- Research article
- Open Access
Design of a Mars atmosphere simulation chamber and testing a Raman Laser Spectrometer (RLS) under conditions pertinent to Mars rover missions
© Motamedi et al. 2015
- Received: 30 January 2015
- Accepted: 28 August 2015
- Published: 22 September 2015
Raman spectrometry is a powerful technique for the rapid identification of most minerals and organic chemicals without sample preparation. In this context, the European Space Agency (ESA) and NASA selected a Raman spectrometer in the payload of the future ExoMars and Mars 2020 missions to identify organic compounds and mineral products indicative of biological activity on Mars. Little is known, however, about the effects of Mars atmospheric conditions on instrument performance and on the Raman spectra. The objective of this study was to i) design and construct a versatile simulation chamber to reproduce the atmospheric conditions expected inside a rover on Mars, ii) to test the performance of a previously designed breadboard miniaturized Raman laser spectrometer (RLS) inside the chamber. The Mars Atmosphere Simulation Chamber (MASC) is a temperature and atmosphere controlled chamber. It includes an innovative heating-cooling system to create homogeneous temperatures inside the chamber that can be varied between 243 K and 283 K, while the charged coupled device (CCD) of the Raman spectrometer can be independently cooled (e.g., 233 K). A vacuum and gas control system permits evacuation of the chamber and the subsequent introduction of any (dried) gas mixture at partial pressures between 1 mbar and several bars. The minimum CCD temperature was found to depend on the surrounding MASC temperature and atmosphere. A vertical shift of 3 pixels on the CCD was observed for the Raman signals upon lowering the temperature from 283 to 253 K. We show that the RLS instrument gives reliable Raman spectra over the tested range of temperatures and from a vacuum of 4 x 10−5 mbar to a CO2 atmosphere at pressure relevant to Mars (8 mbar). For example, the Raman spectra of three test minerals, calcite, aragonite and baryte, showed identifiable Raman peaks with Raman shift values within ± 1 cm−1 of those reported in previous works under terrestrial conditions. This confirms that a RLS instrument is useful for the identification of minerals during future missions to Mars; once a necessary detector recalibration was carried out, the system performed well under 8 mbar pressure and 243 – 283 K. The MASC was found to be a versatile instrument; it can provide important information on instrument performance under Martian conditions and other temperatures and atmospheric conditions can also be simulated.
- Mars simulation chamber
- Cooling-vacuum system
- Martian atmosphere
- Raman laser spectrometer
Fundamental questions remain about the geological history of the planet Mars [1–3]. One key question is whether free water has been persistent on the Mars surface to support life. The presence of unaltered recent volcanic rocks and minerals (e.g., olivine) suggests that the surface is currently dry [4, 5]. Previous studies, however, have shown that the planet experienced major climate changes and that the earlier conditions were warmer and wetter . For example, the weathering and erosion products are evidence of the presence of water in the early geological history of Mars, during the Noachian era [5–7]. The geographic extent of minerals such as hydrated, evaporite or sedimentary minerals (e.g., hydrated sulphates, carbonates, phyllosilicates) is still being determined and how long this wet period lasted is still matter of debate [6–8]. Therefore, planetary scientists are interested in the accurate in situ determination of the surface mineralogy and mineral composition on Mars by advanced techniques and instruments on board Mars landers and rovers [9–14]. The instruments are usually miniaturized versions of those routinely used on Earth. Little is known, however, about the effects of different atmospheric conditions on the performance of such instruments and on the response of the minerals to be analysed.
Kolesov and Geiger reported that the temperature may affect the structure of minerals and the Raman peak shape and intensity . In the case of techniques that use plasmas, such as Laser-induced breakdown spectroscopy (LIBS), the characteristics of the plasma and its expansion depends on the ambient pressure  and thermal distortions of the components of the instrument itself can affect its calibration or performance. Thus it is essential to simulate conditions similar to those expected during the space missions, in order to predict and take into account the accuracy and precision of instrumental data, or if necessary adapt the design.
