2014
DOI: 10.1073/pnas.1324178111
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Charge gradient microscopy

Abstract: Here we present a simple and fast method to reliably image polarization charges using charge gradient microscopy (CGM). We collected the current from the grounded CGM probe while scanning a periodically poled lithium niobate single crystal and single-crystal LiTaO 3 thin film on the Cr electrode. We observed current signals at the domains and domain walls originating from the displacement current and the relocation or removal of surface charges, which enabled us to visualize the ferroelectric domains at a scan… Show more

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Cited by 46 publications
(67 citation statements)
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“…In such a case the screening charges of the same polarity will be supplied from the grounded tip to the film surface. Therefore, the current polarity flowing to the tip will be positive for positive domains and negative for negative domains, whereas the CGM current will be negligible for the domains having in-plane direction of polarization 24 .
Figure 4Charge gradient microscopy (CGM) imaging of ( b – d ) BFO/NGO and ( f – h ) BFO/LSCO/NGO film heterostructures at different applied tip-forces. ( a ) and ( e ) show the AFM topography of the CGM scan areas, respectively.
…”
Section: Resultsmentioning
confidence: 99%
“…In such a case the screening charges of the same polarity will be supplied from the grounded tip to the film surface. Therefore, the current polarity flowing to the tip will be positive for positive domains and negative for negative domains, whereas the CGM current will be negligible for the domains having in-plane direction of polarization 24 .
Figure 4Charge gradient microscopy (CGM) imaging of ( b – d ) BFO/NGO and ( f – h ) BFO/LSCO/NGO film heterostructures at different applied tip-forces. ( a ) and ( e ) show the AFM topography of the CGM scan areas, respectively.
…”
Section: Resultsmentioning
confidence: 99%
“…This phenomenon was observed after switching on the Z + polar surface. Although it does not lead to the formation of the stable isolated domain, it changes spatial distribution of the screening charges [27][28][29] (Fig. 3c).…”
mentioning
confidence: 99%
“…So, by monitoring the currents at fixed locations on Earth, variations in the charge densities of the passing storm clouds can be mapped. This is almost exactly what Hong et al 1 have done except, rather than map largescale electrical storms, they have invented an analogous technique to determine nanoscale charge variations on the surfaces of inorganic functional materials.…”
Section: J Marty Gregg and Amit Kumarmentioning
confidence: 79%