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1

Lai, Z., C. Chen, R. Beardsley, et al. "Initial Spread of <sup>137</sup>Cs over the shelf of Japan: a study using the high-resolution global-coastal nesting ocean model." Biogeosciences Discussions 10, no. 2 (2013): 1929–55. http://dx.doi.org/10.5194/bgd-10-1929-2013.

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Abstract. The 2011 Tohoku earthquake caused radionuclide 137Cs be directly released into the ocean from the Fukushima Dai-ichi nuclear power plants. A high-resolution global-coastal nesting ocean model was established to simulate the initial spread of 137Cs as conservative tracer over the shelf of Japan after the accident. The major advantage in the current model system is to use unstructured grids to resolve the power plant and the coastal geometry with a grid resolution much higher than that used in previous modeling experiments. Therefore, it gives us an opportunity to examine the necessity
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2

Kristiansen, N. I., A. Stohl, D. J. L. Olivié, et al. "Evaluation of observed and modelled aerosol lifetimes using radioactive tracers of opportunity and an ensemble of 19 global models." Atmospheric Chemistry and Physics 16, no. 5 (2016): 3525–61. http://dx.doi.org/10.5194/acp-16-3525-2016.

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Abstract. Aerosols have important impacts on air quality and climate, but the processes affecting their removal from the atmosphere are not fully understood and are poorly constrained by observations. This makes modelled aerosol lifetimes uncertain. In this study, we make use of an observational constraint on aerosol lifetimes provided by radionuclide measurements and investigate the causes of differences within a set of global models. During the Fukushima Dai-Ichi nuclear power plant accident of March 2011, the radioactive isotopes cesium-137 (137Cs) and xenon-133 (133Xe) were released in lar
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3

van der Perk, Marcel, Ondrej Slávik, and Emil Fulajtár. "Assessment of Spatial Variation of Cesium‐137 in Small Catchments." Journal of Environmental Quality 31, no. 6 (2002): 1930–39. http://dx.doi.org/10.2134/jeq2002.1930a.

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ABSTRACTSurface contamination by bomb‐derived and Chernobyl‐derived 137Cs has been subject to changes due to physical decay and lateral transport of contaminated soil particles, which have resulted in an ongoing transfer of radionuclides from terrestrial ecosystems to surface water, river bed sediments, and flood plains. Knowledge of the different sources of spatial variation of 137Cs is particularly essential for estimating 137Cs transfer to fluvial systems and for successfully applying 137Cs as an environmental tracer in soil erosion studies. This study combined a straightforward sediment re
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4

Nenadovic, Snezana, Milos Nenadovic, Ivana Vukanac, Aleksandar Djordjevic, Slavoljub Dragicevic, and Milutin Ljesevic. "Vertical distribution of 137Cs in cultivated and undisturbed areas." Nuclear Technology and Radiation Protection 25, no. 1 (2010): 30–36. http://dx.doi.org/10.2298/ntrp1001030n.

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This paper introduces the distribution background and unique characteristics of 137Cs in cultivated and undisturbed areas. The samples were taken from three measuring points of the depth of 1 m. We examined all visible horizons and determined their classifications. There were four horizons in one profile. All four horizons had a different zone thickness. 137Cs is an artificial radionuclide that has been produced primarily as a result of atmospheric thermonuclear weapon tests since the 1950. Also, the great amount of 137Cs (~85 PBq) was released in the atmosphere during the Chernobyl accident.
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5

Kristiansen, N. I., A. Stohl, D. J. L. Olivié, et al. "Evaluation of observed and modelled aerosol lifetimes using radioactive tracers of opportunity and an ensemble of 19 global models." Atmospheric Chemistry and Physics Discussions 15, no. 17 (2015): 24513–85. http://dx.doi.org/10.5194/acpd-15-24513-2015.

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Abstract. Aerosols have important impacts on air quality and climate, but the processes affecting their removal from the atmosphere are not fully understood and are poorly constrained by observations. This makes modelled aerosol lifetimes uncertain. In this study, we make use of an observational constraint on aerosol lifetimes provided by radionuclide measurements and investigate the causes of differences within a set of global models. During the Fukushima Dai-Ichi nuclear power plant accident of March 2011, the radioactive isotopes cesium-137 (137Cs) and xenon-133 (133Xe) were released in lar
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6

Tosic, Radislav, Slavoljub Dragicevic, Istvan Bikit, et al. "Estimating the soil erosion and deposition rate using 137Cs tracer method in the catchment of Drenova reservoir (B&H)." Nuclear Technology and Radiation Protection 27, no. 3 (2012): 247–53. http://dx.doi.org/10.2298/ntrp1203247t.