Worldwide there are several atmospheric simulation chambers that are capable of reproducing Martian conditions to some extent [17–19]. In the context of testing instrument, however, many are too small and do not allow housing an instrument and samples simultaneously. The instrument and the samples to be analysed are usually separated physically by viewports/windows and the experiments are not performed under fully realistic conditions. Therefore, we designed and built a versatile Mars Atmosphere Simulation Chamber (MASC) with a large volume to house both the instruments and the samples, and to simulate the conditions inside a rover during the next space missions to Mars.
In this paper, we first describe the design of the new MASC chamber and the protocol for experiments under the conditions expected inside the rover during the ExoMars mission. Finally, we test a prototype Raman Laser Spectrometer (RLS) instrument previously designed for the ExoMars mission by the Dutch Organization for Applied Research (TNO) on a set of three test minerals.
Design requirements and technical description of the Mars Atmosphere Simulation Chamber (MASC) and Raman Laser Spectrometer (RLS)
The MASC is a cylindrical stainless steel chamber, volume 0.261 m3 (100 cm length and a diameter of 57.6 cm), with doors at each end to ensure a high versatility. Previous work related to ExoMars Raman studies by Sobron and Wang  estimated that the rover operation temperature range would be between 243 K and 283 K during Raman measurements and we await final operating conditions to be released by ESA. The major requirement in the design of the chamber was to provide stable temperatures and pressures (6–10 mbar of pure CO2 atmosphere and a temperature range between 243 K and 283 K) that could be varied in line with experimental requirements. In addition, rapid changes in temperature would subject the optics of space instruments to thermal stresses. Therefore, it was required to control the rate of heating or cooling of different parts of the MASC. To fully assess the effect of low pressure on the instrument performance, it was desirable to design a chamber with the flexibility to produce stable pressures from a vacuum (~4 × 10−5 mbar) to a pressure of a 6–10 mbar of CO2 as expected on Mars. Moreover, the water content inside the MASC had to be kept low, for example on Mars the water content is ~ 0.03 % .
The chamber contains a variety of electrical/optical feed-throughs, viewports and vacuum measurement gauges, as well as other instruments. A sample holder was fitted with 3D stages so that different samples could be analysed without the need for opening the chamber in between sample analyses. As the majority of planetary instruments will include CCDs as detectors (e.g., for ExoMars Cameras, X-ray Diffraction (XRD), X-ray fluorescence (XRF) and Raman laser spectrometer (RLS instrument), the MASC was fitted with a separate cooling circuit for the CCD of the space instrument.
The MASC was insulated from the ambient laboratory conditions by a double wall, with an interstitial space of 60 mm. This enabled us to reach a 10−6 mbar vacuum over the full length of the chamber, after several cycles of pumping and outgassing at 393 K. In addition, the outer wall and the two main doors of the MASC were covered with a flexible 20 mm thick insulation layer of Thermoplastic elastomeric foam (TPE).
To cool/heat the main doors, a Lauda XT-150 cooling machine, with silicone oil as the cooling medium, was used. The main doors were produced from a single piece of steel such that the silicone oil cannot leak inside the chamber and contaminate the instruments. The Lauda was considered a simple, safe and reliable machine with an accuracy of ± 0.05 K. The power outputs of the Lauda at 293 and 233 K were 1.50 and 0.06 kW respectively, which was sufficient for the heating/cooling of the MASC when operated between 243 and 283 K.
The inside of the chamber, i.e. the cooling screen and mounting plates, upon which experiments were performed or instruments tested, needs to be temperature controlled. Due to their design structure and position inside the MASC there would be a risk that these parts could leak and contaminate the chamber interior. Therefore, we used a non-corrosive cooling medium in a secondary closed system in thermal contact through heat exchanges with the primary silicone cooling circuit. Freon (C2Cl3F3) was selected as a safe cooling medium (nontoxic and non-flammable) and was passed through cooling pipes in the mounting plates and the cooling screen in a liquid state (at ~ 6 bars at room temperature).
