Radioecological Situation in the Cooling Pond of Chornobyl NPP
Oleg NASVIT
Research Innovative Implementation Enterprise “Stroom”, Office “Stroom-Kyiv”
28A, Artema St.,Kyiv, 04053, Ukraine: nasvit@public.icyb.kiev.ua

Abstract
Analysis of the monitoring data on the radionuclides specific activity in water of the Cooling
Pond of Chornobyl NPP revealed the regular seasonal cycling of the 137Cs concentration but did notreveal this for 90Sr. It is strongly supposed that this phenomenon is caused by the microbialcontrolled seasonal dependant flux of 137Cs from the bottom sediments to the water. Analysis of the137
Cs profiles in deep water sediment (silt) provides additional forcible argument in favour of this
supposition.
The data obtained during radioecological survey carried out in August 2001 proved that on theeve of its decommissioning the Cooling Pond of Chornobyl NPP entered the stage of stabilisation ofradioecological situation. The amounts of major radionuclides accumulated in the bottom sedimentsof the Cooling Pond are estimated to be 4,400, 650 and 18 Ci for 137Cs, 90Sr and 241Am, respectively.
About 70% of 137Cs, 50% of 90Sr and 80% of 241Am that are present in the Cooling Pond willremain under the water after the water level will have been dropped down to the natural elevation.
The data on the concentration of 137Cs and 90Sr in different fish and water plant species as well as inbivale mollusc Dreisena are also presented.

1. Introduction
The Cooling Pond of the Chornobyl Nuclear Power Plant, which is situated in the northern part ofUkraine, is an artificial reservoir, created on the right-bank flood plain of Prypiat river for cooling of four
reactor units of NPP. Banks of the Cooling Pond are formed by both an above-land terracing of the riverand a protecting dike of 25 km in length. The diked-off area includes river bed, old arms and lakes. The
water surface area of the Cooling Pond is about 22 km2, volume – about 0.15 km3, length – 11 km, andwidth – 2 km. The mean depth of the Cooling Pond is 6.6 m, maximum depth – about 18 m, and water
elevation 5-7 m over the Prypiat river level. To compensate water losses due to leakage and evaporation,water is permanently pumped from Prypiat river to the Cooling Pond.
After a devastating accident happened at Chornobyl NPP on 26 April 1986, a large amount ofradioactive materials released from the completely destroyed Unit #4 caused radioactive contamination of
the environment, especially severe in the vicinity of NPP.
The Cooling Pond on the bank of which Chornobyl NPP is situated was contaminated byradioactive fallout, mainly dispersed fuel particles that felt directly on the water surface. In addition, 5,000
m3 of heavily contaminated water from the reactor basement was released to the Cooling Pond, and during
the decontamination activities a massive amount of soil removed from the nearby sites with high level ofTable 1. 137Cs and 90Sr in components of Cooling Pond ecosystem in Summer 1986, kBq/kg
f.w., kBq/l [2].
13790Component
Cs
Sr
Water, up to
1.7
0.05
Bottom sediments
10-3801-100
Aquatic plants
50-18015-45
Molluscs
18-35
35-60
Fish (carp)
100-260
2-3
74

