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cesium 137 sedimentation
Reproduction of sediment deposition and prediction of
2020612 Introduction Radionuclides, including radioactive 137 Cs, released from the FDNPP accident following the earthquake and tsunami of 11 March 2011, have risen to
The application of caesium-137 measurements to estimate
2011311 In this , the 137 Cs technique was employed to investigate recent sedimentation rates in a Chinese polygonal karst depression. The results indicated that
Geochemical mobility of 137Cs in marine environments
20221230 Abstract. Cesium-137, a unique geochemical tracer, behaves as a particle-reactive species in freshwater that is useful as a geochronometer, and soluble in
Distribution and budget of 137 Cs in the China Seas PubMed
2020529 Cesium-137 is one of the most abundant anthropogenic radionuclides released by atmospheric nuclear testing and nuclear accidents, and accordingly it may
Application of Radioactive Fallout Cesium‐137 for Measuring
199041 Most 137 Cs movement in the environment is by physical processes; therefore, 137 Cs is a unique tracer for studying erosion and sedimentation. Cesium-137
Dating Sediment in a Fast Sedimentation Reservoir using Cesium‐137
201576 Reservoir sedimentation records provide a unique o Dating Sediment in a Fast Sedimentation Reservoir using Cesium‐137 and Lead‐210 Zhang 2015 Soil
Cesium-137 and mercury contamination in lake sediments
199971 In the present study, the sedimentation of 137Cs and mercury in lake sediments was analyzed with emphasis on the role of fluvial discharge through ground
Use of caesium-137 as a tracer of erosion and sedimentation
1993101 The caesium 137 technique has become an important tool for investigating soil erosion. It permits retrospective assessment of medium-term erosion rates. The
(PDF) Césium-137 et études environnementales
Most 137Cs movement in the environment is by physical processes; therefor, 137Cs is a unique tracer for studying erosion and sedimentation. Cesium-137 loss from a watershed has been shown to
(PDF) Caesium-137 as a soil erosion tracer: A
200611 Most 137Cs movement in the environment is by physical processes; therefor, 137Cs is a unique tracer for studying erosion and sedimentation. Cesium-137 loss from a watershed has been shown to
Caesium-137 as a soil erosion tracer: a review Semantic
This stone describes a method of soil erosion and soil movement measurements using 137 Cs as a tracer. This technique has been used successfully employed for more than 30 years. Caesium-137 is a valuable tracer to study soil erosion. Its chemical and biological move- ment in soil is limited. Practically all redeposition of caesium-137 in soil after fallout
Application of radioactive fallout cesium-137 for measuring
Most {sup 137}Cs movement in the environment is by physical processes; therefore, {sup 137}Cs is a unique tracer for studying erosion and sedimentation. Cesium-137 loss from a watershed has been shown to correlate strongly with soil loss calculated by the Universal Soil Loss Equation (USLE) or measured from small runoff plates.
A rapid method for 137Cs preconcentration from seawater
2021725 A rapid method was developed herein for preconcentrating and determining 137 Cs in seawater. The coagulant polyaluminum chloride was used to accelerate the ammonium phosphomolybdate sedimentation for preconcentrating 137 Cs from large volumes of seawater, followed by direct measurement with gamma-ray
Evaluation of Cesium‐137 Conversion Models and Parameter
201551 The 137 Cs technique has been widely used to provide soil redistribution estimates since the 1970s. However, most 137 Cs-conversion models remain theoretical and largely unvalidated. Our objectives were to validate the four widely used conversion models, examine model parameter sensitivity, and evaluate the potential of using kriging
Cesium-137, metals and organic carbon in the sediments of
198411 The sedimentation rates, estimated by Cs-137 geochronology, range from 04 to > 3 cm year −1. The sedimentation rates in the Burwell Bay region are two or more, times those in the Point of Shoals and in the Rocklanding Channel and Shoal, reflecting the weaker currents in the Burwell Bay region. Cesium-137, an artificial radionuclide with
Conversion Models for Use in Soil-Erosion, Soil
Using cesium-137 to assess the variability of net soil erosion and its association with topography in a Canadian Prairie landscape. Catena, 14, 439–451 Use of caesium-137 as a tracer of erosion and sedimentation: Handbook for the application of the caesium-137 technique. Exeter: University of Exeter. Google Scholar
ESSD A worldwide meta-analysis (1977–2020) of sediment
20211027 Information about sedimentation rates based on 137 Cs analyses was provided in 34.6 % of the publications. The 1963 peak level was generally used for estimating this average sedimentation rate. -240, americium-241, cesium-137, and cobalt-60 in Columbia River sediments from Hanford to the Columbia River Estuary, Environ.
