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Introduction to meda rm 100 magnetometer products, usa
The meda rm 100 magnetic passometer uses micrometric measurement techniques to complete high precision measurements through two subsystems. The first system is the user-controlled magnetic field offset unit, with a dynamic range of ± 100,000 nt (1g) and a resolution of 0. 1 nt. The second subsystem is a low noise simulation output magnetometer that measures the difference between the environment and offset the magnetic field. The margin of the magnetic field offset and measured can be shown directly on the vacuum screen of the front plate of the instrument. At the same time, the measured magnetic field margin can also be exported directly through the simulation output interface of the backboard of the instrument. Magnetic field margin accuracy of ± 0. 01 per cent meets the nist criteria。
The u. S. Meda rm 100 magnetometer function can be remotely controlled by program, data transmission can be via rs232 interface or 10bCase-t is connected to the ultimatum, using the scpi command format. Porter rates range from 9,600 to 115,200. Ethernet connectivity allows rm100 to be controlled through lan or the internet。
The accuracy and traceability of the meda rm 100 magnetometer in the united states makes it highly suitable for use in the marking system and for other magnetometers and magnetic sensors。
Main features of the meda rm 100 magnetometer in the united states
Resolution: 100,000 nt (1g) magnetic field lower resolution 0. 1 nt
Basic precision: ±0. 01% meeting nist standards
Stability: 0. 5 ppm/°c
Range: ±200,000nt (2g)
Simulation output for recording or other uses
One-key environment magnetic field offsets and measurements
Rs232 interface and 10bCase-t ethernet connection for remote design and data acquisition
Mathematical function: zero, minimum, maximum, average, peak-peak
Data storage (16,384 samples) and mapping functions
Set upper and lower alarms
Major application of meda rm 100 magnetometer, usa
Magnetic characteristics of vehicles
The magnetic field changes over time
Magnetization of materials
The magneticity of rocks
Isopolar rectangular and magnetic field drift of artificial satellite equipment
