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exc1.py
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exc1.py
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import matplotlib.pyplot as plt
import numpy as np
import functions
import matplotlib.colors
import time
import sys
import constants
import akashiwo_dist
# Set the backend
matplotlib.use('TkAgg')
# ------- Other constants -----------
width = 64
length = 64
max_iter = 5000
omega = 1
lid_vel = 2
# ----- Steady state check parameters ------
window = 100
threshold = 1e-5
consecutive = 5
boundary = (True, True, False, True)
# Initialize rho and u
rho = np.ones((width, length))
u = np.zeros((width, length, 2))
# Initialize density function w.r.t. rho and u
f = functions.equilibrium(rho, u)
# calculate corresponding Reynolds number
Re = functions.calculate_re(omega=omega, length=length, lid_vel=lid_vel)
# create a directory to save the figures
import os
if not os.path.exists('LB_plankton_figs'):
os.makedirs('LB_plankton_figs')
steady_state_iteration = None
u_at_point = np.zeros(max_iter)
for t in range(max_iter):
# Streaming step
f = functions.streaming(f, width, length, boundary, lid_vel)
# Collision step
f, rho, u = functions.collision(f, omega)
# Check steady state at point (32, 32)
velocity_at_32_32 = np.linalg.norm(u[32, 32, :])
u_at_point[t] = velocity_at_32_32
if t >= window and steady_state_iteration is None:
if functions.check_steady_state(u_at_point[:t+1], threshold=threshold, window=window, consecutive=consecutive):
steady_state_iteration = t
print(f"Steady state reached at iteration {t}. Velocity at (32, 32): {velocity_at_32_32}.")
steady_state_velocity = u.copy()
break
# Save figure every 250 iterations
if (t + 1) % 250 == 0:
fig = plt.figure(figsize=(12, 10))
plt.streamplot(np.arange(width), np.arange(length), u[:,:, 0].T, u[:,:, 1].T, color='r')
plt.contourf(np.arange(width), np.arange(length), np.linalg.norm(u, axis=2).T, cmap='turbo',levels=100)
plt.colorbar(label='Mag. of U (mm/s)')
plt.title('Velocity Field, iter = %d' % (t+1))
plt.xlabel('X')
plt.ylabel('Y')
plt.savefig(f"LB_plankton_figs/figat_{t+1}.png")
plt.close() # Add this line to close the figure after saving
# Plot fluid speed at point (64, 64) over time
plt.figure(figsize=(10, 6))
plt.plot(np.arange(max_iter), u_at_point, color='black')
plt.title('Fluid Speed @(32,32)')
plt.xlabel('Iteration')
plt.ylabel('Fluid parcel velocity (mm/s)')
plt.grid(True)
plt.tight_layout()
plt.savefig(f"LB_plankton_figs/U_Parcel.png")
plt.show()
# Plot velocity field at steady state
if steady_state_iteration is not None:
fig = plt.figure(figsize=(12, 10))
plt.streamplot(np.arange(width), np.arange(length), u[:,:, 0].T, u[:,:, 1].T, color='r')
plt.contourf(np.arange(width), np.arange(length), np.linalg.norm(u, axis=2).T, cmap='turbo',levels=100)
x0, vc, ini_velocities, p0 = akashiwo_dist.ini_swimspeed_cells(width=width, length=length, num_cells=1000)
plt.quiver(x0[:, 0], x0[:, 1], ini_velocities[:,0]/1000, ini_velocities[:,1]/1000, color='lime', scale=10) # convert to mm/s plt.colorbar(label='|u|')
plt.title(f'Initialization of H.Akashiwo at steady state (iter: {t}), Re: {Re}') # convert to mm/s
