3.2 A gravity station is located on land at an altitude h average rock density in the area of the station is p 2.67 g/cm. The theoretical value of gravity is g= 980,900.00 mGal, the observed gravity is g 980,700.50 mGal. 1. Calculate the free air correction. 2. Calculate the Bouguer correction. 3. Calculate the free-air gravity anomaly. 4. Calculate the Bouguer gravity anomaly. %3D 500 m above sea level. The Round the results to two decimal places. Useful information Universal gravitational constant G = 6.67-10-11 N-m2/kg?; 1 mGal = 105 m/s²; 1N=1 kg 1 m/s²; T= 3.14.

3.2 A gravity station is located on land at an altitude h average rock density in the area of the station is p 2.67 g/cm. The theoretical value of gravity is g= 980,900.00 mGal, the observed gravity is g 980,700.50 mGal. 1. Calculate the free air correction. 2. Calculate the Bouguer correction. 3. Calculate the free-air gravity anomaly. 4. Calculate the Bouguer gravity anomaly. %3D 500 m above sea level. The Round the results to two decimal places. Useful information Universal gravitational constant G = 6.67-10-11 N-m2/kg?; 1 mGal = 105 m/s²; 1N=1 kg 1 m/s²; T= 3.14.

Elements Of Electromagnetics

7th Edition

ISBN:9780190698614

Author:Sadiku, Matthew N. O.

Publisher:Sadiku, Matthew N. O.

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3.2 A gravity station is located on land at an altitude h 500 m above sea level. The
average rock density in the area of the station is p = 2.67 g/cm3. The theoretical value
of gravity is g= 980,900.00 mGal, the observed gravity is g 980,700.50 mGal.
1. Calculate the free air correction.
2. Calculate the Bouguer correction.
3. Calculate the free-air gravity anomaly.
4. Calculate the Bouguer gravity anomaly.
Round the results to two decimal places.
Useful information
Universal gravitational constant G = 6.67-10-11 N-m2/kg²;
1 mGal = 105 m/s3;
1N =1 kg 1 m/s2;
T = 3.14.

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