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Moving to Kelly Lake – and putting our knowledge to the test

Posted on July 6th, 2011 by Margarita Marinova

After three Deepworker seasons at Pavilion Lake – and multiple years of science scuba exploration before that – we are moving to Kelly Lake this year. You already knew that – but how do the two tie together? What will be similar and what will be different?

Kelly Lake and Pavilion Lake are similar in that they both have microbialites, and with similar morphologies (shapes) too! But at Pavilion the microbialites are just about everywhere – while at Kelly Lake they are only in a few locations. Why is that? We have done some scuba diving in Kelly Lake, but because of the limitations of how much time we can spend underwater, we haven’t been able to really map where the microbialites occur. So this year we’ll use the Deepworker submersibles to really get a close look at where all the Kelly microbialites are and how they look. They could all be similar to what we see at Pavilion – but until we go and look we just don’t know.

And speaking of mapping – we already have bathymetry (depth) and SONAR (surface hardness and roughness) data for Kelly Lake, which gives us at least some idea of where to go look for what we think are microbialites. But this data also shows us some interesting features that we haven’t seen in Pavilion Lake. For example, some of the sonar images look like gullies – the scours that are formed when water running down a hill causes a landslide. But this is underwater, so how did it form? Or there are some wavey features – what about those? Again, until we go and look, we just don’t know.

Our move to Kelly Lake is also interesting in an operational sense. After three years of having the submarines at Pavilion Lake, we largely knew what to expect. We knew how to plan missions, how long they would take, where to find the type of microbialites that a specific scientist was interested in. Because Kelly Lake is new, we have put together everything that we had learned from Pavilion Lake – both in terms of the science and the submarine exploration – and are using it to exploring our new Kelly Lake world. We have the bathymetry and sonar data, which are like having remote sensing data for another planet. So given that, how well can we do in planning the best missions, with the highest productivity and success for the selected tasks? This is really like going to another planet and using all of our training! The added pressure here is that we expect to only spend one season at Kelly Lake with the Deepworkers, which means that we have to do it all the first time: from general exploration of the lake, to selecting the best samples to collect, to which microbialites and features are of the greatest interest and should be imaged and explored the most.

This move isn’t to say that we have learned everything that we wanted to know about Pavilion Lake, but it does mean that our Deepworker exploration there has already yielded detailed maps of morphology distribution and mapping in the lake, and future work can focus on understanding choice locations through scuba diving. It is time to move to a lake like Kelly, where similar microbialites are present, but the environment is just different enough that it will put our understanding of how everything forms to the test.

Analogue science – above the water at Desert RATS

Posted on September 11th, 2010 by Margarita Marinova

Rocks, rocks everywhere! This time we are not in the underwater wonder of Pavilion Lake, but in the desert and volcanic fields between Flagstaff and the Grand Canyon in Arizona.

But wait! Is that a rover peaking from behind that volcano?

Exploring these volcanic fields are rovers, habitats, robots small and big – all part of the NASA Desert RATS project. The goal: test equipment and procedures for planetary exploration of the Moon, Mars, and beyond. It’s an amazing operation where crews in rovers explore the surface, bring samples back to the habitat to be examined, robots small and big map the surroundings, and science crews back on “Earth” follow and coordinate it all. What does that add up to? Over 150 people learning about operations, science, engineering, and human factors to help us plan our next big exploration and science adventure in space!

At the start of the mission, the rover is docked to the habitat. For the following 7-day mission, the crew will explore and live in the rover. (Image: D. Reid)

This week I am part of the Strategic Science Operations Team (SSOT), which is the NASA way of saying “look at the day’s science, how does it all fit into understanding the area’s geology, and decide what should be studied the next day!” Our day starts after everyone else is done, at 8pm, since we need the data from the rover crews, the reports from the command center, and the reports of the day-time science team. Starting at 8pm, we put all of this information together to really understand what new discoveries were made during the day. My role is specifically to analyze the data from Rover A: looking at video notes, images and samples that the crew took, as well as notes and GigaPan images by the day-time science team.

