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Environmental Geochemical Characteristics of Selenium in Northeast China

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Abstract—

Selenium is an important element for human health. Many studies have identified selenium deficiency in soil and water as an important factor in causing Keshan Disease (KD) in Northeast China. Previous studies have mainly focused on soil selenium content, staple food selenium content, and human selenium level, but there are few systematic studies on soil selenium’s existing forms and their migration from soil to crops and the human body. This paper focused on inferring the barrier factors in the migration of selenium from soil to crop and the human body and transformation of its compounds. It provides a reference basis for the etiological analysis, prevention, control, and elimination of KD. The study used 121 183 samples of topsoil (0−20 cm), 30 295 soil parent samples of selenium and other geochemical indices in northeast China, and crop seeds and human hair samples from the KD endemic area. The surface soil selenium was dominantly selenium-sufficient in Northeast China. However, the soil selenium levels were generally low. The average topsoil selenium in Northeast China was 0.20 mg/kg, significantly lower than the world’s average soil selenium content (0.4 mg/kg) and slightly lower than the Chinese average soil selenium content (0.24 mg/kg). Soil selenium mainly existed in strongly bounding by organic bound, with humic acid, and residue forms. The amount of selenium available to plants was sufficient in the selenium-sufficient and KD-endemic areas. However, the average selenium content of human hair was deficient, on average, with 0.16 mg/kg in KD endemic area. We assume that lower soil selenium content may be the basic factor influencing the biogeochemical deficiency of selenium in Northeast China. The sequestration of selenium by clay chemical constituents, such as iron and aluminum oxides and soil organic matter, especially in acidic soils, is another direct contributing factor to the low selenium content in biogeochemical food chain, which increases the risk of KD in the population.

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ACKNOWLEDGMENTS

We would like to express our sincere acknowledgements to the Associated editor (Dr. V.V. Ermakov) and anonymous reviewers for their critical and constructive comments and suggestions.

Funding

This work was supported by the International Geological Correlation Programs (IGCP665) and China Geological Survey (DD20160316 and DD20190520).

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Authors and Affiliations

  1. Shenyang Center of China Geological Survey, 110034, Shenyang, PR China

    H. M. Dai, Y. H. Zhang, S. Liang, C. Q. Chen, K. Liu & Y. H. Song

  2. Key Laboratory of black soil Evolution and Ecological Effect, Ministry of Natural Resources, 110034, Shenyang, China

    H. M. Dai, Y. H. Zhang, S. Liang, C. Q. Chen, K. Liu & Y. H. Song

  3. Key Laboratory of black soil Evolution and Ecological Effect, 110034, Shenyang, Liao Ning Province, China

    H. M. Dai, Y. H. Zhang, S. Liang, C. Q. Chen, K. Liu & Y. H. Song

  4. V.V. Dokuchaev Soil Science Institute, 111019, Moscow, Russia

    I. Savin

  5. Natural Resources Survey Institute of Heilongjiang Province, 150036, Harbin, PR China

    Y. J. Cui

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  1. H. M. Dai
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Dai, H.M., Savin, I., Zhang, Y.H. et al. Environmental Geochemical Characteristics of Selenium in Northeast China. Geochem. Int. 62, 314–326 (2024). https://doi.org/10.1134/S0016702923020106

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