#!/usr/bin/env python # coding: utf-8 # In[1]: import numpy as np from scipy.special import hankel2 from examples.seismic.acoustic import AcousticWaveSolver from examples.seismic import Model, RickerSource, Receiver, TimeAxis, AcquisitionGeometry from devito import set_log_level from benchmarks.user.tools.plotter import LinePlotter import matplotlib.pyplot as plt from matplotlib import cm get_ipython().run_line_magic('matplotlib', 'inline') # In[2]: # Switch to error logging so that info is printed but runtime is hidden from devito import configuration configuration['log-level'] = 'ERROR' # In[3]: # Model with fixed time step value class ModelBench(Model): """ Physical model used for accuracy benchmarking. The critical dt is made small enough to ignore time discretization errors """ @property def critical_dt(self): """Critical computational time step value.""" return .1 # # Verification # # We compute the error between the numerical and reference solutions for varying spatial discretization order and grid spacing. We also compare the time to solution to the error for these parameters. # In[4]: # Discretization order orders = (2, 4, 6, 8, 10) norder = len(orders) # In[5]: # Number of time steps nt = 1501 # Time axis dt = 0.1 t0 = 0. tn = dt * (nt-1) time = np.linspace(t0, tn, nt) print("t0, tn, dt, nt; %.4f %.4f %.4f %d" % (t0, tn, dt, nt)) # Source peak frequency in KHz f0 = .09 # In[6]: # Domain sizes and gird spacing shapes = ((201, 2.0), (161, 2.5), (101, 4.0)) dx = [2.0, 2.5, 4.0] nshapes = len(shapes) # In[7]: # Fine grid model c0 = 1.5 model = ModelBench(vp=c0, origin=(0., 0.), spacing=(.5, .5), bcs="damp", shape=(801, 801), space_order=20, nbl=40, dtype=np.float64) # In[8]: # Source and receiver geometries src_coordinates = np.empty((1, 2)) src_coordinates[0, :] = 200. # Single receiver offset 100 m from source rec_coordinates = np.empty((1, 2)) rec_coordinates[:, :] = 260. print("The computational Grid has (%s, %s) grid points " "and a physical extent of (%sm, %sm)" % (*model.grid.shape, *model.grid.extent)) print("Source is at the center with coordinates (%sm, %sm)" % tuple(src_coordinates[0])) print("Receiver (single receiver) is located at (%sm, %sm) " % tuple(rec_coordinates[0])) # Note: gets time sampling from model.critical_dt geometry = AcquisitionGeometry(model, rec_coordinates, src_coordinates, t0=t0, tn=tn, src_type='Ricker', f0=f0, t0w=1.5/f0) # # Reference solution for numerical convergence # In[9]: solver = AcousticWaveSolver(model, geometry, kernel='OT2', space_order=8) ref_rec, ref_u, _ = solver.forward() # # Analytical solution for comparison with the reference numerical solution # # The analytical solution of the 2D acoustic wave-equation with a source pulse is defined as: # # $$ # \begin{aligned} # u_s(r, t) &= \frac{1}{2\pi} \int_{-\infty}^{\infty} \{ -i \pi H_0^{(2)}\left(k r \right) q(\omega) e^{i\omega t} d\omega\}\\[10pt] # r &= \sqrt{(x - x_{src})^2+(y - y_{src})^2} # \end{aligned} # $$ # # where $H_0^{(2)}$ is the Hankel function of the second kind, $F(\omega)$ is the Fourier spectrum of the source time function at angular frequencies $\omega$ and $k = \frac{\omega}{v}$ is the wavenumber. # # We look at the analytical and numerical solution at a single grid point. We ensure that this grid point is on-the-grid for all discretizations analyised