The use of environmental radionuclides as tracers in soil
200321 The recent developments in the use of the 137 Cs technique in soil erosion and sedimentation studies have paved the way to both extending the approach to other environmental radionuclides and expanding applications exploiting the essentially unique advantages provided by the technique to controlling soil erosion and sedimentation and
A comprehensive study on sedimentation rate and sediment
202168 The 137 Cs—based sedimentation rates were estimated by the 1963 key time marker by adopting the peak method as 90% of the radionuclide discharge happened somewhere Ritchie JC, McHenry JR (1990) Application of radioactive fallout cesium-137 for measuring soil erosion and sediment accumulation rates and patterns: a review. J
Cesium-137, a tool for the assessment and the management
1998515 @misc{etde_, title = {Cesium-137, a tool for the assessment and the management of erosion risks; Césium-137 et érosion des sols} author = {Bernard, C., Mabit, L., Laverdière, M. R., and Wicherek, S.} abstractNote = {Cesium-137 (137Cs) is a radioisotope that was artificially introduced in the environment through the extensive high
Principes de la méthode du césium-137
La figure 8 présente les principes de la méthode du 137 Cs (Mabit 1999). Suite aux précipitations, le 137 Cs s’est déposé à la surface de la Terre où il a été rapidement adsorbé par
Predicting sediment and cesium-137 discharge from
201431 This stone reports simulations of soil erosion, sediment movement, and the resulting migration of cesium-137 (137 Cs) in eastern Fukushima Prefecture after the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident in Japan. We quantified these processes with a simple, novel, and fast simulation model developed previously with the
(PDF) Using lake sedimentation rates to quantify the
2011913 Data used to estimate sedimentation rates in Moon Lak e: (a) lead-210 (210 Pb) and (b) cesium-1 37 (137 Cs). The slope does not appreciably c hange with or without the data points shown as squares
Land degradation assessment using fallout cesium-137 in a
2023324 Cesium-137 activity in the reference site is about 2842 Bqm−2. It varies from 2288 to 4464 Bqm−2 in the burnt site, from 1951 to 3440 Bqm−2 in the forest site, and from 1359 to 2448 Bqm−2 in the agricultural site. and its relatively long half-life make 137 Cs a good tracer for soil erosion and sedimentation studies (Azbouche
Application of Radioactive Fallout Cesium‐137 for Measuring
199041 Radioactive fallout 137 Cs (cesium-137) deposited across the landscape from atmospheric nuclear tests is strongly absorbed on soil particles limiting its movement by chemical and biological processes. Most 137 Cs movement in the environment is by physical processes; therefore, 137 Cs is a unique tracer for studying erosion and sedimentation.
(PDF) Use of cesium-137 as a tracer in the study of
199311 This stone describes a procedure for deriving estimates of sedimentation rates for individual points on the floodplain based on measurements of the total 137Cs inventory and the 137Cs content of
A preliminary assessment of the potential for using caesium-137
2022220 The caesium-137 contents of soil profiles have been used to estimate soil erosion losses from different topographic and land use conditions at Lishi, Shanxi Province, and Luochuan, Shaanxi Province. At uncultivated sites the caesium-137 has accumulated in the upper soil profile, whilst it has been mixed within the plough layer of cultivated soils.