PyHydroGeophysX.forward package#

Submodules#

PyHydroGeophysX.forward.ert_forward module#

Forward modeling utilities for Electrical Resistivity Tomography (ERT).

class PyHydroGeophysX.forward.ert_forward.ERTForwardModeling(mesh: pygimli.Mesh, data: pygimli.DataContainer | None = None)[source]#

Bases: object

Class for forward modeling of Electrical Resistivity Tomography (ERT) data.

create_synthetic_data(xpos: ndarray, ypos: ndarray | None = None, mesh: pygimli.Mesh | None = None, res_models: ndarray | None = None, schemeName: str = 'wa', noise_level: float = 0.05, absolute_error: float = 0.0, relative_error: float = 0.05, save_path: str | None = None, show_data: bool = False, seed: int | None = None, xbound: float = 100, ybound: float = 100) → Tuple[pygimli.DataContainer, pygimli.Mesh][source]#

Create synthetic ERT data using forward modeling.

This method simulates an ERT survey by placing electrodes, creating a measurement scheme, performing forward modeling to generate synthetic data, and adding noise.

Parameters:

xpos – X-coordinates of electrodes
ypos – Y-coordinates of electrodes (if None, uses flat surface)
mesh – Mesh for forward modeling
res_models – Resistivity model values
schemeName – Name of measurement scheme (‘wa’, ‘dd’, etc.)
noise_level – Level of Gaussian noise to add
absolute_error – Absolute error for data estimation
relative_error – Relative error for data estimation
save_path – Path to save synthetic data (if None, does not save)
show_data – Whether to display data after creation
seed – Random seed for noise generation
xbound – X boundary extension for mesh
ybound – Y boundary extension for mesh

Returns:

Tuple of (synthetic ERT data container, simulation mesh)

forward(resistivity_model: ndarray, log_transform: bool = True) → ndarray[source]#

Compute forward response for a given resistivity model.

Parameters:

resistivity_model – Resistivity model values
log_transform – Whether resistivity_model is log-transformed

Returns:

Forward response (apparent resistivity)

forward_and_jacobian(resistivity_model: ndarray, log_transform: bool = True) → Tuple[ndarray, ndarray][source]#

Compute forward response and Jacobian matrix.

Parameters:

resistivity_model – Resistivity model values
log_transform – Whether resistivity_model is log-transformed

Returns:

Tuple of (forward response, Jacobian matrix)

get_coverage(resistivity_model: ndarray, log_transform: bool = True) → ndarray[source]#

Compute coverage (resolution) for a given resistivity model.

Parameters:

resistivity_model – Resistivity model values
log_transform – Whether resistivity_model is log-transformed

Returns:

Coverage values for each cell

set_data(data: pygimli.DataContainer) → None[source]#

Set ERT data for forward modeling.

Parameters:: data – ERT data container

set_mesh(mesh: pygimli.Mesh) → None[source]#

Set mesh for forward modeling.

Parameters:: mesh – PyGIMLI mesh

PyHydroGeophysX.forward.ert_forward.ertforandjac(fob, rhomodel, xr)[source]#

Forward model and Jacobian for ERT.

Parameters:

fob (pygimli.ERTModelling) – ERT forward operator.
rhomodel (pg.RVector) – Resistivity model.
xr (np.ndarray) – Log-transformed model parameter.

Returns:

Log-transformed forward response. J (np.ndarray): Jacobian matrix.

Return type:

dr (np.ndarray)

PyHydroGeophysX.forward.ert_forward.ertforandjac2(fob, xr, mesh)[source]#

Alternative ERT forward model and Jacobian using log-resistivity values.

Parameters:

fob (pygimli.ERTModelling) – ERT forward operator.
xr (np.ndarray) – Log-transformed model parameter.
mesh (pg.Mesh) – Mesh for the forward model.

Returns:

Log-transformed forward response. J (np.ndarray): Jacobian matrix.

