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Geomagnetic line motion-speed measuring instrument

A technology of motion speed and magnetic force lines, applied in the field of geomagnetic magnetic force line motion speed measuring instruments, can solve problems such as deepening understanding, and achieve the effect of simple structure and convenient use

Inactive Publication Date: 2003-08-27
马龙
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  • Summary
  • Abstract
  • Description
  • Claims
  • Application Information

AI Technical Summary

Problems solved by technology

[0002] The south and north magnetic poles of the earth do not overlap with the rotation axis of the earth, indicating that the movement of the magnetic source that excites the earth's magnetic field inside the earth is not consistent with the rotation of the earth, but because the magnetic source that excites the earth's magnetic field is located in the deep Near the junction between the core and the mantle, people cannot directly observe the motion of the material that excites the Earth's magnetic field. They can only infer the motion state of the material that excites the Earth's magnetic field at a depth of thousands of kilometers inside the Earth by measuring the motion speed of the geomagnetic field lines on the Earth's surface. , therefore, if the movement speed of the geomagnetic field lines can be measured at different locations around the world, it will help to deepen human understanding of the movement state of the magnetic source that excites the earth's magnetic field inside the earth

Method used

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  • Geomagnetic line motion-speed measuring instrument
  • Geomagnetic line motion-speed measuring instrument
  • Geomagnetic line motion-speed measuring instrument

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Embodiment Construction

[0014] Such as figure 1 , figure 2 As shown in Fig. 3, the geomagnetic field line velocity measuring instrument of the present invention comprises an annular electromagnetic wire coil 2 installed on an instrument seat 1 made of a non-magnetic material, and a part of the annular outer surface of the electromagnetic wire coil 2 is provided with a magnetically conductive The magnetic shielding sleeve 3 made of material, the bottom end of the magnetic shielding sleeve 3 is fixed on the upper end surface of the instrument base 1 . The two ends of the electromagnetic wire coil 2 are connected with the voltmeter 4 through wires.

[0015] The annular electromagnetic wire coil 2 is a rectangular frame, which is installed upright on the instrument base 1, the magnetic shielding sleeve 3 is set on the left column or the right column of the rectangular frame of the electromagnetic wire coil 2, and the voltmeter 4 is fixed on the instrument base 1 on the upper end face.

[0016] A comp...

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Abstract

The instrument comprises the electromagnetic annular winding installed on the seat mode from non-magnetic material. The magnetic shielding cover made of magnetic material is setup on a part of annular external surface of said electromagnetic winding. The two ends of the electromagnetic winding through conducting wires are connected to the voltmeter. The electromotive force generated by the moving magnetic line of the geomagnetism to cut the electromagnetic winding can be measured by the voltmeter. Based on the formula V=U / NBL, where B as the magnetic induction of the geomagnetic field at the measuring place, L as the length of the magnetic shielding cover, N as number of turns of the winding. Thus, V as the moving speed of geomagnetic field can be obtained.

Description

technical field [0001] The invention relates to a measuring instrument for measuring the moving speed of the geomagnetic magnetic force line which can measure the moving speed of the geomagnetic magnetic force line. Background technique [0002] The south and north magnetic poles of the earth do not overlap with the rotation axis of the earth, indicating that the movement of the magnetic source that excites the earth's magnetic field inside the earth is not consistent with the rotation of the earth, but because the magnetic source that excites the earth's magnetic field is located in the deep Near the junction between the core and the mantle, people cannot directly observe the motion of the material that excites the Earth's magnetic field. They can only infer the motion state of the material that excites the Earth's magnetic field at a depth of thousands of kilometers inside the Earth by measuring the motion speed of the geomagnetic field lines on the Earth's surface. , Ther...

Claims

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Application Information

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IPC IPC(8): G01V1/40
Inventor 马龙
Owner 马龙