InSight Surface Operations, 26 Nov 2018- 21 Dec 2022 |
InSight Surface Operations, 26 Nov 2018- 21 Dec 2022 |
Mar 20 2019, 04:39 PM
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#526
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Senior Member Group: Members Posts: 4246 Joined: 17-January 05 Member No.: 152 |
Thanks for the update. I'm curious what makes them say "dustless", as pressure wouldn't tell you that - perhaps simultaneous imaging?
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Mar 21 2019, 04:25 AM
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#527
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Solar System Cartographer Group: Members Posts: 10151 Joined: 5-April 05 From: Canada Member No.: 227 |
They have the radiometer too, it would probably record the dimming caused by the passing shadow or the entrained dust. But I think what they mean - or i should have said - is they see lots of vortices in the met and/or other data but have yet to see a visible DD.
Phil -------------------- ... because the Solar System ain't gonna map itself.
Also to be found posting similar content on https://mastodon.social/@PhilStooke Maps for download (free PD: https://upload.wikimedia.org/wikipedia/comm...Cartography.pdf NOTE: everything created by me which I post on UMSF is considered to be in the public domain (NOT CC, public domain) |
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Mar 21 2019, 02:02 PM
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#528
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Senior Member Group: Members Posts: 2428 Joined: 30-January 13 From: Penang, Malaysia. Member No.: 6853 |
HP3 Mission update / Logbook entry: 21 March 2019, defines the next steps for the mole link
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Mar 22 2019, 04:38 AM
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#529
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Senior Member Group: Members Posts: 2428 Joined: 30-January 13 From: Penang, Malaysia. Member No.: 6853 |
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Mar 22 2019, 10:13 PM
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#530
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Newbie Group: Members Posts: 10 Joined: 30-May 08 Member No.: 4166 |
Anothe SEIS post.
https://www.seis-insight.eu/fr/actualites/4...mmissioning-end Evaluation of the commisioning phase of seismometer SEIS on mars The instrument commisioning period of SEIS, which began after the wind and thermal sheild (WTS) was set in place saturday 2 february 2019, will finish up on 5 april next. During this period many crucial operations have been successfully undertaken involving the seismic data recorders, notably the VBB pendulums. Thermal stability: WTS is a peaceful shelter After the deployment of the WTS shield over SEIS during sol 66, engineers were immediately impressed by the improvement in the thermal environment it acheived. In order to characterise the amount of stabilisation offered by this portable "seismic cave", it was decided to temporarily disable the heaters that usually protect the instrument during the coldest part of the day on mars. Simulations indicated that with WTS the daily temperature variations would be small enough for it to be safe to shut down the heaters for several days without risk to the instrument. Subsequent analysis by thermal engineers show that the protective bell of WTS is working perfectly. Thanks to the improved thermal protection provided by WTS (which merely adds to several barriers already in place, such as the spherical enclosure under vacuum housing the VBB pendulums, the RWEB heat shield, or the TCDM device situated among the pendulums) SEIS's six sensors could be turned on for the first time on sol 70 without interruption. Activating TCDM: the ultimate thermal protection for the pendulums The VBB pendulums of SEIS are equipped with a mechanism specifically made for mars (and not present on earthly seismometers) whose purpose is to reduce as much as possible the residual thermal variation of the spherical vacuum vessel in which they're installed. Called TCDM, this ingenious device passively displaces the center of gravity according to the temperature. It works on the principle of differential thermal expansion of two metals which expand or contract according to the temperature changes in the sphere like an accordion. In order to neutralise the temperature changes as much as possible, the orientation of TCDM requires a fine adjustment. During sol 77, engineers implemented a first adjustment to reduce as much as possible the thermal sensitivity of each pendulum independently of the others (other strategies could be tried, such as a reduction of noise in a specific frequency band, or an adjustment maximising the sensitivity of all three pendulums combined). The TCDM