Return type:

dr (np.ndarray)

PyHydroGeophysX.forward.ert_forward.ertforward(fob, mesh, rhomodel, xr)[source]#

Forward model for ERT.

Parameters:

fob (pygimli.ERTModelling) – ERT forward operator.
mesh (pg.Mesh) – Mesh for the forward model.
rhomodel (pg.RVector) – Resistivity model vector.
xr (np.ndarray) – Log-transformed model parameter (resistivity).

Returns:

Log-transformed forward response. rhomodel (pg.RVector): Updated resistivity model.

Return type:

dr (np.ndarray)

PyHydroGeophysX.forward.ert_forward.ertforward2(fob, xr, mesh)[source]#

Simplified ERT forward model.

Parameters:

fob (pygimli.ERTModelling) – ERT forward operator.
xr (np.ndarray) – Log-transformed model parameter.
mesh (pg.Mesh) – Mesh for the forward model.

Returns:

Log-transformed forward response.

Return type:

dr (np.ndarray)

PyHydroGeophysX.forward.fdem_forward module#

Forward modeling utilities for Frequency-Domain Electromagnetic (FDEM) data.

Uses SimPEG’s frequency-domain module for 1D layered-earth simulations.

class PyHydroGeophysX.forward.fdem_forward.FDEMForwardModeling(thicknesses: ndarray, survey_config: FDEMSurveyConfig | None = None, survey: simpeg.electromagnetics.frequency_domain.Survey | None = None)[source]#

Bases: object

Forward modeling of Frequency-Domain EM data using SimPEG.

Supports 1D layered-earth conductivity models.

forward(conductivity: ndarray) → ndarray[source]#: Compute FDEM response for a given conductivity model.

forward_with_noise(conductivity: ndarray, noise_level: float = 0.05, seed: int | None = None) → Tuple[ndarray, ndarray, ndarray][source]#: Compute noisy and clean FDEM responses with data uncertainties.

static hydro_to_fdem(water_content: ndarray, porosity: ndarray, layer_thicknesses: ndarray, **petro_params)[source]#: Convert hydrological properties to FDEM response via petrophysics.

class PyHydroGeophysX.forward.fdem_forward.FDEMSurveyConfig(source_location: ndarray | None = None, source_radius: float = 10.0, receiver_location: ndarray | None = None, receiver_orientation: str = 'z', receiver_component: str = 'secondary', frequencies: ndarray | None = None, waveform_type: str = 'dipole')[source]#

Bases: object

Configuration for FDEM survey geometry.

frequencies: ndarray = None#

receiver_component: str = 'secondary'#

receiver_location: ndarray = None#

receiver_orientation: str = 'z'#

source_location: ndarray = None#

source_radius: float = 10.0#

waveform_type: str = 'dipole'#

PyHydroGeophysX.forward.srt_forward module#

Forward modeling utilities for Seismic Refraction Tomography (SRT).

class PyHydroGeophysX.forward.srt_forward.SeismicForwardModeling(mesh: pygimli.Mesh, scheme: pygimli.DataContainer | None = None)[source]#

Bases: object

Class for forward modeling of Seismic Refraction Tomography (SRT) data.

classmethod create_synthetic_data(sensor_x: ndarray, surface_points: ndarray | None = None, mesh: pygimli.Mesh | None = None, velocity_model: ndarray | None = None, slowness: bool = False, shot_distance: float = 5, noise_level: float = 0.05, noise_abs: float = 1e-05, save_path: str | None = None, show_data: bool = False, verbose: bool = False, seed: int | None = None) → Tuple[pygimli.DataContainer, pygimli.Mesh][source]#

Create synthetic seismic data using forward modeling.

This method simulates a seismic survey by placing geophones along a surface, creating a measurement scheme, and performing forward modeling to generate synthetic travel time data.

