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Scipy の scipy.integrate.solve_ivp を使って Lane-Emden 方程式を数値的 に解いてみたでござる。コードは以下の通りにござる。同じコードを GitHub にも置いておいたでござる。
#!/usr/pkg/bin/python3.9 # # Time-stamp: <2022/05/02 20:15:11 (CST) daisuke> # # importing argparse module import argparse # importing sys module import sys # importing pathlib module import pathlib # importing numpy module import numpy # importing scipy module import scipy.integrate # initialising a parser desc = 'solving Lane-Emden equation numerically' parser = argparse.ArgumentParser (description=desc) # adding arguments parser.add_argument ('-n', '--n', type=float, default=0.0, help='index n of polytrope (default: 0.0)') parser.add_argument ('-s', '--step', type=float, default=0.00001, help='step size of radius (default: 0.00001)') parser.add_argument ('-o', '--output', default='', \ help='output file name') # parsing arguments args = parser.parse_args () # parameters n = args.n step = args.step file_output = args.output # existence check of output file path_output = pathlib.Path (file_output) if (path_output.exists ()): # printing message print ("ERROR: output file '%s' exists, exiting...") # exit sys.exit () # check of polytropic index n if (n > 4.95): # printing message print ("ERROR: choose polytropic index between 0 and 4.95, exiting...") # exit sys.exit () # # Lane-Emden equation # def laneemden (t, y): # making a list with a dimension same as y dy = numpy.zeros_like (y) # Lane-Emden equation dy[0] = y[1] dy[1] = -y[0]**n - 2.0 * y[1] / t # returning values return dy # # event trigger # def cross_zero (t, y): return y[0] cross_zero.terminal = True cross_zero.direction = -1 # initial values y_init = [ 1.0, 0.0 ] # output dimensionless radius values xi_max = 350.0 n_step = int (xi_max / step) t_eval = numpy.linspace (step, xi_max, n_step) # solving equation sol = scipy.integrate.solve_ivp (laneemden, [step, xi_max], y_init, \ t_eval=t_eval, dense_output=True, \ events=cross_zero, \ rtol=10**-12, atol=10**-15) # quick-and-dirty job for finding the surface for i in range ( len (sol.y[0]) ): if (sol.y[0][i] > 0.0): xi_surface = (i+1)*step else: break with open (file_output, 'w') as fh: # writing a header header = "#\n" header += "# xi, theta, r_over_R, rho_over_rho_c, P_over_P_c\n" header += "#\n" header += "# polytropic index n = %f\n" % n header += "# xi_surface = %f\n" % xi_surface header += "#\n" fh.write (header) # printing results for i in range ( len (sol.y[0]) ): # xi xi = (i + 1) * step # theta theta = sol.y[0][i] # stop writing data if theta is negative if (theta < 0.0): break # normalised radius r_over_R = xi / xi_surface # normalised density rho_over_rho_c = theta**n # normalised pressure P_over_P_c = theta**(n+1) # output data data = "%15.13f %15.13f %15.13f %15.13f %15.13f\n" \ % (xi, theta, r_over_R, rho_over_rho_c, P_over_P_c) # writing data to output file fh.write (data)
例えば、 n=3 の場合を計算させるには、以下のようにすればよいでござる。
幾つかの polytropic index について計算して、その結果を図にしてみたでご ざる。% ./laneemden.py -n 3.0 -o laneemden_n30.data