Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

Relative Motion Analysis - Velocity01:24

Relative Motion Analysis - Velocity

382
A stroke engine has a slider-crank mechanism that converts rotational motion from the crank into linear motion of the slider or vice versa. This mechanism consists of three main parts: the crank, the connecting rod, and the slider.
When an external force is exerted, it sets the crank into a rotational movement. This, in turn, instigates the motion of the connecting rod, leading to what is referred to as a general plane motion. This process involves two key points - point A on the connecting rod...
382
Precipitation Gravimetry01:03

Precipitation Gravimetry

6.6K
Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
6.6K
Average and Instantaneous Velocity Vectors01:12

Average and Instantaneous Velocity Vectors

6.2K
To calculate other physical quantities in kinematics, the time variable must be introduced. The time variable not only allows us to state where an object is (its position) during its motion, but also how fast it’s moving. The speed at which an object is moving is given by the rate at which the position changes with time. For each position, a particular time is assigned. If the details of the motion at each instant are not important, the rate is usually expressed as the average velocity v.
6.2K
Deriving the Speed of Sound in a Liquid01:09

Deriving the Speed of Sound in a Liquid

510
As with waves on a string, the speed of sound or a mechanical wave in a fluid depends on the fluid's elastic modulus and inertia. The two relevant physical quantities are the bulk modulus and the density of the material. Indeed, it turns out that the relationship between speed and the bulk modulus and density in fluids is the same as that between the speed and the Young's modulus and density in solids.
The speed of sound in fluids can be derived by considering a mechanical wave...
510
Instantaneous Velocity - II01:10

Instantaneous Velocity - II

9.4K
Instantaneous velocity is the quantity that measures how fast an object is moving along its path. In other words, the instantaneous velocity of an object is the limit of the average velocity as the elapsed time approaches zero, or the derivative of displacement with respect to time. Like average velocity, the instantaneous velocity is a vector with the dimensions of length per unit time. Instantaneous velocity can have both positive and negative values. The instantaneous velocity can be...
9.4K
Velocity and Position by Integral Method01:13

Velocity and Position by Integral Method

6.1K
If acceleration as a function of time is known, then velocity and position functions can be derived using integral calculus. For constant acceleration, the integral equations refer to the first and second kinematic equations for velocity and position functions, respectively.
Consider an example to calculate the velocity and position from the acceleration function. A motorboat is traveling at a constant velocity of 5.0 m/s when it starts to decelerate to arrive at the dock. Its acceleration is...
6.1K

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Identification of Solid-Electrolyte Interphase Species by Joint Characterization of Li-Ion Battery Chemistry by Mass Spectrometry and Electrochemical Reaction Networks.

Journal of the American Chemical Society·2026
Same author

Accelerated Full Waveform Inversion by Deep Compressed Learning.

Sensors (Basel, Switzerland)·2026
Same author

Encoder-Decoder Architecture for 3D Seismic Inversion.

Sensors (Basel, Switzerland)·2023
Same author

Solvent-based paint and varnish removers: a focused toxicologic review of existing and alternative constituents.

Journal of applied toxicology : JAT·2020

Related Experiment Video

Updated: Jul 13, 2025

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

9.4K

Learning-Based Seismic Velocity Inversion with Synthetic and Field Data.

Stuart Farris1, Robert Clapp1, Mauricio Araya-Polo2

  • 1Department of Geophysics, Stanford University, Stanford, CA 94305, USA.

Sensors (Basel, Switzerland)
|October 14, 2023
PubMed
Summary
This summary is machine-generated.

Deep learning models trained on field seismic data accurately recover subsurface velocity models in complex geology. Synthetic data shows promise when field data is scarce, but requires domain expertise to bridge the data gap.

Keywords:
deep learningfield datainverse problemsseismic propagation velocitysynthetic training data

More Related Videos

Cortical Bone Assessment Using Ultrasonic Guided Waves: A Reproducibility Study in a Healthy Population
09:02

Cortical Bone Assessment Using Ultrasonic Guided Waves: A Reproducibility Study in a Healthy Population

Published on: January 31, 2025

520
Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar
07:14

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar

Published on: May 1, 2018

7.8K

Related Experiment Videos

Last Updated: Jul 13, 2025

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

9.4K
Cortical Bone Assessment Using Ultrasonic Guided Waves: A Reproducibility Study in a Healthy Population
09:02

Cortical Bone Assessment Using Ultrasonic Guided Waves: A Reproducibility Study in a Healthy Population

Published on: January 31, 2025

520
Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar
07:14

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar

Published on: May 1, 2018

7.8K

Area of Science:

  • Geophysics
  • Machine Learning
  • Subsurface Modeling

Background:

  • Accurate acoustic subsurface velocity models are crucial for industrial exploration.
  • Traditional inversion methods face challenges in complex geological regions.
  • Deep learning (DL) offers a potential alternative but requires robust validation with field data.

Purpose of the Study:

  • To analyze deep learning's capability for velocity model recovery using field and synthetic seismic data.
  • To evaluate the impact of training data selection and augmentation on DL model performance.
  • To assess DL's effectiveness in challenging geological settings like the Gulf of Mexico.

Main Methods:

  • Utilized labeled field-recorded and synthetically generated seismograms for training DL models.
  • Evaluated model performance using quantitative metrics (MSE, SSIM, R2).
  • Assessed the geological plausibility and impact on geophysical migration images.

Main Results:

  • Models trained on field data outperformed those trained on synthetic data across all metrics.
  • Field-data trained models produced more geologically plausible results and sharper migration images.
  • Synthetic data models showed potential but required advanced techniques to bridge the domain gap.

Conclusions:

  • Deep learning, particularly with field-recorded seismograms, can significantly advance velocity model-building workflows.
  • Synthetic data can be a viable alternative when field data is limited, provided domain expertise is applied.
  • Earth scientists' expertise is vital for curating effective synthetic datasets.