ToF-SIMS analysis of carbonaceous particles in the sample catcher of the Hayabusa spacecraft
© Naraoka et al.; licensee Springer. 2015
Received: 30 April 2014
Accepted: 20 February 2015
Published: 10 May 2015
Three carbonaceous category 3 particles (RA-QD02-0180, RB-QD04-0037-01, and RB-QD04-0047-02) returned in the sample catcher from the Hayabusa spacecraft were analyzed by time of flight-secondary ion mass spectrometry (ToF-SIMS) to establish an analytical procedure for determination of their origins. By the different analytical schemes, the three particles gave distinct elemental and molecular ions, in which the organic carbons commonly appear to be associated with nitrogen, silicon, and/or fluorine. The particles could be debris of silicon rubber and fluorinated compounds and are therefore man-made artifacts rather than natural organic matter.
KeywordsHayabusa spacecraft Category 3 particle Carbonaceous material ToF-SIMS analysis
The Hayabusa spacecraft successfully collected surface particles of asteroid Itokawa. The first analysis of the particles by the Hayabusa sample preliminary examination team (HASPET) has revealed a direct link between asteroidal materials and meteorites (e.g., Nakamura et al. 2011; Yurimoto et al. 2011). The particles used for the first analyses were composed mainly of silicate minerals including olivine, pyroxene, and feldspar with minor amounts of sulfide and oxide, which were classified as categories 1 and 2 particles and were confirmed as regolith of Itokawa. As one of the initial analyses, the possible presence of organic matter was explored for categories 1 and 2 particles by Raman and FT-IR spectroscopy (Kitajima et al. 2011) and by amino acid analysis and time of flight-secondary ion mass spectrometry (ToF-SIMS) analysis of the solvent extracts. However, no indigenous carbonaceous materials or organic compounds were identified in these particles (Naraoka et al. 2012). Even though investigations of categories 1 and 2 particles have been made over the world, there is no report of carbonaceous materials.
Category 3 particles are defined as having predominantly carbon signatures based on their chemical composition using field emission scanning electron microscope (FE-SEM) with energy dispersion spectrometer (EDS) at Extraterrestrial Sample Curation Center (ESCuC) in JAXA. In contrast to the category 4 particles defined as man-made artifacts (aluminum flakes, quartz glass, and stainless steel) from the sample catcher or micromanipulator, the origins of category 3 particles are not clear. Currently, 58 particles have been classified into category 3 from the 459 particles categorized at ESCuC/JAXA (Uesugi et al. 2014). Apart from the dominant carbon (C), the category 3 particles often show small nitrogen (N) and oxygen (O) peaks with trace amounts of fluorine and sulfur peaks by SEM/EDS.
Time of flight-secondary ion mass spectrometry (ToF-SIMS) has been applied to chemical analysis of solid surfaces with a high spatial resolution (approximately submicrometer) using primary ion beams of gallium (Ga), gold (Au), bismuth (Bi) as well as C60, Au3, or Bi3 clusters for primary ionization (e.g., Mahoney 2009). Both positive and negative secondary ions of metals and organic fragments from the sample surface can be analyzed by ToF-SIMS with a mass resolution of approximately 10,000 (m/Δm at m/z approximately 400). In this study, three category 3 particles were analyzed by ToF-SIMS using Au+ ion beams to establish a method in the analytical sequence of Itokawa grains and to clarify the chemical composition related to their origins.
The category 3 particles are generally ca. 20 to 100 μm in size (major axis) with blocky or fibrous shape. The blocky samples sometimes show irregular features including a horn-like texture possibly produced by tearing. They often contain distinct small grains of silicate, stainless steel, and aluminum on their surfaces by the SEM/EDS analyses (Uesugi et al. 2014). SEM analyses have been performed at lower electron energy (approximately 10 keV) under approximately 60 Pa N2 atmosphere using a dry (i.e., oil-free) pumping system to avoid the damage and contamination of particle samples (Yada et al. 2014). After the SEM observation, each particle was fixed onto a gold (Au) or indium (In) plate (0.3 mm in thickness) by pressing with 5-mm-thick sapphire glass under N2 atmosphere at ESCuC (Uesugi et al. 2014). Three category 3 particles (RB-QD04-0047-02, RB-QD04-0037-01, and RA-QD02-0180) were allocated for ToF-SIMS analysis. These were the typical particles of the blocky-shaped samples, which were classified as type I (38 of a total of 52 category 3 particles; Uesugi et al. 2014). The samples are described in the following paragraphs in their analytical order.