The portable "Houston" in the Arizona Desert. This is the command center for the Desert RATS project. (Image: D. Reid)

It’s amazing to see the close-up images that the crew takes, and just how much more you can see and understand from walking across the area compared to orbital images! It’s like seeing a picture of New York or Paris, compared to actually going there! The crew can really give us a better perspective on what it is they see, and their interpretations of the geology are invaluable!
By 5am we have to finish our analysis, the planning for the following day, the new day plans for the crew – and uploaded it all to the command center.

At base camp, seeing all the pieces come together, I stand in awe. This is what it means to plan for a monumental mission like exploring the Moon. There are so many pieces, and they all have to come together flawlessly. A robot purrs to life as it starts moving up the hill to provide better communications. The crew is getting ready for another day of exploration, reading their updated day plans sent from the science team during the night. The day-time science team is ready and counting down the minutes to the morning brief with the crew. In the quietness of the desert, everyone is ready to go, and the sun comes up as if to give the go-ahead for another day of exploration.

~ mars.

Greg Baiden – NASA Desert Rats – Strategic Science Operations Team (SSOT)

Posted on September 11th, 2010 by Greg Baiden

It is the middle of night and our team is busy reviewing the samples collected yesterday and planning the next few days traverses. The results of the work are going great! Today our teams traversed the vc1 cone collecting many samples of  high quality with full communications.  Tomorrow starts twice a day comms for the final few days.  What a great experience!!

A helo flight to prepare for next year

Posted on July 23rd, 2010 by Marc Seibert

On the way back from Kelly Lake, we swung by Pavilion Lake to take some shots of the live sub operations underway. This is a very beautiful part of the world.

Next year the team will be diving into a lake called Kelly Lake, and potentially Pavilion Lake at the same time.  This creates a challenge for the communications team.  Both sites must have broadband access to the Space Network Research Federation (SNRF) and the Internet, and be able to communicate from site to site at all times.

Satellite connectivity is great, but in this environment the “terrain mask” (steep rise of the terrain all around us) makes it difficult to hit a satcom “bird” in the sky from these high northern latitudes.  On top of this, satellite transponder time can be expensive (especially considering the amount of “megahertz” or transponder we need!), and adds a significant “latency” to the communications link (in both directions) because the satellites are orbiting so far above the Earth.  This latency can cause problems for some of the operations conducted by this team, and terrestrial interfaces tend to have very low latency.

We took a Trackstick with us in the helicopter, and you can see the path we flew here (thanks to Google Earth!)

So we took off in a helicopter in Lillooet, and flew to Kelly Lake to visit and survey the terrestrial (ground/mountain-based) communications options for communications near the lake.  If we can avoid using a satcom link, we’ll have greater bandwidth and network performance at the 2011 test operations.

We found several options for connectivity or relay on a few mountains surrounding Kelly Lake, and even some options to link the two lakes together for next year’s mission.  This begins a year’s worth of planning “now”.  ; )

- Marc

Pavilion Lake, looking south

One of the DeepWorker chase boats, looking south.

Pavilion Lake Research Project: Wrapping up 2010

Posted on July 20th, 2010 by Allyson Brady

The PLRP 2010 field season has come to a close and I am both saddened by the fact that operations are finished for another year but excited by the prospect of adding the data we’ve collected this year to our growing body of knowledge about this unique lake. I am in awe of the work that has been done by this amazing team and of how much we’ve grown, while maintaining the sense of adventure and camaraderie that to me, helps to define the PLRP.

We’ve taken great strides towards answering many of our research questions and in the process, with every answer we have come up with many more questions that will keep the PLRP team occupied for quite some time. Fortunately, our family continues to grow and every year we welcome new individuals who bring a unique perspective and desire to tease out the mysteries Pavilion has to offer. We have also been blessed this year by the addition of two little members to the PLRP family, Darlene Lim’s daughter Amelia and Greg Slater’s son Joseph. We look forward to the day when they are exploring the lake alongside us.