Parameters:

sensor_x – X-coordinates of geophones
surface_points – Surface coordinates for placing geophones [[x,y],…] If None, geophones will be placed on flat surface
mesh – Mesh for forward modeling
velocity_model – Velocity model values
slowness – Whether velocity_model is slowness (1/v)
shot_distance – Distance between shots
noise_level – Level of relative noise to add
noise_abs – Level of absolute noise to add
save_path – Path to save synthetic data (if None, does not save)
show_data – Whether to display data after creation
verbose – Whether to show verbose output
seed – Random seed for noise generation

Returns:

Tuple of (synthetic seismic data container, simulation mesh)

static draw_first_picks(ax, data, tt=None, plotva=False, **kwargs)[source]#

Plot first arrivals as lines.

Parameters:

ax (matplotlib.axes) – axis to draw the lines in
data (:gimliapi:`GIMLI::DataContainer`) – data containing shots (“s”), geophones (“g”) and traveltimes (“t”)
tt (array, optional) – traveltimes to use instead of data(“t”)
plotva (bool, optional) – plot apparent velocity instead of traveltimes

Returns:

ax – the modified axis

Return type:

matplotlib.axes

forward(velocity_model: ndarray, slowness: bool = True) → ndarray[source]#

Compute forward response for a given velocity model.

Parameters:

velocity_model – Velocity model values (or slowness if slowness=True)
slowness – Whether velocity_model is slowness (1/v)

Returns:

Forward response (travel times)

set_mesh(mesh: pygimli.Mesh) → None[source]#

Set mesh for forward modeling.

Parameters:: mesh – PyGIMLI mesh

set_scheme(scheme: pygimli.DataContainer) → None[source]#

Set seismic data scheme for forward modeling.

Parameters:: scheme – Seismic data scheme

PyHydroGeophysX.forward.tdem_forward module#

Forward modeling utilities for Time-Domain Electromagnetic (TDEM) simulations.

This module provides classes for 1D TDEM forward modeling using SimPEG, including support for layered Earth models derived from hydrological data.

class PyHydroGeophysX.forward.tdem_forward.TDEMForwardModeling(thicknesses: ndarray, survey_config: TDEMSurveyConfig | None = None, survey: simpeg.electromagnetics.time_domain.Survey | None = None)[source]#

Bases: object

Class for forward modeling of Time-Domain Electromagnetic (TDEM) data.

This class provides functionality for 1D layered Earth TDEM forward modeling using SimPEG’s time_domain module.

Example

>>> # Define layer model
>>> thicknesses = np.array([10.0, 30.0])
>>> conductivity = np.array([0.01, 0.1, 0.001])  # S/m
>>>
>>> # Create forward modeler
>>> fwd = TDEMForwardModeling(thicknesses=thicknesses)
>>>
>>> # Compute response
>>> response = fwd.forward(conductivity)

forward(conductivity: ndarray, log_input: bool = False) → ndarray[source]#

Compute forward response for a given conductivity model.

Parameters:

conductivity – Conductivity values for each layer (S/m)
log_input – If True, conductivity is log-transformed

Returns:

Forward response (magnetic flux density, T)

forward_with_noise(conductivity: ndarray, noise_level: float = 0.05, seed: int | None = None, log_input: bool = False) → Tuple[ndarray, ndarray, ndarray][source]#

Compute forward response with added Gaussian noise.

Parameters:

conductivity – Conductivity values for each layer (S/m)
noise_level – Relative noise level (default 5%)
seed – Random seed for reproducibility
log_input – If True, conductivity is log-transformed

Returns:

Tuple of (noisy_data, clean_data, uncertainties)

get_times() → ndarray[source]#: Get the time channels from the survey.

property n_data: int#: Number of data points.

class PyHydroGeophysX.forward.tdem_forward.TDEMSurveyConfig(source_location: ndarray | None = None, source_radius: float = 10.0, source_current: float = 1.0, receiver_location: ndarray | None = None, receiver_orientation: str = 'z', times: ndarray | None = None, waveform_type: str = 'step_off')[source]#

Bases: object

Configuration for TDEM survey geometry.