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There are many limitations associated with traditional approaches to estimation of soil erosion and deposition rates. Recently attention has been focused on 137Cs and successful usage of this isotope in soil erosion studies. This paper presents the results of measurements of 137Cs in soil profiles which were sampled within catchments of Drenova reservoir. The proportional model and a simplified version of the mass balance model were used to estimate the mean soil loss or deposition redistributions rates. The aim of this study is to estimate the soil erosion and deposition rates using 137Cs tra
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7

Leivadaros, Petros, Christos Tsabaris, Dionisis L. Patiris, et al. "Recent 137Cs Distribution in the Aegean Sea, Greece." Journal of Marine Science and Engineering 10, no. 11 (2022): 1719. http://dx.doi.org/10.3390/jmse10111719.

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Recent spatial and vertical distributions of 137Cs activity concentration in the Aegean Sea are presented almost 30 years after the Chernobyl accident. The study aims to provide the current radioactivity levels of 137Cs in the Aegean Sea and to combine the 137Cs activity concentration with typical oceanographic parameters (T, S) in order to utilize them as tracers to identify/validate the different water masses that are present in the Aegean Sea. This work was performed in the frame of the “KRIPIS” project in 2017 for continuous investigations of the deep basins from all over the Aegean Sea an
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8

Smith, John N., Katherine M. Ellis, and Linas R. Kilius. "129I and 137Cs tracer measurements in the Arctic Ocean." Deep Sea Research Part I: Oceanographic Research Papers 45, no. 6 (1998): 959–84. http://dx.doi.org/10.1016/s0967-0637(97)00107-6.

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9

Li, Jun Jie, Ding Qiang Li, and Mu Ning Zhuo. "Characterization and Evaluation of Soil Erosion in Shenzhen: Using Environmental Radionuclides." Applied Mechanics and Materials 522-524 (February 2014): 211–22. http://dx.doi.org/10.4028/www.scientific.net/amm.522-524.211.

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Nuclear tracer technology is quantitative and it has a high priority, which provides a unique method for understanding the mechanism of urban soil and water loss.137Cs +210Pbexcombination tracer was applied to study the characterization and evaluation of soil Erosion in Shenzhen. The results indicate that the following: 1)Disturbances from urbanization has greatly changed surface soil in Shenzhen.137Cs background inventory in Shenzhen range at 99 Bq/m2-653 Bq/m2. 2)210Pbexbackground inventory increase with altitude rise, which is attributed to the movement of water vapor. 3)Soil erosion in She
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10

Duong Duc, Thang, Bac Vuong Thu, Dung Bui Dac, et al. "Determination of recovery efficiency of ¹³⁷Cs in seawaterusing co-precipitation method." Nuclear Science and Technology 10, no. 1 (2021): 40–46. http://dx.doi.org/10.53747/jnst.v10i1.30.

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Recovery efficiency of 137Cs in seawater samples with different volumes of 40, 50, 60, 80 and 100 liters using co-precipitation method by ferrocyanide compounds has been determined. 134Cs nuclide was used as a tracer to determine recovery efficiency. The results showed that the recovery efficiency of 134Cs ranged from 92.62% to 99.26% with mean value of (95.22 ± 2.61)% for different sample volumes. Average recovery efficiency for samples with a volume of 50 liters was (95.70 ± 2.50)% and uncertainty when determining 137Cs in seawater samples were still less than 20%. Therefore, reducing the vo
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11

Jia, Song Wei. "Using Magnetic Measurements to Trace Sediment Sources in Jiangjiagou Valley of Yunnan Province." Applied Mechanics and Materials 295-298 (February 2013): 2097–101. http://dx.doi.org/10.4028/www.scientific.net/amm.295-298.2097.

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Jiangjiagou valley is an area with most developed debris flow valleys in China. Based on Jiangjiagou valley, according to the difference of magnetic characteristics in sediment and soil, this paper studied quantitatively the sediment sources. The results showed that sediments mainly came from landslide debris, accounting for 97.56%; the contributive ratio of grassland and sloped farmland for main channel sediments was very low. It was accordance with using 137Cs tracer technique. But there are still some limitations, and further strengthen research and discussion with combination of 137Cs isot
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12

Nazari Samani, A., R. J. Wasson, and Arash Malekian. "Application of multiple sediment fingerprinting techniques to determine the sediment source contribution of gully erosion: Review and case study from Boushehr province, southwestern Iran." Progress in Physical Geography: Earth and Environment 35, no. 3 (2011): 375–91. http://dx.doi.org/10.1177/0309133311401643.

