Bead Depth Quantification

Bead depth quantification is the measurement of how far detectable beads lie beneath a sample surface or within a three-dimensional biological or engineered construct. The approach typically combines imaging with spatial calibration: bead signals are identified in optical sections, and their positions along the z-axis are converted into depth relative to a defined reference plane. In bioengineering, these measurements help characterize bead distribution, penetration, and localization in scaffolds, hydrogels, tissues, or microfluidic systems. Quantifying depth can reveal structural organization and transport behavior, support validation of engineered materials, and provide spatial data for evaluating how particles interact with complex biological environments.

Bead Depth Quantification - Related Videos

Research

JoVE Journal - Biochemistry

LERLIC-MS/MS for In-depth Characterization and Quantification of Glutamine and Asparagine Deamidation in Shotgun Proteomics

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Cited by 6 •

2017

Here we present a step-by-step protocol of the long-length electrostatic repulsion-hydrophilic interaction chromatography-tandem mass spectrometry (LERLIC-MS/MS) method. This is a novel methodology that enables for the first time quantification and characterization of the glutamine and asparagine deamidation isoforms by shotgun proteomics.

Quantification of Hydrogen Concentrations in Surface and Interface Layers and Bulk Materials through Depth Profiling with Nuclear Reaction Analysis

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Cited by 21 •

2016

We illustrate the application of 1H(15N,αγ)12C resonant nuclear reaction analysis (NRA) to quantitatively evaluate the density of hydrogen atoms on the surface, in the volume, and at an interfacial layer of solid materials. The near-surface hydrogen depth profiling of a Pd(110) single crystal and of SiO2/Si(100) stacks is described.

Education

JoVE Core - Civil Engineering

Uniform Depth Channel Flow

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2025

Uniform depth channel flow keeps fluid depth consistent along channels such as irrigation canals. In natural channels, such as rivers, approximate uniform flow is often assumed. This condition occurs when the channel’s bottom slope matches the energy slope, balancing potential energy lost from gravity with head loss due to shear stress. This balance prevents depth changes along the channel length, resulting in a steady, uniform flow.Uniform flow in open channels with a constant cross-section...

Depth Perception and Spatial Vision

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2024

Depth perception is the ability to perceive objects three-dimensionally. It relies on two types of cues: binocular and monocular. Binocular cues depend on the combination of images from both eyes and how the eyes work together. Since the eyes are in slightly different positions, each eye captures a slightly different image. This disparity between images, known as binocular disparity, helps the brain interpret depth. When the brain compares these images, it determines the distance to an object.

Uniform Depth Channel Flow: Problem Solving

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2025

To calculate the flow rate for a trapezoidal channel, first, identify the bottom width, side slope, and flow depth of the channel. The cross-sectional area (A) corresponding to the depth of flow (y), channel bottom width (B), and side slope (θ) is determined by:Next, calculate the wetted perimeter, which includes the bottom width and the sloped side lengths in contact with the water. Using the values of the cross-sectional area and the wetted perimeter, determine the hydraulic radius by...

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