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Рынок труда является составной частью рынка экономических ресурсов. Полноценный национальный рынок труда формируется под влиянием ряда факторов, обеспечивающих единство как экономики страны в целом, так и отдельных ее подсистем. Как экономическое явление рынок труда возникает не сам по себе, а в силу наличия рыночных отношений в экономике и достижения определенного уровня их развития.

The present article describes the practical methods of solution to Molodenskiy's problem. The solution uses the integral equation for the density of a single layer and the corresponding formulas for the heights of the quasigeoid and the deflections of the vertical. (Author), Trans. from Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy (USSR) 11p 1971, by John M. Willis.

A method of simultaneous adjustment of geodetic coordinates and quasigeoid heights is described. It is proposed to alternate the preliminary adjustment of the individual triangulation links with the calculation of quasiqeoid heights at the astronomic net stations by means of Molodenskiy's formula for astrogravimetric leveling. (Author), Trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Sbornik (USSR) n176 p59-67 1969, by John M. Willis.

The method of adjusting an astrogeodetic net model is illustrated on a model net. The computation results are tabulated and the overall total is given. (Author), Trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy (USSR) n176 p68-87 1969, by John M. Willis.

The paper considers the problem of allowing for the effect of the central zone on the value of Molodenskiy's correction G sub 1 to the gravity anomaly delta g. The value of the correction may be unstable when the radius L of that zone is varied. In the general case, the elevation of the integration surface should be represented in its separate parts as a function of the plane coordinates, permitting the calculation of second derivatives., Trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy (USSR) n176 p88-97 1969, by John M. Willis.

The boundary condition for the disturbing potential used in the theory of the earth's figure may be set up for the surface to be determined, and need not be referred to the sphere or ellipsoid in the case of determining a regularized geoid, nor to the surface which is obtained by plotting only normal heights from the reference surface when studying the earth's surface and its exterior gravity field. Errors arising from integration on an unknown surface do not exceed the products T zeta/R or TO, where zeta is the quasigeoidal or geoidal height, R is the earth's radius, and O is the plumbline deflection. The above errors are evaluated in more detail in the case of Molodenskiy's solution to determine the figure of the regularized geoid with a relative error on the order of the square of the earth's flattening. No need arises to determine the vertical gravity gradient. (Author), Trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy (USSR) n176 p9-14 1969, by John M. Willis.

Molodenskiy's integral formulas for radial and lengthwise displacements in the preliminary calculation of a triangulation by the method of development, as compared with their variant given in the monograph by Molodenskiy and others, are refined by recognizing that the angle between the normals to the quasigeoid and reference ellipsoid differs from the plumbline deflection on the physical surface of the earth., Trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy (USSR) n176 p54-58 1969, by John M. Willis.

Metody Vychisleniya na Osnove Intergralnogo Uravneniya Molodenskogo dlya Vozmushcayushchego Potentsyala, trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy (USSR), v157 p1-46 1965.

O Popravkakh za Silu Tyazhesti pri Nivelirovanii v Vysokogornom Raione, trans. of Geodeziya i Kartografiya (USSR), n10 p3-7 1965.

It is demonstrated that the method proposed by I. F. Monin (Astronomicheskiy zhurnal (Astronomical Journal). 1963, XL, No. 1, pp. 179-183) is not applicable to practical use. It is further shown that the first and the second methods of Molodensky (Trudy TsNIIGAiK (Transactions of the Central Scientific-Research Institute of Geodesy, Aerial Surveying, and Cartography), 1949, issue 68, 5-11, and 1960, issue 131) of numerical solution of his integral equation for density of a single layer substituted for the attraction of anomalous masses in the interior of the Earth promptly lead to a higher accuracy than that of the Stokes' theory applied to the real Earth. The results of calculations carried out (Trudy TsNIIGAiK, 1950, issue 75, 11-77, and 1954, issue 103, 65-117) by Yeremeyev and Yurkina in accordance with the first of these methods are also much more accurate as compared with the Stokes' approximation, and are in fact near the correct values. (Author), Zamechaniya po Povodu Kratkogo Soobshcheniya I. F. Monina o Vychislenii Uklonenii Otvesa, trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy (USSR) v157 p135-8 1965.

On the basis of the solution proposed by Molodenskiy for his integral equation of density of a single layer on the physical surface of the Earth (the said layer being substituted for the attraction of all the anomolous masses in the interior of the Earth), expressions for determining the second vertical derivatives of the disturbing potential were obtained. (Author), Vychislenie Pervoi i Vtoroi Vertikalnykh Proizvodnykh Sily Tyazhesti po Kartam ee Anomaliy, trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy. (USSR) v157 p116-24 1965.