radiation was also placed in the Cooling Pond [1]. According to various estimates, the Cooling Pond in
total received from 2,200 to 13,000 TBq (60 to 360 thousands Ci) of radionuclides [1, 2, 3]. Specificgross-beta activity of water in the beginning of May, 1986 was about 105 Bq/l, mainly due to 131I and othershort-living radionuclides. Radioecological investigations performed in Summer, 1986, showed highlevels of 137Cs and 90Sr specific activity in all components of the Cooling Pond ecosystem (Table 1).
During 1986 due to physical decay short-living radionuclides gradually eliminated from the spectrumof radioactive contamination of the Cooling Pond ecosystem, and about 95-98% of remaining radioactivity,
including long-living nuclides such as 137Cs, 90Sr, 238, 239, 240, 241Pu and 241Am settled to the bottom due toprocesses of sedimentation. After survey of bottom sediments had been carried out in 1989 and 1991, theestimates was done of the inventory of long-living radionuclides in the Cooling Pond. According to theseestimates the Cooling Pond contains about 170 TBq (4,600 Ci) of 137Cs, 35 TBq (950 Ci) of 90Sr and 0.8
TBq (22 Ci) of 239,240Pu [1].
In December 2000, the Unit #3, the last operating one at Chornobyl Nuclear Power Plant was shut
down. In some years Chornobyl NPP will not need the Cooling Pond anymore. Considering the future fateof the Cooling Pond and respective necessary actions, one should take into account the followings: fromone hand, keeping the existing water level is rather expensive and, from the other hand, leaving the
Cooling Pond without pumping of water from the river would drain a large part of bottom and may causeradiological problems for personnel of the industrial site due to wind resuspension of dried sediments
containing transuranics.
The problem of possible resuspension of bottom sediments is being studied now in a number ofprojects. But another side of the problem, i.e. what will happen to water bodies, which will remain on theplace of the Cooling Pond after it will have been drained, is still without proper attention ofradioecologists. Assessment of the future state of the Cooling Pond is possible only on the basis ofcomprehensive description of the existing situation and using of validated models of radionuclides
migration which take into account specificity of biological processes during the transition period.
The objectives of this work are to summarise the existing information on the levels of radioactive
contamination of the components of the Cooling Pond ecosystem, to reveal probable processes governingthese levels of radioactive contamination, and to provide the information to forecast the futureradioecological situation in this water-body.

Cooling Pondof Chornobyl NPP
NPP
Bathymetry andsampling stations

Constructions
Elevation, m Depth, m< 96.5> 14.596.5 – 99.0 12.0 – 14.5
99.0 – 101.5 9.5 – 12.0
101.5 – 104
7.0 – 9.5
104 – 106.5
4.5 – 7.0
106.5 – 111
0 – 4.5
Prypiat river with old arms

Sediment cores
Fish
Water
Water plants

Fig. 1. Scheme of the Cooling Pond of Chornobyl NPP with bathymetry and samplingstations location.
75

2. Materials and Methods
2.1. Water samples
Water samples from the Cooling Pond were taken at the regular intervals since the beginning of 1987
within the program of radioecological monitoring of the exclusion zone. During 1987 samples were taken
4 – 6 times per month, in 1988 – 2 times per month, since 1989 and up to now – monthly. The number ofsample sites varied from 5 to 10. During 1987 – 1992 from 1 to 10 litres were sampled for total (without
separation for suspended and dissolved fractions) 137Cs and 90Sr activity determination. In 1987 – 1988
direct gamma-spectrometric measurements of water samples were performed. In 1989 – 1992 137Cs wascollected by sorption on FEZHEL (potassium-iron ferrocyanide) at natural pH without prior filtration of
the water.
Since 1993 surface water samples are taken at 5 sites shown in Fig. 1. On each site a sample of 20 l istaken. In the laboratory sample is filtered through paper filter (blue band), and dissolved 137Cs is collectedby sorption on FEZHEL at natural pH. Filter and sorbent are measured separately for determination of
associated with suspended matter and dissolved 137Cs.
Since 1997 the radiochemical isolation of 90Sr from water by the sulphate method [4], which wasused since the beginning of regular observations, was modified and collection by sorption (complexation)
on VS-15M1 (synthetic selective sorption fibre material with grafted macro cycles groups) at natural pH
was introduced at the first stage [5].
2.2. Bottom sediments samples
Samples of bottom sediments were collected in July and August 2001 with ДТШ-3 (DETESHA-3)
corer at water depths 0 – 6 m, and a weighted gravity coring rig with 70 cm transparent cylindrical nozzle
was used at water depths more than 6 m. For investigation of the depth distribution as well as the total
inventory of 137Cs in deep-water sediments, cores (5.8 cm diameter and up to 70 cm long) were cut on site
into slices as a rule 5 cm thick, but in a number of cases the slice thickness was adjusted to observed
natural boundaries of core material with different properties.
Cores of shallow sediments (water depth less than 6 m), represented by sands, silted sands andtransformed primary soils were cut into three layers: 1 cm top, 1 cm bottom, the rest. All sediment
samples were analysed for bulk density, content of water and radionuclides.
2.3. Biotic samples
Biotic samples were taken in August, 2001 during radioecological survey of the Cooling Pond.
Fish was sampled by fishing net. All fishes were caught at the same site shown in Fig. 1. Each fish
was weighted and measured in length. About 100 g of fresh muscle tissue was dissected from each fishand packed into plastic vials for 137Cs measurements. Selected samples were taken for 90Sr analysis. Scales
were taken from each fish for determination of age.
Dreissena molluscs were collected from concrete hydrotechnical constructions with scraper or frombottom (3-7 m depth) with dredger together with sediments sampling, and ground for analysis.
Plants were collected in the littoral zone at 11 sites around the Cooling Pond. The above-sedimentparts of plants were sampled. Plant tissues were rinsed, air-dried and ground for analysis. The fresh anddry weight was determined.
Seston samples were collected with phytoplankton net (gauze Nr. 76) in pileup of planktonic algae,
mainly blue-green. Samples were air-dried, weighted and ground for analysis.
Samples of invertebrates, plants and seston were measured for 137Cs. Selected samples were taken for90
Sr analysis.

