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Thixotropic substances. Thixotropy

(from the Greek thixis - touch and trope - turn, change * A. thixotropy of rocks; N. Thixotropie der Gesteine; F. thixotropie des roches; and. capacidad tixotropica de rocas, tixtropia de rocas) - a physicochemical phenomenon that occurs in some colloidal dispersed systems, for example, in cohesive rocks, and consisting in their spontaneous liquefaction under the influence of mechanical action (shaking, stirring, vibration, exposure to ultrasound, etc.) and the subsequent restoration of the structure while eliminating these influences. Thixotropy is explained by the reversible weakening of the structural bonds between the mineral particles of the cohesive rock. Under a certain mechanical action, bound and immobilized water passes into free water, which leads to a decrease in the strength of structural bonds and liquefaction of the rock. Termination of exposure leads to the reverse transition of water from a free to a bound state and hardening of the rock (thixotropic hardening).

Fragility is an indicator characterizing the tendency of rocks to thixotropic softening. It is customary to measure it with the average radius of the base of a cylindrical sample (mm) after vibration at a vibration frequency of 67 Hz and an amplitude of 1 mm. The initial radius of the sample is 8 mm and the height of the cylinder is 20 mm. The value of the fluctuation index varies from 8-9 for non-thixotropic rocks to 15 or more for highly thixotropic rocks. A more general indicator is the structural strength limit under dynamic action, defined as the limiting alternating acceleration at which the rock strength does not decrease. It is measured in m / s 2. Thixotropic hardening is characterized by the recovery time (s), during which the maximum strength of the rock is achieved during recovery.

Thixotropy is determined by the qualitative and quantitative composition of their dispersed phase, the shape of particles and their hydrophilicity, the composition and concentration of pore moisture, etc. The main influence is exerted by the granulometric composition of the rock. Thixotropic phenomena are typical for rocks with a clay particle content of at least 1.5-2%.

Thixotropy is widespread in nature and has both a negative and a positive effect on technological processes in the development of wet cohesive rocks. For example, when transporting such rocks, thixotropic liquefaction causes their intensive adhesion to the working surfaces of the transport equipment, reducing its productivity by 1.5 times. On the other hand, thixotropy is used in drilling and pile driving. Thixotropy is the cause of landslides.

Thixotropy (thixotropy) (from the Greek. θίξις - touch and τροπή - change) - the ability of a substance to reduce the viscosity (liquefy) from mechanical action and increase the viscosity (thicken) at rest.

Thixotropic liquids

Thixotropy should not be confused with pseudoplasticity. For pseudoplastic fluids, the viscosity decreases with increasing shear stress, while thixotropic fluids have a viscosity decreases over time at constant shear stress.

Thixotropic fluids are fluids in which, at a constant strain rate, the shear stress decreases over time.

The viscosity of some fluids at constant ambient conditions and shear rates change over time. If the viscosity of a liquid decreases over time, then the liquid is called thixotropic, if it increases, it is called rheopex.

Both behaviors can occur both together with the types of fluid flow described above, and only at certain shear rates. The time interval can vary greatly for different substances: some materials reach a constant value in a matter of seconds, others in a few days. Rheopex materials are quite rare, in contrast to thixotropic materials, which include lubricants, viscous printing inks, and paints.

Thixotropic liquid

Thixotropic liquids(from the Greek. θίξισ - touch and τροπέ - change) - liquids in which, at a constant strain rate, the shear stress decreases with time.

The viscosity of some fluids at constant ambient conditions and shear rates change over time. If the viscosity of a liquid decreases with time, then the liquid is called thixotropic, and if, on the contrary, it increases, then - rheopex.

Both behaviors can occur both together with the types of fluid flow described above, and only at certain shear rates. The time interval can vary greatly for different substances: some materials reach a constant value in a matter of seconds, others in a few days. Rheopex materials are quite rare, in contrast to thixotropic materials, which include lubricants, viscous printing inks, and paints.

