Forward Simulation of Gradiometry Data on a Tree Mesh#

Here we use the module SimPEG.potential_fields.gravity to predict gravity gradiometry data for a synthetic density contrast model. The simulation is carried out on a tree mesh. For this tutorial, we focus on the following:

  • How to define the survey when we want multiple field components

  • How to predict gravity gradiometry data for a density contrast model

  • How to construct tree meshes based on topography and survey geometry

  • The units of the density contrast model and resulting data

Import Modules#

import numpy as np
from scipy.interpolate import LinearNDInterpolator
import matplotlib as mpl
import matplotlib.pyplot as plt

from discretize import TreeMesh
from discretize.utils import mkvc, refine_tree_xyz
from SimPEG.utils import plot2Ddata, model_builder, surface2ind_topo
from SimPEG import maps
from SimPEG.potential_fields import gravity

# sphinx_gallery_thumbnail_number = 2

Defining Topography#

Surface topography is defined as an (N, 3) numpy array. We create it here but the topography could also be loaded from a file.

[x_topo, y_topo] = np.meshgrid(np.linspace(-200, 200, 41), np.linspace(-200, 200, 41))
z_topo = -15 * np.exp(-(x_topo ** 2 + y_topo ** 2) / 80 ** 2)
x_topo, y_topo, z_topo = mkvc(x_topo), mkvc(y_topo), mkvc(z_topo)
xyz_topo = np.c_[x_topo, y_topo, z_topo]

Defining the Survey#

Here, we define survey that will be used for the forward simulation. Gravity surveys are simple to create. The user only needs an (N, 3) array to define the xyz locations of the observation locations, and a list of field components which are to be measured.

# Define the observation locations as an (N, 3) numpy array or load them
x = np.linspace(-80.0, 80.0, 17)
y = np.linspace(-80.0, 80.0, 17)
x, y = np.meshgrid(x, y)
x, y = mkvc(x.T), mkvc(y.T)
fun_interp = LinearNDInterpolator(np.c_[x_topo, y_topo], z_topo)
z = fun_interp(np.c_[x, y]) + 5
receiver_locations = np.c_[x, y, z]

# Define the component(s) of the field we want to simulate as strings within
# a list. Here we measure the x, y and z components of the gravity anomaly at
# each observation location.
components = ["gxz", "gyz", "gzz"]

# Use the observation locations and components to define the receivers. To
# simulate data, the receivers must be defined as a list.
receiver_list = gravity.receivers.Point(receiver_locations, components=components)

receiver_list = [receiver_list]

# Defining the source field.
source_field = gravity.sources.SourceField(receiver_list=receiver_list)

# Defining the survey
survey = gravity.survey.Survey(source_field)

Defining an OcTree Mesh#

Here, we create the OcTree mesh that will be used in the forward simulation.

dx = 5  # minimum cell width (base mesh cell width) in x
dy = 5  # minimum cell width (base mesh cell width) in y
dz = 5  # minimum cell width (base mesh cell width) in z

x_length = 240.0  # domain width in x
y_length = 240.0  # domain width in y
z_length = 120.0  # domain width in z

# Compute number of base mesh cells required in x and y
nbcx = 2 ** int(np.round(np.log(x_length / dx) / np.log(2.0)))
nbcy = 2 ** int(np.round(np.log(y_length / dy) / np.log(2.0)))
nbcz = 2 ** int(np.round(np.log(z_length / dz) / np.log(2.0)))

# Define the base mesh
hx = [(dx, nbcx)]
hy = [(dy, nbcy)]
hz = [(dz, nbcz)]
mesh = TreeMesh([hx, hy, hz], x0="CCN")

# Refine based on surface topography
mesh = refine_tree_xyz(
    mesh, xyz_topo, octree_levels=[2, 2], method="surface", finalize=False
)

# Refine box based on region of interest
xp, yp, zp = np.meshgrid([-100.0, 100.0], [-100.0, 100.0], [-80.0, 0.0])
xyz = np.c_[mkvc(xp), mkvc(yp), mkvc(zp)]

mesh = refine_tree_xyz(mesh, xyz, octree_levels=[2, 2], method="box", finalize=False)

mesh.finalize()

Density Contrast Model and Mapping on OcTree Mesh#

Here, we create the density contrast model that will be used to simulate gravity gradiometry data and the mapping from the model to the mesh. The model consists of a less dense block and a more dense sphere.