DeepWorker Pilots and Nuytco Team: 2010

The PLRP provides a wealth of research opportunities, and not just those focused on understanding the processes leading to the formation of the structures at Pavilion Lake but also to understanding fundamental biological, chemical and physical processes. The research contributions from our participating scientists and graduate students have resulted in a number of recent publications and are essential to increasing our understanding of Earth and astrobiological systems. We’re very proud of the role that the PLRP has played in developing operational technologies and protocols that not only help us meet our science objectives but provide important input into future space science missions.

With the addition of our two newest scientist pilots, astronauts Chris Hadfield and Stan Love, we had 34 DeepWorker missions over 10 days of operations. This year we were aided greatly in our pre-season flight planning by the wonderful team from NASA Ames led by Matt Deans and David Lees who developed an amazing flight planning tool that enabled us to search images and flight paths from previous years while building flight plans in Google Earth. Flights this year were planned to collect images of the remaining unexplored regions of the lake, to record detailed images of areas of interest identified from 2008 and 2009 data and to use the submersibles in combination with other analytical tools such as a conductivity, temperature and depth (CTD) instrument and our autonomous underwater vehicle(s) (AUV). Our ability to review post-flight video data in the field, an effort pioneered in 2009, added greatly to our productivity as this information was used immediately by the science backroom team to modify existing flight plans to best optimize our data collection. As part of the daily flight debriefs, we have also continued to apply metrics associated with scientific productivity to understand factors that influence scientific exploration. New this year to the DeepWorker flight repertoire were long ~ 5 hour flights and two night flights to investigate the grazing activity that we suspect may occur in the lake. To add to the innovations this year, Nick Wilkinson designed a fantastic, interactive program for use in classifying the microbialite images. This new tool will allow us to efficiently organize and process our field data over the coming months. Stay tuned for updates.

The Amazing Pavilion Lake Research Project Team: 2010!

In case our DeepWorker operations didn’t keep us busy enough, we had a number of other important activities included in the field schedule this year. The UBC and University of Delaware AUV teams produced fantastic images of the lake bottom that were often used to compliment the DeepWorker flights and give us a better picture of where interesting structures and features are in the lake. Numerous SCUBA dives were performed by our intrepid team of divers to collect water and microbialite samples that were shared between various research groups in an effort to combine and compliment analytical findings. These samples will be characterized from a virology, microbial lipid, isotopic and genetic point of view to provide more information about the role of biology in the formation of the microbialites and what biosignatures may be left behind. Water samples were collected from nearby lakes including Crown, Turquoise, Pear and Kelly Lake to continue to help us put Pavilion Lake in context. Kelly Lake, which also hosts microbialites and has been an area of interest to the PLRP team for many years, was also the focus of significant AUV activities this year. Microbial mats were once again collected from the Cariboo Plateau lakes and giant pancakes were eaten by all (well, almost all). As a new participatory activity this year, our visiting teacherswere given the task of selecting a SCUBA dive based on their understanding of the research questions of interest (on their first day no less!). I’m happy to report that they eagerly interviewed members of the team before presenting their selected dive and rationale to the group for inclusion in the next day’s diving schedule. Community Day was another great success this year with the team happy to show off our work and answer questions from the many visitors we had to the site. Busy indeed!

We plan on continuing our updates throughout the year as we analyze samples and work through the amazing amount of data that were collected. Thanks to all who have read about our activities and through this process, have joined in our adventure. See you next year!

~ Allyson

Robotic Choreography

Posted on July 19th, 2010 by Alex Forrest

DORA and UBC-Gavia in the water ready to deploy in Pavilion Lake.

Its now been just over a week since the end of our adventures at Pavilion Lake and, as I start trying to look at all the data we’ve collected, I can’t help but be impressed with our successes. In addition to the image mosaicing that I was working on, and showed pictures of in an earlier post, my specific focus of being up at the lake was running coordinated missions between the two autonomous underwater vehicles (AUVs), that we had on-site from the University of British Columbia and the University of Delaware, and the Deepworker vehicles. Our mission planning goals were twofold; joint objectives and joint missions.

Joint objective style missions measure parameters that are relatively static in time (i.e. photos of microbialites). This means that coordinating different platforms isn’t necessary but coordinating their datasets are. This requires that the timestamps of each data stream be precisely set and that the dataset is georeferenced to a high degree of accuracy. This work was started last year but continued this year by using the collected images from Deepworker and comparing it with AUV collected data (e.g. high-precision bathymetry).