in the further verification. # In[10]: # Source and receiver coordinates sx, sz = src_coordinates[0, :] rx, rz = rec_coordinates[0, :] # Define a Ricker wavelet shifted to zero lag for the Fourier transform def ricker(f, T, dt, t0): t = np.linspace(-t0, T-t0, int(T/dt)) tt = (np.pi**2) * (f**2) * (t**2) y = (1.0 - 2.0 * tt) * np.exp(- tt) return y def analytical(nt, model, time, **kwargs): dt = kwargs.get('dt', model.critical_dt) # Fourier constants nf = int(nt/2 + 1) fnyq = 1. / (2 * dt) df = 1.0 / time[-1] faxis = df * np.arange(nf) wavelet = ricker(f0, time[-1], dt, 1.5/f0) # Take the Fourier transform of the source time-function R = np.fft.fft(wavelet) R = R[0:nf] nf = len(R) # Compute the Hankel function and multiply by the source spectrum U_a = np.zeros((nf), dtype=complex) for a in range(1, nf-1): k = 2 * np.pi * faxis[a] / c0 tmp = k * np.sqrt(((rx - sx))**2 + ((rz - sz))**2) U_a[a] = -1j * np.pi * hankel2(0.0, tmp) * R[a] # Do inverse fft on 0:dt:T and you have analytical solution U_t = 1.0/(2.0 * np.pi) * np.real(np.fft.ifft(U_a[:], nt)) # The analytic solution needs be scaled by dx^2 to convert to pressure return np.real(U_t) * (model.spacing[0]**2) # In[11]: time1 = np.linspace(0.0, 3000., 30001) U_t = analytical(30001, model, time1, dt=time1[1] - time1[0]) U_t = U_t[0:1501] # In[12]: #NBVAL_IGNORE_OUTPUT print("Numerical data min,max,abs; %+.6e %+.6e %+.6e" % (np.min(ref_rec.data), np.max(ref_rec.data), np.max(np.abs(ref_rec.data)) )) print("Analytic data min,max,abs; %+.6e %+.6e %+.6e" % (np.min(U_t), np.max(U_t), (np.max(np.abs(U_t))))) # In[13]: # Plot wavefield and source/rec position plt.figure(figsize=(8,8)) amax = np.max(np.abs(ref_u.data[1,:,:])) plt.imshow(ref_u.data[1,:,:], vmin=-1.0 * amax, vmax=+1.0 * amax, cmap="seismic") plt.plot(2*sx+40, 2*sz+40, 'r*', markersize=11, label='source') # plot position of the source in model, add nbl for correct position plt.plot(2*rx+40, 2*rz+40, 'k^', markersize=8, label='receiver') # plot position of the receiver in model, add nbl for correct position plt.legend() plt.xlabel('x position (m)') plt.ylabel('z position (m)') plt.savefig('wavefieldperf.pdf') # Plot trace plt.figure(figsize=(12,8)) plt.subplot(2,1,1) plt.plot(time, ref_rec.data[:, 0], '-b', label='numerical') plt.plot(time, U_t[:], '--r', label='analytical') plt.xlim([0,150]) plt.ylim([1.15*np.min(U_t[:]), 1.15*np.max(U_t[:])]) plt.xlabel('time (ms)') plt.ylabel('amplitude') plt.legend() plt.subplot(2,1,2) plt.plot(time, 100 *(ref_rec.data[:, 0] - U_t[:]), '-b', label='difference x100') plt.xlim([0,150]) plt.ylim([1.15*np.min(U_t[:]), 1.15*np.max(U_t[:])]) plt.xlabel('time (ms)') plt.ylabel('amplitude x100') plt.legend() plt.savefig('ref.pdf') plt.show() # In[14]: #NBVAL_IGNORE_OUTPUT error_time = np.zeros(5) error_time[0] = np.linalg.norm(U_t[:-1] - ref_rec.data[:-1, 0], 2) / np.sqrt(nt) errors_plot = [(time, U_t[:-1] - ref_rec.data[:-1, 0])] print(error_time[0]) # # Convergence in time # # # We first show the convergence of the time discretization for a fix high-order spatial discretization (20th order). # # After we show that the time discretization converges in $O(dt^2)$ and therefore only contains the error in time, we will take the numerical solution for `dt=.1ms` as a reference for the spatial discretization analysis. # # # In[15]: #NBVAL_IGNORE_OUTPUT