All references and citations used throughout the present document, see e.g. references in square brackets and last paragraph of the specification, are incorporated herein by reference in their entirety.
The present disclosure is related to spectrometers, and more particularly to high resolution and highly integrated mid-wave and long-wave infrared point spectrometers for spacecrafts.
Successful implementation of small spacecraft missions, singly or in fleets, to accomplish high priority planetary exploration requires small, highly capable, and readily-replicable science instruments.
Imaging and point spectrometers are known from the Dawn [1], Hayabusa2 [2], and OSIRIS-REx [3] missions to asteroids. However, separate instruments are used to assess the reflected and emitted light ranges, and these large instruments are not compatible with the emerging classes of small satellites and small landers. A small neutron spectrometer (e.g., Mini-NS in LunaH-Map [4], developed for the Moon) can quantify H abundance coarsely for a slow asteroid flyby, but precise estimates require weeks to months of integration with inherently low spatial resolution, making volatile heterogeneity assessment for small asteroids difficult to impossible. For multiple flybys on a compact platform, a point spectrometer with integrated wavelength range coverage is both feasible and scientifically compelling.
Looking more broadly, similar questions of high priority turn up in the science and exploration of planetary surfaces across the solar system from asteroids to terrestrial bodies to icy worlds. With the number of small satellite (e.g., SIMPLEx [5]) and small lander (e.g., CLPS [6], PRISM [7]) opportunities on the rise, the need for an instrument with compact design and science performance has increased.
The inventors have conceived the mid-wave and long-wave infrared point spectrometer (MLPS) according to the present disclosure when seeking an instrument for a multi-spacecraft near-earth asteroid (NEA) Cubesat® mission concept to provide quantitative answers to three specific questions relevant to how small bodies (NEAs, asteroids, Martian moons, comets, etc.) formed and can act as tracers for the dynamical evolution of the solar system: (1) What is the quantity of water in each object? (2) In what phase(s) is the water incorporated (i.e. ice vs. hydrated silicate minerals)? and (3) Are organics or other volatiles present, and if so, what types and in what form?
The disclosed methods, systems and devices address and provide practical solutions to the above-mentioned problems and needs.
The disclosed methods and systems can be used to determine the form, abundance, distribution, and time variation of volatiles. The described MLPS' wavelength range, spectral resolution, and signal-to-noise ratio (SNR) in, for example, the 2-4 μm range may be optimized to discriminate the form and quantity of water at the surface, OH, adsorbed H2O, or H2O ice, via measurement of the OH/H2O stretch vibration at, for example ˜3 μm. Moreover, with sufficient integration time on a sunlit surface, the disclosed MLPS may also be used to sense the H2O bend at, for example, ˜6 μm in its 5.5-12 μm channel.
Additional volatiles like C—H in aliphatic organics, NH4+ in minerals, and NH3, CO2, and CH4 ices also have diagnostic absorptions in the disclosed MLPS' 2-4 μm spectral range. The mentioned dual wavelength range may also be used to measure volatile content and temperature simultaneously for surfaces providing both accurate quantification by correction of thermal emission addition to the 3 μm feature as well as understanding temperature controls on volatile distribution. Applications include mapping the heterogeneity of water-rich asteroids (Takir & Emery, 2012) [8], quantification of water on airless bodies like the Moon (e.g. Pieters et al., 2009) [9], and investigation of ice-organic mixtures in bodies of the outer solar system (see, for example, Materese, Astrophys. J. 2015) [10].
Embodiments in accordance with the teachings of the present disclosure may be used to determine the composition of rocks and soils and study the stratigraphy and the evolution of the planetary surfaces. The disclosed MLPS long-wave infrared wavelength range can be used to capture the Si—O feature (8-12 μm) related to silicate polymerization and can thus resolve the presence of key minerals, identify discrete silicate lithologies, and distinguish amorphous versus crystalline materials. These characteristics enable quantitative modeling of surface composition, tracing the history of interior, volcanic, and impact processes affecting a planetary surface. Examples include mapping the degree of silicate alteration in asteroids (e.g. McAdam et al., 2015, Icarus) [11], compositional discrimination of igneous units on the Moon, see e.g. Paige et al., 2010 [12], and mapping stratigraphic variation on Mars, see Rogers et al., 2018 [13].
