Javascript must be enabled to continue!
Nanoscale subsurface imaging via resonant difference-frequency atomic force ultrasonic microscopy
View through CrossRef
A scanning probe microscope methodology, called resonant difference-frequency atomic force ultrasonic microscopy (RDF-AFUM), has been developed. It employs an ultrasonic wave launched from the bottom of a sample while the cantilever of an atomic force microscope, driven at a frequency differing from the ultrasonic frequency by one of the contact resonance frequencies of the cantilever, engages the sample top surface. The nonlinear mixing of the oscillating cantilever and the ultrasonic wave in the region defined by the cantilever tip–sample surface interaction force generates difference-frequency oscillations at the cantilever contact resonance. The resonance-enhanced difference-frequency signals are used to create images of nanoscale near-surface and subsurface features. An analytical model is presented for assessing the RDF-AFUM phase signal resulting from near-surface variations in the sample contact stiffness and from the interaction of the bulk wave with subsurface structures. The application of the model to RDF-AFUM phase measurements of a 12.7μm thick film of LaRC™-CP2 polyimide polymer containing a monolayer of gold nanoparticles embedded 7μm below the specimen surface reveals variations in the Young modulus of the material of approximately 24% over regions roughly 10–35nm wide. The magnitude of the modulus variations suggests the occurrence of contiguous amorphous and crystalline phases within the bulk of the polymer. The RDF-AFUM micrograph indicates a preferential growth of the crystalline phase in the vicinity of the gold nanoparticles.
Title: Nanoscale subsurface imaging via resonant difference-frequency atomic force ultrasonic microscopy
Description:
A scanning probe microscope methodology, called resonant difference-frequency atomic force ultrasonic microscopy (RDF-AFUM), has been developed.
It employs an ultrasonic wave launched from the bottom of a sample while the cantilever of an atomic force microscope, driven at a frequency differing from the ultrasonic frequency by one of the contact resonance frequencies of the cantilever, engages the sample top surface.
The nonlinear mixing of the oscillating cantilever and the ultrasonic wave in the region defined by the cantilever tip–sample surface interaction force generates difference-frequency oscillations at the cantilever contact resonance.
The resonance-enhanced difference-frequency signals are used to create images of nanoscale near-surface and subsurface features.
An analytical model is presented for assessing the RDF-AFUM phase signal resulting from near-surface variations in the sample contact stiffness and from the interaction of the bulk wave with subsurface structures.
The application of the model to RDF-AFUM phase measurements of a 12.
7μm thick film of LaRC™-CP2 polyimide polymer containing a monolayer of gold nanoparticles embedded 7μm below the specimen surface reveals variations in the Young modulus of the material of approximately 24% over regions roughly 10–35nm wide.
The magnitude of the modulus variations suggests the occurrence of contiguous amorphous and crystalline phases within the bulk of the polymer.
The RDF-AFUM micrograph indicates a preferential growth of the crystalline phase in the vicinity of the gold nanoparticles.
Related Results
Flexural sensitivity of high resonant atomic force microscopy cantilever based on optical lever detection
Flexural sensitivity of high resonant atomic force microscopy cantilever based on optical lever detection
Flexural sensitivity is a key parameter of atomic force microscopy. In order to improve the dynamic atomic force microscopy’s flexural sensitivity, a scanning method that drives th...
Deformations caused by subsurface heat islands: a study on the Chicago Loop
Deformations caused by subsurface heat islands: a study on the Chicago Loop
The ground beneath urban areas is warming up due to anthropogenic activity, leading to subsurface urban heat islands [1]. A recent review of the literature suggests that subsurface...
Atomic electron tomography: 3D structures without crystals
Atomic electron tomography: 3D structures without crystals
BACKGROUND
To understand material properties and functionality at the most fundamental level, one must know the three-dimensional (3D) positions of atoms with high prec...
Modelling subsurface melt of Swiss glaciers
Modelling subsurface melt of Swiss glaciers
Glacier subsurface melt, consisting of englacial and basal melt, is far less understood than surface mass balance. Yet it represents a potentially relevant component of glacier ret...
Characterization and Comparison of Outcrop and Subsurface Unconventional Shale Samples
Characterization and Comparison of Outcrop and Subsurface Unconventional Shale Samples
Abstract
Subsurface unconventional shale samples are always scarce. Outcrop analogs are often used as an alternative to enhance the understanding of the correspondin...
ARIA (Askaryan Regolith Imaging Array): An Instrument Concept for Novel Radio Frequency Characterization of Planetary Subsurfaces
ARIA (Askaryan Regolith Imaging Array): An Instrument Concept for Novel Radio Frequency Characterization of Planetary Subsurfaces
Planetary bodies can be affected by a number of geologic processes, including impacts, volcanism, volatile deposition, mass wasting, and weathering. Local stratigraphic sequences r...
Progress of functionalized atomic force microscopy in the study of the properties of nanometric dielectric materials
Progress of functionalized atomic force microscopy in the study of the properties of nanometric dielectric materials
The rapid development of the electrical and electronic industry requires components with miniaturization, flexibility, and intelligence. As an important material for the preparatio...