dt = [0.1000, 0.0800, 0.0750, 0.0625, 0.0500] nnt = (np.divide(150.0, dt) + 1).astype(int) for i in range(1, 5): # Time axis t0 = 0.0 tn = 150.0 time = np.linspace(t0, tn, nnt[i]) # Source geometry src_coordinates = np.empty((1, 2)) src_coordinates[0, :] = 200. # Single receiver offset 100 m from source rec_coordinates = np.empty((1, 2)) rec_coordinates[:, :] = 260. geometry = AcquisitionGeometry(model, rec_coordinates, src_coordinates, t0=t0, tn=tn, src_type='Ricker', f0=f0, t0w=1.5/f0) # Note: incorrect data size will be generated here due to AcquisitionGeometry bug ... # temporarily fixed below by resizing the output from the solver geometry.resample(dt[i]) print("geometry.time_axes; ", geometry.time_axis) solver = AcousticWaveSolver(model, geometry, time_order=2, space_order=8) ref_rec1, ref_u1, _ = solver.forward(dt=dt[i]) ref_rec1_data = ref_rec1.data[0:nnt[i],:] time1 = np.linspace(0.0, 3000., 20*(nnt[i]-1) + 1) U_t1 = analytical(20*(nnt[i]-1) + 1, model, time1, dt=time1[1] - time1[0]) U_t1 = U_t1[0:nnt[i]] error_time[i] = np.linalg.norm(U_t1[:-1] - ref_rec1_data[:-1, 0], 2) / np.sqrt(nnt[i]-1) ratio_d = dt[i-1]/dt[i] if i > 0 else 1.0 ratio_e = error_time[i-1]/error_time[i] if i > 0 else 1.0 print("error for dt=%.4f is %12.6e -- ratio dt^2,ratio err; %12.6f %12.6f \n" % (dt[i], error_time[i], ratio_d**2, ratio_e)) errors_plot.append((geometry.time_axis.time_values, U_t1[:-1] - ref_rec1_data[:-1, 0])) # In[16]: plt.figure(figsize=(20, 10)) theory = [t**2 for t in dt] theory = [error_time[0]*th/theory[0] for th in theory] plt.loglog([t for t in dt], error_time, '-ob', label=('Numerical'), linewidth=4, markersize=10) plt.loglog([t for t in dt], theory, '-^r', label=('Theory (2nd order)'), linewidth=4, markersize=10) for x, y, a in zip([t for t in dt], theory, [('dt = %s ms' % (t)) for t in dt]): plt.annotate(a, xy=(x, y), xytext=(4, 2), textcoords='offset points', size=20, horizontalalignment='left', verticalalignment='top') plt.xlabel("Time-step $dt$ (ms)", fontsize=20) plt.ylabel("$|| u_{num} - u_{ana}||_2$", fontsize=20) plt.tick_params(axis='both', which='both', labelsize=20) plt.tight_layout() plt.xlim((0.05, 0.1)) plt.legend(fontsize=20, ncol=4, fancybox=True, loc='best') plt.savefig("TimeConvergence.pdf", format='pdf', facecolor='white', orientation='landscape', bbox_inches='tight') plt.show() # In[17]: #NBVAL_IGNORE_OUTPUT stylel = ('--y', '--b', '--r', '--g', '--c') start_t = lambda dt: int(50/dt) end_t = lambda dt: int(100/dt) plt.figure(figsize=(20, 10)) for i, dti in enumerate(dt): timei, erri = errors_plot[i] s, e = start_t(dti), end_t(dti) if i == 0: plt.plot(timei[s:e], U_t[s:e], 'k', label='analytical', linewidth=2) plt.plot(timei[s:e], 100*erri[s:e], stylel[i], label="100 x error dt=%sms"%dti, linewidth=2) plt.xlim([50,100]) plt.xlabel("Time (ms)", fontsize=20) plt.legend(fontsize=20) plt.show() # In[18]: #NBVAL_IGNORE_OUTPUT pf = np.polyfit(np.log([t for t in dt]), np.log(error_time), deg=1) print("Convergence rate in time is: %.4f" % pf[0]) assert np.isclose(pf[0], 1.9, atol=0, rtol=.1) # # Convergence in space # We have a correct reference solution we can use for space discretization analysis # In[19]: #NBVAL_IGNORE_OUTPUT errorl2 = np.zeros((norder, nshapes)) timing = np.zeros((norder, nshapes)) set_log_level("ERROR") ind_o = -1 for spc in