II Development of high – sensitivity dispersion laser interferometer Last years interest to sensitive seismographs was stimulated with possibility to predict earthquake. A key to the understanding of the state of stress of the earth and the association phenomena of tectonic activity and earthquakes is a knowledge of the spatial distribution of the earth strain. The development of the laser as a source of coherent optical radiation has permitted the application of interferometric techniques to the problem of earth strain measurement. In other work authors represent the laser interferometer technique that allows the displacements to be measured with the instrumental resolution up to 1 pm. Besides dispersion interferometers (DI) are currently used for determining the nonlinearity of refraction of optical medium induced by the field of an intense light wave. Areas of application The laser interferometers are found a wide using in measurements of space movements of the objects in the mechanical engineering, geodesy and during geophysical surveys. The high accuracy of positioning is required while processing of sensitive devices for computer engineering and nanoelectronics. Introduction Traditional interferometric methods for measuring using different geometric paths for interacting waves possess disadvantages typical of spatially separated beams: beams propagate in different optical elements along paths with different optical elements along their lengths. The advantage of dispersion interferometers consists in the fact that interacting waves propagate along the same geometric path. Thus, the requirements on both the optical properties of elements (quality, transparency) and stability of individual elements of the optical layout of interferometers drop out. The process of second-harmonic generation in nonlinear crystal has permitted the application of the process of optical frequency conversion to the problem of earth strain measurement and of determination of dispersion of refractive index using dispersion interferometers. The operation of DI was analyzed mainly in constant-field approximation. In the given work it is offered to spend the analysis of process of frequency conversion in DI using the constant-intensity approximation. The analysis of harmonic generation process in the constant-intensity approximation allowed one to suggest a new method of determination of displacement (for example, earth’s strain) and refractive index dispersion. As a result of analysis in this approximation, in contrast to the constant-field approximation, the minima of intensity of the second-harmonic dependent on the phase mismatch. This fact allows simple, reliable way with greater accuracy to define displacement and refractive index dispersion. According to results of the theoretical analysis reception highly sensitive DI with wide frequency and dynamic ranges is expected. Description The proposal offers two variants of the dispersion interferometer. The first variant assumes the case when the between two crystals with quadratic susceptibility the medium is placed. It is shown that second-harmonic intensity is a function of phase difference of interacting waves. The change of length of the medium caused in particularly by the earth strain induces an additional phase difference and this leads to a corresponding shift of the interference function I 2out ( ) along the abscissa. By the comparison of the interference patterns in the presence and the absence of the earth's strain (or of investigated medium), this strain (or dispersion of refraction index) can be determined from the displacement of these patterns. It is obtained that in the constant-intensity approximation definition of zero of a curve of synchronism more precisely, than in the constant-field approximation. Hence expected accuracy in measurement should be above, than in the existing methods of the measurement based on the constant-field approximation. The use of dispersion interferometer with the crystal and medium inside the laser resonator (second variant) allows to increase the interferometer sensitivity. At the exit from the interferometer in the constant-intensity approximation for the first variant of medium location we obtain with the corresponding boundary conditions the following expression for the second-harmonic intensity 2 I first 2, output I 2 ( )e 2 i i i e sin 2 ctg2 1 cctg1 , 2 22 2 2 (1) 2 2 2 , 2 222 , 12 1 2 I10 , 22 1 2 I1 (), first 21 (d ) 2 (d ) , 4 4 are the nonlinear wave coupling coefficients, 1, 2 are the absorptions where 12 212 1, 2 coefficients, 2k2 k1 is the phase mismatch. It can be seen from (1) that secondharmonic intensity is a function of phase difference of interacting waves and oscillates with varying of . At the exit of interferometer the recorded secondharmonic intensity through the phase difference of the both waves depends on the medium parameters. The change of length of the medium (for example, an air gap or gas) caused in particularly by the earth strain induces an additional phase difference and this leads to a corresponding shift of the interference function I 2out ( ) along the abscissa. By the comparison of the interference patterns in the presence and the absence of the earth's strain (or of medium studied) determined from the displacement of these patterns. One of the ways of increase in the conversion efficiency of frequency is the location of a nonlinear crystal inside the optical resonator (see Fig.1). \\inIn this case (the second variant of the DI), owing to the additional multifold passes of a crystal (2), the effective length of a nonlinear interaction increases, and the energy exchange between the waves is mainly determined by the phase relationships. Fig.1 At the exit from the interferometer in the constant-intensity approximation for the second variant the second-harmonic intensity expression has the form 2 i i sec ond i ond 2 e (2) I 2sec sin 2 ctg2 1 ctg2 , ,output I 2 ()e 22 22 2 sec ond 21 2d 2 (2d ) 21 2 , where 1, 2 (2d ) are the phase shifts of the fundamental frequency and harmonic waves in the medium of length d . 