Characterization of ablation craters associated to Laser Induced Breakdown Spectroscopy (LIBS) measurements
Lena Bassel, Alain Queffelec, Maud Mulliez, Bruno Bousquet, Julian Guezenoc, Rémy Chapoulie and Clément Melkebeke
PACEA is a research laboratory for the French National Centre for Research (CNRS), the University of Bordeaux, and the French Ministry of Culture and Communication. Our research mostly focuses on Paleolithic cultures in Europe and Africa and their environments, biological anthropology, funerary practices, and rock art.
Confocal technology has proven to be an effective technique to investigate and characterize the size, diameter and depth of the craters of different LIBS instruments
The purpose of this study is dual: 1) to characterize the ablation craters associated to Laser Induced Breakdown Spectroscopy (LIBS) measurements on a fresco sample (Figure 1); and 2), to compare the craters on a 2-cent euro coin (Figure 2) associated to a portable instrument (EasyLIBS) and a laboratory instrument.
Part 1 – ANALYSES OF ABLATION CRATERS ON A FRESCO SAMPLE
A study on the dimension and depth of the ablation craters associated with the LIBS measurements was conducted. The craters were analyzed using the 3D optical profilometer S neox in Confocal mode. For this purpose, six ablation craters were formed following 1, 3, 8, 10, 15 and 20 laser shots (Figure 3). An initial qualitative observation established that the crater is accompanied by a dark aureole, which demonstrates that the matter was highly heated upon impact. This is termed the heat-affected zone or HAZ, which is well known in laser ablation.
The average size of the craters is approximately 800 µm x 400 µm on all of the craters formed. The crater formed by 20 shots was subject to a more in-depth study (Figure 4). Indeed, within the crater, a hollower area is observed, with dimensions of approximately 160 µm x 100 µm. The same observation was made for each of the ablation craters.
A profile taken along each of the craters demonstrates that the depth of the craters increases with the number of shots (Figure 5). The sample was hollowed out over around 100 µm in the deepest area after 20 shots.
Part 2 – COMPARISON OF ABLATION CRATERS ASSOCIATED TO TWO DIFFERENT LIBS INSTRUMENTS (EASYLIBS AND A LABORATORY INSTRUMENT)
In the case of the EasyLIBS intrument, a broad even ring can be observed demarcating the craters formed (Figure 6). Overall, the craters are very flat and shallow: it appears that a molten mass has been formed that has remained at the crater site and has not been ejected.
For the measurements carried out with the laboratory instrument, matter ejections are visible all around the crater (Figure 7). In addition, the craters formed using the laboratory instrument all have “edges” where the matter accumulates. The height of these edges in relation to the surface of the coin varies between 4 µm and 20 µm depending on the number of shots fired.
The comparison of the depth of the craters between the EasyLIBS and the Laboratory Instrument for different amounts of laser shots is shown in Table 1. In addition, Figure 8 and Figure 9 show 2D pictures of the resulting craters for both LIBS instruments after 50 and 500 shots, respectively.
The 3D optical profilometer S neox has been shown to be an accurate, fast and easy-to-use tool to investigate ablation craters associated to Laser Induced Breakdown Spectroscopy measurements. The 3D optical profilometry allowed qualitative and quantitative analysis, in particular, Confocal technology has proven to be an effective technique to investigate and characterize the size, diameter and depth of the craters of different LIBS instruments.
This is important to archaeologists, curators, since they need to assess the benefits/risk before applying micro-destructive methods on patrimonial artifacts.