source_location#

[x, y, z] location of source center (m)

Type:: numpy.ndarray

source_radius#

Radius of circular loop source (m)

Type:: float

source_current#

Peak current amplitude (A)

Type:: float

receiver_location#

[x, y, z] location of receiver (m)

Type:: numpy.ndarray

receiver_orientation#

Component to measure (‘x’, ‘y’, or ‘z’)

Type:: str

times#

Time channels for measurement (s)

Type:: numpy.ndarray

waveform_type#

Type of waveform (‘step_off’, ‘ramp_off’, ‘custom’)

Type:: str

receiver_location: ndarray = None#

receiver_orientation: str = 'z'#

source_current: float = 1.0#

source_location: ndarray = None#

source_radius: float = 10.0#

times: ndarray = None#

waveform_type: str = 'step_off'#

PyHydroGeophysX.forward.tdem_forward.create_tdem_survey(times: ndarray, source_radius: float = 10.0, source_current: float = 1.0, source_location: ndarray | None = None, receiver_location: ndarray | None = None, receiver_orientation: str = 'z', waveform_type: str = 'step_off') → simpeg.electromagnetics.time_domain.Survey[source]#

Create a TDEM survey for 1D sounding.

Parameters:

times – Time channels (s)
source_radius – Loop radius (m)
source_current – Peak current (A)
source_location – Source center [x, y, z] (m)
receiver_location – Receiver position [x, y, z] (m)
receiver_orientation – Measurement component (‘x’, ‘y’, ‘z’)
waveform_type – Waveform type (‘step_off’, ‘ramp_off’)

Returns:

SimPEG TDEM Survey object

PyHydroGeophysX.forward.tdem_forward.hydro_to_tdem(water_content: ndarray, porosity: ndarray, layer_thicknesses: ndarray, sigma_w: float | ndarray = 0.05, m: float | ndarray = 1.5, n: float | ndarray = 2.0, sigma_s: float | ndarray = 0.0, times: ndarray | None = None, source_radius: float = 10.0, noise_level: float = 0.05, seed: int | None = None, verbose: bool = False) → Tuple[ndarray, ndarray, ndarray, ndarray][source]#

Convert hydrological properties to TDEM response.

This function takes water content and porosity from hydrological models and computes the expected TDEM response using petrophysical relationships.

Parameters:

water_content – Water content for each layer (-)
porosity – Porosity for each layer (-)
layer_thicknesses – Thickness of each layer except bottom (m)
sigma_w – Pore water conductivity (S/m)
m – Cementation exponent
n – Saturation exponent
sigma_s – Surface conductivity (S/m)
times – Time channels (s), default is logspace(-5, -2, 31)
source_radius – Loop radius (m)
noise_level – Relative noise level for synthetic data
seed – Random seed for reproducibility
verbose – Print progress information

Returns:

Tuple of (noisy_data, clean_data, uncertainties, conductivity)

Module contents#

Forward modeling utilities for geophysical simulations.

class PyHydroGeophysX.forward.ERTForwardModeling(mesh: pygimli.Mesh, data: pygimli.DataContainer | None = None)[source]#

Bases: object

Class for forward modeling of Electrical Resistivity Tomography (ERT) data.

Create synthetic ERT data using forward modeling.

This method simulates an ERT survey by placing electrodes, creating a measurement scheme, performing forward modeling to generate synthetic data, and adding noise.

Parameters:

xpos – X-coordinates of electrodes
ypos – Y-coordinates of electrodes (if None, uses flat surface)
mesh – Mesh for forward modeling
res_models – Resistivity model values
schemeName – Name of measurement scheme (‘wa’, ‘dd’, etc.)
noise_level – Level of Gaussian noise to add
absolute_error – Absolute error for data estimation
relative_error – Relative error for data estimation
save_path – Path to save synthetic data (if None, does not save)
show_data – Whether to display data after creation
seed – Random seed for noise generation
xbound – X boundary extension for mesh
ybound – Y boundary extension for mesh

Returns:

Tuple of (synthetic ERT data container, simulation mesh)

forward(resistivity_model: ndarray, log_transform: bool = True) → ndarray[source]#

Compute forward response for a given resistivity model.

