Vol. 2 No. 2 (2019)
Open Access
Peer Reviewed

IDENTIFICATION OF BURIED ARCHEOLOGICAL OBJECTS WITH RADIAL DERIVATIVES OF MICRO GRAVITY DATA

Authors

Muhammad Zuhdi , Bakti Sukrisna , Syamsuddin Syamsuddin

DOI:

10.29303/ipr.v2i2.25

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Received: Mar 16, 2019
Accepted: May 30, 2019
Published: May 30, 2019

Abstract

The development of recent gravimetric technology allows us to measure gravity anomalies with accuracy of micro Gal. Micro gravity is able to detect very small gravity anomalies such as anomaly due to buried archeological objects below the earth surface. Radial Derivatives of gravity data is used to sharpen anomaly due to lateral changes of density contrast. Horizontal derivatives carried out by previous researchers have some weaknesses, i.e. the loss of derivative values in certain directions and inconsistence values at the source boundary of the same anomaly edge. To solve the horizontal derivative problem, a radial derivative is made. Radial derivative is derivative of gravity anomaly over horizontal distance in the radial direction from a certain point which is considered as the center of anomaly. There are two kind of radial derivative i.e. First Radial Derivative (FRD) and Second Radial Derivative (SRD). Blade Pattern is another way to enrich the ability of SRD to detect boundary of anomaly source. Synthetic gravity data of buried archeological object was made by counting the response of forward modelling. All of programs and calculation of the models in this research is performed based on Matlab® program. The results of the tests on the synthetic data of the model show that the radial derivative is able to detect the boundaries in buried temples due to density contrast. The advantage of radial derivatives which is a horizontal derivative in the direction of radial compared to ordinary horizontal derivatives is the ability to detect vertical boundaries of various anomaly due to horizontal layers and capable of showing density contrast in almost all directions.

References

Tsuboi and Kato (1952). The First and Second Vertical Derivative of Gravity, Journal of Physics of The Earth. Vol 1, no 2.

Rao, B.S.R., Murthy, I.V.R., and Rao, Y.S.F.,1971, A Second Derivative Method of Interpretation of Gravity Anomalies of Anticlines,Geophysics Department, Andhra University, Waltair, India.

Abdelrahman, E. M., El-Araby, H. M., El-Araby, T. M., and Abbo-Ezz, E. R., 2003, A least-squares derivatives analysis of gravity anomalies due to faulted thin slabs, Geophysics, Vol. 68, No. 2 (March-April 2003); P. 535–543, 11 Figs., 3 Tables.10.1190/1.1567222

Oruc, B., 2010, Edge Detection and Depth Estimation Using a Tilt Angle Map from Gravity Gradient Data of the Kozaklı-Central Anatolia Region, Turkey, Pure Appl. Geophys. 2010 Springer Basel AG DOI 10.1007/s00024-010-0211-0

Aydogan, D., 2011, Extraction of lineaments from gravity anomali maps using the gradient calculation: Application to Central Anatolia, Earth Planets Space, 63, 903–913, 2011

Tatchum, C.N., Tabod, T. C., Koumetio, F., and Manguelle-Dicoum, E., 2011, A Gravity Model Study for Differentiating Vertical and Dipping Geological Contacts with Application to a Bouguer Gravity Anomali Over the Foumban Shear Zone, Cameroon, Geophysica (2011), 47(1–2), 43–55.

Aku, M. O., 2014, Application Of Second Vertical Derivative Analytical Method To Bouguer Data For The Purpose Of Delineation Of Lithological Boundaries, Science World Journal Vol 9 (No 3) 2014

Askari, A., 2014, Edge detection of gravity anomali sources via the tilt angle, total horizontal derivative, total horizontal derivative of the tilt angle and new normalized total horizontal derivative, Scholars Journal of Engineering and Technology (SJET) ISSN 2321-435X (Online) Sch. J. Eng. Tech., 2014; 2(6B):842-846 ISSN 2347-9523 (Print)

Wahyudi. E. J., Kynantoro, Y., and Alawiyah, S., 2016, Second Vertical Derivative Using 3-D Gravity Data for Fault Structure Interpretation, International Conference on Energy Sciences (ICES 2016) IOP Publishing IOP Conf. Series: Journal of Physics: Conf. Series 877 (2017) 012039 doi :10.1088/1742-6596/877/1/012039.

Muhammad Zuhdi, Sismanto, Ari Setiawan, Jarot Setyowiyoto, Adi Susilo, Muhammad Sarkowi, Radial Derivative And Radial Inversion For Interpreting 4D Gravity Anomaly Due To Fluids Injection Around Reservoir. Telkomnika, Vol.16, No.6, December 2018, pp.2855~2863

Kadir, W. G. A., 1999, “Survey Gravitasi 4D dan dinamika Sumber Bawah Permukaanâ€: Proceeding Himpunan Ahli Geofisika Indonesia, 94-99.

Author Biographies

Muhammad Zuhdi, FKIP Universitas Mataram

I was born in Yogyakarta at Desember 29th, 1970. Graduated at Geophysics Dept. Universitas Gadjah Mada. Get Master Degree from Geeophysics Dept. Institut Teknologi Bandung.

Bakti Sukrisna, FMIPA Universitas Mataram

I was born in surakarta 56 years ago.

Syamsuddin Syamsuddin, FMIPA Universitas Mataram

I was born in Bima 48 years ago.

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How to Cite

Zuhdi, M., Sukrisna, B., & Syamsuddin, S. (2019). IDENTIFICATION OF BURIED ARCHEOLOGICAL OBJECTS WITH RADIAL DERIVATIVES OF MICRO GRAVITY DATA. Indonesian Physical Review, 2(2), 84. https://doi.org/10.29303/ipr.v2i2.25