OrbitalHub

NASA JPL dixit:

“Starting next year, scientists will get their first look deep below the surface of Mars. That’s when NASA will send the first robotic lander dedicated to exploring the planet’s subsurface. InSight, which stands for Interior Exploration using Seismic Investigations, will study marsquakes to learn about the Martian crust, mantle and core.

When rocks crack or shift, they give off seismic waves that bounce throughout a planet. These waves, better known as quakes, travel at different speeds depending on the geologic material they travel through. Seismometers, like InSight’s SEIS instrument, measure the size, frequency and speed of these quakes, offering scientists a snapshot of the material they pass through.

Mars’ geologic record includes lighter rocks and minerals — which rose from the planet’s interior to form the Martian crust — and heavier rocks and minerals that sank to form the Martian mantle and core. By learning about the layering of these materials, scientists can explain why some rocky planets turn into an “Earth” rather than a “Mars” or “Venus” — a factor that is essential to understanding where life can appear in the universe.

Each time a quake happens on Mars, it will give InSight a “snapshot” of the planet’s interior. The InSight team estimates the spacecraft will see between a couple dozen to several hundred quakes over the course of the mission. Small meteorites, which pass through the thin Martian atmosphere on a regular basis, will also serve as seismic “snapshots.” One challenge will be getting a complete look at Mars using only one location. Most seismology on Earth takes measurements from multiple stations. InSight will have the planet’s only seismometer, requiring scientists to parse the data in creative ways.

InSight will measure more than seismology. The Doppler shift from a radio signal on the lander can reveal whether the planet’s core is still molten; a self-burrowing probe is designed to measure heat from the interior. Wind, pressure and temperature sensors will allow scientists to subtract vibrational “noise” caused by weather. Combining all this data will give us the most complete picture of Mars yet.”

Video credit: NASA Jet Propulsion Laboratory

NASA Goddard dixit:

“Mars has two moons, Phobos and Deimos. Both are small, airless bodies with irregular shapes. Because they lack protective atmospheres and magnetospheres, Phobos and Deimos are directly exposed to the solar wind for part of their orbits. Now, a study from NASA’s Goddard Space Flight Center suggests that the solar wind creates a complex electrical environment around Phobos, giving its night side and shadowed craters a static electric charge. This could impact plans for future robotic and human explorers to study the moons of Mars.”

Video credit: NASA Goddard

NASA dixit:

“NASA’s InSight spacecraft arrived at Vandenberg Air Force Base, California, to begin final preparations for launch. InSight will be the first mission to look deep beneath the Martian surface, studying the planet’s interior by listening for marsquakes and measuring its heat output. It will be the first planetary spacecraft to launch from this west coast launch facility. The launch period for InSight opens May 5, 2018 and continues through June 8, 2018. “

Video credit: NASA

NASA dixit:

“These observations of Phobos and Saturn were taken by the Super Resolution Channel of the High Resolution Stereo Camera on Mars Express. The video comprises 30 separate images acquired during Mars Express orbit 16 346 on 26 November 2016. The slight up and down movement of Saturn and Phobos in these images is caused by the oscillation of the spacecraft’s orientation after completing the turn towards the moon. Phobos can be seen in the foreground, partially illuminated, with Saturn visible as a small ringed dot in the distance.”

Video credit: NASA

NASA dixit:

“Even if rovers, balloons, and airplanes continuously move around and near the surface of Mars one day, we should never judge a planet by its cover. Today’s desert-like Martian surface likely hides the presence of water below ground. To “follow the water” to where it is today, we must go beneath the surface of the planet with subsurface explorers. The subsurface of Mars may resemble some of the colder parts of Earth. For example, in Antarctica or Iceland, we know that water is stored in a layer of permafrost and beneath that, as liquid groundwater. Even if the ancient surface water on Mars evaporated, there may still be substantial reservoirs of water, in either liquid or frozen form, in the subsurface.

The very first subsurface exploration of Mars for NASA will be in partnership with the European Space Agency (ESA) in their Mars Express mission. This spacecraft carries a subsurface radar instrument that will use a 40-meter (130-foot) antenna to detect and map subsurface water. Electric signals will be sent down the antenna, creating low-frequency radar waves. The radar waves will penetrate the Martian surface as deep as five kilometers (three miles) and will be reflected back to the spacecraft by different subsurface features, including water. This data will give us a three-dimensional understanding of where and how much water may be distributed in the Martian subsurface.

A lander on Mars Express called Beagle 2 will also carry the first robotic mole. Mimicking the behavior of the small furry earth-bound creatures that burrow into the ground, robotic moles will drill underground by pulverizing rock and soil, avoiding the need for a complex drill stem. Beagle 2’s mole will only have the ability to penetrate less than a meter (less than 3 feet) below the surface.

A much more capable mole is under development in NASA’s technology program. Weighing about 20 kilograms (44 pounds), it will be capable of drilling hundreds of meters (hundreds of yards) into the ground and possibly deeper at a rate of 10-20 meters (33 – 66 feet) a day. Excavated soil would be moved to the back of the mole and a small tube leading to the surface would help alleviate the pressure from the growing mounds of soil. The tube would also send soil samples back to the surface and carry power to the robotic mole. The samples sent up to the surface would be studied for scientific data such as mineral content and oxidation levels of subsurface soil. A mole drilling at the polar cap would study the layers of ice that tell the story of its history, much like the rings of a tree reveal many things from its past. All of this data would provide clues in the search for ancient, or possibly current, life.

Once we know in more detail where the water lies, the next step is to drill in those locations. To get to the zone where frozen water–and possible dormant life–might be present, we will probably need to drill to a depth of 200 meters (656 feet). Liquid groundwater will be even deeper. That’s no easy feat, but it’s critical for understanding the possibility of past or present life on Mars and for confirming that water resources are available for future human explorers.

Deep subsurface access on Mars will have unique challenges. First of all, unlike on Earth, we will not be able to use a drill to go through mud, water, or probably even gas pressure to carry the cuttings away from the bit. We will need new systems for fluidless drilling. Second, we will need an effective means of keeping the hole open while the drilling proceeds. On Earth, this task is normally done with steel casing, which is very heavy. Engineers are actively seeking alternative ways that don’t require us to send heavy equipment to Mars given the expense. Finally, we will have to develop systems that allow the drill to make operational decisions for itself. On Earth, drills can get stuck very quickly, so a Mars robotic drill or subsurface explorer must know how to recognize, avoid, and solve problems on its own.”

Video credit: NASA

ESA dixit:

“Since arriving at Mars in October 2016, the ExoMars Trace Gas Orbiter has been aerobraking its way into a close orbit of the Red Planet by using the top of the atmosphere to create drag and slow down. It is almost in the right orbit to begin observations – only a few hundred kilometres to go! With aerobraking complete, additional manoeuvres will bring the craft into a near-circular two-hour orbit, about 400 km above the plane, by the end of April. The mission’s main goal is to take a detailed inventory of the atmosphere, sniffing out gases like methane, which may be an indicator of active geological or biological activity. The camera will help to identify surface features that may be related to gas emissions. The spacecraft will also look for water-ice hidden below the surface, which could influence the choice of landing sites for future exploration. It will also relay large volumes of science data from NASA’s rovers on the surface back to Earth and from the ESA–Roscosmos ExoMars rover, which is planned for launch in 2020.”

Video credit: ESA