When studying the influence of two parameters (time and shear rate) on the viscosity of materials for thixotropic fluids, the following curves will be obtained. [ clarify]

The descending and ascending curves do not coincide and form a "hysteresis loop", which is caused by a decrease in the viscosity of the fluid during prolonged deformations. This phenomenon can be reversible or not: some systems can regain their initial viscosity after a period of rest, other systems never.

see also

Thixotropy

Rocks (from the Greek thixis - touch and trope - turn, change * a. thixotropy of rocks; n. Thixotropie der Gesteine; f. thixotropie des roches; and. capacidad tixotropica de rocas, tixtropia de rocas) - physical and chemical. a phenomenon that occurs in certain colloidal dispersed systems, for example. in coherent g. p., and consisting in their spontaneous dilution under the influence of mechanical. exposure (shaking, stirring, vibration, exposure to ultrasound, etc.) and subsequent restoration of the structure while eliminating these influences. T. is explained by the reversible weakening of the structural bonds between the mineral particles of the cohesive rock. With a certain mechanical. the impact occurs the transition of bound and immobilized water into free, which leads to a decrease in the strength of structural bonds and liquefaction of the rock. Termination of exposure leads to the reverse transition of water from a free to a bound state and hardening of the rock (thixotropic hardening).
An indicator characterizing the tendency of the g. Item to thixotropic softening is fragility. It is customary to measure it by the average radius of the cylindrical base. sample (mm) after vibration at a vibration frequency of 67 Hz and an amplitude of 1 mm. The initial radius of the sample is 8 mm and the height of the cylinder is 20 mm. The value of the fluctuation index varies from 8-9 for non-thixotropic rocks to 15 or more for highly thixotropic rocks. A more general indicator is the structural strength limit at dynamic. impact, defined as the limiting alternating acceleration, when the rock is not reduced. It is measured in m / s2. Thixotropic hardening is characterized by the recovery time (s), during which the max. rock strength.
T. is determined by qualities. and quantities. the composition of their dispersed phase, the shape of particles and their hydrophilicity, the composition and concentration of pore moisture, etc. Main. influenced by granulometric. composition of the breed. Thixotropic phenomena are typical for rocks with a clay particle content of at least 1.5-2%.
T. is widespread in nature and has both negative and positive. influence on technol. processes in the development of wet cohesive rocks. For example, during the transportation of such rocks, thixotropic liquefaction causes their intensive adhesion to the working surfaces of the transport. equipment, reducing its productivity by 1.5 times. On the other hand, T. is used for drilling and piling. T. is the cause of landslides. A. V. Dugartsyrenov.


Mining encyclopedia. - M .: Soviet encyclopedia. Edited by E. A. Kozlovsky. 1984-1991 .

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Thixotropy

Thixotropy

The ability of certain dispersed systems to liquefy reversibly at sufficiently intense mechanical. exposure (stirring, shaking) and harden (lose) when at rest. T. is a characteristic property of coagulants. structures that can be destroyed an unlimited number of times, and each time their properties are fully restored. Examples of typical thixotropic structures are systems formed during coagulation of aqueous colloidal dispersions of iron hydroxide, aluminum hydroxide, vanadium pentoxide, bentonite suspensions, and kaolin.

Mechanic the properties of thixotropic structures are characterized by the values ​​of three parameters (P. A. Rebinder): the greatest eff. viscosity h 0 practically intact structure, the smallest eff. viscosity h m maximum fractured structure and ultimate shear stress P 0 . Dependence eff. viscosity h on the applied shear stress P can be described by ur-niy

For small values P that do not violate rest or cause a very slow flow, the structure has the properties of a solid, since its recovery under these conditions exceeds the rate of destruction. At R>>R 0, the system turns out to be extremely destroyed and has a low viscosity h m... The magnitude P 0 characterizes an unbroken structure. The process of restoring a destroyed structure at rest can be characterized by an increase in strength over time.

In some cases, the application of small P and deformation at a low rate accelerates the growth of strength and structuring of dispersed systems; this phenomenon is called. reopex and e y. Sometimes concentrated dispersed systems (pastes) exhibit dylatans and I - an increase in h with an increase in the deformation rate, accompanied by a certain increase in the volume occupied by the system: upon deformation, solid particles form a looser framework and the existing liquid medium turns out to be not enough to provide the system.

T. dispersed systems has a great practical. meaning. Thixotropic properties must be possessed by greases, paints and varnishes, ceramic. masses, flushing, used when drilling wells, pl. food products. I. H. Vlodavets.

Physical encyclopedia. In 5 volumes. - M .: Soviet encyclopedia. Chief Editor A.M. Prokhorov. 1988 .


Synonyms:

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