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Gravity Methods

Lateral density contrasts in the subsurface produce tiny variations in gravitational acceleration, on the order of parts per million of \(g\). Gravity surveying measures those variations, strips away every predictable effect (instrument drift, tides, latitude, elevation, terrain), and interprets what remains as geology.

Learning Objectives

Undergraduate Core: By the end of this module, you will be able to:

  • Relate anomaly sign and amplitude to density contrast and source geometry.
  • Apply drift, latitude, free-air, Bouguer, and terrain corrections with consistent units and signs.
  • Estimate idealized source depth from a half-width measurement.
  • Explain why multiple density models can fit the same gravity anomaly.
Graduate Extension

Evaluate regional–residual separation, parameter trade-offs, equivalent-source behavior, and uncertainty in density-contrast inversion.

Practice this module Teach with active-learning slides

Interactive Lecture

Activities

Demo

  • Buried-Body Anomaly Modeler


    Drag a sphere or horizontal cylinder in the subsurface, set its density contrast, and watch the surface anomaly respond in real time.

Classroom Lab

🧰 Microgravity search for a limestone cavity — reduce a full base-loop dataset, document correction signs, estimate an idealized source depth, and write a qualified engineering recommendation.

Research Code: PyHydroGeophysX

Potential-field inversion

Gravity and magnetic data can be inverted together for subsurface density and susceptibility structure. PyHydroGeophysX, developed in Dr. Chen's group, includes a gravity and magnetics inversion example (source) alongside its electrical, seismic, and EM tools.

Data and Notebooks

  • 📊 Activity datasets live in the Data area.
  • 🚀 A Colab notebook version of the drift-correction exercise is in Notebooks.