Lecture 6b - Inverting Resistivity Soundings

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Flashcards about inverse modeling, error metrics, and resistivity sounding, covering key concepts and processes.

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20 Terms

1
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What is inverse modeling?

Estimating the model from the data, starting with data to arrive at a best fit model.

2
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What are the characteristics of most inversion problems?

Usually nonlinear and solved with an iterative numerical technique.

3
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What are the inputs required for inverse modeling?

Measured data and acquisition parameters, initial estimate of subsurface model.

4
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Why are initial estimates of subsurface models needed in inverse modeling?

To help the numerical computer algorithms converge on an appropriate solution since most inverse models are highly nonlinear.

5
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What is the first component within an iteration of inverse modeling?

Calculating the surface response from model parameters.

6
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What is said when the misfit is sufficiently small and the model can be accepted?

The algorithm has converged.

7
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What are the characteristics observed in the example sounding data?

High resistivity, decreased resistivity, starts to increase again.

8
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What was considered to be the apparent resistivity of the first and shallowest layer?

About 600 ohm meters.

9
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What do the model parameters represent for resistivity sounding?

The layers thicknesses and resistivities.

10
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What should interpretations align with in the absence of external information?

Soil, geology, or hydrological conditions.

11
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What could a submeter thickness of relatively low resistivity reflect?

Soil.

12
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What could a relatively low resistivity beneath the top layer represent?

A very clay-rich layer or an increasing influence of water.

13
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What is the most common way to quantify misfit and derive an optimum?

Least Squares.

14
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What it is calculated within the square brackets in the equation to calculate e?

The difference between observed and modeled apparent resistivities.

15
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How to normalize the error metric to account for the numbers of measurements involved?

Normalizing by dividing by the number of measurements included.

16
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What are common sources of error in resistivity inversion?

Random error from the measurement instrument, poor electrode contact with the ground.

17
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What does the model assume about resistivity?

Lateral continuity i.e. resistivity only varies vertically.

18
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What is the idea behind equivalence analysis?

Running the inversion repeatedly, making small perturbations each time to the data.

19
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For resistivity sounding, what do the model parameters represent?

Thicknesses and the resistivities of the layers.

20
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What is data inversion?

Iterative numerical modeling process, repeatedly runs a Ford model, automatically adjusting parameters until the model output best fits the measured data.