Jove
Visualize
Contact Us

Related Concept Videos

General External Flow Characteristics01:26

General External Flow Characteristics

243
The study of external flow is essential for creating structures and objects that interact efficiently and safely with moving fluids, such as air or water. When a body is immersed in a flowing fluid, it experiences two primary forces: drag, which opposes motion along the flow direction, and lift, which acts perpendicular to the flow. The shape, size, and orientation of the object influence these forces.Streamlined and Blunt Bodies in External FlowObjects in fluid flow are classified as...
243
Steady, Laminar Flow in Circular Tubes01:23

Steady, Laminar Flow in Circular Tubes

280
Hagen-Poiseuille flow describes a viscous fluid's steady, incompressible flow through a cylindrical tube with a constant radius R. This flow profile is often applied to understand fluid transport in narrow channels, such as capillaries. It serves as a foundational example of laminar flow. In this model, cylindrical coordinates (r,θ,z) are used to describe the radial (r), angular (θ), and axial (z) dimensions within the tube. For Hagen-Poiseuille flow, the velocity profile is...
280
Standing Waves in a Cavity01:28

Standing Waves in a Cavity

971
A household microwave and lasers are examples of standing electromagnetic waves in a cavity. When two conducting metal plates are placed parallel at the nodal planes, it creates a cavity where standing waves are formed. The cavity between the two planes is analogous to a stretched string held at the points x = 0 and x = L. Here, the distance 'L' between the two planes must be an integer multiple of half of the wavelength. The wavelengths that satisfy this condition are given by:
971
Plane Potential Flows01:23

Plane Potential Flows

425
Plane potential flows simplify fluid motion by assuming the fluid to be irrotational and incompressible. These characteristics allow these flows to be described by a velocity potential function, ϕ, representing the flow speed in a given direction, and a stream function, ψ, that visualizes the flow path, both governed by Laplace's equation. These parameters help in estimating flow patterns, velocity distributions, and pressure fields around various hydraulic structures.
Uniform...
425
Couette Flow01:22

Couette Flow

348
Couette flow represents the flow of fluid between two parallel plates, with one plate fixed and the other moving with a constant velocity. This configuration allows for a simplified analysis using the Navier-Stokes equations, which govern fluid motion under conditions of viscosity and incompressibility. For Couette flow, the assumptions include a steady, laminar, incompressible flow with a zero-pressure gradient in the flow direction. This flow type is beneficial for understanding shear-driven...
348
Gradually Varying Flow01:29

Gradually Varying Flow

96
Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
96

You might also read

Related Articles

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

Sort by
Same author

A Softsensor for Wind Measurements in Karst Caves.

Sensors (Basel, Switzerland)·2026
See all related articles
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 Experiment Video

Updated: Aug 4, 2025

A Microfluidic Model of Biomimetically Breathing Pulmonary Acinar Airways
09:39

A Microfluidic Model of Biomimetically Breathing Pulmonary Acinar Airways

Published on: May 9, 2016

8.0K

How do caves breathe: The airflow patterns in karst underground.

Franci Gabrovšek1

  • 1Karst Research Institute, ZRC SAZU, Postojna, Slovenia.

Plos One
|April 3, 2023
PubMed
Summary

Cave airflow, driven by temperature differences, is significantly influenced by passage geometry. This study models how cave passage shapes affect air density, pressure, and seasonal airflow patterns.

Area of Science:

  • Geology
  • Environmental Science
  • Atmospheric Science

Background:

  • Caves and karst fracture systems create unique subsurface atmospheres.
  • Understanding cave airflow is crucial for subsurface atmospheric properties and air-water-rock chemical interactions.
  • The chimney effect, driven by air density differences, is the primary driver of cave airflow.

Purpose of the Study:

  • To investigate the relationship between cave airflow patterns and passage geometry.
  • To analyze how thermal equilibrium and relaxation length influence airflow velocity.
  • To explore the impact of non-uniform passage shapes and V-shaped profiles on airflow dynamics.

Main Methods:

  • Development and application of a numerical model simulating airflow in a passage coupled to a rock mass.

More Related Videos

Visualizing Hyporheic Flow Through Bedforms Using Dye Experiments and Simulation
09:49

Visualizing Hyporheic Flow Through Bedforms Using Dye Experiments and Simulation

Published on: November 18, 2015

12.3K
Investigating the Three-dimensional Flow Separation Induced by a Model Vocal Fold Polyp
09:58

Investigating the Three-dimensional Flow Separation Induced by a Model Vocal Fold Polyp

Published on: February 3, 2014

8.5K

Related Experiment Videos

Last Updated: Aug 4, 2025

A Microfluidic Model of Biomimetically Breathing Pulmonary Acinar Airways
09:39

A Microfluidic Model of Biomimetically Breathing Pulmonary Acinar Airways

Published on: May 9, 2016

8.0K
Visualizing Hyporheic Flow Through Bedforms Using Dye Experiments and Simulation
09:49

Visualizing Hyporheic Flow Through Bedforms Using Dye Experiments and Simulation

Published on: November 18, 2015

12.3K
Investigating the Three-dimensional Flow Separation Induced by a Model Vocal Fold Polyp
09:58

Investigating the Three-dimensional Flow Separation Induced by a Model Vocal Fold Polyp

Published on: February 3, 2014

8.5K
  • Analysis of thermal equilibrium and characteristic relaxation length of air entering the subsurface.
  • Examination of airflow behavior in passages with varying outlines, cross-sections, and longitudinal profiles.
  • Main Results:

    • Passage geometry, including non-uniform outlines and V-shaped profiles, significantly affects airflow velocity and direction.
    • Relaxation length depends on flow direction in non-uniform passages, leading to different airflow velocities seasonally.
    • Instability in V-shaped passages creates a feedback loop between relaxation length and airflow velocity.

    Conclusions:

    • Cave passage geometry is a critical factor modulating airflow, impacting subsurface atmospheric conditions.
    • Thermal inertia and heat transfer in rock influence relaxation lengths and create hysteresis in airflow behavior.
    • Snow and ice can further alter cave airflow patterns, highlighting the complexity of subsurface atmospheric dynamics.