Water Loaded Subsidence Calculator

Water-loaded tectonic subsidence after removing the sediment load and replacing it with water: Y = S(rho_m - rho_s)/(rho_m - rho_w) - Wd.

Description

Water-loaded tectonic subsidence after removing the sediment load and replacing it with water: Y = S(rho_m - rho_s)/(rho_m - rho_w) - Wd.

Water Loaded Subsidence Calculator: Water-loaded tectonic subsidence after removing the sediment load and replacing it with water: Y = S(rho_m - rho_s)/(rho_m - rho_w) - Wd.

When to use Water Loaded Subsidence

Use this geological calculation for a transparent first-pass interpretation of measured rock, soil, fluid, well, stratigraphic, isotopic, geophysical, or seismic data under an explicitly selected model.

Decompacted thickness (m)
Backstripped-unit decompacted thickness in metres.
Sediment density (kg/m^3)
Mean sediment density in kilograms per cubic metre.
Paleo-water depth (m)
Paleo-water depth at deposition in metres (positive down).
Mantle density (kg/m^3)
Mantle (asthenosphere) density in kilograms per cubic metre; default 3330.
Water density (kg/m^3)
Paleo-water density in kilograms per cubic metre; default 1000.

How Water Loaded Subsidence works

Water-loaded tectonic subsidence after removing the sediment load and replacing it with water: Y = S(rho_m - rho_s)/(rho_m - rho_w) - Wd. The tool evaluates the supplied inputs together and returns the named outputs below; it does not infer omitted operating conditions or change the units shown.1

Water-loaded subsidence (m)
Water-loaded tectonic subsidence in metres.

Limitations and assumptions

  • Gravity, magnetic, flexural, and subsidence interpretations are non-unique and depend on datum, corrections, density or susceptibility contrasts, regional removal, geometry, elastic assumptions, and noise. A corrected anomaly is not a unique subsurface model.
  • Use finite inputs in the displayed units and preserve more precision than the final presentation requires. Independently verify safety-critical, financial, compliance, or production decisions.

Alternative or Complementary approaches

Compare independent measurements and models, retain units and analytical metadata, propagate uncertainty, and validate interpretations against logs, cores, maps, laboratory data, or field observations.

References

  1. Geophysics — Wikipedia contributors

Similar or alternative tools

  • Air Loaded Subsidence Calculator

    Air-loaded tectonic subsidence with the water column replaced by air (zero load): Y = S(rho_m - rho_s)/rho_m - Wd.

  • Backstripping Subsidence Calculator

    Water-loaded backstripped tectonic subsidence (Steckler & Watts 1978) with a eustatic correction: Y = S(rho_m - rho_s)/(rho_m - rho_w) - Wd + dSL * rho_w/(rho_m - rho_w). Positive sea-level change means past sea level was higher than present.

  • Subsidence Rate Calculator

    Average tectonic-plus-loaded subsidence rate over an interval: amount divided by duration.

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