1, 2 are the phase shifts experienced by the waves on reflection from the mirror (M2) at frequencies 1 and 21 , respectively. It can be seen from (2) that the second-harmonic intensity is a function of sec ond and oscillates with varying sec ond . Analogously to first variant the change of the medium length induces an additional phase difference and this leads to a corresponding shift of the interference function I 2output( ) along the abscissa. In intracavity frequency conversion, even small phase variations in interacting waves lead to significant variations of the harmonic intensity. Therefore, displacements of phase mismatch can be found by determining these variations. The comparison of the both variants has been performed on the base of the analytical investigation in the constant-intensity approximation. The results of the graphical analysis of the DI function both for the case when the nonlinear crystal is out of the cavity and for the intracavity case is shown (see Fig.2). The use of DI with the crystal and medium inside the laser resonator allows to increase the interferometer sensitivity. The comparison of the curves 1, 2 and 3 shows that by the choice of optimum values of phase mismatching and basic radiation intensity, one can vary not only the interference pattern period, but also the character of I 2output( ) dependence, i.e. the steepness of the curve leading to increase of DI sensitivity. Thus, if the amplification at the laser transition is enough for the intracavity case, then it is reasonable to deal with this variant. Nevertheless, another (first) variant takes place. Fig.2. Dependencies of the second-harmonic intensity on the phase mismatch at 2 21 0.1; 1(1,3,4,6), 0.6 (2,5) and 1 0.5(1,4),1(2,3,5,6) for the intracavity case (1-3) and for the case when the medium is out of the cavity (4-6). Expected accuracy In this work the obtaining of measured values with greater accuracy, rather than in existing ways of definition of displacements of interference patterns is supposed. This statement is based on preliminary researches: -the existing methods of determination of displacements were mainly based on traditional interferometric methods where for measuring using different geometric paths for interacting waves possess disadvantages typical of spatially separated beams: beams propagate in different optical elements along paths with different optical elements along their lengths. The advantage of dispersion interferometers consists in the fact that interacting waves propagate along the same geometric path. Hence, the requirements on both the optical properties of elements (quality, transparency) and stability of individual elements of the optical layout of interferometers drop out. Thus, the new way of definition of displacements, differing from earlier existing the technique is offered. The offered method is more exact, simple and reliable. - the displacements of interference patterns can be determined directly from the experimental measurements of shifts of minima or maxima of secondharmonic intensity; - the position of the zeros of a curve of the synchronism for first three zeros of the dependences of intensity of a harmonic on length of the nonlinear medium, calculated in the constant-intensity approximation are more exact and are correct, than in widely used constant-field approximation. Hence expected accuracy in measurement should be above, than in the existing methods of the measurement based on the constant-field approximation. One of the important stages of the proposal project is creation of pilot equipment for displacements measurement of interference patterns. Within the limits of this project it is necessary to solve a problem of experimental measurement of interference patterns (foe example, an earth's strain). In the scientific plan following steps in the future must be are executed for decision of this problem: 1. Development of construction of experimental equipment for special schemes of displacement measurement (for example, caused by the earth strain)- first variant. 2. Development of construction of experimental equipment for special schemes of displacement measurement (for example, caused by the earth strain) - second variant. 3. Experimental definition of shifts of the interference function (secondharmonic intensity) when the location of the medium inside the laser resonator. 4. Experimental definition of shifts of the interference function (secondharmonic intensity) when the location of the medium out of the cavity. References: 1.Z.H.Tagiev, R.J.Kasumova, R.A.Salmanova, N.V.Kerimova, “Constant Intensity Approximation in the Theory of Nonlinear Waves”, J. Opt. B: Quantum Semiclas. Opt. 3, (2001), 84-87 2.Z.H.Tagiev, R.J.Kasumova, R.A.Salmanova, N.V.Kerimova, “The Theory of Nonlinear Dispersion Interferometers in the Constant Intensity Approximation" Opt.Spectrosk., 2001, v.91, 968-971 [Opt.Spectrosc., 2001, v.91, 909-912].