76

2.3. Radioactivity measurements.
Gamma-spectrometry was performed using Ge(Li) detector and MCA. Beta-measurements were
performed using beta-spectrometer AKC-1 and low-background counting devises UMF-1500M.
3. Results and discussion
3.1. Water
Annually averaged specific activities of total 137Cs and 90Sr in water of the Cooling Pond arepresented in Fig. 2. In general this data is in good agreement with the results presented earlier for 1986 –1995 [2, 6]. It is well known that 137Cs and 90Sr content in water is influenced by several main processes.
Among them the interaction in a system “water-suspended matter-bottom sediments” is of major
importance for water-bodies with medium and high level of biological productivity and/or high level ofsuspended particles concentration. During the first year after the accident the observed fast declining of
137
Cs and 90Sr specific activity in water was caused by their trapping with suspended matter and settling to
the bottom. Slowing down of declining for 137Cs and even increasing of concentrations of 90Sr observed in

1000

Specific activity, B q/l

137C s
90Sr
100

10

1
1986

1988

1990

1992

1994

1996

1998

2000

Years

Fig. 2. Total 137Cs and 90Sr in water of the Cooling Pond, annually averaged.
the third and fourth years were caused, probably, by the additional release of these radionuclides to waterfrom the fuel particles due to their destruction. From 1990 to 1997 almost equal declining of both
radionuclides was observed and since 1997 both radionuclides tend to have about stable concentration.
Some minor discrepancies in figures and declining rates between 137Cs and 90Sr specific activities for
1992-1995 presented in publications [2, 6] and in Fig. 2 could be explained by the fact that the latter wasprovided on the basis of more regular observations.
Monthly averaged specific activities of total 137Cs and 90Sr in water of the Cooling Pond are presented
in Fig. 3. As it could be seen from Fig. 3 regular observations of 137Cs in the Cooling Pond waterproviding the possibility of the analysis on monthly basis were started in late 1986 (actually in December)and of 90Sr – in spring 1988, although this analysis has never been done before. It was just noticed thathigher specific activities of 137Cs in water of the Cooling Pond were observed usually in summer andduring the year the variations with a factor of 2-3 were observed. If one get a look of plots presenting
monthly averaged specific activities of total 137Cs and 90Sr in water of the Cooling Pond on the backgroundof grid-lines marking the beginning of the year (Fig. 3), he could assume the presence of regular seasonalchanges of at least 137Cs concentrations.
To reveal the seasonal regularities the period of 1993 – 2000 was taken as less influenced by generalprocesses of radionuclide concentration reduction. For this period the detailed analysis of seasonal77