The cooling system was filled to 90 % of the volume to allow expansion of the Freon whenever the temperature was raised. Currently the temperature inside the chamber can be varied between 243 and 283 K, but the stainless steel structure of the chamber allows the temperature to be varied over a larger range of temperatures if required.
Protection of the electrical/ optical feed-through on the doors
Atmosphere control inside the MASC
Simulated Martian conditions were achieved by using an atmosphere gas control system. For simplicity, initial testing was conducted with 100 % CO2, which represents a reliable proxy for the Martian atmosphere. The chamber, however, has the flexibility to simulate different gas compositions and pressures. Also, by using copper O-rings and a larger turbo molecular pump, it will be possible to obtain a lower vacuum for testing instrument under lunar conditions.
Martian pressure conditions were simulated inside the MASC by first evacuating the chamber and then flushing with CO2. To maintain stable Martian conditions, the MASC needs to be leak tight. EPDM O-rings (ethylene-propylene-diene rubber, hydrogen peroxide cured) were chosen for the large entrance doors because of their resistance to low temperature (down to 233 K) in combination with their compatibility to clean applications in the pharmaceutical/food industry.
The fact that the Martian atmosphere only contains ~ 0.03 % water also had to be considered. The large surface area of the chamber’s wall, main doors and multiple electrical/optical feed-throughs could lead to extensive outgassing. The vacuum system comprises an oil free dry-compression diaphragm pump (Pfeiffer PKT01300) that was powered by a turbo molecular pump (Pieffer TMH 071P) to reach an initial vacuum of ~ 10−5 mbar. Even when the chamber contained a spectrometer, an optical head, samples and all optical fibres and electrical cables, the pump down time was rapid and H2O was quickly and effectively removed from the system without the need for an additional cold finger (the pressure dropped below 4 × 10−5 mbar in 2 hours). In addition, a parallel arrangement of Nafion tubes cleans the CO2 gas of water. This method of water removal uses a dry helium flow around the permeable Nafion tube to flush the water across the membrane wall . A particle filter of 0.5 mm mesh was mounted on the CO2 feeding line to prevent deposition of solid particles in the tank.
Cooling the CCD of the RLS
An additional cooling system was implemented to minimize thermal noise/ dark noise of the CCD in the RLS instrument. In our cooling design of the CCD, a Peltier cooler was mounted on the CCD and connected via a braided copper thermal strap (~25 mm wide and 5 mm thick) to a copper cooling block. Inside the MASC, this copper cooling block was mounted to a small flange in the chamber door. From the outside of the MASC, the copper cooling block was connected to an Etscheid water cooler with the cooling capacity of 750 kcal/h at 288 K. This cooler was located directly under the chamber to avoid unnecessary heat exchange.
Design of a sample holder with 3D linear stages
Efficient use of the chamber required that multiple samples could be analysed sequentially. Three linear positioning stages (manufactured by the Physik Instrumente Company, Germany) were combined to form a 3D linear stage. These three linear positioning stages can carry up to 20 kg, push/pull up to 50 N and have an accuracy of about ± 0.1 mm. A sample holder was mechanically connected to the upper linear stage. The sample tray was 83 mm in length and 35 mm wide and could hold ten samples. Samples were solid pieces of mineral mounted in epoxy (cylinders with diameters of 10 mm) and 3 mm apart to allow potential use of laser ablation techniques.