The teachings of the present disclosure may further be exploited to determine the thermophysical and geotechnical planetary surface properties. Multiple time-of-day measurements in the mid-wave and long-wave spectral ranges can provide detailed measurements of diurnal temperature range to determine surface thermal inertia, effected by rock abundance, particle size, and porosity. Long-wave infrared data in the transparency feature region (5.5-8 μm) also allow independent estimation of grain size.
In addition to their relevance for planetary science, the mentioned capabilities offered by the teachings of the present disclosure also provide information relevant to exploration and planetary defense. The described MLPS enables assessment of the quantity and extractability of resources from water-rich targets for In Situ Resource Utilization (ISRU) as well as generates geotechnical data for interaction with planetary surfaces and for studies of asteroid properties.
Further aspects of the disclosure are provided in the description, drawings and claims of the present application.
According to a first aspect of the present disclosure, a spectrometer is disclosed, comprising: an optical assembly including a telescope, a grating and a relay system; and a focal plane module including a first detector and a second detector, wherein: i) the optical assembly is configured to: receive light from an object or scene through the telescope, thereby focusing the light, and split focused light by the relay system into a first beam within a first spectral range and a second beam within a second spectral range different from the first spectral range, and ii) the focal plane module is configured to: receive the first beam by the first detector to generate a first output signal in correspondence with a spectral content of the first beam, and receive the second beam by the second detector to generate a second output signal in correspondence with a spectral content of the second beam.
According to a second aspect of the present disclosure, a method of spectrometry is provided, comprising: receiving light from an object or a scene; focusing the light; splitting the light into a first beam within a first spectral range and a second beam within a second spectral range; focusing the first beam on a first detector and the second beam on a second detector; generating by the first detector a first output signal in correspondence with a spectral content of the first beam; and generating by the second detector a second output signal in correspondence with a spectral content of the second beam
Light received through system panel (151) is guided to optical assembly (110) using the calibration mirror (181) in (180). As will be described more in detail, the received light is split up in optical assembly (110) and refocused to form two spectra passing through the focal plane module (120) including a first detector (130) and second detector (140).
With continued reference to
With further reference to
With continued reference to
With reference again to
Referring back to
With further reference to
Referring back to
Making reference to
In view of what described throughout the disclosure, the person skilled in the art will appreciate that the disclosed methods and devices leverage, customize and extend three different technologies, i.e. bi-faceted gratings [14], barrier infrared detectors BIRDs [15,16], and thermopile detectors to make it possible to measure the medium-wave infrared (e.g. λ=2 μm to 4 μm) and the long-wave infrared (e.g. λ=5.5 μm to 12 μm) simultaneously in a payload that fits in a, for example, 2 U volume. The disclosed concept can be used to design flight spectrometers that will cover the broad solar reflectance plus thermal emission spectral range with a compact and low-cost instrument suitable for small spacecraft reconnaissance of asteroids, the Moon, and planetary satellites as well as mass-constrained landed missions.
Medium-Wave Infrared Performance
The radiant power, or radiant flux, measured in watts (W), reaching BIRD is expressed as follows
Φ=τatmτZnSeηoηgLsAiΩfsd/n2 (1)
where
τatm—the atmosphere transmission,
TZnSe—the transmission of the ZnSe window,
ηo—the efficiency of all the reflective optics, the splitting efficiency of the grating considered,
ηg=the efficiency grating
Ls—the radiance of the blackbody as the source,
Ai—the image area on the detector,
Ωfsd—the projected solid angle field stop subtends at the detector,
n—the refractive index of air.
All the items in Eq. (1) and the following equations except geometrical ones are spectral dependent. The labels for spectral subscript are omit for simplicity. The spectral radiance Ls is defined by Planck's equation
where c is the speed of light in vacuum, kB the Boltzmann constant, h the Planck constant. The projected solid angle Ωfsd is calculated using the following equation,
The image area on the detector Ai is determined by As/m2, where As and m are the source area and magnification, respectively. The source area is defined by the pinhole size located in front of the blackbody. The number of photons reaching BIRD can be calculated based on the power in Eq. (1) as follows
where tint is the integration time, and hc/λ the photon energy. Then the signal output from BIRD due to N photons in term of electron number is
S=QN (5)
where Q is quantum efficiency. The noise in term of electron number is show as
ntot=√{square root over ((nread)2+(ndark)2+(ndigit)2+(nphoton)2)} (6)
where nread is read noise, ndark dark current noise, ndigit digitization noise, and nphoton=√{square root over (QN)} is the noise in photo-generated signal, or photon short-noise.