Comparing multibeam bathymetry collected with DORA with detailed imagery from UBC-Gavia.

Joint missions involved a significantly greater degree of coordination as it involved running the vehicles at the same time as the Deepworkers. Our experiment this year was to look at the area of increased salinity at the bottom of the lake. To this end had the Deepworkers crossing the bottom of the basin at about 1 m from the bottom (> 55 m depth), while running UBC-Gavia at 40 m depth. The greatest debate was trying to decide what the minimum safe distance was to be between the two platforms! In the end we ran AUV missions down to 48 m without any problems. Although we’re just starting to process all of this data now, from both styles of missions, we’re excited about what new perspectives these combined datasets might hold.

-Alex

The Cariboo Plateau: home of giant pancakes, and smelly lakes

Posted on July 18th, 2010 by Eric Collins

We’re up at 7, skipping breakfast and congregating down at the dock to find our rubber boots and tie the canoe onto the roof of our rented SUV. Over an hour of mental exertion later (remembering forgotten equipment and forgotten knots), the spotless yellow canoe is lashed onto the too-small roof rack and we’re ready to go. Our mission today is deceptively simple: collect slimy mud from three small lakes on the Cariboo Plateau (yep, that’s how you spell it), about an hour and half north of the Pavilion Lake research station. Though it sounds simple, before we’re finished we’ll face rocky off-road drives, deep sucking quicksand-like mud, and flocks of hungry mosquitoes. However, our first challenge comes less than an hour into the drive, in the cozy town of Clinton, and it comes in an unlikely form: pancakes.

These aren’t just any pancakes, these are PANCAKES. Hungry-researcher sized pancakes — the size of a large microbialite. The pancakes here are a PLRP tradition, and I’m proud to say that our little group vanquished these planetary-scale hotcakes with hardly a hiccup. I must however admit that the four of us — Allyson (PLRP Acting PI), Jen (McMaster student), Henry, and myself (McMaster postdoc) — had a little help, in the form of 2-dimensional likenesses of Darlene (PLRP PI) and Greg (McMaster PI), who provided essential moral support in our endeavor.

After fueling up on carbohydrates and coffee, it’s time to find our lakes. We have GPS coordinates from previous visits, but in the end it comes down to brain power and hazy recollections when tracking down these mysterious bodies of briny water. “We’re looking for two cement blocks…. no, the road doesn’t have a name” was a typical direction on our course.

Sampling microbial mats using advanced scientific instruments

We arrive at the unofficially-titled Probe Lake and haul the canoe down to the shoreline, which is black with flies feasting on the remains of millions upon millions of desiccated larvae. I take a step into the reeking muck, en route to the brownish-green mats beyond, and am warned, as the mud approaches the top of my rubber boot, that “it’s deeper than it looks.” Thankfully I don’t have to wade too far through the mud because of a brilliant tool built by Allyson, consisting of half a plastic bottle taped to the end of a long pipe. Holes drilled through the bottom allow water to pass through while collecting the firm mats. Using this instrument I collected several jars of mats to return to McMaster University, where I will analyze the diversity of microorganisms in the mats and link this to biosignatures like fatty acids. Meanwhile, Jen and Allyson have launched the canoe and are taking water samples from the middle of the small lake. Previous research has found that these lakes are very salty and highly alkaline, or basic: they have a pH of about 10.1. The high pH is caused by very high concentrations of carbonate in the water.

Watch a tutorial on carbonate chemistry at the PLRP website.

One reason we are interested in these strange lakes is that although they are rich in carbonate ions, the microbial communities do not precipitate the carbonates and form microbialite structures as in Pavilion Lake. Understanding these differences may help to explain why the Pavilion Lake microbialites are so unique. These lakes may also be modern-day analogs to briny pools that existed early in Earth’s history, perhaps even before the rise of oxygen. Biomarkers are chemical compounds created by microbes that can be preserved over geological time scales in rocks. By identifying the microbial community members and their biomarkers in these lakes we may aid in identifying members of ancient microbial communities that are today preserved only as biomarkers in rocks.