RB-QD04-0047-02 is a blocky particle (approximately 28 μm in size) composed of only C and O. This particle is apparently very hard with no deformation noticeable during the sample processing, whereas other particles were deformed or crushed during the handling (Uesugi et al. 2014). The particle was pressed onto a Au plate. After the FT-IR measurement at ESCuC/JAXA, NanoSIMS analysis was performed at Kochi Institute for Core Sample Research of JAMSTEC to measure stable isotope ratios of hydrogen (δD), carbon (δ13C), and nitrogen (δ15N) in order to discriminate the particle origins: extraterrestrial material vs. terrestrial contamination (Ito et al. 2014). The sample was rastered with the focused Cs+ beam after coating of the surface with Au (10 to 20 nm) for mitigation of electrical charging. The detailed procedure of NanoSIMS analysis was given elsewhere (Ito et al. 2014).
RB-QD04-0037-01 is a blocky particle (approximately 48 μm) showing major C, N, and O peaks by SEM/EDS with tiny olivine grains (approximately 3 μm) on the surface of the particle. The particle was crushed into two fragments during mounting onto the In plate. Only one fragment was subjected to ToF-SIMS analysis prior to NanoSIMS analysis to prevent damaging the sample surface. Even though both RB-QD04-0047-02 and RB-QD04-0037-01 samples were preserved in a N2-purged container during transportation, the sample loading to ToF-SIMS needed about 30 min of exposure to normal atmospheric conditions.
RA-QD02-0180 is also a blocky particle (approximately 55 μm) characterized by K, Na, and Cl peaks in addition to C, N, and O by SEM/EDS. The elemental signature suggested the existence of salts, which may be deliquescent under atmospheric conditions. Therefore, this sample was handled with a special care under a N2 atmosphere for transportation and loading for the ToF-SIMS analysis. The O2- and H2O-free analytical system called the cryo-ToF-SIMS/SEM system has been reported elsewhere (Kuroda et al. 2013; Masumi et al. 2014).
The ToF-SIMS measurement was performed using a TRIFT III spectrometer (ULVAC-PHI, Inc., Chigasaki, Kanagawa, Japan) at Nagoya University. Positive and negative ion spectra were obtained using a 22-keV Au+ gold primary ion at a current of 1.2 nA, with a pulse width of 1.4 ns (bunched for spectral analysis, spectrum mode) or 8.0 ns (not bunched for image analysis, image mode). The angle between the primary Au+ ion beam and the sample surface was 40°. The measured surface areas were 30 × 30 to 80 × 80 μm, and approximately 2 million total ion counts were obtained in acquisition time of about 5 min. A low-energy pulsed electron ion gun (28.0 eV) was used for surface charge compensation.
Results and discussion
Alteration and contamination during sample preparation
To characterize and categorize the Hayabusa particles for allocation, every particle has been analyzed initially by the SEM/EDS at ESCuC (Yada et al. 2014; Uesugi et al. 2014). It has been known that the surface of the organic materials is damaged by electron beams and that amorphous carbon films build up where the electron beams impinge by way of various carbon contaminants including oils, gasket materials, and other residual gases in the common SEM system (e.g., Knox 1976; Bret et al. 2005). To minimize the damage and organic contamination, the SEM analysis of ESCuC was performed at lower electron energy (10 keV) under approximately 60 Pa N2 atmosphere using the dry (i.e., oil-free) pumping system. Because the surface of organic polymers can be damaged by electron energies as low as a few tens of electron volts (Gilmore and Seath 2002), the organic surface could be altered and contaminated by the SEM analyses as well as during the sample preparation. Nevertheless, the distinctive ion distributions have been observed for each particle as follows:
In contrast, the positive ion became stronger in m/z 132.88 (Cs+) after pre-sputtering, in which more than 90% of the total ions were due to Cs+. Except for slight increases of m/z 12.00 (C+) and 26.98 (Si+) that were observed using ROI (Additional file 1: Figure S1A), there is no difference in the ion signal between the particle and the blank. The identification of Si+ (observed at m/z 27.977 for a true mass of 27.9764) was correctly made to discriminate from CO+ (m/z 27.995 for 27.9944) and C2H4 + (m/z 28.031 for 28.0308) as shown in Additional file 1: Figure S1C.
Various analytical methods are preferred to characterize the properties of category 3 particles (Uesugi et al. 2014). An initial analysis of the Hayabusa particles has been carried out by SEM/EDS on a copper (Cu) holder under low pressure of N2, where the particle can be handled by micromanipulation. In contrast, ToF-SIMS and NanoSIMS analyses of the microparticles require fixing of particle on the metal (e.g., Au or In) or the use of an organic adhesive. Although the organic adhesive was not used, to avoid organic contamination in the present study, the Au or In plate gave a strong background of m/z 197 and 115, respectively, resulting in weak emission of other ions from the particle. The reconstruction of mass spectra using ROI is effective in discriminating the ion peaks of the particle relative to those of the background. In addition, several ions assigned as organic fragments were emitted from the metal (Figure 1). The pre-sputtering by Au+ beam could be effective in removing contamination from the sample surface. Furthermore, it is recommended that the ToF-SIMS analysis will be performed prior to the SEM analysis, because the organic surface is damaged by electron beams during the SEM analysis.
