Issues

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2020

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vol. 18 /

Issue 3

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A. V. Panko, I. G. Kovzun, V. A. Prokopenko, O. M. Nikipelova, O. A. Tsyganovich,, V. O. Oliinyk, K. E. Panova
«Influence of Nanostructured Iron–Aluminosilicates on Catastrophic Processes on Marine Slopes and Artificial Dams»
599–618 (2020)

PACS numbers: 47.61.Ne, 83.80.Nb, 91.50.Jc, 91.67.Ty, 92.10,Wa, 92.20.Vn, 92.40.Gc

Using modern physicochemical methods, the colloidal, nanochemical, and nanostructural transformations of suspensions of iron–aluminosilicate compositions are investigated in model geomechanochemical biocolloid processes. Mechanisms of catastrophic processes and their effect on highly dispersed nanostructured deep marine pelitic sediments in combination with coarse-dispersed carbonate–iron–aluminosilicate sand (turbidites) are considered. Model conditions for displacement of marine turbidite–pelitic compositions in the composition of coastal shelf silt with a depth of up to 200 m and underwater continental slopes at depths of 200–2000 m as well as their behaviour at depths of 2–8 km and interaction in deep water (under 8–10 km) intercontinental trenches and dips with magmatic semi-molten iron–aluminosilicate materials are also considered. The mechanisms of complex processes of formation, displacement, flow as well as coagulation–condensation nanostructuring and compaction of iron–aluminosilicate compositions with the preservation of the developed nano- and microporous state are first considered and substantiated according to the laws of physicochemical geomechanics and colloidal nanoscience. The role of the wind and thermal influences as well as their superficial turbulent and underwater laminar (thermophilic) waves on the flowing of iron–aluminosilicate sediments during catastrophic phenomena is considered. The important role and influence on such phenomena of effects of hyperanomaly and ultraanomaly of viscosity of iron–aluminosilicate dispersions during their transition from elastic state to plastic one is mentioned. The corresponding models of the mentioned phenomena and the accompanying rheological processes are given.

Keywords: catastrophic phenomena, rheology, sea sediments, biocolloidal transformations, nanostructural transformations

https://doi.org/10.15407/nnn.18.03.599

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