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Soil erosion by water is one of the most important causes of land degradation in arid and semi-arid regions. Quantitative determination of the relative contributions of sediment sources within catchments is an essential task before developing any appropriate management strategy in order to control soil erosion and sediment transport. In this paper a multi-parameter fingerprinting method is used to determine the sediment contribution of gully erosion (Scg) in three catchments in Iran, with different areas and drainage densities. Tracers including carbon, nitrogen, C/N, phosphorus and 137Cs whic
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13

Kobayashi, Natsuko I., Ryohei Sugita, Tatsuya Nobori, Keitaro Tanoi, and Tomoko M. Nakanishi. "Tracer experiment using 42K+ and 137Cs+ revealed the different transport rates of potassium and caesium within rice roots." Functional Plant Biology 43, no. 2 (2016): 151. http://dx.doi.org/10.1071/fp15245.

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The differences in the transport characteristics in planta between potassium (K+) and caesium (Cs+) was investigated using their radionuclides, 42K+ and 137Cs+. A tracer experiment using nutrient solutions supplemented with 42K and 137Cs revealed that the ratio of the root’s K+ uptake rate to its Cs+ uptake rate was 7–11 times higher than the K+ : Cs+ concentration ratio in the solution, and the number was varied depending on the K concentration in the solution and also on the growth condition. After entering through the root tissues, the 42K+ : 137Cs+ ratio in the shoots was 4.28 times higher
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14

Pappa, F. K., D. L. Patiris, G. Eleftheriou, et al. "Dispersion of 137Cs concentration in the basins of the Aegean Sea." HNPS Proceedings 19 (January 1, 2020): 135. http://dx.doi.org/10.12681/hnps.2525.

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The anthropogenic radionuclide 137Cs is used as a valuable oceanographic tracer for the study of sea water masses identification and water movement. In the present work, 137Cs activity concentrations have been investigated in deep basins of Aegean Sea. Seawater samples were collected from five different sampling stations, during scientific oceanic campaigns from the period March to April 2008. The applied methodology was based on the adsorption of radiocaesium from dissolved AMP (Ammonium Phosphomolybdate Hydrate) in 20 L water samples. Moreover, during the pre- concentration procedure, the 13
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15

Seleznev, Andrian A., Ilia V. Yarmoshenko, and Alexander P. Sergeev. "137Cs in puddle sediments as timescale tracer in urban environment." Journal of Environmental Radioactivity 142 (April 2015): 9–13. http://dx.doi.org/10.1016/j.jenvrad.2015.01.001.

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16

Lai, Z., C. Chen, R. Beardsley, et al. "Initial spread of <sup>137</sup>Cs from the Fukushima Dai-ichi Nuclear Power Plant over the Japan continental shelf: a study using a high-resolution, global-coastal nested ocean model." Biogeosciences 10, no. 8 (2013): 5439–49. http://dx.doi.org/10.5194/bg-10-5439-2013.

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Abstract. The 11 March 2011 tsunami triggered by the M9 and M7.9 earthquakes off the Tōhoku coast destroyed facilities at the Fukushima Dai-ichi Nuclear Power Plant (FNPP) leading to a significant long-term flow of the radionuclide 137Cs into coastal waters. A high-resolution, global-coastal nested ocean model was first constructed to simulate the 11 March tsunami and coastal inundation. Based on the model's success in reproducing the observed tsunami and coastal inundation, model experiments were then conducted with differing grid resolution to assess the initial spread of 137Cs over the east
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17

Dietze, H., and I. Kriest. "Tracer distribution in the Pacific Ocean following a release off Japan – what does an oceanic general circulation model tell us?" Ocean Science Discussions 8, no. 3 (2011): 1441–66. http://dx.doi.org/10.5194/osd-8-1441-2011.

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Abstract. In the aftermath of an earthquake and tsunami on 11 March 2011 considerable amounts of radioactive materials were accidentally released into the sea off Fukushima-Daiichi, Japan. This study uses a three-dimensional eddy-resolving oceanic general circulation model to explore potential pathways of a tracer, similar to 137Cs, from the coast to the open ocean. Results indicate that enhanced concentrations meet a receding spring bloom offshore and that the area of enhanced concentrations offshore is strongly determined by surface mixed layer dynamics. However, huge uncertainties remain. A
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18

Takeda, Akira, Yusuke Unno, Mathew J. B. Swallow, Yasumi Yagasaki, Tetsuo Yasutaka, and Naofumi Akata. "Development of evaluation method for radiocesium availability in soil by biomimetic approach." Radiation Protection Dosimetry 200, no. 16-18 (2024): 1767–71. http://dx.doi.org/10.1093/rpd/ncae129.

