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UNIT 13


                                                    GRAVIMERY



                        I. READING AND LEARNING


                        Task  1.  Read and  memorize  the following  words and word-

                        combinations:
                             altitude – висота над рівнем моря;

                             geodetic grid – геодезична координатна сітка;
                             earth  reference  –  земна  система  координат,  земний
                             орієнтир;

                             perturbing potential – потенціал пертурбації;
                             gravity anomaly – гравітаційна аномалія;
                             oscillation – вібрація, коливання;

                             test mass – дослідницька вага (маса);
                             void – пустота в породі, вакуум;
                             the mass center – центр інерції;

                             the axe of rotation – вісь обертання;
                             integral equation – інтегральне рівняння;
                             gravimeter – гравіметр.


                        Task 2. Read and translate the text.

                                            Text 1. Geodetic gravimetry

                        Geodetic  gravimetry  is  a  section  of  geodesy  dealing  with  the
                  theories and methods of using the results of measurement of the force

                  of  gravity  for  solving  scientific  and  practical  problems  in  geodesy.
                  The basic content of geodetic gravimetry is the theories and methods
                  for determining the external field of the potential W of the force of the

                  Earth’s gravity g from measurements on the Earth’s surface and from
                  astronomical and geodetic materials. It also includes the determination
                  of  altitudes  and  the  treatment  of  astronomical  and  geodetic  grids  in
                  connection with the special features of the Earth’s gravitational field.

                  It is customary to separate from this field the uniform and known field
                  of potential U of the so-called reference earth, which is represented in
                  the form of a level ellipsoid. The mass centers and the axes of rotation

                  of the real and the normal earth coincide. The fundamental problem of
                  geodetic  gravimetry  is  reduced  to  the  derivation  of  the  perturbing
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