of pendulum #1 was turned -5°, that of #2 +20°C, while the TCDM of pendulum #3 was left as is (0°). [Note it says 20°C for #2 but this looks like a typo to me. I think these numbers are degrees of arc, but I'm not sure - rhr] After an analysis of the effects obtained, a further adjustment was made on sol 81 (+1° for VBB #1, +22° for #2, and +2° for #3). After these changes in orientation the adjustments were judged satisfactory by the engineers in charge of performance, which permitted an increase of instrument gain in science mode. The VBB pendulums can work in two modes, engineering (robust but insensitive), and science (more precise but with a risk of saturating the detector) which has a variable gain. Thanks to TCDM the pendulums can now work at their maximum sensitivity. Calibration of the pendulums The calibration of the VBB pendulums represents another essential step in the commisioning phase of SEIS. This step, necessary for correct interpretation of the instrument's data, consists of generating a sequence of artificial vibrations from the large exterior feedback system coil, and observing the reaction of each pendulum to the vibration. On sol 77 the first stage of the calibration began in engineering mode (high gain) at a determined temperature. A second stage of calibration was then performed on sols 85-93 in science mode, this time with one pendulum at a time, and at three different temperatures (its maximum daily value, minimum and medium). Calibration was also performed on the SP sensors at the beginning of february. In addition to the official calibration, two fundamental parameters of the VBB sensors, the natural frequency (the frequency at which it vibrates on its own, which should be as weak as possible), and the quality factor (the rate at which a given perturbation of the pendulum decreases over time) were also determined for the first time on mars and compared with the values measured on earth. The last step in the commissioning process for SEIS consists of a test modifying the known height of the feet of the levelling platform to look at the induced effect, in particular the difference between the response of the short-period (SP) and very-broadband (VBB) sensors. Following the penetration of HP3 In parallel with the calibration efforts, SEIS has also been listening to the vibrations generated by the mole of heat probe HP3 as it forced itself into the ground on sols 92 and 94. Unfortunately the mole stopped its progress as soon as it started. Most likekly a rock or layer of gravel prevents it from going in further, but given the fact that its vertical inclination measurement changed (from the resistance it encountered) it is equally possible that it has become snagged inside its support tube. Data have shown that the SP sensors on SEIS, good for high-frequency measurements, show not only the ground penetration but also the internal movements of the mole's parts. As for VBB, when the mole starts hammering the sensors get saturated. In order to figure out what's blocking the mole as it goes into the ground, a third hammering attempt of 10-15 minutes will shortly occur. With the SP sensors the objective is to determine with maximum precision the movements of the internal parts of the mole when it performs a hammer blow to move forward. A digital filter will be installed in the electronic command system of SEIS to increase the temporal resolution. Depending on what SP hears it may be possible to determine if the mole is advancing even slowly, if it's continually hammering against an obstacle, or whether it's totally blocked. A second digital filter will also be activated to prevent the saturation of the ultra-sensitive VBB during HP3's hammering operations. Because of the differences in seismic wave propagation in different materials it may be possible to see if there's a harder layer around 30cm deep. The red planet under seismic surveillance Spread out over 62 sols, the commissioning phase allows us to test each subsystem effectively. Procedures for downloading data (whether from continual data collection, or on-demand high-resolution data) and for uploading command sequences have also been validated. This more than satisfactory evaluation allows us to begin the scientific campaign, which officially starts 5 april 2019 and lasts one mars year. So on Elysium Planitia everything is now in place for the first detection of mars earthquakes to reveal the interior structure of mars. |
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Mar 28 2019, 08:21 AM
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#531
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Senior Member Group: Members Posts: 2428 Joined: 30-January 13 From: Penang, Malaysia. Member No.: 6853 |
Animated GIF using a pair of processed frames from sol 117 and sol 118, shows a little movement in the HP3 housing.