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Abstract Applicability of biomimetic approach with simulation of plant uptake for assessment of radiocesium availability in soil was investigated. The soil spiked with 137Cs tracer was contacted with wicking material and copper-substituted prussian blue (Cu-PB), which simulate transpirationally induced mass flow and concentration gradient-induced diffusion of radiocesiumin the soil, respectively. Comparison of the removed 137Cs to the wick and the wick + Cu-PB from the soil during the contact period of 12 weeks suggested that the diffusion process has larger contribution than the mass flow pro
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19

Guilderson, T. P., S. J. Tumey, T. A. Brown, and K. O. Buesseler. "The 129-Iodine content of subtropical Pacific waters: impact of Fukushima and other anthropogenic <sup>129</sup>I sources." Biogeosciences Discussions 10, no. 12 (2013): 19935–68. http://dx.doi.org/10.5194/bgd-10-19935-2013.

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Abstract. Results obtained from a dedicated radiochemistry cruise approximately 100 days after the 11 March 2011 Tohoku earthquake and subsequent disaster at the Dia'ichi Fukushima Nuclear Power Plant show that Fukushima derived radionuclides in the nearby ocean environment had penetrated, on average, to ≤250 m depth (1026.5 kg m−3 potential density surface). The excess inventory of Fukushima-derived 129I in the region (∼150 000 km2) sampled during the cruise is estimated to have been between 0.89 and 1.173 billion Bq (∼136 to ∼179 g) of 129I. Based on a tight tracer–tracer relation with 134Cs
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20

Cahill, Richard A., and John D. Steele. "137Cs as a tracer of recent sedimentary processes in Lake Michigan." Hydrobiologia 143, no. 1 (1986): 29–35. http://dx.doi.org/10.1007/bf00026641.

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21

Brandt, J., J. H. Christensen, and L. M. Frohn. "Modelling transport and deposition of caesium and iodine from the Chernobyl accident using the DREAM model." Atmospheric Chemistry and Physics Discussions 2, no. 3 (2002): 825–74. http://dx.doi.org/10.5194/acpd-2-825-2002.

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Abstract. A tracer model, DREAM (the Danish Rimpuff and Eulerian Accidental release Model), has been developed for modelling transport, dispersion and deposition (wet and dry) of radioactive material from accidental releases, as the Chernobyl accident. The model is a combination of a Lagrangian model, that includes the near source dispersion, and an Eulerian model describing the long-range transport. The performance of the transport model has previously been tested within the European Tracer Experiment, ETEX, which included transport and dispersion of an inert, non-depositing tracer from a con
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22

Loba, Aleksandra, Jarosław Waroszewski, Marcin Sykuła, Cezary Kabala, and Markus Egli. "Meteoric 10Be, 137Cs and 239+240Pu as Tracers of Long- and Medium-Term Soil Erosion—A Review." Minerals 12, no. 3 (2022): 359. http://dx.doi.org/10.3390/min12030359.

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Isotopes of meteoric 10Be, 137Cs, 239+240Pu have been proposed as a soil redistribution tracer and applied worldwide as an alternative method to classical field-related techniques (e.g., sediment traps). Meteoric 10Be provides information about long-term soil redistribution rates (millennia), while 137Cs and 239+240Pu give medium-term rates (decades). A significant progress in developing new models and approaches for the calculation of erosion rates has been made; thus, we provide a global review (n = 59) of research articles to present these three isotopes (meteoric 10Be, 239+240Pu and 137Cs)
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23

Guilderson, T. P., S. J. Tumey, T. A. Brown, and K. O. Buesseler. "The 129-iodine content of subtropical Pacific waters: impact of Fukushima and other anthropogenic 129-iodine sources." Biogeosciences 11, no. 17 (2014): 4839–52. http://dx.doi.org/10.5194/bg-11-4839-2014.

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Abstract. Results obtained from a dedicated radiochemistry cruise approximately 100 days after the 11 March 2011 Tohoku earthquake and subsequent disaster at the Fukushima Daiichi Nuclear Power Plant show that Fukushima derived radionuclides in the nearby ocean environment had penetrated, on average, to ≤250 m depth (1026.5 kg m3 potential density surface). The excess inventory of Fukushima-derived 129I in the region (∼150 000 km2) sampled during the cruise is estimated to have been between 0.89 and 1.173 billion Bq (∼136 to ∼179 grams) of 129I. Based on a tight tracer–tracer relation with 134
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24

Kristiansen, N. I., A. Stohl, and G. Wotawa. "Atmospheric removal times of the aerosol-bound radionuclides <sup>137</sup>Cs and <sup>131</sup>I during the months after the Fukushima Dai-ichi nuclear power plant accident – a constraint for air quality and climate models." Atmospheric Chemistry and Physics Discussions 12, no. 5 (2012): 12331–56. http://dx.doi.org/10.5194/acpd-12-12331-2012.

