The experiments were performed in the open, in a travertine quarry (IMEG) near Montemarano (Tuscany, Italy), on an area of flat and soft ground which had been chosen to minimise secondary fragmentation which might normally occur when primary fragments collide with the walls or floor of a chamber.
The Sussex research team, on site during the experiments, consisted of Professor Giuseppe Martelli, Dr. Pamela Rothwell, Miss Christina Tindall (then a 3rd year project student), Mr (now Dr.) Sam Coles and the group's technician, Mr. Brian Blackman. Both Dr. Mario Di Martino and Mr. Walter Ferreri, from the Turin group, also helped during the campaign period, as did Dr. Fabrizio Capaccioni of the CNR, Rome. These experiments were carried out in Italy primarily because of the collaboration between the Sussex and Turin groups - the Astronomical Observatory of Turin provided essential technical support for this project as well as the NAC fast-framing camera, the full-time help of Mario Di Martino and the technical knowledge of Walter Ferreri, principal photographic expert at the Turin Observatory. The targets were disrupted each on different days between the 9th and 13th of September 1989 - a fortunate period of good weather.
A long-lasting professional relationship between Professor Martelli and the management of the IMEG travertine quarry has guaranteed an excellent level of technical support on site in terms of access, electrical power supply and heavy lift equipment (when required for the construction of shelters and blast shields).
Spherical targets of 205 mm diameter were used throughout this experimental campaign. This is the size that had been used in previous series of experiments by the Sussex/Turin group (see e.g. Capaccioni et al. 1984), and the choice was based upon the size of the vacuum tanks used in these earlier experiments, since the targets needed to be small compared to the size of the tanks used in these experiments (~1 m3), but still large enough to provide macroscopic fragments.
The targets were constructed from strong alumina cement mortar, since this mixture gives a good approximation to the mechanical parameters of many natural rocks. The artificial rock, which has a density of 1.77 g cm-3, consisted of alumina cement, Carborundum (SiC) and water in the correct stechiometric ratio. While liquid, the cement mixture was shaken at frequencies ranging from 10 Hz to 100 Hz in order to release any air or gas trapped as bubbles. Once hardened, the targets were 'cured' by leaving them in water for a minimum of 27 days. The fully cured targets were then zonally painted in different colours to facilitate identification of surface fragments and reconstruction after the experiment. The cement of each target had been dyed with different colours to make fragments more clearly visible on the ground and avoid confusion in case the collection of a fragment had been overlooked from a previous experiment.
The targets used in shots 2 and 3 contained a denser and harder central core of diameter 105 mm. It was constructed separately and placed within the target by the following steps:
1. Three small indentations were made in the core using a centre point drill, at a mutual angular separation of 60° around a notional 'equator';
2. Three smooth, thin and rigid metal rods were used to support the core within the mould which was to be used for the main body of the target, accurately positioned to within 1mm. These rods were locked securely in order to prevent any movement while the target cement was being vibrated during the drying/curing process;
3. Mantle cement was poured in from the top of the mould and allowed to solidify and cure as outlined above;
4. The metal rods were removed and a small amount of liquid mantle cement was used to fill the remaining holes.
The density of this core, 2.05 g cm-3, is the highest which could be achieved by increasing the proportion of SiC without upsetting the stechiometric ratio (i.e. keeping the nature of the rock constant).
Table 2.1 gives the physical characteristics of the two types of target materials - classified as 'mantle' (that used in the homogeneous targets and outer mantle of the cored targets) and 'core' (used in the cores of those targets used in shots 2 and 3).
| Core | Mantle | |
| Density (gcm-3) | 2.05 | 1.77 |
| Static compressive strength | 4.0 ´ 108 erg cm-3 | 1.7 ´ 108 erg cm-3 |
| Porosity | ~10% | ~15% |
Table 2.1: Physical properties of the target materials
A number of different impacting techniques are available for carrying out catastrophic disruption experiments, each more or less suitable in particular ways for the aims of various research programmes. These are listed below, with examples of their use and a brief description of their relative merits:

Figure 2.1: A schematic of the modified shaped charge, capable of consistently producing velocities of the order of 10 km s-1. The second, smaller piece of explosive is detonated sympathetically when the initial shock wave reaches it.
Holsapple (1980) carried out an experimental study of the equivalence between high- and hypervelocity impact by projectile and the effect of an explosive charge placed in direct contact with the target at the desired impact site. Although the study applied primarily to nuclear explosions and their TNT equivalents, the results are applicable to the plastic explosive more commonly used these days. The conclusion of this study was that it is straightforward to simulate a simple projectile impact at a specified velocity using a contact (or more precisely, buried) explosive charge, if the ratio of charge depth d, to charge radius r, can be controlled. For a projectile velocity of 6.2 km s-1, which is the detonation velocity of the explosive used in these experiments, the requirement is that this ratio d/r should be 1.8±10% and that r should be approximately
of the target diameter.
The Sussex/Turin group used the contact charge as follows: A small cavity in the base of the artificial rock target was filled with plastic explosive, as shown in Fig. 2.2. The dimensions of the cylindrical cavity were 26 mm (depth) by 25 mm. The target, with contact charge in place, was placed at the centre of a specially constructed steel table of height 1m. This table had at its centre a small hole, though which the detonating cable was passed.

Figure 2.2: Contact charge technique used by the Sussex/Turin group in 1989 and 1992.
Figure 2.2 shows the experimental arrangement with steel table, artificial rock target and contact charge. The explosive used, Gelatin 2b, has a detonation velocity of 6.1 km s-1 and an acoustic impedance similar to that of the target (»7×105 g cm-2 s-1).
A ballistic pendulum was used to find the energy delivered by the explosive, and hence the momentum delivered by an equivalent projectile. This pendulum consisted of a square block of steel weighing 4.7 kg, which had been provided with a cavity identical to that in the base of the target. This block was suspended by four wires, each 6 m long. The cavity was filled with explosive and upon detonation of the explosive, the height gained by the pendulum was recorded by means of fast-framing cameras. Since the impact velocity of the equivalent projectile is fixed (at the detonation velocity of the explosive), the mass is uniquely determined, in this case as 1.85 g.
The contact charge method provides a fairly realistic simulation of a rock-rock impact (see e.g. Housen et al. 1991) because the acoustic impedance of the artificial rock target is well matched by that of the exploding charge located against the target itself. This conclusion has been reinforced by a study of the morphology of some of the fragments coming from the region in direct contact with the explosive charge; in some cases there were clearly evident conical impact structures, as shown in figure 2.3. These formations are very similar to those found in rock which has experienced impact cratering and fragmentation (see e.g. Fujiwara 1985), when the impact pressure exceeds approximately 5 MPs. This is a result of the shear induced by the forward compressional wave and the transverse stress applied to the edges of the transient crater.

Figure 2.3: Two fragments (with an end-on view of the second) originating near the contact point, clearly showing the conical impact structures often found following 'real' impact upon rock targets. The two fragments are both approximately 3 cm in length.
Target disruption was recorded using a single NAC E-10 16 mm fast-framing camera, together with two fast-shuttered CCD TV cameras for quick on-site analysis. The NAC cine camera, using Eastman/Kodak 7222 "Double-X" Negative film, was running at 700 frames per second in all the 1989 experiments. This frame rate, considered sufficient to catch the fastest fragments of observable size (~1 cm), was chosen based upon an estimate of the observed velocity of ejected fragments from other similar experiments (see e.g. Capaccioni et al., 1984) and taking into account the field of view available with the geometric arrangement used here. This choice was soon confirmed to have been well made - Martinsson (1990) indeed reports that the maximum speed observed in the fragment and dust envelope from these experiments is of the order of 20 m s-1 in our experiments, and our own later analysis of the film suggested no fragments moving too fast to be detected. Figure 2.4 shows the arena arrangement used in 1989.

