How to re-photograph Apollo landing sites

 The project involves using a 3U CubeSat, “Arkiv-1,” with a 40 m resolution hyperspectral imager to re-photograph Apollo landing sites at the same solar azimuth and elevation as the Apollo 11 photograph AS11-37-5447, aiming to detect terrain disturbances in iron-oxide absorption bands. The data will be downlinked to a rented container in the Sahara Desert. Below is a detailed plan to execute this, tailored to your specifications and the remote setup.


1. Data Acquisition with Arkiv-1The task is to acquire hyperspectral imagery from the Arkiv-1 3U CubeSat, designed to re-photograph Apollo landing sites (e.g., Apollo 11 at 0.674°N, 23.473°E) under specific lighting conditions to match AS11-37-5447, focusing on iron-oxide absorption bands.
  • Arkiv-1 Specifications:
    • Platform: 3U CubeSat (~10x10x30 cm, ~4 kg).
    • Cost: ~$85k build + $25k launch (e.g., SpaceX Transporter rideshare).
    • Instrument: Hyperspectral imager with 40 m spatial resolution, covering iron-oxide absorption bands (0.9–1.0 µm, near-infrared) with spectral resolution of ~10–20 nm.
    • Orbit: Likely low Earth orbit (LEO, ~500 km) with a steerable imager for lunar observations. Lunar orbits are possible but cost-prohibitive for a 3U CubeSat.
  • Task Requirements:
    • Solar Geometry: AS11-37-5447 was taken on July 20, 1969, at Tranquility Base with a solar elevation of ~10–15° and azimuth of ~90° (east). Use NASA’s SPICE toolkit or Lunar Reconnaissance Orbiter (LRO) ephemeris data to calculate equivalent solar angles for each Apollo site (Apollo 11, 12, 14, 15, 16, 17) during Arkiv-1 overpasses.
    • Target: Detect terrain disturbances (e.g., lander blast zones, ~10–20 m) visible in iron-oxide absorption bands due to regolith disruption (e.g., compaction, exposure of subsurface material).
    • Sites: Six Apollo landing sites, requiring multiple imaging passes to match solar conditions.
  • Acquisition Steps:
    1. Orbit Planning:
      • Use Systems Tool Kit (STK) or FreeFlyer to schedule lunar overpasses when solar azimuth/elevation matches AS11-37-5447. A 500 km LEO orbit provides periodic lunar visibility (e.g., every ~2 weeks for specific sites).
      • Task Arkiv-1 to point its imager at each Apollo site during optimal passes. Ensure the CubeSat’s attitude control system (e.g., reaction wheels) can achieve precise pointing (±0.1°).
    2. Imaging:
      • Capture hyperspectral data cubes (x, y, wavelength) covering 0.4–1.0 µm to include iron-oxide bands. Each image may be ~1 GB due to high spectral resolution (e.g., 100 bands).
      • Verify the imager’s signal-to-noise ratio (SNR >100) for reliable spectral analysis.
    3. Downlink:
      • Transmit raw data to the Sahara container via UHF (400–450 MHz) or S-band (2.2–2.3 GHz). Data rates may be low (10–100 kbps for UHF), requiring multiple passes to downlink large datasets.
      • Use a ground station receiver (e.g., 1–2 m parabolic antenna) in the container, paired with software like GNU Radio or SatNOGS to decode telemetry (e.g., AX.25 protocol).

2. Sahara Container SetupThe rented container in the Sahara must support data reception, processing, and storage under harsh desert conditions.
  • Power:
    • Solar Panels: Install 2–5 kW photovoltaic panels with lithium-ion battery storage (e.g., 10 kWh) to power the ground station, computers, and cooling. The Sahara’s high solar irradiance (~7 kWh/m²/day) supports this.
    • Backup: Use a diesel generator (5 kW) with fuel reserves for sandstorms or low sunlight periods.
  • Cooling:
    • Equip the container with a 5–10 kW air conditioning unit to maintain <30°C internally, protecting electronics from temperatures up to 50°C. Use dust filters to block fine Saharan sand.
    • Insulate the container with reflective panels to reduce heat ingress.
  • Ground Station:
    • Antenna: A steerable 1–2 m parabolic antenna for S-band or a Yagi antenna for UHF. Ensure tracking software aligns with Arkiv-1’s orbit (e.g., using TLE data from Celestrak).
    • Receiver: Software-defined radio (SDR) like USRP B210 for flexible frequency tuning. Store raw packets on 20 TB SSDs.
  • Connectivity:
    • Use Starlink for internet access (50–150 Mbps) to upload processed data or download ephemeris files. Protect the Starlink dish from sand with a sealed enclosure.
    • Alternatively, use a VSAT terminal (~10 Mbps) as a backup.
  • Hardware:
    • Workstation: 64 GB RAM, AMD Ryzen 9 or Intel Xeon, NVIDIA RTX A4000 GPU for hyperspectral processing.
    • Storage: 20–50 TB SSDs with RAID for redundancy.