After sampling each of the two remaining lakes I am more and more amazed by how different each lake is from the others, despite their similar origins and general chemical makeup. For example, the water in Probe Lake and Deer Lake is crystal clear, while Goodenough lake is so full of opaque particulates and brine shrimp larvae that we can’t see the bottom, less than 50 cm below us. The mats in each lake are also starkly different, ranging from pale pinkish flocculent islands to drier dark mats with thick bread pudding consistency, to mats with sharply delineated horizons of purple and green photosynthetic bacteria.

I’m excited to find out how the diversity of the microbial community is different in each lake and what role the lake chemistry might play in structuring these complex, colorful, and infinitely intriguing analogs for life on the early Earth. I’m less excited about washing out the canoe and the car, both of which are caked with stinking black mud, but sometimes that’s just what it takes to be an astrobiologist, and it’s all worth it in the end.

-Eric

What we did at summer camp, Part II

Posted on July 15th, 2010 by Bree and Jen

We are back at the Pavilion Lake Research Project this summer. It is great to return to the lake and rejoin the team. Our first night there, we were given homework. Usually we are the ones assigning homework, but this time it was different. Our task was to select a dive that we thought would help the team with their research and justify why this dive was, in fact, important to the team. We had a list of six dives that would all help the project, but we had to narrow it down to just one. As we started to interview and ask the scientists questions, it was clear that this would not be an easy task. The people that we talked to all had different reasons why each one was important. In the end, we selected one where the divers would measure the angle of the slope using an underwater inclinometer along a transect to see if the slope influences the morphology of the microbialites. The next morning, our dive was executed and we were on the boat to see our dive happen. We recorded the data – the depth, the angle and the sediment – as the divers used a scubaphone to communicate with us while they were underwater. This was very cool science and something we are excited to share with our students as they use inclinometers at school as well.

Divers use an underwater inclinometer to measure slope angle on our selected dive.

Our role at Pavilion Lake is to learn about the science that is happening at the lake and how we can teach about that back in the classroom with our students. Another task that filled our time was gathering resources and ideas for our lesson and activity ideas. We had a chance to interview, in video format, many of the people that are here studying the lake. We had some great interviews and learned in the process. Thank you to all those scientists who took time out of their busy day to let us interview them. As teachers, our summer vacation is just beginning. However, because of our experiences here at Pavilion, we are already looking forward to going back to school in September to share our time at the lake with our students through stories and science activities.

- Jen, Bree, & Leanne

Editor’s Note: Jen Stonehouse, Bree Mireau and Leanne Shortridge are teachers in the Greater Vancouver Area.

Dr. Love’s Underwater Blog, Part 5

Posted on July 12th, 2010 by Stanley Love

What a week it has been!  Today is the last of my six full days here at Pavilion Lake, and it feels like we’ve done a month’s worth of work.  Days begin with breakfast at 7 am and a team meeting at 7:30, and conclude with science debriefs that often end at 10 or 11 pm.  The pace is not quite as fast and relentless as a Shuttle flight…but it’s close.  It’s one more way in which Pavilion Lake is a good analog for an actual space flight.  (Differences include the excellent food and, on the rare occasions when time permits, being able to go fo a long jog with fresh air and lovely mountain scenery!)