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Abstract. Caesium-137 (137Cs) and iodine-131 (131I) are radionuclides of particular concern during nuclear accidents, because they are emitted in large amounts and are of significant health impact. 137Cs and 131I attach to the ambient accumulation-mode (AM) aerosols and share their fate as the aerosols are removed from the atmosphere by scavenging within clouds, precipitation and dry deposition. Here, we estimate their removal times from the atmosphere using a unique high-precision global measurement data set collected over several months after the accident at the Fukushima Dai-ichi nuclear po
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25

Kristiansen, N. I., A. Stohl, and G. Wotawa. "Atmospheric removal times of the aerosol-bound radionuclides <sup>137</sup>Cs and <sup>131</sup>I measured after the Fukushima Dai-ichi nuclear accident – a constraint for air quality and climate models." Atmospheric Chemistry and Physics 12, no. 22 (2012): 10759–69. http://dx.doi.org/10.5194/acp-12-10759-2012.

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Abstract. Caesium-137 (137Cs) and iodine-131 (131I) are radionuclides of particular concern during nuclear accidents, because they are emitted in large amounts and are of significant health impact. 137Cs and 131I attach to the ambient accumulation-mode (AM) aerosols and share their fate as the aerosols are removed from the atmosphere by scavenging within clouds, precipitation and dry deposition. Here, we estimate their removal times from the atmosphere using a unique high-precision global measurement data set collected over several months after the accident at the Fukushima Dai-ichi nuclear po
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26

Kin, Tadahiro, Naoto Araki, Md Kawchar Ahmed Patwary, et al. "Production method of environmental tracer 132Cs by accelerator-based neutron." EPJ Web of Conferences 239 (2020): 20002. http://dx.doi.org/10.1051/epjconf/202023920002.

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Cesium-132 has proposed as an alternative tracer of 137Cs for environment study on radioactive cesium dynamics released by a nuclear power plant accident. In the present study, we conducted a production experiment of the 132Cs by means of accelerator-based neutron method to investigate production amount and radioactive purity. A 12-g Cs2CO3 sample was irradiated by the accelerator-based neutron via the C(d,n) reactions by 1.2 µA of 30-MeV deuterons. As a result, 102 kBq/g of 132Cs was obtained with higher than 98.5% radioactive purity. Following that, a feasibility study of cesium dynamics mea
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27

Vukovic, Zivorad, Mirjana Radenkovic, Srboljub Stankovic, and Dubravka Vukovic. "Distribution and accumulation of heavy metals in the water and sediments of the River Sava." Journal of the Serbian Chemical Society 76, no. 5 (2011): 795–803. http://dx.doi.org/10.2298/jsc100420067v.

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The distribution and accumulation of assorted heavy metals and a long-lived radionuclide (Cu, Zn, Pb, Cd, U, Th and 137Cs) in the water and sediment of the River Sava (in Serbia) were investigated at three locations in the vicinity of industrial and urban settlements (Sabac, Obrenovac, Belgrade). The concentrations of heavy metals in the sediment were found to be in the ranges: 29.6-145.1 mg kg-1 for Cu, 53.2-253.6 mg kg-1 for Zn, 14.2- 78.6 mg kg-1 for Pb, 0.3-24.6 mg kg-1 for Cd and 4.0-12.5 Bq l-1 for 137Cs. These values correlate to the concentrations in the river water if expressed by equ
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28

Basher, LR, KM Matthews, and L. Zhi. "Surface erosion assessment in the South-Canterbury downlands, New Zealand using 137Cs distribution." Soil Research 33, no. 5 (1995): 787. http://dx.doi.org/10.1071/sr9950787.

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Redistribution of the radionuclide tracer 137Cs was used to examine the pattern of erosion and deposition at two sites with contrasting long-term land uses (pasture and cropping) in the South Canterbury downlands, New Zealand. There were clear differences between the two land use types in variation in 137Cs concentrations and areal activity, erosion rates and topsoil depth variability. Erosion and deposition have resulted in greater variability and lower mean levels of 137Cs areal activity under cropping (46.3 mBq cm-2) than pasture (55.0 mBq cm-2). At the cropping site, erosion and deposition
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Ivanov, M. M., V. N. Golosov, and N. N. Ivanova. "The sediment budget and migration of 137Cs in Chernobyl affected area: 30 years of investigations in the Plava River basin, Tula region." Геоморфология и палеогеография 54, no. 1 (2023): 55–73. http://dx.doi.org/10.31857/s294917892301005x.

