Fractional-Order Bioconvection in Trihybrid Nanofluids Flowing Over a Rotating Disk: A Hybrid Neural Network With Genetic Algorithm Method for Entropy Generation Minimization

<p>Fractional-Order Bioconvection in Trihybrid Nanofluids Flowing Over a Rotating Disk: A Hybrid Neural Network With Genetic Algorithm Method for Entropy Generation Minimization</p> : Minimizing entropy generation in complex fluid systems is a primary concern for improving thermodynamic efficiency. This paper investigates bioconvection in a Carreau-Yasuda trihybrid nanofluid over a spinning disk, where fluid memory is modeled using fractional-order derivatives. We provide an analytical energy-based stability framework for the proposed model. Given the high computational cost associated with solving fractional partial differential equations, we propose a Hybrid Neural Network surrogate model combined with a Genetic Algorithm. The Hybrid Neural Network, trained on data obtained via the Finite Difference Method, accurately predicts Nusselt numbers and entropy generation, while the Genetic Algorithm navigates the response surface to identify Pareto-optimal solutions. A deep cas...

Interactive Polar Calculus with SageMath: Area, Arc Length, Multivariable Limits, and Continuity Explained (Part 1)

Introduction to Polar Coordinates | Learn with Visual Examples Centered Equation Box Center Image Example Introduction to Polar Coordinates Description of Image

Part 1: Introduction to Polar Coordinates

What are Polar Coordinates?

Polar coordinates provide an alternative way to represent points in a plane, distinct from the familiar Cartesian (x, y) coordinate system.

  • r: the radial distance from the origin (or pole).
  • θ(theta): the angle formed with the positive x-axis.

Brief Overview of Polar Coordinates and Curves

In the polar coordinate system, instead of using x and y to represent a point, we use r and θ(theta). The radial distance r tells us how far a point is from the origin, while the angle θ (theta) tells us the direction of the point, measured counterclockwise from the positive x-axis.

Equation of a Polar Curve

A polar curve is defined by an equation involving r and θ (theta). For example, a common equation is:

r = f(θ)

This equation describes how the distance from the origin changes as the angle θ (theta) varies.

Importance of Visualizing Polar Equations

Visualizing polar equations allows us to understand complex curves that are difficult to express using Cartesian coordinates. Many natural and scientific phenomena, such as the shape of petals in flowers or the path of planets, can be described with polar coordinates.

Example: Plotting Polar Curves

Let’s explore the curve defined by the polar equation:

r = 2 - cos(2θ)

We can easily visualize this curve using a tool like SageMath. Below is the code to plot this polar curve:

var('theta')
r = 2 - cos(2*theta)
polar_plot(r, 0, 2*pi, figsize=4)
    
Description of Image

This will generate a graph of the curve, which has an interesting shape resembling a "limaçon" (a type of curve that appears often in polar plots). By plotting polar equations like this, we can observe patterns and behaviors that reveal insights into various real-world phenomena, like oscillations and waves.



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