S pecific activity, B q/l

1000,0100,0C s_137T
S r_90
10,0

1,0

0,1
05.01.86

05.01.88

04.01.90

04.01.92

03.01.94

03.01.96

02.01.98

02.01.00

01.01.02

D atesFig. 3. Total 137Cs and 90Sr in water of the Cooling Pond, monthly averaged.
behaviour of the total 137Cs and 90Sr specific activity in water was performed and the general trends were
found (Fig. 4). Using the regression lines in Fig. 4, the seasonal component of specific activity changes
was extracted (Fig. 5). The relative units in chart represent the ratios of the actual monthly data to therespective calculated values (regression lines) and the confidence intervals represent the standard
deviation values.
As it could be seen from Fig. 5, 90Sr does not tend to show the seasonal changes. To the contrary,137
Cs strongly tends to show the regular seasonal changes with minimum values in February-March andmaximum – in June-September with August values exceeding that of February by a factor of 2.5.
There are two main ideas of explanation of the revealed phenomenon. The first is the presence of
seasonally dependant flux of 137Cs to water from the bottom sediments. The second is the seasonal
development of plankton organisms that would influence the total 137Cs specific activity in water. To
check the possible influence of the seasonal plankton development the seasonal behaviour of a ratio of
suspended to total 137Cs in water was studied. It was found that the highest contribution of suspended 137Cs
12,0

6,0
y S r = 1875399e-0 , 000 38x

C s_137T

R 2 = 0,792

5,0

Sr_90
Expon. (S r_90)
4,0

137

3,0

4,0

Sr

Cs

Expon. (C s_137T )

90

8,0

2,0

y C s = 778437e -0 , 000 35x

1,0R 2 = 0,391
0,001.01.93

0,001.01.94

01.01.95

01.01.96

31.12.96

31.12.97

31.12.98

31.12.99

30.12.00

T ime

Fig. 4. Total 137Cs and 90Sr in water of the Cooling Pond in 1993 - 2000, monthly averaged, Bq/l.
78

2,0
Cs

1,8

Sr

Relative units

1,6
1,4
1,2
1,0
0,8
0,6
0,4
0,2
0,0

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
MonthsFig. 5. Seasonal behaviour of total 137Cs and 90Sr in water of the Cooling Pond.
is observed in May and comprise about 25% of total 137Cs in water with mean seasonal value less than
15% (Fig. 6). So, the 137Cs fraction associated with seston, being the composition of plankton organisms,
organic detritus and mineral particles, does not exceed 25% of total 137Cs in water and could not provide
seasonal deviations with a factor of 2.5. That is why the presence of seasonally dependant flux of 137Csfrom the bottom sediments is strongly supposed.
Meanwhile, the seasonal cycling of 137Cs concentrations in water peaking in winter or summer has
been reported to take place in several lakes [7-11]. In each study this phenomenon was attributed todissolution of 137Cs from the bottom sediments by ion exchange with ammonium ions whose elevatedconcentrations are observed under anoxic conditions. It was proved by field measurements and laboratory
experiments that microbially produced NH4+ is the most important in release of 137Cs from sediments intolake water. Nowadays the linkage between Cs and nitrogen transfer, which is mediated by microorganisms,
is considered to be a rather general phenomenon in freshwater systems rich in organic matter [11]. In orderto clarify the real mechanism about the 137Cs seasonal cycling in water of the Cooling Pond, theexperiments should be planed to check the distribution of ammonium ion concentrations in water column
and sediment cores.

0 ,4 0 0
0 ,3 5 0
0 ,3 0 0

R a t io

0 ,2 5 0
0 ,2 0 0
0 ,1 5 0
0 ,1 0 0
0 ,0 5 0

De c

No v

Oct

Sep

A ug

Ju l

Ju n

May

A pr

Mar

Fe b

Ja n

0 ,0 0 0

M o n th s

Fig. 6. Seasonal behaviour of ratio of suspended to total 137Cs in water of the Cooling Pond.

