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GRAVITY SURVEY (i)-Introduction-June, 2004 Gravity Survey Measurements of the gravitational field at a series of different locations over an area of interest. – PowerPoint PPT presentation

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Title: GRAVITY SURVEY (i) -Introduction-


1
GRAVITY SURVEY (i)-Introduction-
June, 2004
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Gravity Survey
  • Measurements of the gravitational field at a
    series of different locations over an area of
    interest. The objective in exploration work is to
    associate variations with differences in the
    distribution of densities and hence rock types.
    Occasionally the whole gravitational field is
    measured or derivatives of the gravitational
    field, but usually the difference between the
    gravity field at two points is measured
  • (From R. E. Sheriff Encyclopedic
    Dictionary of Exploration Geophysics, published
    by the Society of Exploration Geophysics )

3
  • In gravity prospecting, geophysicists measure
    minute variations in the force of gravity from
    rocks up to a few miles beneath the earth's
    surface.
  • Different types of rocks have different
    densities, and the denser rocks have the greater
    gravitational attraction.

4
  • Theory of gravity
  • Use two of Newtons laws
  • Universal law of gravitation
  • Where G6.67 10-11 N m2/kg2 (m3/kg.s2)
  • Second law of motion F mg
  • We can combine them to obtain the gravitational
    acceleration at the surface of the earth

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  • Gravity and potentials
  • g is a vector field
  • where r1 is the unit vector pointing toward the
    center of the Earth
  • Gravitational potential
  • U is a scalar field which makes it easier to work
    with g is a vector field
  • Definition The gravitational potential, U, due
    to a point mass m, at a distance r from m, is the
    work done by the gravitational force in moving a
    unit mass from infinity to to a position r from
    m.

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  • Relating g to U
  • U is a scalar field which makes it easier to work
    with
  • Potentials are additive
  • Gravity is a conservative force
  • And gravitational acceleration can be easily
  • determined from the potential
  • It follows that
  • For smaller scale problems we usually deal with
    g,
  • and sum the vertical component of g

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  • Units for g
  • SI unit for g m/s2
  • 1 cm/s2 1 Gal (for Galileo) 0.01 m/s2
  • milliGal or mGal 10-3 Gal typical unit for
    field studies
  • some text book uses the gravity unit (g.u.)
  • 1 g.u. 0.1 mGal
  • Normal value of g at the surface of the Earth
  • gE 9.8 m/s2 980 cm/s2 980 Gal 980,000
    mGal 9800 g.u.

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Gravity Meter A gravimeter is any instrument
designed to measure spatial variations in
gravitational acceleration
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THANK YOU Question?
Gravity 1/7
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