Abstract:
Method and apparatus for measuring gravity gradients directly. Two retroreflectors are caused to experience free flight and the radiation reflected by those retroreflectors during this free flight is directed to a radiation receiver which senses and measures the temporal variations of intensity of the interfering reflected radiation beams. The rate of change in interference frequency over a number of consecutive time periods of equal duration is determined and the rate of change of this signal frequency is used as a direct measurement of a gravity gradient.
Abstract:
1,225,129. Photo-electric apparatus; electrophysical measurement. ARTHUR D. LITTLE, Inc. Dec.2, 1968 [Dec.18, 1967], No. 57176/68. Headings G1A and GIN. [Also in Divisions F2 and H1J A bearing assembly suitable for use in an accelerometer, seismometer, gravimeter, galvanometer, electro-meter, flowmeter, or pressure gauge, comprises a vertical axle 12 supported radially by magnetic bearings 13-15, upper and lower magnets 22, 24 defining between them a magnetic field, and a magneticallyresponsive mass 10 affixed to the axle and supported axially within the said field. The radial bearing comprises a solid diamagnetic cylinder of graphite or beryllium which may be surrounded by a sheath of copper or aluminium. The cylinder is repelled by a field created by magnets of alternating polarities, Fig.2 (not shown). The mass 10 may consist of a permanent magnet or a paramagnetic or diamagnet body, and may be supported by both repulsive and attractive forces acting against gravity, Fig. 1, or repulsive forces alone, Fig. 7, (not shown). Annular members or polepieces 28 of soft iron may be positioned in the horizontal plane of the mass to modify the magnetic field and provide shielding. Provision is made for the detection and/or correction of axial misalignment. An optical path 42-44 is provided between a radiant energy source 34 and two balanced detectors 38, which are connected to a differential amplifier 40. Relative motion of the mass 10 causes imbalance in the detectors, which is then transmitted to the amplifier to be recorded on a chart-recording self-balancing potentiometer 45. The signal may also control the amount of current entering a coil 30, thus creating a feedback circuit to correct misalignment. In an alternative embodiment, Fig. 12, the axle is provided with cores 150, 151 of copper; axial misalignment is detected by imbalance between the inductances of the coils 152, 153 associated with the cores.
Abstract:
Apparatus for measuring gravity gradients directly. Two retroreflectors are caused to experience free flight, and the radiation reflected by these retroreflectors during free flight is directed to a radiation receiver which senses and measures the temporal variations of intensity of the interfering reflected radiation beams. The time rate of change of the frequency of the output signal of the receiver is directly related to the vertical gradient of gravity. The instrument of this invention has means to correct for any shifting of the retroreflectors relative to each other and to the radiation beam in planes normal to the radiation beam.
Abstract:
A three-axis seismometer in which three masses are suspended for essentially frictionless movement within certain directions in magnetic fields. Detecting means sense movement of the masses and generate signals used to actuate feedback means. The amount of feedback required is used as a measure of seismic motion. Since motion sensing and the measurement of the magnitude of the motion are separated, output of the instrument may be linear. Responses in unwanted frequency ranges may be filtered out.