79

3.2. Bottom sediments
Before the accident the last comprehensive hydrological survey of the Cooling Pond bottom
sediments was performed in 1985 by the Institute of Hydrobiology [12]. Primary soils (sand loam andloam) of different stage of transformation were found to meet at water depths of 3 to 8 m and to be
dominant at depths of 4-7 m. Sands of different extent of silting were met to the water depths of 12 m, andwere found to be dominant at depths of less than 5 m and 6-10 m (Fig. 7). Bottom areas with depths morethan 10 m were occupied by silts.
It was also found that two parts of the Cooling Pond that were sequentially turned into operation in1976 and 1982, and were 9 and 3 years old in 1985, respectively, had different dependencies of silt layer
thickness and annual sedimentation rate upon the water depth to the bottom (Fig. 8). The younger part had
1.5 times less average thickness of the silts layer and 2-3 times more sedimentation rate, being maximal of
about 12 cm/year (the thickness of last-year layer of sediments) [13]. The last finding was very importantfor understanding of the distribution of radionuclides over bottom sediments of the Cooling Pond after theaccident.
20
18

R elative units

16

PS

14

S

12
10
8
6
4
2
0
3-4

4-5

5-6

6-7

7-8

8-9

9-10 10-11 11-12

D ep th , m

Fig. 7. Depth distribution of primary soils (PS) and sands (S) at the bottom of Cooling Pond, 1985.

3 0 ,0

12

h1
10

h2
dh1
dh2

2 0 ,08

1 5 ,06

1 0 ,0

4

5 ,0

2

0 ,0

S e d i m e n ta ti o n r a te , c

S i l t se d i m e n t l a y e

2 5 ,0

0
0

5

10

15

20

D e p th , m

Fig. 8. Average silt sediment layer (h) and annual sedimentation rate (dh) at different depths of
the first (1) and second (2) parts of the Cooling Pond [13].
80Table 2. Specific activity of the top layer of deep-water sediments, kBq/kg d.w.
137

90

Cs
470
580

Average
Maximal239, 240

Sr
41
110

238

Pu
1.4
2.4

Pu
0.67
1.2

241

Am
2.0
4.1

The bottom sediments surveys carried out in 1989, 1991, 1999 were concentrated mostly on theradiological issues and did not contribute a lot to the understanding of development of different soils
distribution over the bottom of the Cooling Pond with respect to different depths.
Investigations carried out in 2001 revealed that primary soils did not degrade completely and still
could be recognised by the presence of roots remains. In most cases, however, being different from thesituation in 1985, wide areas of primary soils are covered by layer of silt (as a rule thin 1 – 1.5 cm, andsometimes up to 6 cm), in many cases mixed with Dreissena bivalve shells. Stable silt accumulation isobserved at depth more than 10 m on the older part of the Cooling Pond, and at more than 11 m on theyounger part.
Deep-water silt sediments present the highest specific activity of radionuclides. In the top layer ofthis sediment represented by recently settled materials the specific activity of all radionuclides other than90
Sr varies insignificantly over the whole area (Table 2). For 90Sr the difference was observed with a factorof 10.
In the areas of stable silt accumulation the density of radioactive contamination was generally foundto correlate with the thickness of accumulated silt. That is why it is not surprising that the highest densitiesof 137Cs contamination, up to 4,000 Ci/km2 or 150 MBq/m2, were found in the younger southern part of theCooling Pond where higher annual sedimentation rates were observed in 1985. The most active samples ofsilt with 137Cs specific activity of about 1.4 MBq/kg d.w. were taken also in the southern part. At water
depths of 11-14 m the most contaminated layer of 1986 is covered with several tens centimeters of more
recent silt sediments (Fig. 9). The most recent top layer within 5-6 cm has more contamination than thenext deeper one (Fig.9) that is against the general tendency of decreasing with time of contamination levelof the settling material. Taking into account the seasonal variations of 137Cs concentrations in water andour considerations on the possible reasons of that, the observed picture might be explained by the presenceof flux of 137Cs from deeper layers of sediment to upper and then to water. In upper layers of sediment theflux of cesium meets different conditions (less anoxic, less ammonium concentrations in the interstitialwater) and is being trapped by the sediment particles. These assumptions should be checked in future
1,6
C o r e # 07.02

