MONITORING OF RADIONUCLIDES IN ... - Terviseamet
MONITORING OF RADIONUCLIDES IN ... - Terviseamet
MONITORING OF RADIONUCLIDES IN ... - Terviseamet
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GEOLOGICAL SURVEY <strong>OF</strong> ESTONIA<br />
<strong>MONITOR<strong>IN</strong>G</strong> <strong>OF</strong> <strong>RADIONUCLIDES</strong> <strong>IN</strong><br />
GROUNDWATER <strong>OF</strong> ESTONIA<br />
RE<strong>IN</strong> PERENS<br />
LEHTE SAVITSKAJA
HYDROGEOLOGICAL MAP <strong>OF</strong> ESTONIA
THE OBJECTIVES <strong>OF</strong> THE NATIONAL<br />
GROUNDWATER <strong>MONITOR<strong>IN</strong>G</strong><br />
- to survey the state of natural groundwater resources<br />
(water supply supply,<br />
, chemical composition, etc.)<br />
-to to monitor the changes (groundwater quality, water table,<br />
water supply) caused by human activities<br />
-to to obtain the information necessary for decision-making<br />
decisio making<br />
on national level and for international co-operation.<br />
co operation.<br />
-help help to elaborate recommendations for the future<br />
at reducing the impact of human activities.
Methodical basis<br />
The total indicative dose of year is<br />
calculated calculate according to European Union<br />
drinking water directive 98/83/EC and<br />
96/29/Euratom recommendations recommendations<br />
from<br />
the results determination 226 226Ra, Ra, 228 228Ra, Ra,<br />
234 U, and 238 238U. U.<br />
Percentage<br />
ercentage of dissolved isotopes of<br />
uranium during the constitution of the<br />
total indicative dose very small (99% of TID constitute<br />
account of 226 226Ra Ra and 228 228Ra. Ra.<br />
Natural radioactivity of the groundwater<br />
is mainly related with the radioactivity of<br />
waterbearing rocks.
Water samples have analysed in<br />
laboratories<br />
Latvian Testing Laboratory of Material<br />
Radioactivity. Laboratory is determining the<br />
dissolution in water of 226 226Ra Ra and 228 228Ra, Ra, but not<br />
concentration of 234 234U U and 238 238U. U.<br />
Laboratory of Radiation and Nuclear Safety<br />
Authority of Finland ( STUK ). Analyses of 226 226Ra Ra ,<br />
228 Ra, 234 U and 238 U.<br />
Radium Institute of St.Petersburg<br />
St. Petersburg<br />
Radiation Protection Centre of Estonia<br />
Institute of Physics University of Tartu
The groundwater bodies of Quaternary aquifer<br />
system
The groundwater bodies of Devonian aquifers
The values of radionuclides and total indicative<br />
dose (TID ) in groundwater of Devonian aquifers
The groundwater bodies of Silurian- Silurian Ordovician<br />
aquifer system
The values of radionuclides and TID of<br />
groundwater of S-O S aquifer system
The distribution of Ordovicin-Cambrian Ordovicin Cambrian aquifer
The values of radionuclides and TID of<br />
groundwater of Ordovician-Cambrian Ordovician Cambrian aquifer
The groundwater bodies of Cambrian-Vendian<br />
Cambrian Vendian<br />
aquifer system
The changes of the groundwater abstraction and<br />
potentiometric levels of Cambrian-Vendian<br />
Cambrian Vendian aquifer<br />
system
The values of radionuclides and TID of<br />
groundwater of Cambrian-Vendian<br />
Cambrian Vendian aquifer system
The values of radionuclides and TID of<br />
groundwater of Voronka aquifer
The values of radionuclides and TID of<br />
groundwater of Gdov aquifer
Concentrations of 210 210Po Po and 210 Pb in<br />
groundwater of Cambrian-Vendian<br />
Cambrian Vendian aquifer system
Concentration of radionuclides and TID in<br />
groundwater of Cambrian-Vendian<br />
Cambrian Vendian aquifer system
Biggest explored concentration of<br />
radionuclides in the groundwater of<br />
Cambrian–Vendian groundwater body is<br />
probably related with big concentrations of<br />
radioactive substances what are occurring at<br />
times in weathering part of crystalline<br />
basement (granite, gneiss, ) in bedrock. They<br />
are with primal origin.
In nowadays the groundwater of Cambrian–Vendian<br />
Cambrian Vendian quifer<br />
system is enriching with radioactive substances thanks to<br />
inflow of the pressuring groundwater of the crystalline<br />
basement
The concentration of radionuclides is lower in area of<br />
buried valleys, where recharge of Cambrian–Vendian<br />
Cambrian Vendian<br />
groundwater body occur with infiltration water.