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The Plava River basin (Tula region) is considered the most polluted with Chernobyl fallout region in Russian Federation. Detailed studies of sediment redistribution and migration of 137Cs produced by Chernobyl were conducted in the basin. The article provides an overview of results from various studies conducted during the last 30 years estimating the rate of erosion and sediment redistribution based on different methodology including 137Cs. Sediment budgets for different parts of the fluvial network were developed based on estimated rates of erosion and accumulation of sediments within the Pl
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Kusumgar, Sheela, D. P. Agrawal, Narendra Bhandari, et al. "Lake Sediments from the Kashmir Himalayas: Inverted 14C Chronology and Its Implications." Radiocarbon 34, no. 3 (1992): 561–65. http://dx.doi.org/10.1017/s0033822200063839.

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We have measured 14C, 210Pb and 137Cs profiles in two representative cores from Manasbal Lake, Kashmir, India. The sedimentation rate derived from 210Pb and 137Cs in the upper part of the core is in the range of 3.4 to 5.5 mm yr−1. In contrast, 14C ages show an inversion at depths &gt;20 cm. These results are attributed to the erosion of the ubiquitous 10–20-m-thick loess mantle, based on the similarity of 14C ages of the inversion layer in the sediments and the paleosols present in the catchment area. Frequency-dependent mineral magnetic susceptibility (χfd), carbon to nitrogen ratios and pig
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Buffoni, G., and A. Cappelletti. "On the accumulation-dispersion processes of the tracer 137Cs in the Italian seas." Journal of Environmental Radioactivity 37, no. 2 (1997): 155–73. http://dx.doi.org/10.1016/s0265-931x(96)00099-9.

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Hardtmayer, Douglas, Kevin Herminghuysen, Susan White, et al. "Determination of molten salt mass using 22Na tracer mixed with 154Eu and 137Cs." Journal of Radioanalytical and Nuclear Chemistry 318, no. 1 (2018): 457–63. http://dx.doi.org/10.1007/s10967-018-5995-x.

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33

Liu, Bing, Zhaoyan Wang, Xiaoming Zhang, et al. "Application of 137Cs tracer technique in floodplain deposition research in mesoscale river basins." Geoderma 439 (November 2023): 116706. http://dx.doi.org/10.1016/j.geoderma.2023.116706.

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34

Arata, Laura, Katrin Meusburger, Alexandra Bürge, et al. "Decision support for the selection of reference sites using <sup>137</sup>Cs as a soil erosion tracer." SOIL 3, no. 3 (2017): 113–22. http://dx.doi.org/10.5194/soil-3-113-2017.

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Abstract. The classical approach of using 137Cs as a soil erosion tracer is based on the comparison between stable reference sites and sites affected by soil redistribution processes; it enables the derivation of soil erosion and deposition rates. The method is associated with potentially large sources of uncertainty with major parts of this uncertainty being associated with the selection of the reference sites. We propose a decision support tool to Check the Suitability of reference Sites (CheSS). Commonly, the variation among 137Cs inventories of spatial replicate reference samples is taken
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35

Evangeliou, N., Y. Balkanski, A. Cozic, and A. P. Møller. "Simulations of the transport and deposition of <sup>137</sup>Cs over Europe after the Chernobyl NPP accident: influence of varying emission-altitude and model horizontal and vertical resolution." Atmospheric Chemistry and Physics Discussions 13, no. 3 (2013): 7681–736. http://dx.doi.org/10.5194/acpd-13-7681-2013.

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Abstract. The coupled model LMDzORINCA has been used to simulate the transport, wet and dry deposition of the radioactive tracer 137Cs after accidental releases. For that reason, two horizontal resolutions were deployed and used in the model, a regular grid of 2.5°×1.25°, and the same grid stretched over Europe to reach a resolution of 0.45°×0.51°. The vertical dimension is represented with two different resolutions, 19 and 39 levels, respectively, extending up to mesopause. Four different simulations are presented in this work; the first uses the regular grid over 19 vertical levels assuming
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Evangeliou, N., Y. Balkanski, A. Cozic, and A. P. Møller. "Simulations of the transport and deposition of <sup>137</sup>Cs over Europe after the Chernobyl Nuclear Power Plant accident: influence of varying emission-altitude and model horizontal and vertical resolution." Atmospheric Chemistry and Physics 13, no. 14 (2013): 7183–98. http://dx.doi.org/10.5194/acp-13-7183-2013.

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Abstract. The coupled model LMDZORINCA has been used to simulate the transport, wet and dry deposition of the radioactive tracer 137Cs after accidental releases. For that reason, two horizontal resolutions were deployed and used in the model, a regular grid of 2.5° × 1.27°, and the same grid stretched over Europe to reach a resolution of 0.66° × 0.51°. The vertical dimension is represented with two different resolutions, 19 and 39 levels respectively, extending up to the mesopause. Four different simulations are presented in this work; the first uses the regular grid over 19 vertical levels as
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Lobb, D. A., R. G. Kachanoski, and M. H. Miller. "Tillage translocation and tillage erosion on shoulder slope landscape positions measured using 137Cs as a tracer." Canadian Journal of Soil Science 75, no. 2 (1995): 211–18. http://dx.doi.org/10.4141/cjss95-029.

