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Transformations and interfacial interactions in dissipative natural marine geoecological systems (MGES) of sediments consisting of various iron-aluminosilicates play a significant role in the geoecological behavior of the resulting ocean suspensions, which significantly affects the life of mankind. This impact has recently increased many times over due to the growing pollution of the oceans by more than 350 thousand species of surfactants. The study of environmental behavior under the influence of geomechanical, physicochemical, and other factors has just begun. The simplified scheme of the impact of various factors on MGES and preliminary verification of the information already obtained indicate the growing role of geomechanical and physicochemical processes in open MGES, which allowed us to draw several significant conclusions. For example, the acceleration of sediment bottom layers movement due to the reduction of suspension viscosity by the resulting alkaline solutions of various sodium silicates and the increased role of information exchange of contacting dissipation compounds in the MGES are noteworthy. Simplified scheme of influence on the MGES: Entry into the MGES system: Flows of information, energy, and substances entering the system → Accumulation of information, energy, and substances in the new system → Export of excess accumulated information, energy, and new substances from the system.

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Geomechanical and Physicochemical Influences on the Movement of Iron-Aluminosilicate Marine Sediments in the Ocean Depths

  • 会议论文

  • 发表日期：

    2025年

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  • I. G. Kovzun,
  • A. V. Panko,
  • V. A. Prokopenko,
  • O. Yu Voitenko,
  • O. M. Nikipelova

摘要

Transformations and interfacial interactions in dissipative natural marine geoecological systems (MGES) of sediments consisting of various iron-aluminosilicates play a significant role in the geoecological behavior of the resulting ocean suspensions, which significantly affects the life of mankind. This impact has recently increased many times over due to the growing pollution of the oceans by more than 350 thousand species of surfactants. The study of environmental behavior under the influence of geomechanical, physicochemical, and other factors has just begun. The simplified scheme of the impact of various factors on MGES and preliminary verification of the information already obtained indicate the growing role of geomechanical and physicochemical processes in open MGES, which allowed us to draw several significant conclusions. For example, the acceleration of sediment bottom layers movement due to the reduction of suspension viscosity by the resulting alkaline solutions of various sodium silicates and the increased role of information exchange of contacting dissipation compounds in the MGES are noteworthy. Simplified scheme of influence on the MGES: Entry into the MGES system: Flows of information, energy, and substances entering the system → Accumulation of information, energy, and substances in the new system → Export of excess accumulated information, energy, and new substances from the system.