1.1. A Small-Scale Exploration Case History
When I was a young geophysicist, I started working in a service company specialized in geophysical methods applied to civil engineering, environmental, and archaeological studies. The main part of my work consisted in acquisition, processing, and interpretation of geophysical data in railway tunnels for estimating their stability conditions. However, from time to time, I was asked to give a geophysical support to small-scale archaeological projects. Although I ventured into the fascinating domain of the archaeological exploration just few times, I was lucky to work in important locations, such as Pompeii and other historical areas in southern Italy. I learned to use the ground penetrating radar, often called geo-radar or briefly GPR (Clark, 1996; Conyers, 2004; Gaffney and Gater, 2003; Himi et al., 2016; Jol, 2008), combined with other geophysical techniques. Thus, I started the hard life of field geophysicist, doing many direct experiences in geophysical surveys in different sites of Italy. I remember that one of the most exciting “adventures” was a small geophysical project addressed to explore the interior of an ancient church built at the beginning of the 17th century in the historical center of Bari (Italy). The problem that I was asked to solve was theoretically simple, but very complex in practice. Based on ambiguous and fragmentary information extracted from ancient documents, the monks knew about the presence of rooms and/or tunnels located below the floor of their church. Unfortunately, nobody was able to confirm either the reliability of the old documents or the underground distribution of the cavities. An additional problem, very difficult to solve, was detecting the exact location of the entry (the trapdoor) of the underground cavities. In fact, the floor of the church was very ancient and precious. For that reason, the monks asked me to detect the original entrance of the cavities and to allow the access from the top. They wanted to avoid any large excavation for limiting the damages to the floor of their church. There was an additional, good motivation for detecting the small entrances with extreme accuracy: reducing the risk of structural collapse. In fact, opening a new way of access different from the original one and entering from the roof of the underground rooms would have affected the stability of the building itself.
We decided to explore the subsoil of the church using the GPR. I would like to recall just some basic information about geo-radar, for who has not any familiarity with this type of geophysical method. GPR uses radar pulses to image the subsurface. It works in the high-frequency range (from megahertz to gigahertz). Thus, resolution is extremely high (from meters to centimeters), but the investigation range is necessarily limited. This is because of the rapid attenuation of high-frequency electromagnetic waves, especially in conductive materials. For these reasons, the use of GPR is mainly directed to civil engineering, archaeological, and environmental applications. A GPR transmitter emits electromagnetic energy into the medium to be investigated. This can be the ground, but it can also be an artificial structure, like the wall of a building. When the electromagnetic waves encounter a boundary between materials characterized by different electric properties, they may be reflected, refracted, or scattered back to a receiving antenna. The signal detected by the receiver can be displayed in real time on the computer screen while the acquisition proceeds. These data can be interpreted immediately, when fast detection of buried objects is required. Alternatively, these data can be analyzed and interpreted later in the office. In the latter case, a complex processing workflow can be applied to enhance the signal-to-noise ratio, to convert the response from time to depth domain, and so forth. Similar to reflection seismic (but using a different type of waves), stack and/or migrated GPR sections (or volumes) represent the final output.
Before starting our survey inside the church, we collected all the available data about the building, including ancient documents, approximate descriptions by the monks, and fragmentary indications by local people. Then we tried to compose the puzzle of this fragmentary “a priori information.” This was useful for limiting the investigation area, for defining an accurate acquisition program, and for optimizing the recording parameters. In this project, we planned to use two antennas having central frequency of 500 and 300 MHz, respectively. That choice was due to the expected size and depth of our targets. In fact, based on the available initial information, we expected to find the top of the rooms/tunnels at depth of less than 1 m below the ground. As I said, the access to these tunnels was expected to have a very small size (the monks talked about possible small trapdoors of about half meter width). Using an antenna of 500 MHz represented an ideal compromise between resolution and depth of investigation. Moreover, using also a 300-MHz antenna allowed us extending the exploration depth down to 4 to 5 m. That was a good setup for detecting relatively large rooms and tunnels and, at the same time, for detecting their small entrance with sufficient accuracy. With my team, I defined a dense network of reference points covering the floor. Finally, we started our survey using the 500-MHz antenna first.
I admit that, moving the antenna on the floor of the ancient church and looking at the GPR display in real time represented a unique experience for me. I was conscious that the target was something with high historical value. What did the tunnels represent? Were there any secret underground paths or something else? What did they hide? Could we discover ancient objects, relics, artifacts, paintings, old coins?
I think that geophysical prospecting addressed to archaeological exploration is one of the most exciting fields of applied geosciences. In fact, it represents a perfect combination of technology, science, and historical culture. Moreover, ability to capture weak signals, curiosity, enthusiasm, impulse toward the discovery, and serendipity are all instinctual attitudes necessary for a successful exploratory process. I felt these sensations all together while I was moving the antenna on the church floor.
Similar emotions motivated me to work for 12 h a day when I performed a similar geophysical survey in the area of Pompeii, just few months later. Back then, I was not conscious about that mix of feelings. Honestly, I did not try to investigate the nature of my emotions. I was just happy to do that work: a perfect integration of technical background and instinctual attitude to exploration.