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Tillage erosion, the net downslope translocation of soil by tillage, was measured on eight shoulder slope landscape positions within two fields in the upland regions of south–western Ontario. Translocation of soil by tillage was measured by labelling plots of soil with 137Cs and measuring its displacement in response to tillage. Paired plots were utilized to compare soil translocation by upslope and downslope tillage. A single sequence of conventional tillage operations, consisting of mouldboard plough, tandem disc (double pass) and C-tine cultivator, translocated 90 kg soil m−1 slope width wh
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KHALILI VAVDARE, S., H. SEDGHI, and A. SARRAF. "DETERMINATION OF SEDIMENTATION RATE IN ANZALI LAGOON OF NORTHERN IRAN USING 137Cs TRACER TECHNIQUE." Applied Ecology and Environmental Research 17, no. 1 (2019): 1337–47. http://dx.doi.org/10.15666/aeer/1701_13371347.

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YAN, Dong-chun, Xin-bao ZHANG, An-bang WEN, Xiu-bin HE, and Yi LONG. "Assessment of sediment yield in a small karst catchment by using 137Cs tracer technique." International Journal of Sediment Research 27, no. 4 (2012): 547–54. http://dx.doi.org/10.1016/s1001-6279(13)60012-8.

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40

Brydsten, Lars, and Mats Jansson. "Studies of estuarine sediment dynamics using 137Cs from the Tjernobyl accident as a tracer." Estuarine, Coastal and Shelf Science 28, no. 3 (1989): 249–59. http://dx.doi.org/10.1016/0272-7714(89)90016-4.

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41

Gingras, Jérôme, and Daniel Boisclair. "Comparison between consumption rates of yellow perch (Perca flavescens) estimated with a digestive tract model and with a radioisotope approach." Canadian Journal of Fisheries and Aquatic Sciences 57, no. 12 (2000): 2547–57. http://dx.doi.org/10.1139/f00-230.

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We compared consumption rates of yellow perch (Perca flavescens) obtained from surveys of complete digestive tract contents (CDTC) with two radioisotope approaches using 137Cs as a biological tracer. We sampled fish of age 1+, 2+, and 3+ from three lakes for a total of six lake - age-class combinations. The two radioisotope methods provided very similar estimates of consumption rates. The relative differences between the CDTC approach and the radioisotope approaches ranged from 67 to 128% when the sampling interval length was 28-35 days. At the time scale of 70 days, the relative differences b
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Dicen, Gerald, Floriane Guillevic, Surya Gupta, et al. "Distribution and sources of fallout 137Cs and 239+240Pu in equatorial and Southern Hemisphere reference soils." Earth System Science Data 17, no. 4 (2025): 1529–49. https://doi.org/10.5194/essd-17-1529-2025.

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Abstract. Past nuclear weapons testing (NWT) and nuclear power plant (NPP) accidents have resulted in the ubiquitous deposition of radionuclides in the environment. These fallout radionuclides (FRNs) are considered the privileged markers (“golden spikes”) of the Anthropocene stratigraphic layers. Their deposition in the 1950s coincided with the “Great Acceleration”, which is characterized by large-scale shifts in the Earth's systems, including increased land-use change and soil degradation. Among the FRNs deposited globally, 137Cs has been the most commonly used to assess soil erosion and/or t
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Kalkan, Kristina, Sofija Forkapic, Slobodan Markovic, et al. "Study of hanging valley in loess-paleosoil sediments with soil erosion assessment using nuclear and erosion potential methods." Nuclear Technology and Radiation Protection 37, no. 1 (2022): 65–77. http://dx.doi.org/10.2298/ntrp2201065k.

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This paper is dealing with soil erosion assessment using two different approaches: nuclear model and erosion potential method, also known as Gavrilovic's method. Complex valley systems on Titel Loess Plateau were selected for investigation. Radiocaesium is favored in many studies as an optimal erosion tracer due to its relatively long half-life, negligible renewal in the environment and strongly binding ability onto soil particles. The use of gamma-spectrometry in environmental testing laboratories acts as a precise and fast measurement technique for determination of 137Cs activity concentrati
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44

Christoudias, T., and J. Lelieveld. "Modelling the global atmospheric transport and deposition of radionuclides from the Fukushima Dai-ichi nuclear accident." Atmospheric Chemistry and Physics 13, no. 3 (2013): 1425–38. http://dx.doi.org/10.5194/acp-13-1425-2013.