# Define density contrast values for each unit in g/cc
background_density = 0.0
block_density = -0.1
sphere_density = 0.1

# Find the indecies for the active mesh cells (e.g. cells below surface)
ind_active = surface2ind_topo(mesh, xyz_topo)

# Define mapping from model to active cells. The model consists of a value for
# each cell below the Earth's surface.
nC = int(ind_active.sum())
model_map = maps.IdentityMap(nP=nC)  # model will be value of active cells

# Define model. Models in SimPEG are vector arrays.
model = background_density * np.ones(nC)

# You could find the indicies of specific cells within the model and change their
# value to add structures.
ind_block = (
    (mesh.gridCC[ind_active, 0] > -50.0)
    & (mesh.gridCC[ind_active, 0] < -20.0)
    & (mesh.gridCC[ind_active, 1] > -15.0)
    & (mesh.gridCC[ind_active, 1] < 15.0)
    & (mesh.gridCC[ind_active, 2] > -50.0)
    & (mesh.gridCC[ind_active, 2] < -30.0)
)
model[ind_block] = block_density

# You can also use SimPEG utilities to add structures to the model more concisely
ind_sphere = model_builder.getIndicesSphere(np.r_[35.0, 0.0, -40.0], 15.0, mesh.gridCC)
ind_sphere = ind_sphere[ind_active]
model[ind_sphere] = sphere_density

# Plot Density Contrast Model
fig = plt.figure(figsize=(9, 4))
plotting_map = maps.InjectActiveCells(mesh, ind_active, np.nan)

ax1 = fig.add_axes([0.1, 0.12, 0.73, 0.78])
mesh.plot_slice(
    plotting_map * model,
    normal="Y",
    ax=ax1,
    ind=int(mesh.h[1].size / 2),
    grid=True,
    clim=(np.min(model), np.max(model)),
    pcolor_opts={"cmap": "viridis"},
)
ax1.set_title("Model slice at y = 0 m")
ax1.set_xlabel("x (m)")
ax1.set_ylabel("z (m)")

ax2 = fig.add_axes([0.85, 0.12, 0.05, 0.78])
norm = mpl.colors.Normalize(vmin=np.min(model), vmax=np.max(model))
cbar = mpl.colorbar.ColorbarBase(
    ax2, norm=norm, orientation="vertical", cmap=mpl.cm.viridis
)
cbar.set_label("$g/cm^3$", rotation=270, labelpad=15, size=12)

plt.show()
Model slice at y = 0 m

Simulation: Gravity Gradiometry Data on an OcTree Mesh#

Here we demonstrate how to predict gravity anomaly data using the integral formulation.

# Define the forward simulation. By setting the 'store_sensitivities' keyword
# argument to "forward_only", we simulate the data without storing the sensitivities
simulation = gravity.simulation.Simulation3DIntegral(
    survey=survey,
    mesh=mesh,
    rhoMap=model_map,
    ind_active=ind_active,
    store_sensitivities="forward_only",
)

# Compute predicted data for some model
dpred = simulation.dpred(model)
n_data = len(dpred)

# Plot
fig = plt.figure(figsize=(10, 3))
n_locations = receiver_locations.shape[0]
v_max = np.max(np.abs(dpred))

ax1 = fig.add_axes([0.1, 0.15, 0.25, 0.78])
cplot1 = plot2Ddata(
    receiver_locations,
    dpred[0:n_data:3],
    ax=ax1,
    ncontour=30,
    clim=(-v_max, v_max),
    contourOpts={"cmap": "bwr"},
)
cplot1[0].set_clim((-v_max, v_max))
ax1.set_title("$\partial g /\partial x$")
ax1.set_xlabel("x (m)")
ax1.set_ylabel("y (m)")

ax2 = fig.add_axes([0.36, 0.15, 0.25, 0.78])
cplot2 = plot2Ddata(
    receiver_locations,
    dpred[1:n_data:3],
    ax=ax2,
    ncontour=30,
    clim=(-v_max, v_max),
    contourOpts={"cmap": "bwr"},
)
cplot2[0].set_clim((-v_max, v_max))
ax2.set_title("$\partial g /\partial y$")
ax2.set_xlabel("x (m)")
ax2.set_yticks([])

ax3 = fig.add_axes([0.62, 0.15, 0.25, 0.78])
cplot3 = plot2Ddata(
    receiver_locations,
    dpred[2:n_data:3],
    ax=ax3,
    ncontour=30,
    clim=(-v_max, v_max),
    contourOpts={"cmap": "bwr"},
)
cplot3[0].set_clim((-v_max, v_max))
ax3.set_title("$\partial g /\partial z$")
ax3.set_xlabel("x (m)")
ax3.set_yticks([])

ax4 = fig.add_axes([0.89, 0.13, 0.02, 0.79])
norm = mpl.colors.Normalize(vmin=-v_max, vmax=v_max)
cbar = mpl.colorbar.ColorbarBase(
    ax4, norm=norm, orientation="vertical", cmap=mpl.cm.bwr
)
cbar.set_label("$mgal/m$", rotation=270, labelpad=15, size=12)

plt.show()
$\partial g /\partial x$, $\partial g /\partial y$, $\partial g /\partial z$

Total running time of the script: ( 0 minutes 7.407 seconds)

Estimated memory usage: 18 MB

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