Subsurface environments are not observed directly. Instead, they are inferred.
In many exploration settings, structure is reconstructed from indirect measurements, sparse signals, and limited access. Verification requires disturbance: drilling, excavation, sampling, injection, or robotic intrusion. These same acts can alter the system under investigation and initiate irreversible commitments before interpretation has converged.
This work examines that condition.

This research addresses exploration in environments where:
The focus spans planetary subsurface geophysics, exploration systems engineering, and decision thresholds under irreversibility, with primary application to lunar and cislunar environments.
Indirect sensing reduces uncertainty but does not eliminate it. Distinct subsurface configurations can produce indistinguishable observations. As data accumulates, ambiguity may narrow but often remains structurally persistent.
Resolving that ambiguity requires intervention. Exploration therefore learns through disturbance. Disturbance is not epistemically neutral. It modifies the physical state of the system, alters the signals used for interpretation, and initiates sequences of access, infrastructure, and dependency.
Exploration therefore is not a progression from sensing to certainty. Instead, it is a transition across thresholds where learning and commitment become coupled.
This work formalizes subsurface exploration as a threshold problem under coupled uncertainty and irreversibility. In these regimes:
The objective is to characterize how knowledge is produced under these constraints, how disturbance reshapes both environment and observability, and how exploration systems behave when uncertainty remains decision-dominant.
This condition arises wherever access is constrained, inference is indirect, and disturbance has persistent effects, including:
Across these systems, a consistent progression appears:
The central issue is is how systems act before what is unknown is sufficiently resolved.

What aspects of subsurface structure are resolvable prior to disturbance?
Characterizes what aspects of subsurface structure are resolvable prior to disturbance, and identifies regimes where additional sensing does not materially reduce ambiguity.

Why do multiple interpretations remain viable as evidence accumulates?
Examines non-uniqueness in geophysical inversion and distinguishes reducible uncertainty from structurally persistent ambiguity.

How does intervention alter the system being observed?
Analyzes how drilling, excavation, and sampling modify system state, including pressure fields, volatile distribution, and mechanical properties, thereby altering subsequent observables.

How do exploration systems shape knowledge production?
Evaluates how system design (e.g. mobility, access geometry, sensing placement, and sequencing) conditions what can be known, when, and at what cost.

When does exploration transition from learning to commitment?
Determines when disturbance yields sufficient information relative to the irreversible commitments it creates, and identifies conditions under which further action remains permissible.

The lunar south polar region represents a high-constraint exploration regime. Subsurface structure, volatile distribution, and regolith properties remain only partially resolved. Verification requires disturbance. These disturbances are unlikely to remain isolated scientific acts.
They may become coupled to:
Under these conditions, exploration activity can rapidly transition into system formation.
The central question then becomes: what constitutes sufficient evidence prior to irreversible lunar commitment?

Several classes of action introduce disproportionately high levels of irreversible exposure:
These classes differ in reversibility, information yield, and their capacity to induce path dependence. Treating them as homogeneous obscures the structure of commitment formation.
A central distinction in this work is between four layers:
A system may satisfy the first two and still fail the third. This distinction is critical in environments where infrastructure, access, and sequencing can advance ahead of evidentiary sufficiency, and where commitments must remain valid as the system evolves.
This research integrates:
The objective is a disciplined characterization of what can be known prior to disturbance, how disturbance alters both system and inference, and when further action remains admissible.
Marine and seabed systems provide operational analogs. They exhibit constrained observability, robotic mediation, environmental sensitivity, infrastructure-driven path dependence, and high costs. These systems offer empirical grounding for exploration dynamics that also govern planetary environments.
This work defines a class of problems at the intersection of geophysics, planetary science, and exploration systems engineering: reliable knowledge cannot be produced without disturbance, and disturbance itself introduces irreversible consequences.
The contribution is a formal treatment of exploration thresholds. It incorporates limits of detectability, persistence of ambiguity, conditions under which disturbance becomes necessary, and conditions under which commitment becomes inadmissible.
Disturbance is both a mechanism of learning and one by which exploration begins to shape the system it seeks to understand.
In disturbance-constrained environments, the transition from observation to intervention defines the boundary between knowledge acquisition and irreversible commitment.
We use cookies to analyze website traffic and optimize your website experience. By accepting our use of cookies, your data will be aggregated with all other user data.