The NanoSIMS analysis prior to ToF-SIMS analysis had a great influence on ion distributions shown by ToF-SIMS, because the Cs ion was too strong to observe indigenous positive ions from the sample. Even if the pre-sputtering was performed prior to analysis, the intensity of Cs+ got stronger resulting in no effective measurement of positive secondary ions. ToF-SIMS analysis is highly recommended before NanoSIMS analysis, even though stable isotopic ratios of C, N, and H may have been slightly enriched in heavy isotopes after the ToF-SIMS analysis (Ito et al. 2014). The δ13C, δ15N, and δD values of RB-QD04-0047-02 before the ToF-SIMS analysis were +3% (±3) (relative to PDB), −4% (±2) (relative to Air), and +103% (relative to SMOW), respectively, whereas those after the ToF-SIMS analysis were +14% (±6), +6% (±2), and +177%, respectively (Ito et al. 2014).
Furthermore, because a primary beam sputters the surface of sample during SIMS analysis, IR spectroscopic measurements should be performed before ToF-SIMS analysis. Some absorption lines of IR spectra were lost after the SIMS analyses (Uesugi et al. 2014).
Characteristics of category 3 particles by ToF-SIMS for their origins
Carbon was detected in all samples of this study by SEM/EDS, and the ToF-SIMS analysis also confirmed carbon distribution in all samples. Based on carbon distribution, each particle is a homogenous organic material except for small olivine grains of RB-QD04-0037-01 and NaCl of RA-QD02-0180 on the surface. Nitrogen was commonly associated with C, and the distributions of fluorine and silicon are similar to those of C in RB-QD04-0047-02 and RB-QD04-0037-01, respectively. On the other hand, extraterrestrial organic materials including insoluble organic matter (IOM) of meteorites are highly heterogeneous in elemental and isotope distributions (e.g., Busemann et al. 2006; Zega et al. 2010; Ito et al. 2014). Even though the cell materials in terrestrial biological samples also show chemical heterogeneities (e.g., membrane, nucleus, organelle, etc.), artificial organic polymers have usually homogeneous chemical compositions on a micrometer scale. In this study, however, chemical and isotopic heterogeneities have not been observed in any particle. In addition, it is important to note that the Si- and F-bearing organic matter usually has not been found in natural environments except for man-made chemicals. The three particles of this study are probably artifacts in origin, even though each has different histories such as cosmic-ray exposure duration, chemical alteration, and mechanical deformation. The man-made chemical origin of the particles is also consistent with the stable isotopic compositions of C, H, and N for terrestrial materials (Ito et al. 2014).
The specific source(s) of the original chemicals is (are) uncertain in the present study. A possible source is the outer cover of the sampler horn of the Hayabusa spacecraft, which was made of polyarylate (Vectran®; Kuraray Co. Ltd., Chiyoda, Tokyo, Japan), although polyarylate usually does not contain Si and F. Silicon rubber is used as the seal materials of clean rooms, and fluoro-rubber (Viton®; DuPont, Wilmington, DE, USA) is used for the gloves of the clean chambers at ESCuC (Uesugi et al. 2014). However, they usually do not contain N. Alteration of the particle surface by the SEM analysis also may be significant. Further investigations are needed to identify the specific source(s).
Three carbonaceous category 3 particles (RA-QD02-0180, RB-QD04-0037-01, and RB-QD04-0047-02) collected from the sample catcher of the Hayabusa spacecraft were analyzed by ToF-SIMS. Multiple analytical techniques can be carried out on the same sample, in which case it is preferable that the ToF-SIMS analysis should be performed before the NanoSIMS analysis to avoid severe contamination from the NanoSIMS primary Cs ion beam. It is also recommended that the ToF-SIMS analysis be carried out before the SEM/EDS analysis to avoid damage and contamination of the surface by electron beam interactions. The pre-sputtering of the sample surface by the primary Au+ ion beam of ToF-SIMS may be effective in removing contamination from the sample surface. Although the three particles showed distinct elemental and molecular ion distributions, the homogenous organic carbon distribution appears to be associated with nitrogen, silicon, and fluorine, which are different to the elemental distributions of C-rich extraterrestrial materials. The particles could be debris of silicon or fluorinated organic compounds and as such are man-made artifacts rather than natural organic matter.
We are grateful to two anonymous reviewers and the handling editor, Prof. Trevor Ireland of Australian National University, for critical and constructive comments, which helped to revise an earlier version of this manuscript.
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