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High-Precision Protable Proton Magnetometer For Detecting Magnetic Fields
Working principle
(I) Proton precession phenomenon
The proton magnetometer works based on the principle of proton
precession (precession). The magnetic moment directions of protons
in many liquids containing hydrogen atoms (such as kerosene, water,
etc.) are randomly distributed when there is no external magnetic
field. When in a stable external magnetic field (such as the
earth's magnetic field), the proton magnetic moment will be
arranged along the direction of the external magnetic field. If a
radio frequency pulse magnetic field perpendicular to the direction
of the earth's magnetic field is applied at this time, the proton
magnetic moment will deviate from the direction of the external
magnetic field. When the radio frequency pulse stops, the proton
magnetic moment will precess around the direction of the earth's
magnetic field.
(II) Measuring the precession frequency
The proton precession frequency is proportional to the strength of
the external magnetic field, and the relationship conforms to the
Larmor equation: , where is the precession frequency, is the proton
gyromagnetic ratio (constant), and is the strength of the external
magnetic field. By measuring the precession frequency of protons,
the strength of the earth's magnetic field can be accurately
calculated. In a proton magnetometer, an induction coil is usually
used to detect the induced electromotive force generated by the
precession of protons. Its frequency is the same as the proton
precession frequency. After signal processing and analysis, the
magnetic field value can be obtained.
Structural composition
(I) Probe part
The probe is a key component of the proton magnetometer. It
contains a container for the proton source liquid and a radio
frequency coil surrounding it. The probe needs to have good sealing
and stability to ensure that the proton source liquid is not
disturbed by the outside world and that the radio frequency coil
can accurately generate and receive signals. In order to improve
the measurement accuracy, the design of the probe often uses
special materials and structures to reduce the interference of
external electromagnetic fields.
(II) Host part
RF pulse generator: It is responsible for generating radio
frequency pulses of precise frequency and intensity, which are
transmitted to the radio frequency coil of the probe to stimulate
the precession of protons. The radio frequency pulse generator of
modern proton magnetometers has high-precision frequency control
capabilities to ensure the accuracy of measurements.
Signal amplifier and filter: The proton precession signal received
from the probe induction coil is usually very weak and needs to be
amplified and filtered at multiple stages. The amplifier has high
gain and low noise characteristics, which can effectively enhance
the signal strength, while the filter can remove clutter and
interference signals to make the measurement signal purer.
Frequency counter and data processing unit: The frequency counter
is used to accurately measure the frequency of proton precession,
and its measurement accuracy can reach an extremely high level. The
data processing unit calculates the magnetic field strength based
on the measured frequency and the Larmor equation, and performs
operations such as storage, display and transmission of the data.
(III) Power supply system
The power supply system provides a stable power supply for the
entire proton magnetometer. Since the instrument has high precision
requirements, the stability of the power supply is crucial. Some
proton magnetometers are equipped with rechargeable batteries and
voltage stabilization circuits to ensure normal operation in
different environments such as field operations, while reducing the
impact of power supply fluctuations on measurement results.
Application
Magnetic mineral exploration: For iron, nickel, cobalt and other
mineral resources with obvious magnetism, the proton magnetometer
can directly detect the strong magnetic field anomaly generated by
the ore body, so as to quickly determine the approximate location
and range of the ore body, and improve the efficiency and accuracy
of mineral exploration.
Indirect exploration of non-magnetic minerals: Some non-magnetic
minerals, such as gold, silver, copper, etc., although they do not
have obvious magnetism, may be accompanied by the paragenesis of
magnetic minerals or changes in geological structure during their
formation and occurrence, resulting in abnormal magnetic fields
around them. Proton magnetometers can provide clues for finding
non-magnetic minerals by detecting these indirect magnetic field
anomalies.
Technical specifications:
Channels | 1. channel(standard configuration, for separate gradient measurement) 2. channels(optional, for simultaneous gradient measurement) |
Measuring range | 20,000 nT ~ 100,000nT |
Accuracy | ±1nT |
Resolution | 0.1nT |
Gradient permitted | ≤8,000nT/m |
Measuring speed | larger than 2s/reading |
Station measuring interval | 2~60s, optional |
Data stored | large than 2 billion points readings, with power-off protection |
GPS Positioning accuracy | higher than 2.5m CEP |
LCD display | 160×160, with backlight |
Keyboard input | 16 keys |
Port | USB standard serial port |
Power source | Rechargeable lithium battery (for 4000 times reading), external power supply optional (12V) |
Console dimension | 206mm × 85mm ×155mm |
Weight | 1.5Kg (including battery) |
Sensor size | φ75mm×155mm |
Sensor weight | 0.8 Kg |
Working temperature | -10 °C~+50 °C |