National Aeronautics and Space Administration + NASA Quest
+ Search Quest
 Find it at NASA
 Go
 Home mission About the Moon impact
 LCROSS - Lunar CRater Observation and Sensing Spacecraft
 Tech Info observation education news


TECHNICAL INFO
Lunar CRater Observation and Sensing Satellite (LCROSS)

INSTRUMENT SYSTEMS

The instrumentation selections and supporting observations provide multiple complementary measurement techniques and, thus, redundancy and robustness to the LCROSS mission. Moreover, multiple measurements and platforms maximize the science return.

The S-S/C payload comprises 9 instruments (Table 1): 5 cameras (1 visible, 2 Near IR, 2 Mid IR) and three spectrometers (1 visible, 2 NIR) and one photometer (Tables 2 & 3). Instrument checkout, impact rehearsal and calibration will be performed during the initial swing-by of the Moon. One hour prior to impact instruments will be powered on and will return data until impact of the S-S/C.

Table 1. LCROSS Measurements and Instruments
Measurement Platform Instrument Products
NIR Spectra λ/Δλ~100 S-S/C NIR Spectrometer (2) Ice, Vapor, Grain
Size, Hydrates
Visible Spectra S-S/C Visible Spectrometer H2O+ (619 nm)
OH (308nm)
Search organics
Thermal Evolution S-S/C Mid IR Camera (2) Pre-impact terrain
Total Water
Ejecta Blanket
Ejecta IR S-S/C NIR Camera (2) Total Water
Context Imagery S-S/C Visible Context Camera Impact location
Plume morphology
Impact Flash S-S/C Visible Photometer Flash light curve

Table 2. LCROSS Payload Instrument Parameters
Instrument Band Center/Range [um] Band Width/Resolution [nm] FOV [deg] Spatial Resolution @ T-15, T-1 min [km] Sample Frequency [Hz]*
VisCam 0.65 50 6 0.2, 0.01 0.5
NIRCamA TBD** TBD 6 0.4, 0.02 0.1
NIRCamB TBD** TBD 6 0.4, 0.02 0.1
MIRCamA 7 20 10 0.6, 0.04 0.1
MIRCamB 12 20 10 0.6, 0.04 0.1
VisSpec 0.27-0.65 9 6 TBD 1
NIRSpecA 1.3-2.4 9 6 TBD 1
NIRSpecB 1.3-2.4 9 6 TBD 1
TLP 0.4-0.8 600 6 TBD 1000
* Sampling frequencies per instrument will be optimized for signal-to-noise observations and to meet the bandwidth
requirements. ** The NIRCams will be used to monitor water absorption on/off the 1.4 micron feature.

Table 3. LCROSS Instrument Suite including Data Handling Unit.
Instrument (totals) Mass (kg)* Vol (cc)* Power (W)** Data Rate (kbps)**
VisCam 0.1 45.4 2.4 219
NIRCams 0.75 712.5 4.8 46
MIRCams 2.5 249.6 6.4 88
VisSpec 1.5 13.3 0.5 200
NIRSpecs 5.0 480.0 5 1.2
TLP <0.5 160 2 0.3
DHU 2.0 1100 6 N/A
Totals 12.4 2760.8 27.1 554.5
*Includes 20% contingency. ** During Nominal Operation Mode.

1. Visible and NIR cameras For the visible sensor, a high-end broadcast-quality CCD video camera outputting PAL format (752H x 582V pixels) will be employed (Figure 1). European-standard PAL camera pixels are more nearly square than pixels for NTSC cameras common in the U.S. and thus offer some advantages for metrological applications like those intended by LCROSS. The baseline near-IR sensors are flightheritage InGaAs sensors, operated at ambient temperatures, with a 12 bit RS-422 output.

2. Visible Spectrometer The LCROSS S-S/C will observe the pre- and post-Centaur-impacted lunar regolith in and outside the targeted crater at a spatial resolution and viewing angle unobtainable from Earth. The visible spectrometer, developed for the LCROSS project by Ocean Optics, shall record the sunlit plume evolution, and track the evolution of OH radicals from sunlight-dissociated water vapor molecules. The visible spectrometer will measure the OH-1 (308nm) and H2O+ (619nm) transitions simultaneous which shall assess the water vapor production.

NIR spectrometer
Figure 1. Fully integrated NIR spectrometer. Connection to telescope is via fiber optics.
3. Near IR Spectrometers The LCROSS S-S/C will monitor spectral bands associated with water vapor, ice, and hydrated minerals in the near infra-red (NIR) spectrum from 1.35 – 2.25 microns, covering the first overtones of the symmetric and asymmetric stretches of water; this band, relatively free from interferences, is more brightly illuminated by sunlight than the fundamentals near 3 microns, more than compensating the weaker absorption of the overtones. (Sunlight will illuminate the plume, 90 degrees to the direction of S-S/C travel, from 10 seconds after impact until the S-S/C itself impacts, ~10 min later.) The regions near 1.4 and 1.9 microns, normally obscured by terrestrial atmospheric background in spectra from icy surfaces, will provide a sensitive indication of water vapor from ice or hydrates. The remainder of the spectral band will reveal -- at a level of detail not available from Earth -- the nature of ice crystals and mineral hydrates.

Two identical NIR spectrometers will be coupled with fiber optics to telescopes, one focused along the impactor trajectory, the second aimed laterally through the plume towards the limb during the last ten seconds before S-S/C impact.

The NIR spectrometers utilize a no-moving-parts optical system from Polychromix. Measuring 8x6x4 cm3, consuming under 2 W, and weighing < 1 kg, each fully integrated spectrometer includes fiber optic input (NA = 0.22) and integral 2-stage TE detector cooling (ΔT > 55°C); an electronically tunable grating collects the 1.35 -2.25 micron spectrum (via Hadamard transform) each second using a singleelement InGaAs detector. Spectral resolution, specifiable in the 9 - 36 nm range, will be selected to maximize signal throughput while maintaining effective speciation. Developed for industrial process monitoring and control, this NIR spectrometer exemplifies leverage of rugged COTS instrumentation. (See Figure 1)

4. Mid IR Cameras Pre- and post- impact thermal images of the impact terrain will be obtained from Mid-IR cameras on the S-S/C to characterize the surface material (rock vs. regolith), obtain the thermal evolution of the plume (which is dependent on the water content), and observe the ejecta blanket and freshly exposed regolith. The baseline mid-IR sensors will be a flight-proven Alphasilicon uncooled micro-bolometer most sensitive in the 7-14 micron spectral range, outputting in PAL format (384H x 288V pixels).

5. Total Luminescent Photometer (TLP) A total visible luminance photometer will be used to observe a possible impact flash. The light flash is due to thermal heating and vaporization or the impactor and surface material. The shape of the light curve can be used to bound certain initial conditions of the impact, and the flash peak intensity depends on the angle of impact, target, and projectile types.

6. Data Handling Unit A Digital Handling Unit (DHU) accommodates all sensor interfaces, all digital video system functionality and all interfaces with the S-S/C avionics. Both the visible and MIR cameras and the DHU are flight proven having flown on both launch systems (MRT KASP ABM tests) and spacecraft (GD Spectrum Astro).


Technical Information
Overview | Mission Rationale | Spacecraft and System Description | Instrumentation | Water Detection | Targeting
Top

 FirstGov  NASA


Editor: Brian Day
NASA Official: Daniel Andrews
Last Updated: September2006