Role of Desorption Processes in Transformation of Dissolved Barium Runoff in the Mixing Zone of River Waters and Seawaters: Experimental Modeling Data
- 作者: Savenko A.V.1
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隶属关系:
- Department of Geology, Moscow State University
- 期: 卷 487, 编号 2 (2019)
- 页面: 950-952
- 栏目: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/195351
- DOI: https://doi.org/10.1134/S1028334X19080154
- ID: 195351
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详细
The sorption–desorption barium balance during interaction between silt–sand terrigenous material and salty seawater is determined experimentally. The mean value of barium desorption in the mixing zone of river waters and seawaters is 13 μg/g, making up an additional supply of 80 000 tons of Ba per year, or 8.6% of its runoff to the ocean, without runoff transformation at the river–sea geochemical barrier being taking into account. The obtained estimate of the role played by desorption in transformation of dissolved barium runoff agrees, in terms of the order of value, with the data of real observations for the majority of mouth zones of the world rivers.
作者简介
A. Savenko
Department of Geology, Moscow State University
编辑信件的主要联系方式.
Email: Alla_Savenko@rambler.ru
俄罗斯联邦,
Moscow, 119234
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