1,4

C o r e # 10.02
C o r e # 12.07

Spe cific activity

1,2

1,0

0,8

0,6

0,4

0,2

0,0
0

10

20

30

40

50

60

70

De p th in co r e , cm

Fig. 9. 137Cs specific activity in bottom sediments (silts), MBq/kg d.w.
81

Table 3. Inventory of radionuclides in the bottom sediments of the Cooling Pond, after [14].
Total content in the
Total content in the bottom sediments in a
Radionuclides
bottom sediments, Cipart which will remain under water, Ci
137
Cs
4,400
about 3,000
90

Sr

650

313

239, 240

Pu

14

11

Pu

7

n.e.*

238
241

Am
18
n.e.*
* - n.e. means not estimated.
investigations.
On the basis of investigations carried out in 2001 the whole inventory of radionuclides in the Cooling
Pond was estimated as well as the part of area which would remain under water after the water level
would had been dropped down [14]. This gave us the possibility to assess the minimal activity ofradionuclides (without taking into account transsedimentation processes) that will remain under water,(Table 3).
So, after the water level in the Cooling Pond will have been dropped down to the natural elevation,
about 70% of 137Cs, 50% of 90Sr and 80% of 239, 240Pu will remain under water and will form the new
radioecological situation in a number of water-bodies on that territory.
3.3. Biota
Fish: Average 137Cs and 90Sr specific activity in fish muscles is presented in Table 4. As it is seen from
Table 4, the highest specific activity of caesium is observed for typical predatory species, perch and pikeperch. Some less activity is observed for omnivorous sabre carp and freshwater catfish that tend to feed
also on other fish. Typical omnivorous species goldfish and lake catfish (the last being facultative predator,
but in the Cooling Pond feeding upon periphyton and detritus [15]) are the next in this downward row.
The lowest concentrations are found in silver bream, rudd, roach and bream which feed upon benthos andplankton organisms and vegetation. Some more concentration observed in chub, being omnivorous andfacultative predator, and silver carp, which feeds upon plankton.
Almost the same row (sequence of species) was reported for 137Cs specific activity in fish of theCooling Pond in 1999 [15], the only exclusion was the highest concentration observed in freshwater
catfish. It should be noticed that not only the sequence of species but also the absolute values of caesium
concentrations were about the same in respective species.
On the contrary to caesium, concentration of 90Sr in fish muscles is rather low, being minimal in lake
Table 4. Average 137Cs and 90Sr specific activity in fish muscles, August 2001, Bq/kg f.w.
Fish species
Silver bream
Rudd
Roach
Bream
Chub
Silver carp
Lake Catfish
Goldfish
Sabre carp
Freshwater Catfish
Pike-perch
Perch

137

Cs
2,400
2,750
3,100
3,100
3,850
3,900
5,100
5,800
6,300
8,100
11,80018,100
82

90

Sr
6.6
10.9
4.3
9.5
1.7
5.3
15.3
2.3
2.7

catfish and predatory species and maximal in mainly planktotrophic species (Table 4).
Molluscs: Periphyton and benthos bivalve molluscs Dreissena were studied. Average 137Cs concentration
was about 2,600 Bq/kg f.w. with the range from 270 to 9,100 Bq/kg f.w., being the highest at the end of
directing dyke, i.e. the most southern part of the habitat. Average 90Sr concentration in Dreissena was
about 760 Bq/kg f.w. with the narrower range from 610 to 1,140 Bq/kg f.w.
Plants: Macrophytes of the Cooling Pond have rather wide ranges of 137Cs and 90Sr contamination. For
each species the ratio of maximal to minimal observed concentration was usually of about 5 to 10 and insome cases up to 80. The narrowest range and respectively the most definite values of 137Cs and 90Sr
specific activity were observed for filamentous algae and Potamogeton pectinatus. The highest
concentration of 137Cs was observed in Ceratophyllum demersum - 86.6 kBq/kg d.w. and of 90Sr in
Phragmites communis – 3.9 kBq/kg (Table 5).
Submerged plants, that are filamentous algae, Miriophylum spicatum, Potamogeton pectinatus,
Ceratophyllum demersum, have higher levels of 137Cs and 90Sr contamination than semi-water ones
(Phragmites communis).
Table 5. 137Cs and 90Sr in macrophytes of the Cooling Pond, August 2001, Bq/kg d.w.
137