Parameters:

resistivity_model – Resistivity model values
log_transform – Whether resistivity_model is log-transformed

Returns:

Forward response (apparent resistivity)

forward_and_jacobian(resistivity_model: ndarray, log_transform: bool = True) → Tuple[ndarray, ndarray][source]#

Compute forward response and Jacobian matrix.

Parameters:

resistivity_model – Resistivity model values
log_transform – Whether resistivity_model is log-transformed

Returns:

Tuple of (forward response, Jacobian matrix)

get_coverage(resistivity_model: ndarray, log_transform: bool = True) → ndarray[source]#

Compute coverage (resolution) for a given resistivity model.

Parameters:

resistivity_model – Resistivity model values
log_transform – Whether resistivity_model is log-transformed

Returns:

Coverage values for each cell

set_data(data: pygimli.DataContainer) → None[source]#

Set ERT data for forward modeling.

Parameters:: data – ERT data container

set_mesh(mesh: pygimli.Mesh) → None[source]#

Set mesh for forward modeling.

Parameters:: mesh – PyGIMLI mesh

class PyHydroGeophysX.forward.FDEMForwardModeling(thicknesses: ndarray, survey_config: FDEMSurveyConfig | None = None, survey: simpeg.electromagnetics.frequency_domain.Survey | None = None)[source]#

Bases: object

Forward modeling of Frequency-Domain EM data using SimPEG.

Supports 1D layered-earth conductivity models.

forward(conductivity: ndarray) → ndarray[source]#: Compute FDEM response for a given conductivity model.

forward_with_noise(conductivity: ndarray, noise_level: float = 0.05, seed: int | None = None) → Tuple[ndarray, ndarray, ndarray][source]#: Compute noisy and clean FDEM responses with data uncertainties.

static hydro_to_fdem(water_content: ndarray, porosity: ndarray, layer_thicknesses: ndarray, **petro_params)[source]#: Convert hydrological properties to FDEM response via petrophysics.

class PyHydroGeophysX.forward.FDEMSurveyConfig(source_location: ndarray | None = None, source_radius: float = 10.0, receiver_location: ndarray | None = None, receiver_orientation: str = 'z', receiver_component: str = 'secondary', frequencies: ndarray | None = None, waveform_type: str = 'dipole')[source]#

Bases: object

Configuration for FDEM survey geometry.

frequencies: ndarray = None#

receiver_component: str = 'secondary'#

receiver_location: ndarray = None#

receiver_orientation: str = 'z'#

source_location: ndarray = None#

source_radius: float = 10.0#

waveform_type: str = 'dipole'#

class PyHydroGeophysX.forward.SeismicForwardModeling(mesh: pygimli.Mesh, scheme: pygimli.DataContainer | None = None)[source]#

Bases: object

Class for forward modeling of Seismic Refraction Tomography (SRT) data.

Create synthetic seismic data using forward modeling.

This method simulates a seismic survey by placing geophones along a surface, creating a measurement scheme, and performing forward modeling to generate synthetic travel time data.

Parameters:

sensor_x – X-coordinates of geophones
surface_points – Surface coordinates for placing geophones [[x,y],…] If None, geophones will be placed on flat surface
mesh – Mesh for forward modeling
velocity_model – Velocity model values
slowness – Whether velocity_model is slowness (1/v)
shot_distance – Distance between shots
noise_level – Level of relative noise to add
noise_abs – Level of absolute noise to add
save_path – Path to save synthetic data (if None, does not save)
show_data – Whether to display data after creation
verbose – Whether to show verbose output
seed – Random seed for noise generation

Returns:

Tuple of (synthetic seismic data container, simulation mesh)

static draw_first_picks(ax, data, tt=None, plotva=False, **kwargs)[source]#

Plot first arrivals as lines.

