Iodine isotopes in surface water in the Northeast Asia

被引:2
|
作者
Kuzmenkova, N. [1 ,5 ]
Liu, J. L. [3 ]
Xing, S. [2 ]
Petrov, V. [1 ]
Rozhkova, A. [1 ,5 ]
Filatova, D. G. [1 ]
Egorin, A. [4 ]
Tokar, E. [4 ]
Liu, Q. [3 ]
Shi, K. L. [2 ]
Kalmykov, S. [1 ]
机构
[1] Lomonosov Moscow State Univ, Dept Chem, Leninskie Gory 1 Bldg 3, Moscow 119991, Russia
[2] Langzhou Univ, Sch Nucl Sci & Technol, Tiashiu South Rd 222, Lanzhou 730000, Peoples R China
[3] Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Shaanxi Key Lab Accelerator Mass Spectrometry Tec, Xian AMS Ctr,Inst Earth Environm, Xian 710061, Peoples R China
[4] RAS, Far East Branch, Inst Chem, Pr 100 Letia Vladivostok 159, Vladivostok 690022, Russia
[5] RAS, Vernadsky Inst Geochem & Analyt Chem, St Kosygin 19, Moscow 119991, Russia
基金
俄罗斯科学基金会;
关键词
Iodine isotopes; Iodine-129; Sea and fresh water; Northeast Asia; RETROSPECTIVE DOSIMETRY; ATMOSPHERIC TRANSPORT; CHERNOBYL ACCIDENT; I-131; DEPOSITION; I-129; SEAWATER; SOILS; SPECIATION; SEA; RECONSTRUCTION;
D O I
10.1007/s10967-022-08726-y
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Iodine isotopes (I-129 and I-127) in the fresh and sea water of Lake Khanka and the Sea of Japan (Peter the Great Bay) were determined. The measured concentration of I-129 in the seawater is (1.87-2.33) x10(7) atoms/L and (29.0-39.9) x10(7) atoms/L in the lake water. The I-129/ I-127 atomic ratios in the fresh water [(0.87-1.13) x10(-8)] are two orders of magnitude higher than those in the sea water [(0.91-1.15) x10(-10)]. I-129 was flowed into sea from the river, deposited and quickly diluted in the seawater, causing a declined I-129 concentration. The orders of magnitude higher stable I-127 concentration in seawater compared to the fresh water enlarged the difference on the I-129/I-127 atomic ratios.
引用
收藏
页码:1093 / 1099
页数:7
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