Temporal variation of 137Cs inventory in the western North Pacific

The temporal variation of water column inventories of ¹³⁷Cs in the western North Pacific was examined. ¹³⁷Cs in seawater of the western North Pacific has originated mainly from global fallout from atmospheric nuclear weapons tests, which occurred in the early 1960's. In the western North Pacific, the water column inventories of ¹³⁷Cs were 5200 Bq·m^-2 in 1973 (GEOSECS station GX225) and 3400 Bq·m^-2 in 1983 (KH-84-3 station AN-1). In 1997, the ¹³⁷Cs inventory was 2600 Bq·m^-2 at station 1 of the IAEA'97 cruise. The global fallout at Tsukuba since 1945 was estimated to be 5600 Bq·m^-2 in 1973, 4600 Bq·m^-2 in 1983 and 3500 Bq·m^-2 in 1997. The water column inventories of ¹³⁷Cs were 93–74% of the estimated global fallout for the same latitude. The typical features of the temporal variation for three vertical profiles taken in 1973, 1983 and 1997 are the decrease of ¹³⁷Cs activity in the mixed layer and the gradual increase of ¹³⁷Cs activity in deeper layers. The proportion of the ¹³⁷Cs inventory in waters down to 1000 meters was 100% in 1973, 88% in 1983 and 75% in 1997. These findings suggest that large amount of the ¹³⁷Cs entering through sea surface would remain in the mixed layer for more than a few decades.     

The reducing rate of radiocesium 137Cs in the North Pacific surface water after the TEPCO fukushima Dai-ichi nuclear power plant accident

Journal of Radioanalytical and Nuclear Chemistry - We started monitoring the radiocesium released from Fukushima in the North Pacific surface water from May 2011 after the accident soon to June...     

Distribution of 137Cs and 134Cs in the North Pacific Ocean: impacts of the TEPCO Fukushima-Daiichi NPP accident

Impact of the TEPCO Fukushima-Daiichi NPP accident, FNPP1, to the North Pacific Ocean occurred through two pathways, namely direct release and atmospheric deposition to wide ocean surface. We collected more than 100 seawater samples in the North Pacific Ocean in April and May 2011 by seven commercial ships as VOS. Since the sample volume was 2 l each, we measured radiocaesium activity at Ogoya Underground Facility to obtain reliable activity. ¹³⁷Cs was detected at all stations and ¹³⁴Cs was detected at most of the stations in the North Pacific Ocean. The ¹³⁷Cs activity ranged from around 1 to 1,000 Bq m^?3 with activity ratios of ¹³⁴Cs/¹³⁷Cs close to 1 which is a signature of radiocaesium originated from the FNPP1 accident. At east of the International Date Line north of 40°N in the Pacific Ocean in April 2011, the ¹³⁴Cs activity ranged from 2 to 12 Bq m^?3.     

Ultra low level deep water <Superscript>137</Superscript>Cs activity in the South Pacific Ocean

We determined ¹³⁷Cs concentrations in deep water samples of the subtropical gyre in the South Pacific collected during the BEAGLE2003 cruise. This was done at an underground facility to achieve extremely low background γ-spectrometry, and we, therefore, obtained reliable values of ¹³⁷Cs activity in the deeper layers. ¹³⁷Cs activity in the layers between 2000 and 4500 m ranged from 7 ± 4 mBq m⁻³ to 25 ± 11 mBq m⁻³. The inventory of ¹³⁷Cs in the water column from 2000 m to the sea bottom was estimated to be 20 ± 8 Bq m⁻² to 94 ± 41 Bq m⁻² in this region.     

Fallout 137Cs in soils from North Western Libya

Fallout levels of ¹³⁷Cs in surface soil from North WesternLibya have been measured using gamma-ray spectrometry. The activity concentrationsof ¹³⁷Cs in soil ranged from 975 to 1720 mBq . kg ^—1 . The areal activity concentrations ranged from 1300 to 2250 mBq .m ^—2 , and were higly correlated with annual precipitation.The effective dose from external exposure to ¹³⁷Cs is found tobe 3 nSv . y ^—1 .     

Fukushima-derived radiocesium in the western North Pacific in 2014

Journal of Radioanalytical and Nuclear Chemistry - In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity...     

