Abstract

Ground-penetrating radar (GPR) and terrestrial laser scanning (TLS) surveys were conducted at a historic cemetery at Cape Canaveral Air Force Station, Florida, U.S., in order to confirm the presence of burials corresponding to grave markers and detect potential unmarked burials. Noise in the GPR data from surface features and subtle terrain differences must be addressed to determine the extent of anomalies of interest. We use singular value decomposition (SVD) to isolate and remove energy from GPR data. SVD allows one to remove unwanted signals that traditional processing techniques cannot. With SVD filtering, we resolve an anomaly adjacent to confirmed burials otherwise overprinted by unwanted signal. The migration of SVD-filtered data produces more distinct, spatially constrained point reflectors. Ground elevation is derived from georeferenced TLS data and compared to that from airborne laser scanning (ALS) to highlight subtle terrain that can assist data interpretation. TLS elevations show a subtle modern mound over the burial plot where ALS elevations show a depression. The targets of interest are approximately 20–30 cm higher in elevation if a topographic correction is performed using TLS versus ALS. In archaeological applications, a notable change is often recorded at the sub-meter scale. The combined approach presented here better resolves geophysical response of buried features and their positions in the ground relative to each other.

Highlights

  • Ground-penetrating radar (GPR) has long been used for determining the location, depth, and shape of human burials e.g., [1,2,3,4,5,6]

  • This paper presents the geophysical findings from the Wilson Brothers Cemetery on Cape Canaveral Air Force Station, Florida (CCAFS, Figure 1a) and the joint data processing and remote sensing techniques used to increase GPR image resolution and refine the shape and depth of anomalies

  • Common-offset GPR data were collected with a 500 MHz shielded antenna and MALÅProEx system, where the system was mounted on a cart and pushed along the ground surface

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Summary

Introduction

Ground-penetrating radar (GPR) has long been used for determining the location, depth, and shape of human burials e.g., [1,2,3,4,5,6]. The method does suffer from several significant limitations, including, but not limited to, high electromagnetic signal attenuation (loss of signal with depth), scattering (energy reflected in multiple directions), and false positives (misidentification) from roots or other buried objects (e.g., [3,7,8]). The GPR response of a grave is sometimes a diffraction pattern (hyperbola-shaped signature often produced by point-like targets) or a disturbed section of strata. In both scenarios, interpretations can be limited. The result is anomalies that comprise more than one target, making it challenging to distinguish individual buried objects

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