Parameters:

ax (matplotlib.axes) – axis to draw the lines in
data (:gimliapi:`GIMLI::DataContainer`) – data containing shots (“s”), geophones (“g”) and traveltimes (“t”)
tt (array, optional) – traveltimes to use instead of data(“t”)
plotva (bool, optional) – plot apparent velocity instead of traveltimes

Returns:

ax – the modified axis

Return type:

matplotlib.axes

forward(velocity_model: ndarray, slowness: bool = True) → ndarray[source]#

Compute forward response for a given velocity model.

Parameters:

velocity_model – Velocity model values (or slowness if slowness=True)
slowness – Whether velocity_model is slowness (1/v)

Returns:

Forward response (travel times)

set_mesh(mesh: pygimli.Mesh) → None[source]#

Set mesh for forward modeling.

Parameters:: mesh – PyGIMLI mesh

set_scheme(scheme: pygimli.DataContainer) → None[source]#

Set seismic data scheme for forward modeling.

Parameters:: scheme – Seismic data scheme

class PyHydroGeophysX.forward.TDEMForwardModeling(thicknesses: ndarray, survey_config: TDEMSurveyConfig | None = None, survey: simpeg.electromagnetics.time_domain.Survey | None = None)[source]#

Bases: object

Class for forward modeling of Time-Domain Electromagnetic (TDEM) data.

This class provides functionality for 1D layered Earth TDEM forward modeling using SimPEG’s time_domain module.

Example

>>> # Define layer model
>>> thicknesses = np.array([10.0, 30.0])
>>> conductivity = np.array([0.01, 0.1, 0.001])  # S/m
>>>
>>> # Create forward modeler
>>> fwd = TDEMForwardModeling(thicknesses=thicknesses)
>>>
>>> # Compute response
>>> response = fwd.forward(conductivity)

forward(conductivity: ndarray, log_input: bool = False) → ndarray[source]#

Compute forward response for a given conductivity model.

Parameters:

conductivity – Conductivity values for each layer (S/m)
log_input – If True, conductivity is log-transformed

Returns:

Forward response (magnetic flux density, T)

forward_with_noise(conductivity: ndarray, noise_level: float = 0.05, seed: int | None = None, log_input: bool = False) → Tuple[ndarray, ndarray, ndarray][source]#

Compute forward response with added Gaussian noise.

Parameters:

conductivity – Conductivity values for each layer (S/m)
noise_level – Relative noise level (default 5%)
seed – Random seed for reproducibility
log_input – If True, conductivity is log-transformed

Returns:

Tuple of (noisy_data, clean_data, uncertainties)

get_times() → ndarray[source]#: Get the time channels from the survey.

property n_data: int#: Number of data points.

class PyHydroGeophysX.forward.TDEMSurveyConfig(source_location: ndarray | None = None, source_radius: float = 10.0, source_current: float = 1.0, receiver_location: ndarray | None = None, receiver_orientation: str = 'z', times: ndarray | None = None, waveform_type: str = 'step_off')[source]#

Bases: object

Configuration for TDEM survey geometry.

source_location#

[x, y, z] location of source center (m)

Type:: numpy.ndarray

source_radius#

Radius of circular loop source (m)

Type:: float

source_current#

Peak current amplitude (A)

Type:: float

receiver_location#

[x, y, z] location of receiver (m)

Type:: numpy.ndarray

receiver_orientation#

Component to measure (‘x’, ‘y’, or ‘z’)

Type:: str

times#

Time channels for measurement (s)

Type:: numpy.ndarray

waveform_type#

Type of waveform (‘step_off’, ‘ramp_off’, ‘custom’)

Type:: str

receiver_location: ndarray = None#

receiver_orientation: str = 'z'#

source_current: float = 1.0#

source_location: ndarray = None#

source_radius: float = 10.0#

times: ndarray = None#

waveform_type: str = 'step_off'#

PyHydroGeophysX.forward.create_tdem_survey(times: ndarray, source_radius: float = 10.0, source_current: float = 1.0, source_location: ndarray | None = None, receiver_location: ndarray | None = None, receiver_orientation: str = 'z', waveform_type: str = 'step_off') → simpeg.electromagnetics.time_domain.Survey[source]#

Create a TDEM survey for 1D sounding.

