Abstract

Defining the origin of ground deformation, which can be a very challenging task, may be approached through several investigative techniques. Ground deformation can originate in response to both natural (e.g., tectonics) and anthropic (e.g., groundwater pumping) contributions. These may either act simultaneously or be somewhat correlated in space and time. For example, the location of structurally controlled basins may be the locus of enhanced human-induced subsidence. In this paper, we investigate the natural and anthropic contributions to ground deformation in the urbanized area of the inner Sarno plain, in the Southern Apennines. We used a multidisciplinary approach based on the collection and analysis of a combination of geomorphological, stratigraphical, structural, hydrogeological, GPS, and DInSAR datasets. Geomorphological, stratigraphical, and structural data suggested the occurrence of a graben-like depocenter, the Sarno basin, bounded by faults with evidence of activity in the last 39 ka. Geodetic data indicated that the Sarno basin also experienced ground deformation (mostly subsidence) in the last 30 years, with a possible anthropogenic contribution due to groundwater pumping. Hydrogeological data suggested that a significant portion of the subsidence detected by geodetic data can be ascribed to groundwater pumping from the alluvial plain aquifer, rather than to a re-activation of faults in the last 30 years. Our interpretation suggested that a positive feedback exists between fault activity and the location of area affected by human-induced subsidence. In fact, fault activity caused the accumulation of poorly consolidated deposits within the Sarno basin, which enhanced groundwater-induced subsidence. The multidisciplinary approach used here was proven to be successful within the study area and could therefore be an effective tool for investigating ground deformation in other urbanized areas worldwide.

Highlights

  • Ground deformation is a complex phenomenon that may derive from both natural and anthropic causes

  • This makes the analysis of the ground deformation a very challenging task, especially in urbanized areas

  • Geomorphological, stratigraphic, and structural analyses of the mountain front-pediment-alluvial plain system were coupled with global navigation satellite system (GNSS) and differential interferometric synthetic aperture radar (DInSAR)

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Summary

Introduction

Ground deformation is a complex phenomenon that may derive from both natural (e.g., tectonics, landslides, and sinkholes) and anthropic (e.g., human-induced subsidence) causes. Natural- and anthropic-induced subsidence may act simultaneously [1] and, in some cases, areas affected by human-induced subsidence have been shown to be clustered within basins bounded by active faults [2,3]. This makes the analysis of the ground deformation a very challenging task, especially in urbanized areas. Further difficulties in the recognition of the causes that drive ground deformation may derive from the location of the investigated urban area.

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