Gazi Baba than for Centar (p=0.001), Karpos (p=0.001), Kisela Voda (p=0.003), Gorce Petrov (p=0.027) and Aerodrom (p=0.031) as well as the higher values in Butel than Centar (p=0.027) and Karpos (p=0.033) were found to be.

Annual indoor radon concentration

0

50

100

150

200

250

Aerodrom Butel Cair Centar GaziBaba

GjorcePetrov

Karpos Kiselavoda

Saraj SutoOrizari

CR

n (B

q m

-3)

withaut basemnt

with basemnt

1.5

1.6

1.7

1.8

1.9

2.0

2.1

2.2

ground first

log1

0C

Rn

(Bq

m-3

)

without basemen

with basement

Influence of the building characteristics to the indoor radon concentrations

The influence of the presence/absence of basement is significant only for the ground floor values.

Geometric mean value of indoor radon concentration in the ground floor in houses with and without basement in the municipalities

Influence of the building characteristics to the indoor radon concentrations

1.51.61.71.81.92.02.12.22.3

groundfloor withbasement

groundfloor

withoutbasement

first floorwith

basement

first floor-without

basement

log1

0C

Rn (Bq

m-3

) central / electrical

solid fuel

The influence of the type oh heating is significant only for the ground floor level.

Geology

The annual indoor radon concentration in the ground floor dwellings were classified according to lithology .From the Basic geological map of the Republic of Macedonia 1:200 000 (Basal series-conglomerates, limestone, Quartz-sericit biotit and shale, Aluvium, Deluvium-proluvium and Conglomerate and sandstones, marls, clay)

Seasonal variation of indoor radon

0

50

100

150

200

250

Aerodrom Butel Cair Centar GaziBaba

GjorcePetrov

Karpos Kiselavoda

Saraj SutoOrizari

CR

n (B

q m

-3)

winter

spring

summer

autmn

Geometric mean values of indoor radon concentration in the municipalities of Skopje, measured in different season.

Seasonal correction factors

y = 0.8596x + 0.1465

R2 = 0.9325

0

0.5

1

1.5

2

2.5

3

1 1.5 2 2.5 3

log10CRa-winter

log1

0C

Ra-a

nnua

l

y = 0.8985x + 0.2359

R2 = 0.8494

0

0.5

1

1.5

2

2.5

3

1 1.5 2 2.5 3

log10CRa-spring

log1

0C

Ra-a

nnua

l y = 0.7819x + 0.6167

R2 = 0.64350

0.51

1.52

2.53

3.5

1 1.5 2 2.5 3

log10CRa-summer

log1

0C

Ra-a

nnua

l

y = 0.8367x + 0.3024

R2 = 0.8537

0

0.5

1

1.5

2

2.5

3

1 1.5 2 2.5 3

log10CRa-autumn

log1

0C

Ra-a

nnua

l

In order to derivate seasonal correction factors for Skopje, the pattern of seasonal variation of indoor radon concentration was analyzed using the data of the seasonal measurements in all dwellings. It was found that a liner function best fits the correlation of annual indoor radon concentration and indoor radon seasonal measurements.

Conclusions The annual mean indoor radon concentrations obtained

for the studied area varies from 18 to 502 Bq m−3, which indicate that in some dwellings indoor radon concentration is not negligible. In general, significant difference between annual mean in different municipality were observed.

The building characteristic: floor level, presence /absence of basement and type of heating significantly affecting a indoor radon concentration. The indoor radon concentration is generally higher in ground floor in houses without basement which use solid fuel type of heating

Seasonal variation of indoor radon concentration is an important factor, were modeled by linear function.

Thanks for your attention!