Alternative Approaches to Study Mining and Mineral Science at ISOLDE-CERN

ISOLDE-CERN is a large-scale facility for the on-line production of exotic radioactive isotopes, with high yields, high elemental selectivity and isotopic purity. Solid-state physics research at ISOLDE-CERN has been ongoing since 1976 and offers opportunities to conduct experiments using various material characterization techniques such as self-diffusion, photoluminescence, emission channelling, Mössbauer spectroscopy and perturbed angular correlations. The expertise of pioneers in our group and the variety of high-quality beams available at ISOLDE offer alternative approaches to research into mining and mineral science. This paper reviews the various beams, techniques and infrastructure that are available at ISOLDE-CERN and presents an investigation of diamond as a typical research example.


Introduction
: Typical target-ion-source unit used at ISOLDE-CERN. CERN is the copyright holder of the image (CERN-EX-0204023-01).
Mineral science involves the investigation of material properties including the chemical, crystal structure, physical and optical properties of minerals and mineralized artefacts. It is not feasible to create the important materials obtained by mining in a factory or laboratory. These materials are usually investigated by using conventional characterization techniques. However, ISOLDE-CERN offers more exotic techniques [1,2] that provide important additional information to help answer questions that cannot be answered by conventional methods. The solid-state physics programme at ISOLDE-CERN thus offers unique analytical instruments and expertise that complement traditional characterization techniques for optimizing materials for various applications. For example, to incorporate short-lived radioisotopes into materials, ISOLDE-CERN offers expertise and instrumentation for ion implantation and subsequent thermal annealing. The ISOLDE laboratory is a radioactive-ion-beam facility and is the oldest running installation at the CERN accelerator complex. The laboratory recently celebrated 50 years of successful operation with 40 years of production of high-quality beam for materials science research. The 1.4 GeV proton beam from the Proton Synchrotron Booster at CERN is directed to independent target-ion-source units at ISOLDE (Figure 1). Depending on the requirements of specific experiments, ISOLDE can produce appropriate targets made of different materials and equipped with different types of ion sources. The ion sources used at ISOLDE are based on surface ionization, plasma ionization or a resonance ionization laser ion source. The target units are coupled to two conceptually different isotope separators. After mass separation, the beam is delivered to the beamlines at the ISOLDE hall. The equipment for materials science research is located in the low-energy-beam area, where the beam is accelerated up to 60 keV.
To illustrate the techniques available at ISOLDE-CERN, we now describe measurements performed in diamond. Implantation into diamond is an interesting subject motivated by the search for suitable n-type dopant atoms, which would lead to an ideal base for semiconducting devices for specific applications. Implanting dopant atoms into diamond allows us to tune several material properties, such as the high thermal conductivity, wide band gap, extreme hardness and high mobility for both p-and n-type carriers. Figure 2 shows photographs of some of the materialcharacterization setups available at ISOLDE-CERN. The optical and electronic properties of materials can be investigated by using the photoluminescence (PL) setup for materials implanted with radioactive isotopes [2,3]. Since ISOLDE-CERN can produce over 1000 different isotopes, the observation of either decay or growth related to implanted long-or short-lived radiotracers allows for distinct chemical identification of chemical species in several material types and compositions [4][5][6]. Recently, a study was proposed at ISOLDE to determine the route by which an unidentified phosphorus vacancy is produced via implantation of 31 Al in diamond [7]. The emission channelling (EC) technique provides information about the lattice location of isotopes implant in the single crystals [8,9]. ISOLDE-CERN is the only laboratory in the world that has an EC setup. The facility is the most convenient "home" for the EC technique, since it provides over 1000 different isotopes of most elements in the periodic table. For a given elemental dopant, the adequate radioactive isotope is selected and implanted into a single crystal. The EC measurements can be performed online or offline, depending on the half-life of the probe. Position-and energy-sensitive detectors are used to detect decay particles in the vicinity of major crystallographic directions and provide accurate information on the lattice location of the dopant. Depending on particle charge and on the lattice site of the radioactive dopants, decay particles such as α, β − , β + and CE can be channelled or blocked on their route out of the crystal. The measurement can be performed as a function of thermal annealing, implantation fluency and temperature. The experimental patterns are determined by fitting via simulations for data interpretation. Even for different lattice sites, the lattice location of the dopant can be determined with unrivalled precision. Recently, the thermal stability of both interstitial and substitutional Mn in ferromagnetic (Ga,Mn)As was investigated by using the EC technique [9]. For instance, 73 As-implanted diamond shows that thermal annealing above 1200 K leads to substitutional lattice occupation at a fraction of approximately 50% [10,11]. The implantation was performed at energies of 120 and 60 keV and with doses of 5×10 12 and 1×10 13 ions/cm 2 for 111 In and 73 As, respectively [10]. The implantation of radioactive As ions was performed at room temperature at ISOLDE-CERN. About 40% of the In ions occupied substitutional lattice sites, whereas over 50% of As ions occupied these sites. Furthermore, the results obtained with the In probe show that implantation at 1373 K yields the same fraction of dopant ions at substitutional sites as does roomtemperature implantation [10]. The experiments performed using 111 In and 73 As as probes show that the implantation damage induced by the heavy-ion implantation process is annealed in two distinct stages [10]. Mössbauer spectroscopy (MS) gives information on the electric-field gradient, magnetic hyperfine field, charge symmetry and binding properties [12,13]. ISOLDE-CERN, offers the possibility to carry out online experiments in which short-lived radioactive isotopes are produced, directly implanted into materials and measured at the beamline. Depending on the lifetime, the implantation and emission Mössbauer spectroscopy (eMS) measurements may occur at the same time or they may be separated in space and time. For example, the Mössbauer isotope 119 Sn presents a 24 keV Mössbauer transition, which is populated in the decay of a 119m Sn isomeric state. At ISOLDE-CERN, the implantation of 119 In and 119 Sb probes as precursor isotopes into materials enables the controlled incorporation of 119 Sn probe atoms into a particular lattice site [12]. The MS technique was used at ISOLDE-CERN to study the incorporation, lattice location and annealing of defects of Sb and Sn ions in diamond [14]. The results obtained covered a broad distribution that reflected the implantation-induced lattice damage. The spectrum was fit with two symmetric doublet components. The samples were also measured as a function of annealing temperature and the analysis required a single line S1 with isomer shift δ=1.74(4) mm/s in addition to a weaker line at 0.52 mm/s. The increasing intensity of S1 evinced the recovery of lattice damage by thermal annealing. The results indicate that, after implantation at room temperature followed by thermal annealing above 1300 K, 40% of the 119 Sn implanted ion probes occupy or are close to regular lattice sites.

