Zobrazeno 1 - 10
of 23
pro vyhledávání: '"D. Yu. Bol'shiyanov"'
Publikováno v:
Water Resources. 48:397-403
Variations in the concentration of 137Cs in lake water over 12–19 years of its migration were reproduced with the use of exponential and sorption–diffusion models in calculations. The concentrations of 137Cs in water of the deep (Нav > 7 m) lake
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b23596de93ee7490176279676add8827
https://doi.org/10.1134/s0097807821030040
https://doi.org/10.1134/s0097807821030040
Publikováno v:
Radiochemistry. 63:127-132
Contamination with 90Sr of the White Sea water in migration during 50 years is reconstructed with the use of a three-component exponential model. Т1, Т2, and Т3, the periods of half-purification of White-Sea water to remove 90Sr were 0.8, 15.4, an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a29399db655a10763059ed0b0625193
https://doi.org/10.1134/s1066362221010185
https://doi.org/10.1134/s1066362221010185
Publikováno v:
Radiochemistry. 62:667-672
For 6 drainless lakes with average depths of ≤12 m, the fallout of 137Cs to water basins is reconstructed by using in calculation the sorption-diffusion model off radionuclide absorption by the bottom and the data of later (in years) monitoring of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08167a4c67494aa29c35f68eed0103c4
https://doi.org/10.1134/s1066362220050148
https://doi.org/10.1134/s1066362220050148
Publikováno v:
Radiochemistry. 61:122-128
The 5–17-year migration of 137Cs in bottom sediments (BSs) of five oligotrophic lakes located on the “Chernobyl” 137Cs fallout plume was studied. The layer-by-layer analysis of the 137Cs levels in BS cores allowed determination of the 137Cs mig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e74ba552b73ff04c3bac0cf67d3a767
https://doi.org/10.1134/s1066362219010181
https://doi.org/10.1134/s1066362219010181
Publikováno v:
Water Resources. 43:533-538
The rate of natural removal of 137Cs from water bodies in Eastern Fennoscandia is evaluated. The half-time T of water purification from global 137Cs in lake–river systems was ~6.5 years and that for river systems was 6.5–10 years. For the 15- and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f50bc5ed69a86f7ac86a16d8e410f97
https://doi.org/10.1134/s0097807816030039
https://doi.org/10.1134/s0097807816030039
Publikováno v:
Radiochemistry. 57:334-340
Sedimentation rate in deep lakes and estiaries of the Baltic, Pechora, and Laptev Seas was determined using global 137Cs as a sedimentogenesis marker. The sedimentation rate in Lake Ladoga and Levinson- Lessing Lake was 0.3–3 mm year−1, and that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4f426a8ea55efbb9c719b7657eab3572
https://doi.org/10.1134/s1066362215030145
https://doi.org/10.1134/s1066362215030145
Publikováno v:
Radiochemistry. 56:319-324
For a sample including 22 lakes, the 137Cs concentrations in water were determined by the sorption-diffusion model. The 137Cs levels in waters of lakes of the Kola Peninsula and Karelian Isthmus are satisfactorily described by the suggested model at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba8a0894c237e4f40b10d617c1133cd0
https://doi.org/10.1134/s1066362214030163
https://doi.org/10.1134/s1066362214030163
Publikováno v:
Lithology and Mineral Resources. 49:177-183
Sedimentation rate of suspensions (0.3–18.2 mm/yr) was determined on the basis of layer-by-layer distribution of 137Cs (global and Chernobyl) in the cores of bottom sediments (BS) from 16 lakes located in the high and moderate latitudes of the Nort
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8840804febb7665539a8c3d09542cc33
https://doi.org/10.1134/s0024490214020023
https://doi.org/10.1134/s0024490214020023
Publikováno v:
Water Resources. 39:556-563
The state of radioactive pollution of Lake Ladoga has been studied. The purification half-life of lake water from 90Sr was found to be 21.7 year. The ratio of 90Sr storage in lake water volume to its storage in silts (0–10 cm layer) was 2: 1. Lake
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15e2950a972d31a9df7a6a60338d44fb
https://doi.org/10.1134/s0097807812050028
https://doi.org/10.1134/s0097807812050028
Publikováno v:
Radiochemistry. 54:205-210
Regional differences in the 90Sr transfer from catchment areas to rivers of the European Russian North and Eastern Siberia and in the rates of natural water clearance were revealed. The annual 90Sr transfer was 0.5–0.6 and 0.2–0.3%, respectively,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78eb854da31df31a0a0adc415f095ac7
https://doi.org/10.1134/s1066362212020191
https://doi.org/10.1134/s1066362212020191