orders: ind_o +=1 ind_spc = -1 for nn, h in shapes: ind_spc += 1 time = np.linspace(0., 150., nt) model_space = ModelBench(vp=c0, origin=(0., 0.), spacing=(h, h), bcs="damp", shape=(nn, nn), space_order=spc, nbl=40, dtype=np.float32) # Source geometry src_coordinates = np.empty((1, 2)) src_coordinates[0, :] = 200. # Single receiver offset 100 m from source rec_coordinates = np.empty((1, 2)) rec_coordinates[:, :] = 260. geometry = AcquisitionGeometry(model_space, rec_coordinates, src_coordinates, t0=t0, tn=tn, src_type='Ricker', f0=f0, t0w=1.5/f0) solver = AcousticWaveSolver(model_space, geometry, time_order=2, space_order=spc) loc_rec, loc_u, summary = solver.forward() # Note: we need to correct for fixed spacing pressure corrections in both analytic # (run at the old model spacing) and numerical (run at the new model spacing) solutions c_ana = 1 / model.spacing[0]**2 c_num = 1 / model_space.spacing[0]**2 # Compare to reference solution # Note: we need to normalize by the factor of grid spacing squared errorl2[ind_o, ind_spc] = np.linalg.norm(loc_rec.data[:-1, 0] * c_num - U_t[:-1] * c_ana, 2) / np.sqrt(U_t.shape[0] - 1) timing[ind_o, ind_spc] = np.max([v for _, v in summary.timings.items()]) print("starting space order %s with (%s, %s) grid points the error is %s for %s seconds runtime" % (spc, nn, nn, errorl2[ind_o, ind_spc], timing[ind_o, ind_spc])) # In[20]: stylel = ('-^k', '-^b', '-^r', '-^g', '-^c') plt.figure(figsize=(20, 10)) for i in range(0, 5): plt.loglog(errorl2[i, :], timing[i, :], stylel[i], label=('order %s' % orders[i]), linewidth=4, markersize=10) for x, y, a in zip(errorl2[i, :], timing[i, :], [('dx = %s m' % (sc)) for sc in dx]): plt.annotate(a, xy=(x, y), xytext=(4, 2), textcoords='offset points', size=20) plt.xlabel("$|| u_{num} - u_{ref}||_{inf}$", fontsize=20) plt.ylabel("Runtime (sec)", fontsize=20) plt.tick_params(axis='both', which='both', labelsize=20) plt.tight_layout() plt.legend(fontsize=20, ncol=3, fancybox=True, loc='lower left') plt.savefig("TimeAccuracy.pdf", format='pdf', facecolor='white', orientation='landscape', bbox_inches='tight') plt.show() # In[21]: stylel = ('-^k', '-^b', '-^r', '-^g', '-^c') style2 = ('--k', '--b', '--r', '--g', '--c') plt.figure(figsize=(20, 10)) for i in range(0, 5): theory = [k**(orders[i]) for k in dx] theory = [errorl2[i, 2]*th/theory[2] for th in theory] plt.loglog([sc for sc in dx], errorl2[i, :], stylel[i], label=('Numerical order %s' % orders[i]), linewidth=4, markersize=10) plt.loglog([sc for sc in dx], theory, style2[i], label=('Theory order %s' % orders[i]), linewidth=4, markersize=10) plt.xlabel("Grid spacing $dx$ (m)", fontsize=20) plt.ylabel("$||u_{num} - u_{ref}||_{inf}$", fontsize=20) plt.tick_params(axis='both', which='both', labelsize=20) plt.tight_layout() plt.legend(fontsize=20, ncol=2, fancybox=True, loc='lower right') # plt.xlim((2.0, 4.0)) plt.savefig("Convergence.pdf", format='pdf', facecolor='white', orientation='landscape', bbox_inches='tight') plt.show() # In[22]: #NBVAL_IGNORE_OUTPUT for i in range(5): pf = np.polyfit(np.log([sc for sc in dx]), np.log(errorl2[i, :]), deg=1)[0] if i==3: pf = np.polyfit(np.log([sc for sc in dx][1:]), np.log(errorl2[i, 1:]), deg=1)[0] print("Convergence rate for order %s is %s" % (orders[i], pf)) if i<4: assert np.isclose(pf, orders[i], atol=0, rtol=.2)