This article has developed a mathematical model of energy processes of Earthquakes of South Kyrgyzstan. Here, an end-to-its-characterized regulatory solution to a one-dimensional reverse problem of seismic was built here.
The author revealed, from the point of view of the practical task of seismic, the best method is the end-and-playing method, which needs to establish the stability of the solution.
Keywords: the natural phenomenon, earthquake, seismic equations, energy process, of course, regulatory solution, Aikonal method, task, method of highlighting features,inverse task.
Introduction. Earthquake. It is known that an earthquake is tectonic deformations of the earth's crust, due to accumulating stress, which come to the surface of the earth in the form of shocks in different power [2]. With each earthquake in the bowels of the Earth, a certain amount of energy is released, which accumulated constantly and continuously. To identify, recognize natural phenomena preceding earthquakes, monitoring (constant tracking) is carried out behind the time (or invariable) physical conditions in the area under consideration, the characteristics of the waves and deformation of the rocks.
To achieve such goals, it is necessary to develop new effective methods of mathematical modeling [8].
1. Formulation of the task. For the seismic equation, consider the reverse task:
where —
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Let the solution of the direct task be given, to solve the inverse task,
Let the conditions be met with respect to the coefficients of the equation
where
Equation (1) is an equation of hyperbolic type, so the task can be considered in the field of ∆(Т) [1]:
The inverse task
is to determine
Let's denote by
The singular and regular part of the solution of the direct decision (1) -(2) will be allocated according to the method of V. G. Romanov (the method of allocating features) for this purpose we present the solution of the problem in the form of [1]:
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where
The last calculations are substituted into equation (1), and we get
Collect the members at the same coefficients
Then we will
To
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To
If we consider that
The inverse problem (13)
— (15) is to define
afunction,
If we define functions
we can also define an unknown function
Using the D'Alembert formula for a direct task (13), (14), we get a solution to a direct problem [7]:
With (17)
2. Let's build a finite difference solution. Let's introduce a grid area for solving problem (13)-(15):
where
The difference analogue of the differential equation (13) will be:
From (19) we get
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From the last expressions we can get the recurrence formula [3]:
The last expressions are substituted sequentially in the right part (21), and also again writing the same recurrent formula and supplying it to (21) and continuing this process we get a difference analogue of the integral formula of Alembert(17):
Suppose that in the last formula (22)
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The difference formulas (22) and (23) constitute a system of difference nonlinear equations of the second kind.
In the difference analogue (22) we wrote without small quantities
Then for
Let's introduce notation
Given these designations from (24) and (25) we will get estimates
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Let
From the last formula, using a discrete analogue of Gronulla-Bellman, we get
The following theorem on the convergence of the finite-difference solution of the difference task (22), (23) to the solution of the differential decision (13) — (15) is proved.
Theorem 1.
Let the solution of the differential task(14) (15) exist
Build a
finite-difference regularized solution.
Let the additional information about solving the direct decision, for solving the inverse task, be given in the form
Then for
Taking into account the introduced norms, we will evaluate the latest equations
Let
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Then again using the Gronole–Bellman formulas, we get an estimate
And if we consider that the ratings (30), we have
The last estimate is an estimate of the regularized solution of the inverse task.
Theorem 2.
Let the solution of the direct task(13)-(15) exist and let
Of course, the difference regularized solution of the original inverse problem (1) — (3) is obtained from formula (16):
Thus, the finite-difference regularized solution of the inverse problem (1) — (3) has the form:
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- Nikonov A. A. Earthquake. M.:, Znanie (past, present, forecast) 1984, p.192.
- Alimkanov A. A. Numerical method of solving a one-dimensional inverse seismic problem with instantaneous and corded sources. NEWS OF UNIVERSITIES OF KYRGYZSTAN — Bishkek — 2015. — No. 11, Republican Scientific and Theoretical Journal; pp. 3–7.