natural radioactivity in zambian building materials collected from lusaka
TRANSCRIPT
J.RADIOANAL.NUCL.CHEM.,LETTERS 199 (3) 229-238 (1995)
NATURAL RADIOACTIVITY IN ZAMBIAN BUILDING MATERIALS COLLECTED FROM LUSAKA
P. Hayumbu, M.B. Zaman, N.C.H. Lubaba*, S.S. Munsanje, D. Muleya**
Nuclear Analytical Laboratory, National Council for Scientific Research,
P.O. Box 310158, Lusaka, Zambia
*Buildinq and Industrial Minerals Research Unit, National Council for Scientific Research, Zambia
**Radiation Protection Services, Ministry of Health, Zambia
Received 12 September 1994 Accepted 24 September 1994
Samples of natural and manufactures building materials collected around Lusaka have been analyzed for natural radionuclides using y- spectrometry. A simple comparison of the specific radioactivities of primordial radio- nuclides in these materials to the world av- erages for soil (25 Bq kg-1 238U, 25 Bg kg-1 232Th, 370 Bq kg -I 40K and 89 Bq kg-1Raeq ) shows that, of the nine types of samples analyzed, only burnt clay bricks (for 238U, 232Th and 4UK), cement roofing tiles (for 238U), building and river sands (for 232Th and 40K) have greater activities than does soil. Radiological evaluation of specific radioactivities in these materials indi- cates that all materials meet the external y-ray dose limitation of 1.5 mSv y-l, that is, all samples have a radium equivalent activity of less than 370 Bq kg -1.
229 Elsevier Science S. A,, Lausanne Akad~miai Kiad6, Budapest
HAYUMBU et al.: NATURAL RADIOACTIVITY IN BUILDING MATERIALS
INTRODUCTION
Knowledge of radioactivity levels in building and
ceramic materials is vital in the assessment of possible
radiological hazards to human health. It is required for
setting up manufacturing standards and guidelines for
the use of these materials. Thus specific radioactivity
of natural building materials and those derived from
industrial wastes and by-products have been reported in
many countries I-4
Levels of natural radioactivity in Zambian building
materials have hitherto not been measured. With this
preliminary task unsolved, it is no wonder that at the
moment Zambia has neither standards nor guidelines pre-
senting the acceptable levels of radioactivity in these
materials.
This paper presents results of a y-spectroscopic de-
termination of 238U, 232Th and 40K in major building
materials used in Lusaka, the Capital of Zambia (where
about 10% of the total population, that is, 25% of the
urban population of the country resides). The results,
on a qualitative basis, are compared to the world aver-
age natural radioactivity levels in soil and are further
discussed on the basis of a criterion formula for accept-
able radiation dose rates attributable to building mate-
rials in developed countries I . This work is part of an
ongoing program for radioactivity monitoring in food and
environmental samples being undertaken by the National
Council for Scientific Research and the Radiation Pro-
tection Services.
230
HAYUMBU et al.: NATURAL RADIOACTIVITY IN BUILDING MATERIALS
TABLE I
Samples of building materials analyzed and their sources
Sample Sample name Source No.
I
2
3
4
5
6
7
8
9
Portland cement
Stone aggregates
Stone aggregates(b)
Concrete blocks
Burnt clay bricks
Cement roofing tiles
Asbestos roofing sheets
Building sand
River sand
Chilanga Cement Ltd.
Crushed Stones Ltd.
United Quarries Ltd.
United Quarries Ltd.
Brick and Tile Ltd.
Ital-Terrazo Ltd.
TAP Ltd.
Kasisi
Kafue
EXPERIMENTAL
Materials
The materials analyzed were river sand, aggregate
stones, cement, roofing tiles, asbestos sheets, burnt
clay bricks, concrete blocks and building sand (Table I).
There is little or no utilization of industrial wastes
in s Zambian construction industry, unlike in the case
of developed countries. This is because the industrial
infrastructure outside the mining centers is rather
small and wastes thereof are not major building materi-
als.
Samples after collection were crushed, pulverized to
a fine powder (<300 mesh) and homogenized in preparation
for spectral collection. A weighed quantity of powdered
sample sufficient to fill a 250 ml cup was used for y-
231
HAYUMBU et al.: NATURAL RADIOACTIVITY IN BUILDING MATERIALS
ray counting. The cup was sealed and left to stand
alone for a month to let the sample attain radioactive
equilibrium 5'6. Spectra of samples were collected using
a high resolution y-spectrometry system described pre- 7
viously .
Methods
The significant primordial radionuclides in building
materials are 238U, 232Th and 40K. Since 98.5% of the
radiological effects of the uranium series are produced
by radium and its progeny, the contribution of 238U and
the other 226Ra precursors are normally ignored 1. The
226Ra (or 238U for samples assumed to be at radioactive
equilibrium like in this work) and 232Th radioactivities
were estimated from 609.3 keV and 583.1 keV y-lines of
214Bi and 208TI, respectively 7. Alternatively, one could
use the 214pb (351.9 keV) and 228Ac (911.1 keV) y-lines.
