For the chemical analysis technique, see 
Gravimetric analysis.
Gravity map of the Southern Ocean around the Antarctic continent
Author-Hannes Grobe, AWI 
This gravity field was computed from sea-surface height measurements  collected by the US Navy GEOSAT altimeter between March, 1985, and  January, 1990. The high density GEOSAT Geodetic Mission data that lie  south of 30 deg. S were declassified by the Navy in May of 1992 and  contribute most of the fine-scale gravity information.
The Antarctic continent itself is shaded in blue depending on the  thickness of the ice sheet (blue shades in steps of 1000 m); light blue  is shelf ice; gray lines are the major ice devides; pink spots are parts  of the continent which are not covered by ice; gray areas have no data. 
Gravimetry is the measurement of the strength of a 
gravitational  field. Gravimetry may be used when either the magnitude of  gravitational field or the properties of matter responsible for its  creation are of interest. The term gravimetry or 
gravimetric is also used in chemistry to define a class of analytical procedures, called 
gravimetric analysis relying upon weighing a sample of material.
 Units of measurement
Gravity is usually measured in units of 
acceleration. In the 
SI system of units, the standard unit of acceleration is 1 
metre per second squared (abbreviated as m/s
2). Other units include the 
gal (sometimes known as a 
galileo, in either case with symbol Gal), which equals 1 
centimetre per second squared, and the 
g (
gn), equal to 9.80665 m/s
2. The value of the 
gn approximately equals the 
acceleration due to gravity at the Earth's surface (although the actual acceleration 
g varies fractionally from place to place).
 How gravity is measured
An instrument used to measure gravity is known as a 
gravimeter, or gravitometer. Since 
general relativity regards the effects of gravity as indistinguishable from the effects of 
acceleration, gravimeters may be regarded as special purpose 
accelerometers. Many 
weighing scales may be regarded as simple gravimeters. In one common form, a 
spring  is used to counteract the force of gravity pulling on an object. The  change in length of the spring may be calibrated to the force required  to balance the gravitational pull. The resulting measurement may be made  in units of force (such as the 
newton), but is more commonly made in units of 
gals.
More sophisticated gravimeters are used when precise measurements are needed. When measuring the 
Earth's gravitational field,  measurements are made to the precision of microgals to find density  variations in the rocks making up the Earth. Several types of  gravimeters exist for making these measurements, including some that are  essentially refined versions of the spring scale described above. These  measurements are used to define 
gravity anomalies.
Besides 
precision, also 
stability is an important property of a gravimeter, as it allows the monitoring of gravity 
changes.  These changes can be the result of mass displacements inside the Earth,  or of vertical movements of the Earth's crust on which measurements are  being made: remember that gravity decreases 0.3 mGal for every metre of  
height. The study of gravity changes belongs to 
geodynamics.
The majority of modern gravimeters use specially-designed 
quartz zero-length springs to support the test mass. Zero length springs do not follow 
Hooke's Law, instead they have a force proportional to their length. The special property of these springs is that the natural 
resonant period of 
oscillation  of the spring-mass system can be made very long - approaching a  thousand seconds. This detunes the test mass from most local vibration  and mechanical 
noise,  increasing the sensitivity and utility of the gravimeter. The springs  are quartz so that magnetic and electric fields do not affect  measurements. The test mass is sealed in an air-tight container so that  tiny changes of barometric pressure from blowing wind and other weather  do not change the buoyancy of the test mass in air.
Spring gravimeters are, in practice, relative instruments which  measure the difference in gravity between different locations. A  relative instrument also requires calibration by comparing instrument  readings taken at locations with known complete or absolute values of  gravity. Absolute gravimeters provide such measurements by determining  the gravitational acceleration of a test mass in vacuum. A test mass is  allowed to fall freely inside a vacuum chamber and its position is  measured with a laser interferometer and timed with an atomic clock. The  laser wavelength is known to ±0.025 
ppb  and the clock is stable to ±0.03 ppb as well. Great care must be taken  to minimize the effects of perturbing forces such as residual air  resistance (even in vacuum) and magnetic forces. Such instruments are  capable of an accuracy of a few parts per billion or 0.002 mGal and  reference their measurement to atomic standards of length and time.  Their primary use is for calibrating relative instruments, monitoring  crustal deformation, and in geophysical studies requiring high accuracy  and stability. However, absolute instruments are somewhat larger and  significantly more expensive than relative spring gravimeters, and are  thus relatively rare.
Gravimeters have been designed to mount in vehicles, including  aircraft, ships and submarines. These special gravimeters isolate  acceleration from the movement of the vehicle, and subtract it from  measurements. The acceleration of the vehicles is often hundreds or  thousands of times stronger than the changes being measured. A  gravimeter (the 
Lunar Surface Gravimeter) was also deployed on  the surface of the moon during the Apollo 17 mission, but did not work  due to a design error. A second device (the 
Traverse Gravimeter Experiment) functioned as anticipated.
 Microgravimetry
Microgravimetry is a rising and important branch developed on the foundation of classical gravimetry.
Microgravity  investigations are carried out in order to solve various problems of  engineering geology, mainly location of voids and their monitoring. Very  detailed measurements of high accuracy can indicate voids of any  origin, provided the size and depth are large enough to produce gravity  effect stronger than is the level of confidence of relevant gravity  signal.
 History
The modern gravimeter was developed by 
Lucien LaCoste and 
Arnold Romberg in 1936.
They also invented most subsequent refinements, including the  ship-mounted gravimeter, in 1965, temperature-resistant instruments for  deep boreholes, and lightweight hand-carried instruments. Most of their  designs remain in use (2005) with refinements in data collection and  data processing.
 See also