By combing Eqs. (5) and (6), we get the SNR as
The noise-equivalent delta temperature (NEDT), the change in temperature that yields a SNR ratio of unity, is
Long-Wave Infrared Performance
Equations (1)-(3) above also applies in this case. In order to obtain thermopile specific response, equations (1)-(3) in [18] may be applied.
The methods and systems described in the present disclosure may be implemented in hardware, software, firmware or any combination thereof. Features described as blocks, modules or components may be implemented together (e.g., in a logic device such as an integrated logic device) or separately (e.g., as separate connected logic devices). The software portion of the methods of the present disclosure may comprise a computer-readable medium which comprises instructions that, when executed, perform, at least in part, the described methods. The computer readable medium may comprise, for example, a random access memory (RAM) and/or a read-only memory (ROM). The instructions may be executed by a processor (e.g., a digital signal processor (DSP), an application specific integrated circuit (ASIC), a field programmable logic array (FPGA), a graphic processing unit (GPU) or a general purpose GPU).
A number of embodiments of the disclosure have been described. Nevertheless, it will be understood that various modifications may be made without departing from the spirit and scope of the present disclosure. Accordingly, other embodiments are within the scope of the following claims.
The examples set forth above are provided to those of ordinary skill in the art as a complete disclosure and description of how to make and use the embodiments of the disclosure, and are not intended to limit the scope of what the inventor/inventors regard as their disclosure.
Modifications of the above-described modes for carrying out the methods and systems herein disclosed that are obvious to persons of skill in the art are intended to be within the scope of the following claims. All patents and publications mentioned in the specification are indicative of the levels of skill of those skilled in the art to which the disclosure pertains. All references cited in this disclosure are incorporated by reference to the same extent as if each reference had been incorporated by reference in its entirety individually.
It is to be understood that the disclosure is not limited to particular methods or systems, which can, of course, vary. It is also to be understood that the terminology used herein is for the purpose of describing particular embodiments only, and is not intended to be limiting. As used in this specification and the appended claims, the singular forms “a,” “an,” and “the” include plural referents unless the content clearly dictates otherwise. The term “plurality” includes two or more referents unless the content clearly dictates otherwise. Unless defined otherwise, all technical and scientific terms used herein have the same meaning as commonly understood by one of ordinary skill in the art to which the disclosure pertains.
The references in the present application, shown in the reference list below, are incorporated herein by reference in their entirety.
The present application claims priority to U.S. Prov. App. No. 62/929,628 filed on Nov. 1, 2019 incorporated herein by reference in its entirety.
This invention was made with government support under Grant No. 80NM0018D004 awarded by NASA (JPL). The government has certain rights in the invention.
Number | Name | Date | Kind |
---|---|---|---|
3748015 | Offner | Jul 1973 | A |
5276321 | Chang | Jan 1994 | A |
5371358 | Chang | Dec 1994 | A |
6100974 | Reininger | Aug 2000 | A |
6222187 | Shivanandan | Apr 2001 | B1 |
6480333 | Maker et al. | Nov 2002 | B1 |
20030057374 | Schuebel | Mar 2003 | A1 |
20050248758 | Carron | Nov 2005 | A1 |
20100072514 | Ting | Mar 2010 | A1 |
20100321688 | Bodkin | Dec 2010 | A1 |
20130228887 | Wehner | Sep 2013 | A1 |
20130250301 | Feitisch | Sep 2013 | A1 |
20150137295 | Wehner | May 2015 | A1 |
20200049554 | Farsad | Feb 2020 | A1 |