Resuspension processes controll variations of 137Cs activity concentrations in the ground-level air

The ¹³⁷Cs activity concentration in the surface air between 1977 and 2007 was decreasing with an ecological half-life of 3.4?years, however, during 2007?C2010 the yearly averaged ¹³⁷Cs activity concentrations were almost constant. The increased atmospheric ¹³⁷Cs and ⁴⁰K levels observed during the winter may be due to surface soil resuspension and radionuclide transport by winds, particularly from open agricultural areas, as confirmed by high correlation coefficient between ¹³⁷Cs and ⁴⁰K atmospheric levels (R?=?0.84), and similar ¹³⁷Cs/⁴⁰K activity ratios in aerosols (0.07) and soils (0.05).     

137Cs and 210Pb radionuclides in open and closed water ecosystems

The aim of this study was to determine the level of radionuclide concentration in sediment cores in two different water ecosystems; one closed and one open. Based on this data the changes in these ecosystems were interpreted. Two sediment cores from the Dobczyce reservoir and the Smreczynski Staw Lake were collected and divided into 1 cm thick sub-samples. The samples were air dried and homogenized. The ¹³⁷Cs and ²¹⁰Pb (²¹⁰Pb_sup, ²¹⁰Pb_total, ²¹⁰Pb_uns) concentrations were measured using gamma and alpha spectrometry. Results showed that the ¹³⁷Cs concentration in the Dobczyce reservoir is lower than in the Smreczynski Staw Lake. Total ²¹⁰Pb concentration in the Dobczyce reservoir was around 70 Bq kg^?1 and in the Smreczynski Staw Lake was about 500 or 1,200 Bq kg^?1 with the decreasing tendency in the sediment core. Sediments are very important constituents of water ecosystems. In spite of the young age of the Dobczyce reservoir, the ¹³⁷Cs and ²¹⁰Pb radionuclides were very useful in understanding of the processes which have taken place in these ecosystems. The estimated sedimentation rate indicated such processes as regular sedimentation, mixing of sediments or floods. In the Smreczynski Staw Lake the changes have reflected the changes which took place in the Tatra Mountains.     

Modes of137Cs desorption from marine sediments by sea water

Sea water is observed to be a good desorbing agent for¹³⁷Cs from marine sediments. Investigations on the sites of¹³⁷Cs binding and their abundance by desorption over extended periods indicated that, whatever the time of contact of sorption,¹³⁷Cs has three modes of desorption: fast component with desorption half-time of 30–50 min, medium component with desorption half-time of 25–50 h and slow component with desorption half-time of 31–112 days. These are expected to be sites of ion exchange, slower exchange and trapped Cs in the clay mineral layer lattices.     

Radionuclide ratios of90Sr/137Cs and239(240)Pu/137Cs in contaminated surface air after the Chernobyl accident in Asutria

Energy straggling in pulse height distributions of plastic scintillation counters of 4 and 10 cm in thickness was measured for 1 GeV/c pions and studied by Monte Carlo simulations. Calculated energy loss distributions are in good agreement with the experimental data and also with the prediction by the Landau straggling function.     

239Pu, 240Pu, 241Pu, 241Am, 137Cs,and 210Pb in seafloor sediments in the western North Pacific Ocean and the Sea of Japan: distributions,sources and budgets

Journal of Radioanalytical and Nuclear Chemistry - Vertical distributions of 239Pu, 240Pu, 241Pu, 241Am, 137Cs, and 210Pb concentrations, and 240Pu/239Pu ratios were determined in seafloor...     

Rapid determination of 137Cs in environmental samples--purification of 137Cs by ammonium molybdophosphate column separation]

A rapid method for the determination of 137Cs in environmental samples was proposed. The principal technic employed in this study is based on column separation of 137Cs using ammonium molybdophosphate mixed with glass fiber to eliminate contribution of natural radionuclides such as 40K and 87Rb. The separation of cesium from potassium and rubidium was performed by the elution with 0.5m ammonium nitrate solution. The time required for separation of cesium was five hours as compared with the conventional cation exchange separation which required thirteen hours. The chemical yield of cesium carrier was normally more than 90 percent. The results obtained were compared with that by the conventional methods using Bio-Rex cation exchange separation and the good agreement between the two methods was obtained.     

