Results 201 to 210 of about 9,373 (256)

Predicting the Dominant Role of Dense Aggregates in Magnetic Hyperthermia via Intracellular-Mimetic Nanoparticle Models. [PDF]

Small
García-Acevedo P, Paz-Castro A, Estébanez J, Piñeiro Y, Rivas J.   +4 more
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Thermal, Structural, and Morphological Analysis of ZnFe₂O₄ Embedded and Non-Embedded in a SiO₂ Matrix for Magnetic and Photocatalytic Applications. [PDF]

Nanomaterials (Basel)
Dippong T, Savolszki-Madaras AM, Reiz RM, Petean I, Cadar O.   +4 more
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Room-Temperature Multiferroic Liquids: Ferroelectric and Ferromagnetic Order in a Hybrid Nanoparticle-Liquid Crystal System. [PDF]

Adv Mater
Nádasi H, Medle Rupnik P, Küster M, Jarosik A, Tuffin R, Bremer M, Klasen-Memmer M, Lisjak D, Sebastián N, Mertelj A, Ludwig F, Eremin A.   +11 more
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Exploring the particle size effect, land use classification, and magnetic characteristics of street dust in urbanized areas in Poland. [PDF]

Sci Rep
Dytłow S, Karasiński G.
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Room-Temperature Ferromagnetism in an Iron-Based Zeolitic Imidazolate Framework Glass. [PDF]

Adv Sci (Weinh)
Guo C, Ge X, Qiao A, Du Z, Cai M, Wang X, Tao H, Zhao X, Yue Y.   +8 more
europepmc   +1 more source

Phragmites australis elevated concentrations of soil-bound heavy metals and magnetic particles in a typical urban plateau lake wetland, China. [PDF]

Heliyon
Yang X, An N, Luo H, Zheng J, Wu J, Yang D.   +5 more
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Comprehensive Study of τ-Phase Mn-Al-C Magnets: Corrosion Resistance, Structural Integrity, and Magnetic Properties. [PDF]

ACS Omega
Rocabert U, Parnicki-Krollik MA, Maccari F, Tankov N, Ener S.   +4 more
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Chemical-pressure Remanent Magnetism in Sedimentary and Metamorphic Rocks

Chemical-pressure Remanent Magnetism in Sedimentary and Metamorphic Rocks
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Chemical remanent magnetization during γFeOOH phase transformations

Journal of Geophysical Research: Solid Earth, 1993
We have studied chemical remanent magnetization (CRM) accompanying the phase transformations lepidocrocite (γFeOOH) → maghemite (γFe2O3) → hematite (αFe2O3) in a field of 50 μT at a series of 13 temperatures from 200 to 650°C. CRM intensity peaked after the 250°C run as paramagnetic lepidocrocite transformed to ferrimagnetic maghemite of single‐domain ...
Özden Özdemir, David J. Dunlop
openaire   +1 more source