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Gravity Method By Dr. Amin E. Khalil
11

Gravity method

May 21, 2015

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Amin Khalil

undergraduate gravity lecture
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Page 1: Gravity method

Gravity Method

ByDr. Amin E. Khalil

Page 2: Gravity method

M1M2 R

2

21

r

MMGF

Page 3: Gravity method

Newton 2nd law

gMF hence

2

212

r

MMGgM

Then

2r

MGg

Page 4: Gravity method

r

R = radius of the earth

6371

km

Earth is considered as sphere and hence radius is constant.

Ideal

Page 5: Gravity method

RealEarth is not sphere and hence radius is not constant.

Hence correction must be applied

Page 6: Gravity method

Why corrections?

Because many factors affect the value of g. As an example:•Earth flattening.•Surface relief.• anomalous masses inside the earth

We want to focus on

Anomalous masses

Page 7: Gravity method

We need first to define reference surface

Geoid

What is geoid? It is equipotential surface where the g is always constant. The equipotential surface is usually taken as the sea level. However, due to some heterogeneity in the earth Geoid may differ slightly from Sea level.

Page 8: Gravity method

Reduction

Reduction is carried out to correct for:•Latitude•Elevation•Excess mass•Terrain•Drift•Isostacy•Earth’s rotation

Page 9: Gravity method

Latitude Corrction

The earth is flattened, i.e the radius at the equator is longer than at the poles.

gn = 978031.85 (1.0 + 0.005278895 sin2(lat) + 0.000023462 sin4(lat)) (mGal)

Page 10: Gravity method

Elevation Correction

geoid

+h

-h

gfa = gobs - gn+ 0.3086h (mGal)

Page 11: Gravity method

Bouguer Correction

+m

-m

gb = gobs - gn + 0.3086h - 0.04193r h (mGal)