40K radioactivities were determined using the 1.46 MeV
y_line 1,8,9
Spectral analysis was done using GANAAS I0 whose pro-
gram modules end with a report of activities of radio-
nuclides evaluated according to Eq. (I).
C a
A : -- (I) a s
Y
where A a - is the activity of the radionuclide (Bq),
- is the detector efficiency for the analyti-
cal y-line,
P - is the absolute transition probability of Y
y-decay through the analytical y-line, and
C - is the count rate of the radionuclide for a the analytical y-line (cts s-l).
~2 ~2
HAYUMBU et al.: NATURAL RADIOACTIVITY IN BUILDING MATERIALS
Specific activities of radionuclides in analyzed
samples result when activities derived from Eq. (I)
are divided by.the mass of the sample as shown by
Eq. (2). A a
A = s M s
(2)
where A s
M s
- is the specific activity of the sample (Bq kg 1)-
and
- is the mass of the sample (kg).
In order to radiologically compare the specific radio-
activities of building materials which contain Ra, Th and
K, a common index called the radium equivalent activity
Ra was used I . The radium equivalent activity is a eq
weighted sum of activities of the above three radio-
nuclides based on the estimation that 370 Bq kg -I 226Ra,
259 Bq kg -I 232Th or 4810 Bq kg -I 40K produce the same
y-ray dose rates given by Eq. (3).
Raeq = 370 + + 4810 (3) or
Raeq = ARa + (AThX 1.43) + (AKX 0.077) (3a)
where232Th ARa,40ThA and A K are the activities of 226Ra,
and K, respectively, in Bq kg -I.
RESULTS AND DISCUSSION
Table 2 lists the measured activities of 238U, 232Th
and 40K for the collected samples (serial numbers I to
9) along with Raeq calculated using Eq. (3). The Table 2
233
HAYUMBU et al.: NATURAL RADIOACTIVITY IN BUILDING MATERIALS
TABLE 2
-I Specific activities of building materials (Bk kg )
Sample Sample name 238 u 232Th 40 K 226N~ N o . eq
I. Portland cement
2. Stone aggregate
3. Stone Aggregate(b)
4. Concrete blocks
5. Burnt clay bricks
6. Cement roofing tiles
7. Asbestos roofing sheets 15•
8. Building sand 25•
9. River sand
10. Clays bricks 12 12
11. Tiles
12. Sand bricks 12
13. Cement plaster 12
14. Unmixed cement 12
15. Carbonate rock 11
16. Soil 11
23• 32• 134• 79•
6• 6• 111• 8 23•
5• 12• 37• 8 25•
7• 10• 43• 8 25•
32• 81• 412• 180•
55• 21 • 116• 94•
24• 149• 8 61 • 5
26• 714• 7 117•
16• 44• 971• 154•
59• 96•
52• 81•
44• 44•
48• 26•
11 26
2 8 74 19
25 25 370 89
includes, for comparison, values of radioactivities in
similar samples (serial numbers 10 to 16) reported in the
literature. Although two samples, especially if they are
from different locations, are unlikely to be identical,
it may be seen that values of radioactivities found by
us are comparable to reported results. For example, the
activities of 238U and 232Th in our Portland cement
(serial number I) are within the range of values reported
for cement plaster (serial number 13) and unmixed cement
(serial number 14). Cement being a mixture of minerals,
the radioactivities in different cement samples are
234
HAYUMBU et al.: NATURAL RADIOACTIVITY IN BUILDING MATERIALS
likely to vary, depending on the radioactivities of the
component minerals.
Table 3 has been compiled to show the radioactive
status of Zambian building materials in comparison to
those of other countries. As stated earlier and shown
in the table, the radioactivities in building materials
do vary from one place to the other. If we consider the
case of stone aggregates, the Ra value is 24 for Zambia eq
(Lusaka), 115 for Australia, 322 for Germany, 74 for
Norway, 141 for Sweden and 59 for U.K. It should be
stressed here that even these values are not the repre-
sentative values for the countries mentioned but for the
localities from where the samples had been collected I .
The ultimate objective of measuring radioactivities
in building materials is to make an estimate of radia-
tion dose likely to be delivered externally if a building
is constructed using them. To limit the radiation dose
from building materials to 1.5 mSv y-l, a number of mod-
els have been suggested by various workers. One such
model, proposed to serve as a criterion in the then Fed-
eral Republic of Germany at the beginning of the 1980s I,
was
IIARa ATh AK } ~7 -T6 +-T+ TT6 <1 (4)
This criterion, which only considers the.external
hazard due to y-rays corresponds to a maximum radium
equivalent activity of 370 Bq kg -I for the material.
From Table 2, it is apparent that Zambian materials meet
this criterion. Table 3 shows that building materials
used in Lusaka have comparable levels of radioactivity
to natural building materials used in other countries
calculated on the basis of Eq. (4).