Techniques
Perturbed angular correlations (PAC) experiments provide information about the local structure of matter via hyperfine interactions [15][16][17]. A conventional PAC experiment detects two γ rays emitted in succession from a nuclear decay. The first is detected, selecting a spin-aligned ensemble; the second is then emitted from this ensemble anisotropically with respect to the first γ ray. Here, because nuclear decay conserves angular momentum, the probability of a γ ray being emitted in a certain direction depends on the orientation of the nuclear spin I. The spin orientations of the PAC probes initially are randomly distributed, so radiation is emitted isotropically in space. To observe an anisotropic angular distribution of radiation, an ensemble of nuclei is selected with an aligned spin distribution. This selection is done by detecting the first γ ray of the cascade in a given direction. Note that the probability of emission of the second γ ray is therefore anisotropic with respect to the direction of the first γ ray, with an anisotropy coefficient that depends on the properties of the nuclear decay cascade. Once the PAC probe is incorporated into a crystal lattice, information about the local structure may be obtained via hyperfine interactions. Outside the ISOLDE-CERN laboratories, PAC measurements of diamond were performed using 181 Hf probes [18]. The samples consisted of (100) cleaved single-crystal diamond. Two distinct electric-field gradients, V zz(1) =5.5×10 21 V/m 2 and V zz(2) =9.6×10 21 V/ m 2 , were observed in fractions of 5% for each local environment. The results show that these low probe fractions experience axially symmetric electric-field gradients. Moreover, the bulk of the probe ions is strongly disturbed by higher electric-field gradients. These results are consistent with measurements made using 111 In probes [19]. The measurement made with the 181 Hf probes was crucial to complement the measurement with the 111 In probes to verify the possible existence of after-effects [20,21] coming from the electroncapture decay of 111 In. Type-IIa diamond with a band gap of about 5.3 eV is a perfect insulator and would likely allow such effects. Later, the measurement results were compared with experimental results obtained using 111m Cd probes [22]. The results indicate that the loss of anisotropy in the PAC signal is not due to after-effects but to extended lattice damage produced by the implantation process that remained even after thermal annealing at high temperatures. Therefore, the authors suggest that low-dose implantation at a range of energies is more appropriate for dopant incorporation at regular, defect-free lattice sites. Radiotracer diffusion provides information about the thermal motion of lattice ions and is the oldest technique used in nuclear solid-state physics [23]. At ISOLDE-CERN, the Online Diffusion Chamber (ODC) serves to measure the diffusion profile of Copyright © Schell J AMMS.MS.ID.000592. 4(4).2020 radioactive isotopes in materials, even if probes are short lived. The study of how host elements self-diffuse in a crystalline lattice is of considerable importance for materials science (Figure 3). The ODC allows for a very direct measurement of diffusion profiles, which is highly indicative of the diffusion mechanism in the material of interest. The self-diffusion method [24] has yet to be used for investigating diamond. Recently, the technique was used to study the incorporation of Cd into a titanium dioxide lattice [25]. For instance, this radiotracer technique was used to investigate the diffusion of all constituent elements in equi-atomic CoCrFeNi and CoCrFeMnNi [24]. The constituent elements have significantly different diffusion rates, with Mn diffusing the fastest and Ni and Co the slowest.

Conclusion
This short communication describes various possible applications of radioactive-ion beams produced at the ISOLDE-CERN facility in nuclear solid-state physics and for studying the incorporation of probe atoms into solids. Having been successfully applied in diamond, these methods can also be used for investigations in mining and mineral science. The incorporation of radioactive isotopes can be controlled systematically by implantation and annealing. A careful annealing procedure gradually corrects defect bonds between carbon atoms, thereby leading to the recovery of the regular lattice structure in the local environment of the probe isotopes. To propose investigations of materials at ISOLDE-CERN, please contact the physics coordinator and the solid-state physics coordinator [26]. Scientific proposals are evaluated by the ISOLDE and Neutron Time-of-Flight Committee (INTC) [27].