3. Processing WorkflowProcess the raw hyperspectral data to detect terrain disturbances in iron-oxide absorption bands.
  1. Data Decoding:
    • Decode telemetry packets using GNU Radio or CubeSat-specific software to reconstruct hyperspectral data cubes (HDF5 or ENVI format).
  2. Preprocessing:
    • Radiometric Calibration: Convert raw digital numbers to radiance (W/m²/sr/µm) using calibration coefficients from the imager’s manufacturer.
    • Geometric Correction: Georeference images to lunar coordinates (e.g., Mean Earth/Polar Axis system) using Arkiv-1’s attitude and position data. Use USGS ISIS for lunar projections.
    • Illumination Correction: Normalize for solar illumination variations using the solar zenith angle from AS11-37-5447. No atmospheric correction is needed (lunar surface).
  3. Spectral Analysis:
    • Band Selection: Extract bands covering 0.9–1.0 µm for iron-oxide absorption (e.g., FeO, Fe₂O₃). Use Python’s spectral or hyperspy libraries.
    • Continuum Removal: Apply continuum-removed reflectance to enhance absorption features. Compare spectra from disturbed areas (e.g., lander zones) to undisturbed regolith.
    • Spectral Angle Mapping (SAM): Use ENVI or Python to quantify spectral differences between disturbed and undisturbed areas, highlighting iron-oxide anomalies.
  4. Terrain Disturbance Detection:
    • Image Alignment: Overlay Arkiv-1 images with LRO Narrow Angle Camera (NAC) images (0.5 m resolution, available via USGS) to locate Apollo site features (e.g., lander, rover tracks).
    • Change Detection: At 40 m resolution, focus on large-scale disturbances (e.g., lander blast zones, ~10–20 m). Use difference imaging or SAM to identify altered albedo or spectral signatures.
    • Validation: Cross-reference findings with LRO data to compensate for Arkiv-1’s coarse resolution.
  5. Output:
    • Generate GeoTIFF or ENVI files showing iron-oxide absorption anomalies for each Apollo site.
    • Produce spectral plots comparing disturbed vs. undisturbed regolith.
    • Store results on local SSDs and upload to a cloud platform (e.g., AWS S3) via Starlink for sharing.

4. Challenges and Mitigations
  • Resolution Limitation: 40 m resolution limits detection to large-scale disturbances. Supplement with LRO NAC imagery for finer details (e.g., footprints).
  • Solar Angle Matching: Precise timing is critical. Use SPICE or STK to predict overpasses within ±1° of target solar angles. Multiple passes may be needed.
  • Data Volume: Hyperspectral data (~1 GB per image) and slow downlink rates (10–100 kbps) may delay acquisition. Prioritize key bands (0.9–1.0 µm) to reduce data size.
  • Sahara Environment: Protect equipment from heat (up to 50°C) and sandstorms (winds up to 100 km/h). Use sealed enclosures and regular maintenance.
  • Logistics: Fuel and spare parts delivery to the Sahara is challenging. Stockpile supplies and train local staff for basic operations.

5. Recommendations
  • Start with Apollo 11: Focus initial imaging on Tranquility Base to validate the workflow before scaling to other sites.
  • Leverage LRO Data: Freely available LRO NAC images (https://pds-imaging.jpl.nasa.gov/) provide high-resolution context to interpret Arkiv-1’s coarse data.
  • Automate Processing: Use Python scripts to automate spectral analysis and change detection, reducing manual effort in the remote container.
  • Collaborate: Partner with lunar science groups (e.g., NASA’s SSERVI) for ephemeris data or processing expertise.

6. Tools and Resources

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