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The magnetic behaviour has been summarized, as below, together with an extensive table of data. ... Notable examples include: oxygen, O 2; nitric oxide, NO; nitrogen ...
[1] [2] In contrast to conventional bulk magnets and molecule-based magnets, collective long-range magnetic ordering of magnetic moments is not necessary. [ 2 ] Although the term "single-molecule magnet" was first employed in 1996, [ 3 ] the first single-molecule magnet, [Mn 12 O 12 (OAc) 16 (H 2 O) 4 ] (nicknamed "Mn 12 ") was reported in 1991.
Calculated magnetization curve for a superconducting slab, based on Bean's model. The superconducting slab is initially at H = 0. Increasing H to critical field H* causes the blue curve; dropping H back to 0 and reversing direction to increase it to -H* causes the green curve; dropping H back to 0 again and increase H to H* causes the orange curve.
In contrast with this behavior, diamagnetic materials are repelled by magnetic fields and form induced magnetic fields in the direction opposite to that of the applied magnetic field. [1] Paramagnetic materials include most chemical elements and some compounds ; [ 2 ] they have a relative magnetic permeability slightly greater than 1 (i.e., a ...
Taking for example the H 2 O molecules in liquid phase without the contamination of oxygen-17, the value of K is 1.02×10 10 s −2 and the correlation time is on the order of picoseconds = s, while hydrogen nuclei 1 H at 1.5 tesla precess at a Larmor frequency of approximately 64 MHz (Simplified. BPP theory uses angular frequency indeed).
For example, the magnetic susceptibility of diamagnets such as water is χ v = −9.05 × 10 −6. The most strongly diamagnetic material is bismuth, χ v = −1.66 × 10 −4, although pyrolytic carbon may have a susceptibility of χ v = −4.00 × 10 −4 in one plane. Nevertheless, these values are orders of magnitude smaller than the ...
Additionally, the anisotropy of magnetic susceptibility (AMS) within a sample determines parameters as directions of paleocurrents, maturity of paleosol, flow direction of magma injection, tectonic strain, etc. [2] It is a non-destructive tool which quantifies the average alignment and orientation of magnetic particles within a sample.
Magnetotactic bacteria (or MTB) are a polyphyletic group of bacteria that orient themselves along the magnetic field lines of Earth's magnetic field. [1] Discovered in 1963 by Salvatore Bellini and rediscovered in 1975 by Richard Blakemore, this alignment is believed to aid these organisms in reaching regions of optimal oxygen concentration. [2]