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Geophysical Survey
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The interpretation of geophysical data involves solving an inverse problem: inferring the causes (subsurface properties) from the effects (measured data). Geophysical inversion is inherently non-unique. Multiple disparate subsurface models can often produce statistically identical datasets.
The concept of Geophysical Equivalence is central to this uncertainty. For instance, in electrical resistivity tomography, a thin, highly conductive layer can produc… -
Hydrostatic Equation
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Comparative Table of Density Assumptions
The choice of density model profoundly impacts the resulting pressure profile calculated from the hydrostatic equation. The following table summarizes key assumptions.
| Context | Fluid Type | Density Model ($\rho$) | Resulting Pressure Profile | Primary Limitation |