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D. V. Georgievskii and A. S. Kirillov, "Acceleration and deceleration of a heavy viscoplastic layer (glacier) along an inclined plane," Mech. Solids. 38 (3), 88-94 (2003)
Year 2003 Volume 38 Number 3 Pages 88-94
Title Acceleration and deceleration of a heavy viscoplastic layer (glacier) along an inclined plane
Author(s) D. V. Georgievskii (Moscow)
A. S. Kirillov (Moscow)
Abstract The problem of deformation of a heavy viscoplastic layer with high viscosity on an inclined plane models the behavior of geophysical structures on an inclined bed in the gravity field. Such structures include snow-dust avalanches formed by soft snow [1], yielding parts of the upper layers of the earth crust [2, 3], rock salt in a limit state [4], rain-induced landslide [5], and glacier formations [6]. The latter are characterized by a massive non-deformable crust occupying about 95% of the glacier thickness and a thin shear layer at its base. The fact that ice has a viscoplastic nature was noted in [7, pp. 166]: "Since no ultimate long-term strength has been observed in ice, we introduce the notion of its "virtually ultimate state" in which the time-evolution of its deformation is so insignificant that further deformation may be assumed absent... one can define long-term strength, which is of great importance for characterizing the time-evolution of the bearing capacity of ice." This long-term strength is in fact the shear yield stress. Experimentally determined values of material functions for a wide range of ice structures and snow flows of avalanche type can be found in the review [8].

Steady-state plane-parallel motion of a viscoplastic layer on an inclined plane is one of the classical problems studied long ago [9]. In this motion, the region next to the free surface of the layer is occupied by a rigid zone, which is always present and may fill up the entire layer, provided that the gravity force is insufficient for flow initiation. The stability of this flow with respect to two-dimensional perturbations was studied in [10]. There exist numerous generalizations of this problem for viscoplastic fluids with nonlinear viscosity or elastic compressibility and for double-layer or stratified flows [11].

On the other hand, there are many investigations of the motion of phase boundaries in materials subjected to nonstationary shear. In such problems, boundary conditions are prescribed on an unknown boundary whose motion is found in the process of solving the problem (problems of Stefan type). Monograph [1] contains a fairly complete review of the studies regarding unsteady deformations, with the motion of rigid zones taken into account.

In the present paper, we determine the parameters of the nonstationary one-dimensional shear of a viscoplastic layer on an inclined plane in the gravity field. We determine the time-variation of the thickness of the rigid zone near the free boundary, as well as some other characteristics of the flow. The problem with unknown boundary is reduced to a problem with a boundary fixed in time. A method is proposed for solving problems similar to the one just mentioned. We study the asymptotic behavior of solutions as t→∞ in the case of the Reynolds number being much smaller than the Froude number.
References
1.  M. E. Eglit, "Dynamics of snow avalanches," Trudy. Matem. In-ta AN SSSR, Vol. 186, pp. 162-167, 1989.
2.  Kh. Ramberg, The Gravity Force and Deformations of the Earth Crust [in Russian], Nedra, Moscow, 1985.
3.  W. K. Nowacki, "On the dynamics description of the rock failure process," Arch. Mech. Stosow., Vol. 38, No. 1-2, pp. 25-37, 1986.
4.  A. K. Chernikov, "Variational methods for problems of viscoplastic salt rock flow," Izv. Vuzov. Gorny Zh., No. 10, pp. 29-33, 1985.
5.  A. Ya. Sagomonyan, "Rain erosion of soil on hill slopes," Vestnik MGU [Bulletin of Moscow State University], Ser. 1, Mat. Mekh., No. 4, pp. 28-34, 2000.
6.  B. A. Savel'ev and D. A. Latalin, "Artificial ice platforms," in Advances in Science and Technology. Ser. Oceanology. Volume 7 [in Russian], pp.  3-193, VINITI, Moscow, 1986.
7.  B. A. Savel'ev, Glaciology [in Russian], Izd-vo MGU, Moscow, 1991.
8.  A. N. Nazarov, "Principles of mathematical modeling of friction and entrainment in flows of avalanche type," Vestnik MGU [Bulletin of Moscow State University], Ser. Mat. Mekh., No. 4, pp. 79-85, 1995.
9.  M. P. Volarovich, "A study of rheological properties of dispersed systems," Kolloidn. Zh., Vol. 16, No. 3, pp. 227-240, 1954.
10.  D. V. Georgievskii, Stability of Deformation Processes in Viscoplastic Bodies [in Russian], Izd-vo URSS, Moscow, 1998.
11.  A. T. Listrov and A. D. Chernyshev, "On steady-state flow of a viscoplastic medium with nonlinear viscosity," Doklady AN. SSSR, Vol. 158, No. 4, pp. 805-807, 1964.
12.  P. M. Ogibalov and A. Kh. Mirzadzhanzade, Nonstationary Motion of Viscoplastic Media [in Russian], Nauka, Moscow, 1977.
13.  A. A. Il'yushin, "Deformation of viscoplastic bodies," Uchen. Zapiski MGU, Mekh., Vol. 39, pp. 3-81, 1940.
14.  G. I. Barenblatt and A. Yu. Ishlinskii, "On the impact of a viscoplastic beam against a rigid obstacle," PMM [Applied Mathematics and Mechanics], Vol. 26, No. 3, pp. 497-502, 1962.
15.  S. N. Kruzhkov, "On some problems with unknown boundary for the heat equation," PMM [Applied Mathematics and Mechanics], Vol. 31, No. 6, pp. 1009-1020, 1967.
16.  A. V. Gnoevoi, D. M. Klimov, A. G. Petrov, and V. M. Chesnokov, "Flow of a viscoplastic medium between parallel circular plates moving toward or away from one another," Izv. AN. MZhG [Fluid Dynamics], No. 1, pp. 9-17, 1996.
Received 15 January 2003
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