Stan preparing for flight in DeepWorker

With two more “flights” in the Deepworker submarine under my belt since last I wrote, I’ve gotten a lot more familiar with the machine.  Although the miniature submarine looks nothing like a space suit, there are a lot of similarities.  And someday, when humans visit near-Earth asteroids or other objects with very low surface gravity, I expect they’ll do their spacewalks in something that looks a lot more like a Deepworker than a traditional person-shaped space suit. Here’s why.  A small asteroid has such weak gravity that even the slightest nudge with a hand or foot would send a spacewalking astronaut soaring high above the surface, and it might take hours to come back down.  A stronger shove might send an astronaut away at a speed higher than the escape velocity, in which case gravity would not bring them back ever!  Not so good.  On the International Space Station, which of course has no noticeable gravity of its own, astronauts keep from floating away by holding on to special handrails.  Asteroid do not come equipped with handrails.  They do have rough surfaces which might provide hand- and foot-holds, but unfortunately most asteroids are not solid blocks of material.  Instead they are “rubble piles,” flying clumps of sand, gravel, and boulders held together not by material strength, but by their own weak self-gravity.  So if you were moving hand-over-hand across the surface of the asteroid and accidentally pushed yourself off on a suborbital trajectory, you could grab onto a rock to keep yourself down–and the rock would simply come away with you! The practical result is that hands and feet are probably not the best way to move around an asteroid.  Better might be a suit with tiny thrusters that you could use to maneuver yourself around the landscape.  But if you’re not using your hands and feet to move around like a person climbing a tree, there’s no need to enclose them in a flexible suit.  Instead, you could keep them inside a hard pressure shell where they could be used to control thrusters, manipulators, and onboard systems.  Such an arrangement might look a lot like a Deepworker.  As a side benefit, the operator might be a bit more comfortable than in a traditional space suit.

Stan and DeepWorker 7.

Our underwater work here at Pavilion Lake ends this afternoon.  I’ll be the pilot for one of the last two “flights.”  The flight planner, Dr. “Mars” Marinova (who was just recently awarded her Ph.D. from the Geological and Planetary Sciences division at Caltech, where I worked as a postdoc more years ago than I care to admit), set up an especially interesting flight plan for me.  I’ll visit one of the “deep mounds,” outcroppings of microbialites growing on isolated boulders on the otherwise rather flat and monotonous central floor of the lake.  Then I’ll head off to do some vertical transects along the western shore.  These transects begin in deep water, then move upslope through the depth zone where the microbialite population is richest.  As I fly the transects I’ll record video of what I see from the submarine, and keep a running monologue (also recorded on board) of my observations.  It should be a lot of fun…and I’m sure I’ll miss piloting the submarines when the field season ends.
This wraps up Dr. Love’s Underwater Blog.  If I’m fortunate enough to be able to participate here next field season and spend more quality time underwater, I’ll be sure to reactivate the blog.
-Stan

Pavilion Lake and Beyond: How to Effectively Explore Other Worlds?

Posted on July 7th, 2010 by Mike Gernhardt

Mike Gernhardt with the DeepWorker barge in the background

This is my third year as a submarine pilot/scientist on the Pavilion Lake Research Project (PLRP) and it is really exciting and informative to be part of this team and to watch the progression and trends in the science and operational methods that are being applied to this expedition.  I originally became involved in the PLRP because of the use of the dual DeepWorker submersible system as an operational analog to the dual Lunar Electric Rover system that my team at NASA is developing.  The really special thing about PLRP is that it’s not a simulation, its real world-class science and the methods that we use to plan the flights collect and analyze the data, and the lessons we learn are directly relevant to future space exploration. It’s also pretty cool that we are seeing things that human eyes have never seen before and in that sense it’s analogous to finding life on Mars or some other planet.

Mike Gernhardt and Bill Todd (front) work as CapCom on the surface vehicle, while Steve Wittig (back) captains the nav boat

The main contributions of our NASA Exploration Analogs and Mission Development team (EAMD) are to perform the operational research necessary to characterize the productivity and effectiveness of the operation and then systematically analyze the data and use the results to refine the operational methods over a multi-year period with the aim of achieving the highest level of scientific return from the human and machine assets deployed during the expedition.  To this end we have developed a variety of metrics that characterize the data, and observation quality along with the operational performance and timeline data.  These metrics are then correlated with the scientific merit metrics that we have developed with the PLRP team to understand the right balance between operational discipline and scientific flexibility. Is the right answer going to be totally rigid flight plans and flight rules to control every minute or the exploration dives, or complete scientific flexibility to explore whatever seems most interesting at the time? Probably neither,  the optimal mix is most likely  somewhere in between and this multi-year research program provides a unique opportunity to find that optimal mix here on earth so that we don’t have to learn those lesson out in space were the expense and consequences are much higher.

-Mike

Mike Gernhardt, ready for deployment in DeepWorker.