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Astrakhan–Mangyshlak Water Conduit. The Corrosion State on the Internal Surface and Methods for Its Corrosion Protection. Part I. Corrosion Deposits

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Abstract

The operation conditions of the inner surface of the long-distance Astrakhan–Mangyshlak fresh-water main and the properties of corrosion deposits on it are considered. It is shown that most of the surface operates in a weakly mineralized fresh water with a yearly temperature variation of no more than 14°C and in conditions of almost complete deaeration. The properties and composition of the deposits change along the pipeline symbatically with the water composition.

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REFERENCES

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Authors and Affiliations

  1. Karpov Research Institute of Physical Chemistry (Russian State Scientific Center), ul. Vorontsovo pole 10, Moscow, 103064, Russia

    I. I. Reformatskaya, I. I. Ashcheulova, S. G. Prutchenko & D. V. Kostin

  2. Research Institute of Water Supply, Sewerage, Hydraulic Structures, and Engineering Hydrogeology, Moscow, Russia

    G. A. Ivleva

  3. The Western Affiliation of KazTransOil, Aktau, Kazakhstan

    T. S. Taubaldiev & S. K. Murinov

  4. Research Institute of Oil and Water, Almaty, Kazakhstan

    K. Kh. Tastanov

Authors
  1. I. I. Reformatskaya
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  2. I. I. Ashcheulova
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  3. G. A. Ivleva
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  4. T. S. Taubaldiev
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  5. S. K. Murinov
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  6. K. Kh. Tastanov
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  7. S. G. Prutchenko
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  8. D. V. Kostin
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Reformatskaya, I.I., Ashcheulova, I.I., Ivleva, G.A. et al. Astrakhan–Mangyshlak Water Conduit. The Corrosion State on the Internal Surface and Methods for Its Corrosion Protection. Part I. Corrosion Deposits. Protection of Metals 38, 590–594 (2002). https://doi.org/10.1023/A:1021226222535

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  • DOI: https://doi.org/10.1023/A:1021226222535

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