simpeg.potential_fields.magnetics.SimulationEquivalentSourceLayer#
- class simpeg.potential_fields.magnetics.SimulationEquivalentSourceLayer(mesh, cell_z_top, cell_z_bottom, engine='geoana', numba_parallel=True, **kwargs)[source]#
- Bases: - BaseEquivalentSourceLayerSimulation,- Simulation3DIntegral- Equivalent source layer simulation - Parameters:
- meshdiscretize.BaseMesh
- A 2D tensor or tree mesh defining discretization along the x and y directions 
- cell_z_topnumpy.ndarrayorfloat
- Define the elevations for the top face of all cells in the layer. If an array it should be the same size as the active cell set. 
- cell_z_bottomnumpy.ndarrayorfloat
- Define the elevations for the bottom face of all cells in the layer. If an array it should be the same size as the active cell set. 
- engine{“geoana”, “choclo”}, optional
- Choose which engine should be used to run the forward model. 
- numba_parallelbool, optional
- If True, the simulation will run in parallel. If False, it will run in serial. If - engineis not- "choclo"this argument will be ignored.
 
- mesh
 - Attributes - The linear operator. - M: ndarray - Active cells in the mesh. - Elevations for the bottom face of all cells in the layer. - Elevations for the top face of all cells in the layer. - Magnetic susceptibility (si) physical property model. - Derivative of Magnetic Susceptibility (SI) wrt the model. - Mapping of the inversion model to Magnetic Susceptibility (SI). - A list of solver objects to clean when the model is updated - SimPEG - Counterobject to store iterations and run-times.- HasModel.deleteTheseOnModelUpdate has been deprecated. - Engine that will be used to run the simulation. - active_cells.ind_active has been deprecated. - The model for a linear problem physical property model. - Mesh for the integral potential field simulations. - The inversion model. - Derivative of The model for a linear problem wrt the model. - Mapping of the inversion model to The model for a linear problem. - Type of magnetization model - Number of data - Number of processes to use for forward modeling. - True if a model is necessary - Run simulation in parallel or single-threaded when using Numba. - dtype of the sensitivity matrix. - Path to directory where sensitivity file is stored. - Options for storing sensitivities. - The survey for the simulation. - Verbose progress printout. - ampDeriv - is_amplitude_data - tmi_projection - Methods - Jtvec(m, v[, f])- Dot product between transposed sensitivity matrix and a vector. - Jtvec_approx(m, v[, f])- Approximation of the Jacobian transpose times a vector for the model provided. - Jvec(m, v[, f])- Dot product between sensitivity matrix and a vector. - Jvec_approx(m, v[, f])- Approximation of the Jacobian times a vector for the model provided. - compute_amplitude(b_xyz)- Compute amplitude of the magnetic field - dpred([m, f])- Predicted data for the model provided. - evaluate_integral(receiver_location, components)- Load in the active nodes of a tensor mesh and computes the magnetic forward relation between a cuboid and a given observation location outside the Earth [obsx, obsy, obsz] - fields(model)- Return the computed geophysical fields for the model provided. - getJ(m[, f])- Sensitivity matrix \(\mathbf{J}\). - getJtJdiag(m[, W, f])- Compute diagonal of \(\mathbf{J}^T \mathbf{J}`\). - Return linear operator. - make_synthetic_data(m[, relative_error, ...])- Make synthetic data for the model and Gaussian noise provided. - normalized_fields(fields)- Return the normalized B fields - residual(m, dobs[, f])- The data residual. 