Design of the CCD detector
The RLS instrument used for this study was an elegant breadboard for the ExoMars mission, originally designed as a combined Raman and Laser Induced Breakdown Spectroscopy (LIBS) instrument . In order to decrease the weight and power usage of the payload aboard the ExoMars mission, the LIBS capability had in the meantime been removed from the flight mode instrument. Therefore, the effect of Mars atmospheric conditions on the LIBS performance of the instrument is not discussed in this article. The Raman modality uses a 659 nm laser with a maximum output of 20 mW. The RLS focal plane assembly incorporates a charge coupled device (CCD), a thermal/mechanical interface (cold finger) and proximity electronics. The proximity electronics include CCD bias voltage filters and a pre-amplifier circuit for amplifying the analogue video output signal produced by the on-chip amplifier. The thermal design of the spectrometer allows the CCD to be operated between −40 °C and room temperature, with the CCD thermally isolated from the rest of the spectrometer including the proximity electronics. The spectrometer was designed to project multiple grating orders at different heights of the CCD. This way the instrument could be used over a broad wavelength range (for LIBS) and still offer a high spectral resolution (for Raman and LIBS). The CCD was a back-illuminated e2v Technologies CCD42-40 with an imaging area comprising 2048 × 2048, 13.5 μm pixels. The device is Ultraviolet (UV)-enhanced, with a quantum efficiency of at least 50 % between 240 and 840 nm and imaging pixels with a full-well capacity in excess of 105 electrons. The device is a full-frame CCD but is usually operated in pseudo frame transfer mode in order to reduce smearing effects at short integration times (which can result in cross contamination of the spectral orders). The CCD is bonded to a ceramic Dual-In-Line (DIL) package but is flight representative with respect to its functional and thermal performance (including the mechanical interface to the rest of the spectrometer). The analogue video output from the focal plane assembly is digitised using a correlated double-sampling circuit and low-noise analogue-to-digital converter. A programmable digital signal processor (DSP) enables flexible detector operating modes, including synchronised CCD readout and laser emission.
Temperature control inside the MASC
A representative low temperature experiment under Martian conditions inside MASC consists of five stages: (1) loading the sample tray, (2) evacuating the MASC to remove all water (4 × 10−5 mbar), (3) pumping 8 mbar of CO2 into the MASC, (4) setting the Lauda cooling machine to a specific temperature (5) recording the temperature data.
The sensors on the left cooling plate front and the middle of the chamber were directly cooled by the Freon passing through the cooling pipe and cooling screen. Consequently, these sensors recorded the lowest temperature of ~ 244 and 248 K respectively. In contrast, due to the open structure of the 3D linear stages, there was relatively poor thermal conductivity between the cooling plate and the sample tray. Thermal straps were included in the design but better thermal conduction is needed to reduce the sample tray below ~ 250 K. The temperature on the left door only reached ~ 285 K, because local heaters maintain the electrical feed-throughs at 293 K. Therefore an aluminium cover was designed to insulate the inside of the MASC from thermal radiation of the doors.
Cooling of the CCD
Calibration testing of the CCD
Data acquisition used a single 40 s integration. With the 659 nm laser, the most relevant Raman scattering modes can be detected on the 3rd diffraction order between 660 and 840 nm. The spectral resolution was ~ 0.2 nm (~4 cm−1), i.e. doublet peaks separated by less than 4 cm−1 cannot be fully resolved. In an independent set of experiments, the same resolution of the spectrometer was determined under ambient conditions based on the peak width measured for the sharp line of a mercury calibration lamp: 0.2 nm FWHM [24–26]. The accuracy of Raman shift values, however, was ~ 0.4 cm−1. For Mars missions this accuracy would be sufficient to distinguish between minerals such as calcite and aragonite (a polymorph of calcite, both having the chemical composition CaCO3 but with a different molecular structure). These two minerals have lattice vibration modes (collective vibrations within the crystals) at ~ 283 and 274.5 cm−1 respectively, see below.
To assess the capability of the RLS instrument under Martian environmental conditions, we studied the Raman spectra of calcite, aragonite and baryte inside the MASC at different temperatures and pressures. The choice of those three minerals relates to ExoMars’ priority objective of searching for signs of water in the shallow subsurface. Indeed, calcite can form in sedimentary, igneous and metamorphic rocks. Aragonite is formed by biological and physical processes, including precipitation from marine and freshwater environments  and baryte can also be an indicator of hydrothermal circulation [28, 29].