Natural radionuclides and 137Cs activity concentration in the bottom sediment cores from Kuwait Bay

Summary The activity concentration of natural radionuclides and ¹³⁷Cs in the bottom sediments cores from Kuwait Bay have been determined by γ-ray spectrometry. Particular attention was devoted to the exact determination of two uranium isotopes: ²³⁵U and ²³⁸U in order to find any presence of depleted uranium dispersed during the 1991 Gulf War. The calculated ²³⁸U/²³⁵U activity ratios for all the surface (15 cm) as well as the core profile (up to 70 cm in depth) samples were within the limit of one standard deviation close to the value of 21.5 for natural uranium. Simultaneous instrumental determination of the unsupported ²¹⁰Pb and ²²⁶Ra in a few sediment core profiles was used for quantification of sediment accumulation rates. The calculated sedimentation rates (for the constant atmospheric ²¹⁰Pb flux rate - CRS model) ranged from 0.2 to 0.6 cm ^. y^-1 and were close to the data calculated by the Weibull distribution of ¹³⁷Cs in undisturbed sediment cores.     

Distribution of3H,137Cs and239,240Pu in the surface seawater around Korea

The concentrations of³H,¹³⁷Cs and^239,240Pu were determined in surface seawaters collected at 21 sampling stations around Korea from October of 1994 to May of 1995. The results were consistent with the past data observed in the North Pacific. The concentrations of³H and¹³⁷Cs did not show much difference no matter where the samples were taken. Due to the limited distribution of sampling points, no systematic change in³H and¹³⁷Cs levels with latitude was observed. On the other hand,^239,240Pu concentration in the East Sea (Japan Sea) was somewhat higher than that in the South and the Yellow Seas, although the data on^239,240Pu concentration were not enough to explain the reason. The activity ratios of^239,240Pu/¹³⁷Cs in surface seawater ranged from 0.13% to 0.44% with a mean of 0.25±0.08%. The activity ratios were lower than those of the global fall-out level, 1.1%. This result presumably arose from the different behavior of the two radionuclides in seawater.     

Leaching behavior of137Cs in cement

To assess the safety of disposal of a radioactive waste-cement composite, the leaching of¹³⁷Cs from a waste composite into a surrounding fluid has been studied. Leaching tests were carried out in accordance with a method recommended by IAEA.¹ The leachability was measured as a function of bentonite clay to cement ratio. The fraction of¹³⁷-Cs leached from a specimen of Portland cement is 0.03–0.13 at a leaching time of 400 d. Results presented in this paper are examples of data obtained in a 10 y mortar and concrete testing project, which will influence the design of the engineered trench system for a future Yugoslav radioactive waste storage center.^2,3     

Application of Cu·FeHCF coated acrylic fibre for the separation of Cs isotopes in drinking water to determine fallout 137Cs

Ten fresh water samples of wells and rivers from the environment of Tarapur Maharashtra Site were analyzed to evaluate and establish the fall out level of ¹³⁷Cs activity concentration using large volume of water samples. A radiochemical separation method suitable for the analysis of large volume of water sample based on the adsorption of Cs isotopes on coated acrylic fibres was standardized. ¹³⁴Cs isotope was used for monitoring the radiochemical recovery of the analysis. Radiochemical recovery was obtained in the range of 74?C98% for a sample volume of 250?L or more. The fall out level ¹³⁷Cs concentration in river/dam water was found to be in the range of 0.205 to 0.268?mBq?L^?1. The fall out level annual effective dose through water ingestion pathway for a member of public was evaluated to be 2.27?×?10^?9?Sv.     

Elevated rice 137Cs concentrations near the water inlet in paddy fields after the Fukushima nuclear accident

Journal of Radioanalytical and Nuclear Chemistry - The reasons why rice 137Cs concentrations increase near the water inlet were investigated using rectangular experimental plots settled in paddy...     

Time-series observations of 210Po and 210Pb radioactivity in the western North Pacific

We carried out time-series observations of ²¹⁰Po and ²¹⁰Pb radioactivity in the western North Pacific Ocean. The sinking fluxes of particulate organic carbon (POC) in the mesopelagic zone were estimated from ²¹⁰Po radioactivity during several seasons in the subarctic and subtropical regions of the western North Pacific. The seasonal changes of POC fluxes at a depth of 400 m were larger in the subarctic region than in the subtropical region. The annual mean POC flux at a depth of 400 m was larger in the subarctic region (57 mgC m^?2 day^?1) than in the subtropical region (36 mgC m^?2 day^?1). The annual mean of the e-ratio (the ratio of POC flux to primary productivity) in the subarctic region (18 %) was about twice the e-ratio in the subtropical region (10 %). These results imply that the efficiency of the biological pump is larger in the subarctic region than in the subtropical region of the western North Pacific.