20200096388 | Pagano | Mar 2020 | A1 |
20200249091 | Scherer | Aug 2020 | A1 |
20220099489 | Weidmann | Mar 2022 | A1 |
Entry |
---|
A. D. Rogers, et al., “Areally Extensive Surface Bedrock Exposures on Mars: Many Are Clastic Rocks, Not Lavas,” Geophys. Res. Lett. 45(4), 1767-1777 (2018). 12 Pages. |
A. Soibel, et al., “Mid-wavelength infrared InAsSb/InSbnBn detectorwith extended cut-off wavelength,” Appl. Phys. Lett. 109(10), 103505 (2016). 6 pages. |
C. K. Materese, et al., “Ice chemistry on outer solar system bodies: electron radiolysis of N2-, CH4-, and CO-containing ices,” Astrophys.J. 812(2), 150 (Oct. 20, 2015). 10 Pages. |
C. M. Pieters, et al., “Character and spatial distributionofOH/H2O on thesurface ofthe Moon seen by M3 on Chandrayaan-1,” Science326 (5952), 568-572 (2009). 7 Pages. |
D. Daou, “Small innovativemissionsforplanetaryexploration,”in European Planetary Science Congress 2017 (Abstract#EPSC2017-146, 2017). 2 Pages. |
D. L. Johnson, et al., “The RicorK508 cryocooleroperationalexperienceon Mars,” AIP Conf. Proc. 1573(1), 1792-1799 (2014). 10 Pages. |
D. Takir and J.P. Emery, “Outer Main Belt asteroids: Identification and distribution offour 3-μm spectral groups,” Icarus219(2), 641-654 (2012). 15 Pages. |
D. Z.-Y. Ting, et al., “A high-performance Io ng wavelength superlattice complementary barrier infrared detector,” Appl. Phys.Lett. 95(2), 023508 (Apr. 8, 2009). 5 Pages. |
D. Z.-Y. Ting, et al., “Exclusion, extraction, and junction placement effects in the complementary barrier infrared detector,” Appl. Phys. Lett. 102(12), 121109 (Jan. 28, 2013). 6 Pages. |
E. B. Johnson, et al., “Developmentofthe LunaH-Map miniature neutron spectrometer,” Proc SPIE 10392, 103920H (2017). 12 pages. |
G. Mariani and M. Kenyon, “Room-temperature remote sensing: Far-infrared imaging based on thermopiletechnology,” in 2015 40thInternational Conference on Infrared, Millimeter, and Terahertz Waves(IRMMW-THz) (2015), pp. 1-2. 3 Pages. |
M. C. De Sanctis, et al., “The VIR Spectrometer,” SpaceSci. Rev. 163(1), 329-369 (2011). 42 Pages. |
M. C. Foote and E.W. Jones, “High-performance micromachined thermopile linear arrays,” Proc. SPIE3379, 192-197 (Jul. 22, 1998). 8 Pages. |
M. C. Foote, et al., “Thermopile detector arrays forspace science applications,” in International Workshop onThermal Detectors forSpace Based Planetary, Solar, and Earth Science Applications (TDW, 2003), 6 pages. |
M. C. Foote, et al., “Uncooled thermopile infrareddetectorlinear arrays with detectivity greater than 10/sup 9/cmHz/sup 1/2//W,” in IEEE transactions on Electron Devices (IEEE, Sep. 1998), 45, pp. 1896-1902. 8 Pages. |
M. M. McAdam, et al., “Aqueous alteration on asteroids: Linking the mineralogy and spectroscopyofCM and CI chondrites,” Icarus 245, 320- 332 (2015). 14 Pages. |
P. Maker, et al., “New Convex Grating Types Manufactured by electron Beam Lithography,” in Diffractive Optics and Micro-Optics 10, OSATechnical Digest Series (1998), pp. 234-236. 5 pages. |
P. Mouroulis, etal, “Con vex grating types for concentric imaging spectrometers,” Appl. Opt. 37(31), 7200-7208 (1998). 10 Pages. |
P. Mouroulis et al., “Optical design of a coastal ocean imaging spectrometer,” Opt. Express16(12), 9087 (2008). 11 pages. |
P. R. Christensen, et al., “The OSIRIS-REx Thermal Emission Spectrometer (OTES) Instrument,” SpaceSci. Rev.214(5), 87 (2018). 40 Pages. |
P. Voosen,“NASA to pay privatespace companies formoon rides,” Science 362(6417),875-876 (2018). 4 Pages. |
T. D. Glotch, et al., “Highly Silicic Compositions on the moon,” Science329(5998), 1510-1513(2010). 6 Pages. |
T. Okada, et al., “Thermal Infrared Imaging Experiments of C-Type Asteroid 162173 Ryugu on Hayabusa2,” Space Sci. Rev. 208(1),255-286 (2017), 33 pages. |
W. Wilson, et al., “Recentadvances in blazed grating fabrication by electron-beam lithography,” Proc. SPIE 5173, 51730E (2003) 14 pages. |
Number | Date | Country | |
---|---|---|---|
20210131872 A1 | May 2021 | US |
Number | Date | Country | |
---|---|---|---|
62929628 | Nov 2019 | US |