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Abstract. We modeled the global atmospheric dispersion and deposition of radionuclides released from the Fukushima Dai-ichi nuclear power plant accident. The EMAC atmospheric chemistry – general circulation model was used, with circulation dynamics nudged towards ERA-Interim reanalysis data. We applied a resolution of approximately 0.5 degrees in latitude and longitude (T255). The model accounts for emissions and transport of the radioactive isotopes 131I and 137Cs, and removal processes through precipitation, particle sedimentation and dry deposition. In addition, we simulated the release of
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Robbins, John A., Alena Mudroch, and Barry G. Oliver. "Transport and Storage of 137Cs and 210Pb in Sediments of Lake St. Clair." Canadian Journal of Fisheries and Aquatic Sciences 47, no. 3 (1990): 572–87. http://dx.doi.org/10.1139/f90-066.

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In 1985 cores were collected by diver from areas with fine-grained sediments in Lake St. Clair. Although the lake is shallow, rapidly flushed, and possesses only a thin layer of postglacial sediment (ca. 30 cm max.), 8% of the estimated, 137Cs loading from atmospheric nuclear testing in the mid-1960s and 13% of the potential standing crop of excess 210Pb were retained. A sediment column transport model including eddy diffusive mixing, advection and resuspension, acceptably described the vertical distribution of these radionuclides as well as stable lead and implied that such efficient retentio
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Garraffo, Zulema D., Hae-Cheol Kim, Avichal Mehra, Todd Spindler, Ilya Rivin, and Hendrik L. Tolman. "Modeling of 137Cs as a Tracer in a Regional Model for the Western Pacific, after the Fukushima–Daiichi Nuclear Power Plant Accident of March 2011." Weather and Forecasting 31, no. 2 (2016): 553–79. http://dx.doi.org/10.1175/waf-d-13-00101.1.

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Abstract In this study, results are presented from the first operational ocean tracer dispersion model operated by the National Oceanic and Atmospheric Administration/National Weather Service/National Centers for Environmental Prediction (NOAA/NWS/NCEP). This study addresses the dispersion of radionuclide contaminants after the Fukushima–Daiichi nuclear accident that was triggered by the 11 March 2011 earthquake and tsunami. The tracer capabilities of the Hybrid Coordinate Ocean Model (HYCOM) were used in a regional domain for the northwestern Pacific, with nesting lateral boundary conditions
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Zheng, Jian, Keiko Tagami, Wenting Bu, et al. "135Cs/137Cs Isotopic Ratio as a New Tracer of Radiocesium Released from the Fukushima Nuclear Accident." Environmental Science & Technology 48, no. 10 (2014): 5433–38. http://dx.doi.org/10.1021/es500403h.

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48

Suhartini, Nita, Barokah Aliyanta, and Arief Adhari. "PLANTS COVERING INFLUENCE TO THE RADIOISOTOPES EXISTENCE OF Cs-137 AND Pb-210 IN THE SOIL." Jurnal Forum Nuklir 14, no. 1 (2020): 7. http://dx.doi.org/10.17146/jfn.2020.14.1.5811.

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PLANTS COVERING INFLUENCE TO THE RADIOISOTOPES EXISTENCE OF 137Cs and 210Pbex IN THE SOIL. Cs-137 and Pbex-210 of environmental radioisotope content in the soil can be useful to estimate the rate of erosion/deposition in an area, by comparing the inventory value of Cs-137 or Pbex-210 in observed site with those in a stable reference site. Cs-137 and Pbex-210 stick very strongly at the surface of the soil (clay), so it can use as a tracer for the movement of soil. Plants very influence the existence of Cs-137 and Pbex-210 environmental radioisotopes as a cover. If without a plant cover, then th
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49

Christoudias, T., and J. Lelieveld. "Modelling the global atmospheric transport and deposition of radionuclides from the Fukushima Dai-ichi nuclear accident." Atmospheric Chemistry and Physics Discussions 12, no. 9 (2012): 24531–55. http://dx.doi.org/10.5194/acpd-12-24531-2012.

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Abstract. We modeled the global atmospheric dispersion and deposition of radionuclides released from the Fukushima Dai-ichi nuclear power plant accident. The EMAC atmospheric chemistry – general circulation model was used, with circulation dynamics nudged towards ERA-Interim reanalysis data. We applied a resolution of approximately 0.5 degrees in latitude and longitude (T255). The model accounts for emissions and transport of the radioactive isotopes 131I and 137Cs, and removal processes through precipitation, particle sedimentation and dry deposition. In addition, we simulated the release of
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50

Geng, Hao-peng. "Application of radionuclide 137Cs as a tracer to estimate soil erosion in the Qilian Shan, N.W. China." Quaternary International 279-280 (November 2012): 164. http://dx.doi.org/10.1016/j.quaint.2012.08.202.

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