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

Stream Function01:20

Stream Function

1.9K
In two-dimensional incompressible fluid flow, the continuity equation is essential for ensuring mass conservation, meaning that any change in fluid entering or exiting a region is balanced by a corresponding change elsewhere. For incompressible flow, where density remains constant, this requirement simplifies to the condition that the divergence of the velocity field must be zero. Mathematically, this is expressed as,
1.9K
Streamlines, Streaklines, and Pathlines01:18

Streamlines, Streaklines, and Pathlines

1.8K
A streamline represents the trajectory that is always tangent to the fluid's velocity vector at any given point. The velocity of a fluid particle is always directed along the streamline, ensuring the particle continuously follows the streamline's path. Streamlines are particularly useful for visualizing the overall direction of flow in a fluid system, and they provide an instantaneous representation of the flow's velocity field. In steady flow, where conditions do not change over...
1.8K
Steady Flow of a Fluid Stream01:27

Steady Flow of a Fluid Stream

602
Consider a control volume, such as a pipe with solid boundaries, through which fluid flows and changes direction due to the impulse exerted by the resulting force from the pipe walls. In steady flow, the mass of fluid entering the control volume at a given time, t, with velocity v1, is equal to the mass leaving after infinitesimal time dt, with velocity v2.
During this process, the momentum of the fluid within the control volume remains constant over the time interval dt. By applying the...
602
Bernoulli's Equation for Flow Along a Streamline01:30

Bernoulli's Equation for Flow Along a Streamline

1.4K
Bernoulli's equation relates the energy conservation in a fluid moving along a streamline. The equation applies to incompressible and inviscid fluids under steady flow. For such a flow, Newton's second law is applied to a small fluid element, which experiences forces due to pressure differences, gravity, and velocity variations. The force balance leads to the following form of Bernoulli's equation:
1.4K
Introduction to Types of Flows01:23

Introduction to Types of Flows

1.8K
Fluid flows are categorized by dimensionality and behavior, with one-dimensional flow being the simplest form, where properties like velocity and pressure change only along a single axis. Water moving through straight pipes exemplifies this flow type, as variations in other directions are minimal. One-dimensional analysis helps simplify understanding such flows, focusing solely on changes along the pipe's length.
Two-dimensional flow involves changes in both length and height, as seen in...
1.8K
Divergence and Stokes' Theorems01:06

Divergence and Stokes' Theorems

3.3K
The divergence and Stokes' theorems are a variation of Green's theorem in a higher dimension. They are also a generalization of the fundamental theorem of calculus. The divergence theorem and Stokes' theorem are in a way similar to each other; The divergence theorem relates to the dot product of a vector, while Stokes' theorem relates to the curl of a vector. Many applications in physics and engineering make use of the divergence and Stokes' theorems, enabling us to write...
3.3K

You might also read

Related Articles

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

Sort by
Same author

Consequences of dam removal for reservoir carbon storage and emissions.

Journal of environmental management·2025
Same author

Forest recovery after deforestation is fueled by mineral weathering at the expense of ecosystem buffering capacity.

Proceedings of the National Academy of Sciences of the United States of America·2025
Same author

Integrating Contaminant Source Indicators, Water Quality Measures, and Ecotoxicity to Characterize Contaminant Mixtures and Per- and Polyfluoroalkyl Substance (PFAS) Variability in an Urban Watershed.

Environmental science & technology·2025
Same author

Ecosystem metabolism estimates from the National Ecological Observatory Network (NEON) stream and river sites.

Scientific data·2025
Same author

Tracing Atmospheric Mercury from Artisanal and Small-Scale Gold Mining.

Environmental science & technology·2025
Same author

Restored forested wetland surprisingly resistant to experimental salinization.

PloS one·2023
Same journal

Wildland Fires in the US between 2007 and 2018: Characterizing Equity in Exposures and Health Impacts.

Environmental science & technology·2026
Same journal

Profiling Active Low-Abundance Microbes in As/Sb-Contaminated Soils via d-Amino Acid-Based In Situ Labeling.

Environmental science & technology·2026
Same journal

Looking beyond Sorption in GAC Filters: How Extended Contact Times and Functionally Distinct Microbial Biomass Enable Enhanced Micropollutant Biodegradation.

Environmental science & technology·2026
Same journal

Integrating Experiments and Models To Unravel Interactions between Soil Organic Matter and Enhanced Weathering.

Environmental science & technology·2026
Same journal

Role of Advanced Direct Extraction Technologies in Reducing Environmental Impacts of Lithium Production.

Environmental science & technology·2026
Same journal

Comparison of High Spatial Resolution PM<sub>2.5</sub>, PM<sub>10</sub>, and NO<sub>2</sub> Estimates Using a Deep Ensemble Machine Learning Framework in a Low Pollution Setting.

Environmental science & technology·2026
See all related articles

Related Experiment Video

Updated: Dec 24, 2025

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
08:19

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System

Published on: May 9, 2021

2.6K

What is a stream?

Martin W Doyle1, Emily S Bernhardt

  • 1Department of Geography, University of North Carolina-Chapel Hill, Chapel Hill, North Carolina, USA. mwdoyle@email.unc.edu

Environmental Science & Technology
|December 8, 2010
PubMed
Summary

No abstract available in PubMed .

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

12.7K
Protocol for Biofilm Streamer Formation in a Microfluidic Device with Micro-pillars
07:19

Protocol for Biofilm Streamer Formation in a Microfluidic Device with Micro-pillars

Published on: August 20, 2014

12.5K

Related Experiment Videos

Last Updated: Dec 24, 2025

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
08:19

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System

Published on: May 9, 2021

2.6K
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

12.7K
Protocol for Biofilm Streamer Formation in a Microfluidic Device with Micro-pillars
07:19

Protocol for Biofilm Streamer Formation in a Microfluidic Device with Micro-pillars

Published on: August 20, 2014

12.5K