The HP3 PI's blog update of 22 March mentioned a short diagnostic hammering on Wednesday, which I suspect resulted in the changes seen between these frames. Hopefully we'll get an update in the coming days from the team and also a few more images, especially from the ICC camera images from much later in the sol when the sun will fill the shadows under the housing |
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Mar 31 2019, 11:07 PM
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#532
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Solar System Cartographer Group: Members Posts: 10151 Joined: 5-April 05 From: Canada Member No.: 227 |
New images fill in the last bit of the horizon - they are the upside-down ones of recent sols. This is a circular projection of just the horizon strip.
Phil -------------------- ... because the Solar System ain't gonna map itself.
Also to be found posting similar content on https://mastodon.social/@PhilStooke Maps for download (free PD: https://upload.wikimedia.org/wikipedia/comm...Cartography.pdf NOTE: everything created by me which I post on UMSF is considered to be in the public domain (NOT CC, public domain) |
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Apr 2 2019, 05:33 AM
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#533
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Senior Member Group: Members Posts: 1084 Joined: 19-February 05 From: Close to Meudon Observatory in France Member No.: 172 |
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Apr 2 2019, 11:20 PM
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#534
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Senior Member Group: Members Posts: 2428 Joined: 30-January 13 From: Penang, Malaysia. Member No.: 6853 |
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Apr 3 2019, 05:19 PM
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#535
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Senior Member Group: Members Posts: 2082 Joined: 13-February 10 From: Ontario Member No.: 5221 |
Fresh update on HP3: https://spaceflightnow.com/2019/04/03/insig...n-be-recovered/
QUOTE Engineers have used InSight’s cameras and seismic sensors to diagnose the HP3 instrument’s situation. During a third short hammering session March 27, ground controllers tuned the lander’s seismometer to listen to the vibrations created by the mole in an attempt to assess whether the probe is pushing against a single rock or a thick layer of gravel. “The character of the seismic signal is changing, especially between the initial hammering … There are changes happening in the response,” Banerdt said March 26, referring to the seismometer’s measurements of the probe’s first hammering operation. “There are changes happening in the response (of the rock),” Banerdt said. “We think we can analyze some of that stuff in terms of both the reverberation of soil versus rock, and also in terms of actual individual substrokes within the hammer itself. The hammer actually has about 5 different sub-strokes as it hits and rebounds and different parts of it absorb the impact.” The obstruction is at around 30 cm; is that too deep for the scoop to excavate nearby and find out how big the obstruction is, or if it's a layer under the whole worksite? |
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Apr 4 2019, 01:26 AM
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#536
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Forum Contributor Group: Members Posts: 1372 Joined: 8-February 04 From: North East Florida, USA. Member No.: 11 |
Fresh update on HP3: https://spaceflightnow.com/2019/04/03/insig...n-be-recovered/ The obstruction is at around 30 cm; is that too deep for the scoop to excavate nearby and find out how big the obstruction is, or if it's a layer under the whole worksite? At the end of the day digging it out or pulling it might be needed. Where the mole is now it's not going to work. |
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Apr 4 2019, 12:47 PM
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#537
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Senior Member Group: Members Posts: 1582 Joined: 14-October 05 From: Vermont Member No.: 530 |
At the end of the day digging it out or pulling it might be needed. Where the mole is now it's not going to work. They seem to think the mole's tendency to turn around obstructions is hindered by the rear end still being in the housing. I couldn't gather whether the seismic data has led to any conclusions, either about what's underground, or what to do. |
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Apr 4 2019, 11:18 PM
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#538
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Senior Member Group: Members Posts: 1084 Joined: 19-February 05 From: Close to Meudon Observatory in France Member No.: 172 |
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Apr 5 2019, 11:15 AM
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#539
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Senior Member Group: Members Posts: 2920 Joined: 14-February 06 From: Very close to the Pyrénées Mountains (France) Member No.: 682 |
Thank you VikingMonnetMars 😃
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Apr 5 2019, 05:47 PM
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#540
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Senior Member Group: Members Posts: 1084 Joined: 19-February 05 From: Close to Meudon Observatory in France Member No.: 172 |
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