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Science Opportunities in Azerbaijan - Science and Technology ...

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<strong>Technology</strong> Profile<br />

Method of Def<strong>in</strong>ition of the L<strong>in</strong>ear Physical-<br />

Mechanical Properties of the Geological<br />

Media <strong>in</strong> Their Natural State<br />

Description<br />

The technology of def<strong>in</strong>ition of true values of the fundamental<br />

elastic moduluses of the l<strong>in</strong>ear elasticity (Lamé coefficients<br />

λ <strong>and</strong> μ, or, that is the same, the Poisson<br />

coefficient ν <strong>and</strong> Е module) of the rocks <strong>and</strong> geological<br />

media <strong>in</strong> their natural states has been de-veloped.<br />

Innovative Aspects <strong>and</strong> Ma<strong>in</strong> Advantages<br />

For the first time the method has been developed that allows<br />

more precisely <strong>and</strong> truly determ<strong>in</strong>e the true values of<br />

fundamental elastic moduluses of the l<strong>in</strong>ear elasticity of the<br />

rocks <strong>and</strong> geological media <strong>in</strong> their natural states, i.e. tak<strong>in</strong>g<br />

unto account their modern geodynamic evolution. This<br />

method operates on the base of field <strong>and</strong> well seismic data.<br />

The exist<strong>in</strong>g <strong>and</strong> widely used (ma<strong>in</strong>ly <strong>in</strong> oil companies)<br />

modern methods (analogues) are based on the l<strong>in</strong>ear theory<br />

of elasticity <strong>and</strong> elastic waves <strong>and</strong> allow determ<strong>in</strong>e only<br />

the effective (“apparent”) values of the required parameters.<br />

The proposed method is based on a more substanti-ated<br />

<strong>and</strong> precise non-classically-l<strong>in</strong>earized theory (NLT) of the<br />

deformed hard materials <strong>and</strong> elastic waves <strong>and</strong> allows<br />

def<strong>in</strong><strong>in</strong>g the true values of those parameters on the base of<br />

<strong>in</strong>formation on velocity of longitud<strong>in</strong>al <strong>and</strong> transverse seismic<br />

waves, non-l<strong>in</strong>ear elastic deformations <strong>and</strong> pressures.<br />

Areas of Application<br />

The method can be used <strong>in</strong> seismic surveys, geophysical<br />

<strong>and</strong> geological surveys of oil companies; seismology; eng<strong>in</strong>eer<strong>in</strong>g<br />

geophysics <strong>and</strong> geology; scientific <strong>in</strong>vestigations<br />

<strong>and</strong> education as well.<br />

Stage of Development<br />

Algorithm of method <strong>and</strong> appropriate computer pack-age<br />

program has been prepared. The <strong>in</strong>terface of the computer<br />

program for usage is be<strong>in</strong>g worked out at present. European<br />

patent for method is <strong>in</strong> process.<br />

The fundamental properties of material, <strong>in</strong>clud<strong>in</strong>g the Poisson<br />

coefficient, should be <strong>in</strong>variant relatively to the level<br />

<strong>and</strong> type of act<strong>in</strong>g external loads <strong>and</strong> for all natural <strong>and</strong> ar-<br />

Contact Details<br />

Institute of Geology<br />

Contact person: Prof. Hatam H. Guliyev<br />

Address: 29 A, H. Javid Avenue<br />

AZ1143, <strong>Azerbaijan</strong>, Baku<br />

Tel: (+994 12) 510 5617<br />

Fax: (+994 12) 497 5285<br />

E-mail: hatam@lan.ab.az<br />

Experimental dependence of Poisson coefficient upon the pressure<br />

(Guliyev, G.G. The def<strong>in</strong>ition of Poisson coefficient <strong>in</strong><br />

stra<strong>in</strong>ed media. Proceed<strong>in</strong>gs of Russian Academy of <strong>Science</strong>s,<br />

2000, vol. 370, №4, pp. 534-537).<br />

tificial materials 0≤ν ≤0,5. The results on figure show that<br />

dur<strong>in</strong>g the experiment the requirements of l<strong>in</strong>ear theory of<br />

elasticity on small deformation <strong>and</strong> the Hooke law have<br />

been distorted. These results reflect the <strong>in</strong>fluences of many<br />

factors that are not taken <strong>in</strong>to account <strong>in</strong> dependencies of<br />

phenomenological theory. The probability of appearance of<br />

such complications us<strong>in</strong>g the real seismic data is high<br />

enough.<br />

Dr. Aghayev Khanlar Boyukaga<br />

E-mail: esmira.agayeva@rambler.ru<br />

19

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