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Bouguer anomaly : ウィキペディア英語版
Bouguer anomaly
In geodesy and geophysics, the Bouguer anomaly (named after Pierre Bouguer) is a gravity anomaly, corrected for the height at which it is measured and the attraction of terrain. The height correction alone gives a free-air gravity anomaly.
==Anomaly==
The Bouguer anomaly is related to the observed gravity g_ as follows:
: g_B = g_ - g_\lambda + \delta g_F - \delta g_B
:g_B = g_ - \delta g_B
Here,
* g_B is the Bouguer anomaly;
* g_ is the observed gravity;
* g_\lambda is the correction for latitude (because the Earth is not a perfect sphere);
* \delta g_F is the free-air correction;
* \delta g_B is the correction for terrain called the ''Bouguer reduction'';
* g_F is the free-air gravity anomaly.
A Bouguer reduction is called ''simple'' or ''incomplete'' if the terrain is approximated by an infinite flat plate called the ''Bouguer plate''. A ''refined'' or ''complete'' Bouguer reduction removes the effects of terrain precisely. The difference between the two, the differential gravitational effect of the unevenness of the terrain, is called the ''terrain effect''. It is always negative.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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