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Comment by koheripbal | Hacker News Reader

I think he means it would need to be calibrated on Mars as the exact ground density and composition isnt known from earth

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Correct. The easiest way to calibrate a GPR is to stick a metal plate in the ground and cover it with a few feet of earth dug up on location. Can’t do that with some awkward rovers and an experimental helicopter.

NASA can do some fancy signal processing to get some useful data but until its properly calibrated, any interpretation of that data especially visual should be taken with a Phobos sized grain of salt.

I still don't understand. Even if you are off about density, aren't you studying the differences in density, so that the image you generate would still be showing where those differences are located relative to each other -- even if scale might be somewhat off if you have your base density off? It doesn't seem like it would be abject failure, but more like incrementally less useful. It sounds like you are saying it is almost at abject failure on the scale of usefulness.

Yes and no. The radar isn’t only looking down into the ground. The antenna pattern has side lobes which can potentially generate large echos in the radargram, e.g. from rocks on the surface etc. you only know that there is something in some distance (or rather time delay).

The useful signal is extremely weak anyway and the clutter from the surface hides the useful signal in many cases unless you habe really strong scatterers (large and highly reflective) buried in the ground.

Plenty of commercial GPR devices operate on Earth just fine with the explicit goal to detect changes in the subsurface's dielectric properties. It doesn't matter if you're on Mars or here, GPR works in the same way and I'm pretty sure that the antenna and the signal processing has been designed for the purpose, possibly even more meticulously than the antennas of commercial GPR pushcarts. Your comment makes something simple sound highly involved and problematic.

Your understanding is correct. It's about detecting variations in dielectric properties across layer interfaces. GPR works just fine for that, whether here or on Mars. The other commenter's negativity and theorized worries about side lobes and reflectors are unwarranted.

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