Related Experiment Video
Updated: May 16, 2026

08:04
Controlling Flow Speeds of Microtubule-Based 3D Active Fluids Using Temperature
Published on: November 26, 2019
How flow speed alters competitive outcome in advective environments
Olga Vasilyeva1, Frithjof Lutscher
1Department of Mathematics and Statistics, University of Ottawa, Ottawa, ON, Canada. ovass031@uottawa.ca
Bulletin of Mathematical Biology
|December 1, 2012
Summary
Advective flow in rivers can alter species competition, shifting dominance or promoting coexistence. This study analyzes the Lotka-Volterra model to predict these flow-induced community changes.
Area of Science:
- Ecology
- Theoretical Biology
- Mathematical Biology
Background:
- Advective environments like rivers shape community composition through biotic interactions and hydrologic constraints.
- Previous simulations indicated that advective flow can alter competitive outcomes between species.
Purpose of the Study:
- To provide a detailed analysis of the Lotka-Volterra advection-diffusion model.
- To determine all possible advection-induced shifts in competitive outcomes.
- To identify predictable patterns in how advection influences species dynamics.
Main Methods:
- Variational techniques were employed for model analysis.
- A spatially implicit approximation was used.
- Bifurcation diagrams were utilized to illustrate results.
Main Results:
- The analysis identified specific, predictable pathways for advection-induced shifts in competitive outcomes.
- The study confirmed and detailed the mechanisms by which flow alters species dominance and coexistence.
- Bifurcation diagrams visually represent the range of possible outcomes.
Conclusions:
- Advection is a significant factor in determining ecological community structure in flowing waters.
- The Lotka-Volterra advection-diffusion model provides a robust framework for understanding these dynamics.
- Ecological shifts driven by advection follow predictable mathematical patterns.
Related Concept Videos
General External Flow Characteristics
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...
Poiseuille's Law and Reynolds Number
Any fluid in a horizontal tube can flow due to pressure differences—fluid flows from high to low pressure. The flow rate (Q) is the ratio of pressure difference and resistance through a horizontal tube. The greater the pressure difference, the higher the flow rate. The flow resistance is expressed as:
Laminar and Turbulent Flow
Fluid dynamics is the study of fluids in motion. Velocity vectors are often used to illustrate fluid motion in applications like meteorology. For example, wind—the fluid motion of air in the atmosphere—can be represented by vectors indicating the speed and direction of the wind at any given point on a map. Another method for representing fluid motion is a streamline. A streamline represents the path of a small volume of fluid as it flows. When the flow pattern changes with time, the streamlines...
Rapidly Varying Flow
Rapidly varying flow (RVF) in open channels is characterized by abrupt changes in flow depth over a short distance, with the rate of depth change relative to distance often approaching unity. These flows are inherently complex due to their transient and multi-dimensional nature, making exact analysis difficult. However, approximate solutions using simplified models provide valuable insights into their behavior.Key Features of Rapidly Varying FlowRVF is commonly observed in scenarios involving...
Uniform Depth Channel Flow
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...
Steady Flow of a Fluid Stream
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...
During this process, the momentum of the fluid within the control volume remains constant over the time interval dt. By applying the...