plt.xlabel('X')
plt.ylabel('Y')
plt.savefig("LB_plankton_figs/Velocity_Field_and_Particle_Positions_Steady_State.png")
plt.show()
print(f"Steady state reached at iteration {t}. Phytoplankton cells initialize")
else:
print("Steady state not reached. Phytoplankton cells do not initialize. Adjust threshold or simulate for longer times")
def calculate_vorticity(u):
du_dy, du_dx = np.gradient(steady_state_velocity[:,:,0])
dv_dy, dv_dx = np.gradient(steady_state_velocity[:,:,1])
fluid_vorticity = dv_dx - du_dy
return fluid_vorticity
fluid_vorticity = calculate_vorticity(steady_state_velocity)
fig = plt.figure(figsize=(10,10))
plt.contourf(np.arange(width), np.arange(length), fluid_vorticity.T, cmap='turbo',levels=100)
plt.colorbar(label='Vorticity $\omega$')
plt.xlabel('X')
plt.ylabel('Y')
plt.title(f'Vorticity at steady state, Re: {Re}')
plt.savefig("LB_plankton_figs/Vorticity_Steady_State.png")
plt.show()
# ===== ONTO SOLVING THE ORDINARY DIFFERENTIAL EQUATIONS USING RK4 =======
# Function to calculate dp/dt
def calculate_dp_dt(p, omega_star, k, Psi):
dp_dt = 1 / (2 * Psi) * (k - (k * p)) * p + 0.5 * np.cross(omega_star, p)
return dp_dt
# Function to calculate dX/dt
def calculate_dX_dt(X, p, u, Phi):
dX_dt = Phi * p + u
return dX_dt
# RK4 integration
def RK4_step(X, p, u, omega_star, k, Phi, Psi, dt):
k1_p = dt * calculate_dp_dt(p, omega_star, k, Psi)
k1_X = dt * calculate_dX_dt(X, p, u, Phi)
k2_p = dt * calculate_dp_dt(p + 0.5 * k1_p, omega_star, k, Psi)
k2_X = dt * calculate_dX_dt(X + 0.5 * k1_X, p + 0.5 * k1_p, u, Phi)
k3_p = dt * calculate_dp_dt(p + 0.5 * k2_p, omega_star, k, Psi)
k3_X = dt * calculate_dX_dt(X + 0.5 * k2_X, p + 0.5 * k2_p, u, Phi)
k4_p = dt * calculate_dp_dt(p + k3_p, omega_star, k, Psi)
k4_X = dt * calculate_dX_dt(X + k3_X, p + k3_p, u, Phi)
dp_dt = (k1_p + 2 * k2_p + 2 * k3_p + k4_p) / 6
dX_dt = (k1_X + 2 * k2_X + 2 * k3_X + k4_X) / 6
return dp_dt, dX_dt
# params
Psi = 2
Phi = np.power(70.0, -3)
# simulation params
width = 64
length = 64
num_cells = 1000
t_max = 10.0 # tmax
dt = 0.1 # step size
num_steps = int(t_max / dt) # time steps
# initial conditions
x0, vc, ini_velocities, p0 = akashiwo_dist.ini_swimspeed_cells(width, length, num_cells)
# y-direction unit vector with shape (1000, 2)
k = np.zeros((num_cells, 2))
k[:, 1] = 1
# arrays for cell positions and orientations
p_values = np.zeros((num_steps, num_cells, 2))
X_values = np.zeros((num_steps, num_cells, 2))
p_values[0] = p0
X_values[0] = x0
# Integration using RK4
for i in range(num_steps):
# calculate fluid vorticity at current cell positions
omega_star = np.array([fluid_vorticity[int(x[1]), int(x[0])] for x in X_values[i]])
omega_star = omega_star.reshape(num_cells,1, 2) # Reshape to have a 2nd dimension with 1 item (I DONT UNDERSTAND THIS PART)
print("Shape of omega_star after reshaping:", omega_star.shape)
# here we calculate derivatives using RK4 with current vorticity
dp_dt, dX_dt = RK4_step(X_values[i], p_values[i], np.zeros((num_cells, 2)), omega_star, k, Phi, Psi, dt)
# update p and X
p_values[i + 1] = p_values[i] + dp_dt
X_values[i + 1] = X_values[i] + dX_dt