Raman spectra of selected minerals were processed using the Origin program and Lorentzian peak fitting was used to provide a more accurate estimation of the height, position and width of the Raman peaks of the selected minerals for this study. To estimate the repeatability of this fitting routine, we acquired the Raman spectrum of a calcite sample ten times and then fitted the 1087 cm−1 peak for the ten individual spectra. The measurements show that this routine can fit the data and find that the value of a Raman peak shift varies within a standard deviation of 0.5 cm−1, which in the wavelength range in question corresponds to ~ 0.02 nm.
In Fig. 7b, the RLS Raman spectrum of calcite (obtained under vacuum condition at 283 K) is characterized by the most intense ν1 symmetric stretching of the CO3 group at 1087.5 cm−1, the ν4 symmetric bending mode at 713.4 cm−1, and one lattice vibration mode at 282.9 cm−1. These peaks are within ~ 1 cm−1 of the data reported in previous literature studies . The possible 2ν2 and ν3 peaks were not detected with the RLS instrument. These weak peaks appear to have been obscured within the background noise. The Raman spectra of calcite under vacuum condition at 253 K (see Fig. 7a) or at 8 mbar CO2 (see Fig. 7c) has peaks with Raman shift within ~ 0.5 cm−1 of those obtained under vacuum condition at 283 K, a scatter which is comparable to the standard error obtained for repeated measurements without changing the temperature and pressure conditions.
Similarly, Figs. 8, 9 also demonstrate that peak positions resolved in the Raman spectra of aragonite and baryte obtained under Martian conditions were within ~ 0.5 cm−1 of those obtained under vacuum condition at 283 K. These results again strongly suggests that there were no significant differences in the Raman spectra related to Martian conditions (low temperature or CO2 atmosphere). The aragonite spectrum shows: the very strong ν1 Raman peak at ~1086 cm−1, the ν4 vibration mode at ~704 cm−1 and a weak lattice vibration modes at 212 cm−1 . In the baryte spectrum, the most intense peak, the ν1 symmetric stretching vibration mode of SO4 tetrahedra, occurs at ~ 989 cm−1. The peak at 461 cm−1 is attributed to the ν2 bending vibration mode. The ν3 asymmetric stretching vibration and ν4 asymmetric bending vibration modes are observed at ~ 1144 cm−1 and 619 cm−1 . Also for these two minerals the spectra fully agree with reference spectra from the literature.
The recently developed MASC at VU University in Amsterdam reached most of its initial design goals as it is able to simulate Martian environmental conditions. The designed operational temperature range inside the MASC was 283 to 243 K and the pressure range was 8 to 10−5 mbar. The unique design of the MASC, having a large volume (0.261 m3) and a separate cooling circuit with a stable low temperature, allowed detailed in situ characterisation of the RLS instrument and samples under Martian conditions. The MASC is not restricted to simulate Martian conditions but can also be used for a whole range of other experiments where a controlled atmospheric composition and temperature is required.
The tested RLS spectrograph showed a vertical offset of about 3 pixels when lowering the temperature from 283 to 253 K. This was corrected for by adapting the read-out protocols, and this problem is not likely to occur in a more conventional Raman spectrometer in first order. Nevertheless, for any instrument to be employed in space it is crucial to check the repeatability and calibration under the expected environmental conditions. No significant horizontal shift on the CCD was observed when lowering the temperature.
The data indicated the accurate performance and calibration of the RLS instrument. Raman spectra obtained under Martian conditions (8 mbar CO2 pressure and 253 K) were indistinguishable from those obtained under vacuum conditions at a temperature of 253 K and also indistinguishable from those measured at 283 K. There was also no significant difference in peak positions of the Raman spectra of calcite, aragonite and baryte under Martian conditions in comparison with literature reference spectra recorded under Earth conditions.
This work was funded by the Netherlands Organization for Science Research (NWO) (No ALW-GO-PL/07-09 and ALW-GO-PL/14). The funding agency played no role in the data interpretation or the writing of the manuscript.
licensee Springer on behalf of EPJ. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited.
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