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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

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