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Ferromagnetic powder has shown the most potential as core materials, however nanocrystalline materials are highly resistive and amorphous materials have benefits of very low coercivities.
Very thin SiNMs under ambient conditions, i.e., terminated with oxide on all sides, are highly resistive because interface states trap most of the free charges.
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In the absence of light, both the InSe as-grown crystals and flakes were found to be highly resistive with resistivity values of ρ > 10 Ωcm at room temperature, as measured by a standard two-probe method and under electric fields of up to ∼1 kV cm 1.
The film was found to be highly resistive, as is expected for undoped material.
Electrical characterization showed that materials were highly resistive, but that their properties varied considerably when the measurements were performed in vacuum or in air.
The topsoil is highly resistive in the northern and northern-eastern part of the study.
This defect-rich interface region could be highly resistive and could affect the leakage current behaviour.
The deeper forearc beneath the Coastal Cordillera is highly resistive and resembles an almost unstructured half-space.
The topsoil is highly resistive and sub-grade soil is lateritic with significant thickness of 13 m which is enough to withstand the imposed traffic load stress.
The volcanic arc of the Western Cordillera is highly resistive with the exception of a few conductive spots which may be associated with certain individual volcanoes or geothermal resources, respectively.
The films were highly resistive (∼10 MΩ) in their virgin state.
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