Plant species
Filamentous algae
Miriophylum spicatum
Potamogeton pectinatus
Ceratophyllum demersum
Phragmites communis

90

Cs

Range
7,900 – 12,700
2,200 – 23,200
5,030 – 22,600
2,100 – 86,600
530 – 6,200

Mean
10,8008,700
12,20020,600
2,340

Sr

Range
300 – 1,460
440 – 3,300
640 – 1,160
320 – 3,260
51 – 3,900

Mean
720
1,080
960
1,120
560

Seston: Seston was collected at three stations and measured for 137Cs and 90Sr concentrations (Table 6) andwas represented mainly by phytoplankton.
Table 6. Specific activity of 137Cs and 90Sr in seston, August 2001, Bq/kg d.w.
Station
MOG
PK39
TPD

137

Cs
10,3007,685
12,430

90

Sr
705
460
1,362

3.4. Dynamics of the 137Cs and 90Sr in the components of Cooling Pond ecosystem
The results obtained together with the previous data [6, 15] gave us the possibility to compile a tablefor comparison of specific activity of 137Cs and 90Sr in components of the Cooling Pond (Table 7). In
comparison to 1995 137Cs concentration in seston in 2001 dropped down by about a factor of 10, andseveral times of decrease were also observed for semi-water plants and fish. Real water plants andTable 7. Specific activity of 137Cs and 90Sr in components of the Cooling Pond, seston and water
plants in kBq/kg d.w., molluscs and fish in kBq/kg f.w.
1991
1995
2001
Ecosystem
137
90
137
90
137
90
components
Cs
Sr
Cs
Sr
Cs
Sr
Seston300 – 1,000 60 - 270
20 - 140
0.1 - 1.5
7.7 - 12.4
0.7 - 1.3
Water plants
15 - 200
30 - 200
Semi-water
3 - 25
0.1 - 0.8
0.5 - 6.2
0.05 - 3.9
Real water
8 - 93
1 - 23
2.1 - 87
0.3 - 3.3
Molluscs
1.2 - 6
10 - 25
1.2 - 3.3
2.0 - 6.5
0.3 - 9.1
0.6 - 1.1Fish
1 - 45
2.4 - 180.0017 - 0.015
83

1000
Pike-perch
Silver breamSpecific activity

Molluscs
Plants

100

10

1
0

50

100

150

200

Months after the aciident

Fig. 10. The dynamics of 137Cs specific activity in the components of Cooling Pond ecosystem,
kBq/kg f.w.
molluscs demonstrated the same levels of concentrations as in 1995. As to 90Sr, almost the same as in1995 or higher concentrations are observed in semi-water plants and seston in 2001. Real water plants andmolluscs demonstrate decreasing of 90Sr concentration.
As it could be seen from the Fig.10, during the last 5 years contamination level of molluscs andplants remained almost the same and during the last two years the stabilisation of fish contamination is
also seems to have taken place.
4. Conclusions
On the eve of decommissioning the Cooling Pond seems to enter a period of stabilisation of theradioecological situation. General trends of radioactivity reduction are being masked by the seasonal
deviations in radionuclides concentration.
It is strongly supposed that seasonal cycling of 137Cs water concentrations are caused by the seasonal
dependant flux of caesium from bottom sediments into water. This supposition to be checked in special
field studies on the Cooling Pond.
About 70% of 137Cs, 50% of 90Sr and 80% of 241Am that are present at the moment in the Cooling
Pond will remain under water after the water level will have been dropped down to the natural elevation.
References
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