Figure 2.4: 1989 Arena arrangement (not to scale) showing the three cameras, target table and the mirrors used to reflect views to the CCD camera equipment
The ground surrounding the experimental table, out to a distance of 30m, was divided into 24 sectors of 15° each - this allowed us to measure fragment positions on the ground, as they were collected, to within a few cm of radial distance and within 1 degree of angle. In order to study the distribution of fragment ejection angles, all fragments which could be found after the shot were collected in plastic bags and labelled with a letter and number code corresponding to their position on the ground.
The four 100 foot reels of film (one recorded for each shot) from the NAC fast-framing camera were processed in Italy by Mr. Walter Ferreri, photographic expert at the Turin Astronomical Observatory. On their arrival at the Sussex laboratory, the films were transcribed from the 16 mm cine format to PAL video tape for the digitising, using the apparatus shown in Fig. 2.5. By playing the 16mm film at standard speed and recording it on a video system, the film sequences were effectively slowed down from the original 700 frames per second to only 24. Given that PAL video has a standard 50 fields per second (where sequential 'odd' and 'even' fields form TV frames) there was no doubt that the cine film would be fully captured. The intention was to grab only one from each pair of fields, thus building a digitised set of all original frames.

Figure 2.5: Apparatus used to transcribe the 1989 cine films (hardware not to scale).
This work was all carried out in our laboratory at Sussex. The room lights were switched off during transcription, and the skylight was covered using black plastic. A standard Fumeo 16mm cine projector (item 1 in Fig. 2.5) was used to project the NAC images onto a matt white board, item 6 above. The CCD camera used (item 2 in Fig. 2.5) was a Philips LDH 0460/01 monochrome video camera incorporating a manual gain control (MGC). The lens (item 3) attached to the camera was a Sony "TV Zoom Lens" type 816358 with aperture at maximum (1.8) and ¦ = 20 mm, chosen to give a full-screen picture of the projected image. A Kodak Wratten-Gelatin ND 1.00 filter (item 4, giving an attenuation factor of 101.00 = 10) was placed in front of the zoom lens and in front of this was an HA3 infra-red filter (item 5) which served the purpose of minimising infra-red glare from the hot-filament projector.
Several 'dry runs' (i.e. without the video recorders running) were carried out with each reel of film, carefully monitoring the CCD output using the oscilloscope in order to find the optimum setting (of 1V peak-to-peak on the video signal) for the MGC. The output from the CCD video camera was then fed through a video timer and recorded separately on both VHS and Betamax machines. This had the advantage that, since both generate standard PAL video signals, either could have been used as input to the video digitiser. Two 'originals' of each resulting video cassette were made, with the total footage on each tape (i.e. all four shots) being about 15 minutes.
Although the system might seem unsuitable, with the projector running at 24 frames per second and the CCD camera recording 25 per second, this did not cause any problems. Clearly all frames of cine film would be caught, with one in 24 being caught twice. It was very clear from the computer-animated sequences just when this had happened - it did not occur within the early frames for any of the 4 shots (see Section 4.3), and thus was not a hindrance.
Before any analysis was made of the NAC high-speed film, the size and mass of fragments from shots 1 and 3 were all measured by hand. The size was measured to an accuracy of 1 mm using a pair of digital callipers and the data entered, together with the mass, into a simple database program called ROX-INP which I myself wrote as part of a 3rd year project at Sussex (Giblin, 1989). The fragment axial sizes were measured according to the top-down method, that is to say the largest dimension was found first and labelled a, then the largest dimension perpendicular to this was found and labelled b, and finally the fragment diameter was measured perpendicular to both of these and labelled c. Fragment masses were measured using a digital balance, to an accuracy of 0.01g. Although shots 1 and 3 were not covered by these measurements, this data provided an essential comparison to the measurements made from the digitised film records, as described in Chapter 4. Table 2.2 summarises the results of these measurements, including the total recovered mass as a fraction of the original target mass.
| Shot | No. weighed | Recovered mass /kg | Fraction | No. 'sized' |
| 1 | 129 | 4.775 | 54 % | 111 |
| 3 | 97 | 5.461 | 63 % | 87 |
Table 2.2: Details of in-hand measurements made upon recovered fragments
The data files created by the ROX-INP program was readable by the software developed for this project, and the data has been used wherever possible. Appendix 6 contains a listing of all fragment data, both from the NAC film records and from the in-hand measurements.