Parameters:

times – Time channels (s)
source_radius – Loop radius (m)
source_current – Peak current (A)
source_location – Source center [x, y, z] (m)
receiver_location – Receiver position [x, y, z] (m)
receiver_orientation – Measurement component (‘x’, ‘y’, ‘z’)
waveform_type – Waveform type (‘step_off’, ‘ramp_off’)

Returns:

SimPEG TDEM Survey object

PyHydroGeophysX.forward.ertforandjac(fob, rhomodel, xr)[source]#

Forward model and Jacobian for ERT.

Parameters:

fob (pygimli.ERTModelling) – ERT forward operator.
rhomodel (pg.RVector) – Resistivity model.
xr (np.ndarray) – Log-transformed model parameter.

Returns:

Log-transformed forward response. J (np.ndarray): Jacobian matrix.

Return type:

dr (np.ndarray)

PyHydroGeophysX.forward.ertforandjac2(fob, xr, mesh)[source]#

Alternative ERT forward model and Jacobian using log-resistivity values.

Parameters:

fob (pygimli.ERTModelling) – ERT forward operator.
xr (np.ndarray) – Log-transformed model parameter.
mesh (pg.Mesh) – Mesh for the forward model.

Returns:

Log-transformed forward response. J (np.ndarray): Jacobian matrix.

Return type:

dr (np.ndarray)

PyHydroGeophysX.forward.ertforward(fob, mesh, rhomodel, xr)[source]#

Forward model for ERT.

Parameters:

fob (pygimli.ERTModelling) – ERT forward operator.
mesh (pg.Mesh) – Mesh for the forward model.
rhomodel (pg.RVector) – Resistivity model vector.
xr (np.ndarray) – Log-transformed model parameter (resistivity).

Returns:

Log-transformed forward response. rhomodel (pg.RVector): Updated resistivity model.

Return type:

dr (np.ndarray)

PyHydroGeophysX.forward.ertforward2(fob, xr, mesh)[source]#

Simplified ERT forward model.

Parameters:

fob (pygimli.ERTModelling) – ERT forward operator.
xr (np.ndarray) – Log-transformed model parameter.
mesh (pg.Mesh) – Mesh for the forward model.

Returns:

Log-transformed forward response.

Return type:

dr (np.ndarray)

PyHydroGeophysX.forward.hydro_to_tdem(water_content: ndarray, porosity: ndarray, layer_thicknesses: ndarray, sigma_w: float | ndarray = 0.05, m: float | ndarray = 1.5, n: float | ndarray = 2.0, sigma_s: float | ndarray = 0.0, times: ndarray | None = None, source_radius: float = 10.0, noise_level: float = 0.05, seed: int | None = None, verbose: bool = False) → Tuple[ndarray, ndarray, ndarray, ndarray][source]#

Convert hydrological properties to TDEM response.

This function takes water content and porosity from hydrological models and computes the expected TDEM response using petrophysical relationships.

Parameters:

water_content – Water content for each layer (-)
porosity – Porosity for each layer (-)
layer_thicknesses – Thickness of each layer except bottom (m)
sigma_w – Pore water conductivity (S/m)
m – Cementation exponent
n – Saturation exponent
sigma_s – Surface conductivity (S/m)
times – Time channels (s), default is logspace(-5, -2, 31)
source_radius – Loop radius (m)
noise_level – Relative noise level for synthetic data
seed – Random seed for reproducibility
verbose – Print progress information

Returns:

Tuple of (noisy_data, clean_data, uncertainties, conductivity)