Preprints
https://doi.org/10.5194/egusphere-2026-2676
https://doi.org/10.5194/egusphere-2026-2676
30 Sep 2026
 | 30 Sep 2026
Status: this preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).

Equal Area, Unequal Connectivity: A Random-Field Framework for Liquefaction Hazard Organization

Şahin Çağlar Tuna

Abstract. Scalar liquefaction hazard descriptors quantify the amount of potentially unstable ground, but they do not describe how susceptible or low-resistance zones are spatially organized. As a result, equal weak-zone area may correspond to fragmented, clustered, or domain-scale connected configurations with different field-scale implications.

This study develops a connectivity-based random-field framework to distinguish weak-zone extent from weak-zone organization in spatially variable liquefaction susceptibility fields. Dataset-informed synthetic Gaussian Random Field realizations were generated from cleaned SPTN160 statistics and investigation-domain geometry. The fields were converted into binary low-resistance weak-zone domains through lower-tail equal-area thresholding and quantified using graph-based connectivity descriptors.

Across a dense Pf−θ parameter space, where Pf is the prescribed weak-zone area fraction and θ is the spatial correlation length, the results reveal a systematic transition from fragmented to clustered and spanning regimes. Low-Pf fields remain fragmented across the explored range, whereas higher-Pf​ fields progressively develop larger connected components and domain-scale continuity. The clearest transition occurs around Pf=0.50, where spanning probability exceeds 0.50 once θ reaches approximately 200 m.

A random-allocation null model shows that spatially correlated fields produce fewer connected components, lower fragmentation, larger dominant components, and stronger top-cluster concentration than random fields with the same weak-zone area fraction. The 2011 Christchurch manifestation field further indicates that observed liquefaction patterns also contain non-random spatial organization beyond affected-area fraction. By separating hazard extent from spatial organization, the framework provides a topology-aware basis for interpreting field-scale liquefaction hazard and for identifying whether susceptible zones imply local, cluster-scale, or system-scale mitigation relevance.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Şahin Çağlar Tuna

Status: open (until 11 Nov 2026)

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Şahin Çağlar Tuna
Şahin Çağlar Tuna
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Short summary
This study shows that risk is not defined only by how much ground is hazardous, but also by how hazardous zones are connected. Using simulated spatial patterns and observations from the 2011 Christchurch earthquake, it demonstrates that equal hazard area can produce fragmented, clustered, or widely connected patterns. This matters for planning because connected hazard zones may affect roads, waterfronts, lifelines, and urban areas at larger scales.
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