235
H A Y U M B U e t al . : N A T U R A L R A D I O A C T I V I T Y I N B U I L D I N G M A T E R I A L S
,-.t
-,-t
O ~ 0
5 - , , t : : a~
0 0 -~0
I1)
-,-4 0
m O ol
.,-4 -~
O m
~ -,..t -,.-t ~
r~
0
0 ffl
.,-t
0
~400
0 r 0"~ O~ ~1 ~ I ~
I.~ ~ 0") ~'~ ~ ~.0 ~ ~l ~ ~
0 0 L~
~ ~ ~ ~ ~ 0
t.r ~.o o oo
t~ ~.o
-I~ �9 m ,-~ ,--I t~ 0 -,--I
,-'4 .;-I 4a
0 O~ l~ ~ ~ 0 ul
0 --4 ~ l:l ~ ~ "0 4a ~ 0
4-4 0
.IJ o
0
I
,Q
r~
0 t~
0
0
0 0
o
0
,nl m
,--4 t0 �9
r~
0 - , - I
~ . q .,-I 0
o O
o 0 ~
-,-I o ~4
4-) �9 o~ D~
.,-4 0
2 3 6
HAYUMBU et al.: NATURAL RADIOACTIVITY IN BUILDING MATERIALS
It should, however, be pointed that addressing the
radiation hazard to respiratory organs due to radon and
its progeny requires reduction of the acceptable maximum -I
Ra to at most 185 Bq kg (Refs (I)-(3)). It is note- eq
worthy thatthis limitation coincides with our qualita-
tive comparison of activities of building materials to
the world average for soil which has an Ra of 89 -I eq
Bq kg (Table 2). In this work we do not discuss inter-
nal exposure because radon concentrations in dwelling
places depend on many factors such as air-flow patterns,
air changes, types and porosity of materials used.
CONCLUSION
The results show that of the nine samples of building
materials analyzed, six of them had Ra activities less eq
than, or comparable to the value calculated for world
average in soil (89 Bq kg-1). The material with the
highest Raeq activity (burnt clay bricks) has twice the
world average value. The results also show that Zambian
building materials meet the criterion limiting the radia-
tion dose from building materials to 1.5 mSv y I (Ref.
(I)). Follow-up studies of direct radon measurements as
well as those using dose limitation models in dwellings
built with these materials will be carried out in order
to ascertain internal radiation exposure.
The authors acknowledge with thanks the companies
which supplied the building materials used in this study.
We would also like to thank the Secretary General of
NCSR for his support during the course of this work.
237
HAYUMBU et al.: NATURAL RADIOACTIVITY IN BUILDING MATERIALS
REFERENCES
I. J. Beretka, P.J. Mathew, Health Phys.~ 48 (1985) 87.
2. G.A. Swedjemark, Health Phys., 51 (1986) 569.
3. W.F. Passchier, Klijn, Van der Heijde, Health Phys., 51 (I 986) 661.
4. A.S. Paschoa, R.R. Pinho, D.A.C. Binns, Monitoring Radon and Environmental Gamma Radiation Indoors and Outdoors at PUC/RJ, Brazil; Proceedings of the Inter- national Workshop on Radon Monitoring in Radioprotec- tion, Environmental Radioactivity and Earth Sciences, (Eds by L. Tommasino, G. Furlan, H.A. Khan, M. Monnin) ICTP, Trieste, Italy, April 3-14, 1989, 381.
5. A. Canet, R. Jacquemin, Methods of Measuring Radium Isotopes: Gamma Spectrometry; Technical Report Series No. 310, Environmental Behaviour of Radium, Vol. I, IAEA, Vienna, 1990, p. 196.
6. G. Smithson, Sampling and Selection of Analytical Methods for Radium; Technical Report Series No. 310, Environmental Behaviour of Radium, Vol. I, IAEA, Vienna, 1990, p. 267.
7. M.B. Zaman, P. Hayumbu, S.S. Munsanje, Int. J. Bio- ChemiPhysics, 2 (1993) 143.
8. Technical Report Series No. 295, Measurement of Radionuclides in Food and Environment, IAEA, Vienna, 1990, p. 63.
9. F. Steger, Final Report: Setting up a Radiation Pro- tection Laboratory for Environmental, Foodstuff and Internal Monitoring at the Radiation Protection Ser- vices, IAEA, Vienna, 1990, p. 11-12.
10. Computer Manual Series No. 3, Nuclear Analysis Soft- ware; Part 2: Gamma Spectrum Analysis, Activity Cal- culations and Neutron Activation Analysis (GANAAS), IAEA, Vienna, 1991.
11. P. Linsalata, Radiat. Phys. Chem., 34 (1989) 241; Int. J. Radiat. Appl. Instrum., Part C.
12. R.H. Mahat, Y.M. Amin, J. Radioanal. Nucl. Chem., Lett., 144 (1990) 375.
238