MODULATED <strong>IN</strong>DICATIVE DOSE <strong>OF</strong> GROUNDWATER<br />
<strong>OF</strong> CAMBRIAN-VENDIAN CAMBRIAN VENDIAN GROUNDWATER BODY
The biggest concentration of radium has been got<br />
in the so-called so called relict water of Cambrian–Vendian<br />
Cambrian Vendian<br />
groundwater body in surroundings of Maardu
Simulated total indicative dose of groundwater of<br />
Cambrian-Vendian<br />
Cambrian Vendian aquifer system
Correlation between the TID and the concentration<br />
of Chlorides in groundwater of Cambrian- Cambrian<br />
Vendian aquifer system
Correlation between the TID and the concentration<br />
of sodium in groundwater of Cambrian-Vendian<br />
Cambrian Vendian<br />
aquifer system
Changes of the chemical composition of the groundwater<br />
of Cambrian-Vendian<br />
Cambrian Vendian aquifer system in Tallinn
Total indicative dose in groundwater of Cambrian- Cambrian<br />
Vendian aquifer system
222 Rn)<br />
Radon ( 222Rn)<br />
Radioactive exposure to radon takes place<br />
by inhalation and accounts for half the<br />
average dose for a human being<br />
The highest concentration of radon<br />
determined in groundwater of Estonia is<br />
45 Bq/l<br />
It does not pose a high risk in drinking<br />
water as it escapes easily after aeration of<br />
the water
Tritium ( 3H) H)<br />
Concentration of tritium ( 3H) H) in<br />
groundwater is prevalently related<br />
human caused radiological<br />
contamination and less with cosmic<br />
emission.<br />
Taking into consideration<br />
groundwater’s very good protection,<br />
big concentration of tritium is not<br />
probable in Estonian groundwater.
Conclusions<br />
From the showed table appears that only<br />
16% % from the explored water of wells<br />
correspond about the total indicative dose<br />
on the requirement of the drinking water<br />
(0,1 mSv/year).<br />
mSv/year).<br />
By the data of explored wells of<br />
Cambrian–Vendian<br />
Cambrian Vendian aquifer system, system,<br />
the<br />
total indicative dose is at the most (66%) (6 %)<br />
between 0,10–0,40<br />
0,10 0,40 mSv/year mSv/year<br />
Concentration of tritium ( 3H H ) in<br />
groundwater of Cambrian-Vendian Cambrian Vendian aquifer<br />
system is low, usually less than 10 Bq/l
In all ll others groundwater bodies and<br />
aquifer systems , witch occur in<br />
Estonia (Ordovician– (Ordovician Cambrian,<br />
Silurian–Ordovician, Silurian Ordovician, Devonian and<br />
Quaternary) Quaternary , the groundwater<br />
accords to limits of drinking water by<br />
the total indicative dose, it means<br />
that TID is lower than 0,1 mSv/year.<br />
mSv/year.
The water of Cambrian–Vendian<br />
Cambrian Vendian<br />
aquifer system not corresponding to<br />
requirement of quality about the<br />
drinking water in part of the total<br />
indicative dose, is problem because<br />
this groundwater are using in<br />
community of water supplies all<br />
West-, West , North- North and East-Estonia East Estonia areas<br />
From all water necessary using 35 %<br />
is satisfying exactly with this aquifer<br />
system
Caused from that Estonian<br />
Groundwater Commission made<br />
proposal to Social Minister to allow to<br />
use groundwater of the Cambrian–<br />
Cambrian<br />
Vendian aquifer system as drinking<br />
water if from this coming annual<br />
indicative dose to 0,2 mSv/ mSv year.<br />
It will be necessary to establish the<br />
continuous programme for<br />
monitoring of radionuclides.<br />
It will be necessary to provide<br />
intercalibration of laboratories
Unified solution is probably missing.<br />
First of all should be analyzed<br />
already existing water intake<br />
possibilities. If in water intake is with<br />
different depth wells, opening to<br />
Cambrian–Vendian<br />
Cambrian Vendian aquifer system, system<br />
and becomes evident that from<br />
upper aquifer (Voronka ( Voronka) ) opening<br />
wells is possible to get drinking<br />
water which corresponds to<br />
requirement of quality, then existing<br />
water intake should be rebuilded.<br />
rebuilded.
It is necessary to weigh in one’s<br />
mind possibilities of mixing different<br />
aquifers water, specially where could<br />
be possible to use Ordovician–<br />
Ordovician<br />
Cambrian or others upper aquifers<br />
water in proportion, what would<br />
assure the quality of drinking water<br />
accordance to requirement.
From the above-said above said would be<br />
necessary to make in working water<br />
intakes exhaustive analysis for<br />
utilizing optimal solutions in<br />
Cambrian–Vendian<br />
Cambrian Vendian aquifer system, system,<br />
what with time would be vastly<br />
economical from the closing existing<br />
water intakes, observation new<br />
drinking water sources and building<br />
intakes..
Thank you for<br />
your attention