A METHOD FOR COMPUTATION OF MEAN GRAVITY INSIDE THE EARTH FOR INCREASING ACCURACY OF ORTHOMETRIC COMPUTATIONS

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AZMOUDEH ARDALAN A.A.; JAZAERI JONGHANI S.SH.

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Journal: Journal of the Earth and Space Physics Year:2005 | Volume:31 | Issue:2 Page(s): 35-44

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Information Journal Paper

Title

A METHOD FOR COMPUTATION OF MEAN GRAVITY INSIDE THE EARTH FOR INCREASING ACCURACY OF ORTHOMETRIC COMPUTATIONS

Author(s)

AZMOUDEH ARDALAN A.A. | JAZAERI JONGHANI S.SH. | Issue Writer Certificate

Keywords

HEIGHTQ3

ORTHOMETRIC HEIGHTQ4

GRAVITY ACCELERATIONQ4

GRAVITY FIELD MODELINGQ4

GRAVITY FIELD INSIDE THE EARTHQ4

Abstract

In this paper a method for computation of mean gravity value within the Earth between the computation point and the geoid needed for precise orthometric HEIGHT computations is presented.The method presented is based on following steps: (1) computation of the global and regional gravity effects using ellipsoidal harmonic expansion to degree and order 360 plus the centrifugal acceleration. (2) Computation of the gravitational effect of terrain masses within the radius of 55km around the computational point applying Newton integral in the equal area map projection. (3) Computation of the gravity at two points on the surface of the Earth and on the geoid using steps 1-2, computing mean and standard deviation of the computed gravity values and increasing the number of points within the Earth to meet the predefined standard deviation for the computation of mean gravity within the Earth. (4) Deriving the mean gravity within the Earth from the steps 1-3. The proposed method for the computation of mean gravity within the Earth is checked against the observed gravity values within the Earth in an exploration borehole. The test computations are made in the following two modes: (a) Computation of gravity values at the observation points in the borehole and comparison of the computed values with the observed values (b) Computing mean gravity within the Earth using the proposed method and the observed gravity values. According to the test computations at a depth of 474.7 m computed gravity differs from the observed gravity by 10.768 mGal and the computed mean gravity from the observed mean gravity by 5.56 mGal.

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APA: Copy

AZMOUDEH ARDALAN, A.A., & JAZAERI JONGHANI, S.SH.. (2005). A METHOD FOR COMPUTATION OF MEAN GRAVITY INSIDE THE EARTH FOR INCREASING ACCURACY OF ORTHOMETRIC COMPUTATIONS. JOURNAL OF THE EARTH AND SPACE PHYSICS, 31(2), 35-44. SID. https://sid.ir/paper/80337/en

Vancouver: Copy

AZMOUDEH ARDALAN A.A., JAZAERI JONGHANI S.SH.. A METHOD FOR COMPUTATION OF MEAN GRAVITY INSIDE THE EARTH FOR INCREASING ACCURACY OF ORTHOMETRIC COMPUTATIONS. JOURNAL OF THE EARTH AND SPACE PHYSICS[Internet]. 2005;31(2):35-44. Available from: https://sid.ir/paper/80337/en

IEEE: Copy

A.A. AZMOUDEH ARDALAN, and S.SH. JAZAERI JONGHANI, “A METHOD FOR COMPUTATION OF MEAN GRAVITY INSIDE THE EARTH FOR INCREASING ACCURACY OF ORTHOMETRIC COMPUTATIONS,” JOURNAL OF THE EARTH AND SPACE PHYSICS, vol. 31, no. 2, pp. 35–44, 2005, [Online]. Available: https://sid.ir/paper/80337/en

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