2G Enterprises 760R-4K Superconducting (SQUID) Rock Magnetometer u-channel System
The most sensitive magnetometer at the IRM for measuring the remanent magnetization of natural materials. It can be used to measure continuous sections of sediments (u-channels) and discrete samples of a variety of sizes (standard pmag core and below).
Specifications:
Magnetometer
- 3-axis SQUID system (measures remanence along x, y, z at the same time).
- Accommodates 1.5 m long u-channels of sediment.
- Or 8 discrete samples at a time (standard paleomagnetic cores, rock cubes, plastic cubes, mounted pieces of material).
- Useable measurement range: 1 x 10-7 emu to 1 x 10-2 emu (1 x 10-10 Am2 -- 1 x 10-5 Am2).
Alternating Field (AF) demagnetizer
- In-line three axis coil system.
- The coils sequentially apply fields along x, y, and z directions in one measurement step as part of a AF demagnetization and remanence measured scheme - there is no need to remove samples during an AF demagnetization run.
- AF range: 1 mT -- 1700 mT
- Includes an additional in-line z-axis DC field coil, allowing anhysteretic remanent magnetization (ARM) to be imparted.
- DC maximum field: 0.1 mT.
Measurement Types
Typically used for:
- Measuring any form of magnetic remanence
- Natural Remanent Magnetization (NRM)
- Anhysteretic Remanent Magnetization (ARM)
- Isothermal Remanent Magnetization (IRM), which can be imparted by an off-line pulse magnetizer.
- Thermal Remanent Magentization (TRM), which can be imparted using a thermal demagnetizer with integrated DC coils.
- Running programmed automated AF demagnetization sequences for determining paleomagnetic directions and magnetic coercivity spectra.
- Rock magnetic measurements. Measurement of ARM and IRM can aid in understanding magnetic mineralogy and is useful, e.g., in environmental studies.
- Measurements of NRM and TRM for paleointensity experiments.
- Anisotropy of ARM (AARM) and TRM (ATRM) measurements.