kai

For better or for worse, all modern homes, offices, and classrooms are fairly tightly enclosed to reduce energy loss. This results in greater than outdoor ambient carbon dioxide levels, higher than most people realize. With ambient global CO2 at 420 parts per million (ppm) it is not unusual for an indoor, occupied space to be well over 1000 ppm, sometimes 1500, 2500, or more. Offices, classrooms, conference halls, even your dining room with a family gathering are in these higher ranges for extended periods of time.

OSHA suggests that the upper, safe limit is exposure to 5000 ppm for up to 8 hours. The International Space Station operates between 3000 and 6500 ppm. And the US Navy submarines are unconfirmed to operated as high as 10,000 ppm. There is little evidence to suggest that any short- or long-term health issues are associated with the upper ranges of CO2 for brief (a few hours) exposures. The astronauts on the ISS live with 5000 ppm for up to a year. While some research shows reduced cognitive function (e.g. math problem solving), there are is no risk of long term damage.

As SAM is hermetically sealed, we must monitor the CO2 levels even more carefully than in our homes, schools, and places of work. While an office might rise over 1500 on a frequent basis, the door is likely being opened, with people moving in and out with the effect of mixing the air.

For these first two mission, SAM is operating in Mode 2 (pressurized, flow-through). The crew is able to adjust valves in the Test Module, airlock and crew quarters and then the speed of the in-bound blower. The combination of the two affects the overall carbon dioxide in SAM.

Crew Inclusion I reached out on Day 2 with concern for the rising CO2. Director of Research Kai Staats logged into the SIMOC Live server to retrieve the data to that moment. SIMOC Live captures carbon dioxide, oxygen, relative humidity, temperature, pressure, and a number of other values for the duration of the mission. This data is exported to a local .csv file which the SIMOC-SAM team members can copy through a data backdoor that bypasses the router which limits crew to email only.

As with all time-series data, it takes a full cycle (in this case day-night-day) to recognize a trend. Indeed, the initial rise in CO2 climbed over 2500. This is nothing to be concerned about, but the crew wanted to bring it down, in part to demonstrate their ability to control the quality of air.

Crew Inclusion I worked extensively with SAM Mission Control to monitor and maintain the carbon dioxide levels. Crew engineer Bailey Burns conducted spot assessments of CO2 throughout the habitat while the SIMOC Live sensor array was capturing a time series dataset from closure to the end of the mission. Bailey’s data confirmed the air flow from SAM Lung to TM to Engineering Bay to Crew Quarters with an increasing density of carbon dioxide.

Mission Control advised that the sound muffler be removed from the outlet at the end of the crew quarters and an additional port be opened in the airlock. While the airlock is not at the termination of the designated airflow path, it does invoke the need to increase the blower in order to keep the lung at a nominal height, and therefore is in fact moving more air with the effect of bringing overall CO2 levels down.

In response to the crew’s request for assistance, acting CapCom Kai Staats wrote, “You have done well to reduce your carbon dioxide over the past two days. You started at roughly 700 ppm (due to all the activity inside SAM prior to entry) and rose to nearly 3000 ppm which is when you reached out for guidance. The day/night activity/sleep cycle is clearly present with a leveling of CO2 while you sleep. But overall, the trend has been down with a reading this morning of just under 1000 ppm. According to the data, you rose at 6 am.”

(see plot above for associated data points and graphical narrative)

The temperature held relatively steady, between 20 and 25C, with a dip to 16C the first night. The relative humidity ranges from 30% to 70%, clearly following a day/night cycle. This is due to “relative” humidity as a measure of moisture in the context of changing temperature, and therefore density of air. But is also due to the fact that at night the A/C units stop running their condensers, therefore the dehumidification function terminates and the humidity rises until the temperature is again high enough to activate the cooling cycle.

In the end, Crew Inclusion I was able to control their CO2 levels effectively (as demonstrated in the graph above). Given initial concerns for CO2 levels, the SAM team now realizes the importance of asking our visiting research crew to reduce their caffeine and processed sugar intake prior to arrival to SAM.

The SIMOC developer team is preparing to open source the entire platform, from back-end server to front-end web client so that developers, educators, and citizen scientists too can benefit from this unique, powerful agent-based model and simulation around the world, for free.

Stay tuned!

by Grant Hawkins, lead developer for SIMOC B2 at Over the Sun, LLC

The final step of integrating Biosphere 2 into SIMOC was validating the outputs. From the beginning, we’ve focused on telling the story of oxygen depletion during Mission 1, as described in the paper Oxygen Loss in Biosphere 2, published in 1994. This paper describes the overall O2 and CO2 behavior within B2 for the first ~18 months of Mission 1, as well as the rates of O2 and CO2 consumption and production for key agents such as the concrete and soil.

First, we compared overall levels of O2 and CO2 throughout the mission:

We also compared net effects of processes specified in the paper:

These figures help us identify where the model is reliable, and where it needs to be improved. Below is the ‘Discussion’ section of a paper we’ve written on this process:

The results of the simulation are directionally accurate, but with a low degree of precision. Relatively few measurements of plant productivity are available from the B2 experiments, and SIMOC’s other validation reference is a highly dissimilar experiment. To improve precision of the plant model, we make the following recommendations:

• Include fruit trees and other perennial plants in addition to vegetables. These made up a large part of the B2 crew’s actual diet, and follow a different growth cycle.
• Model the impact of specific pests and parasites. As records allow, match periods of low productivity for specific plants with their causes – most often fungi or mites. In the case of corn, no edible food was produced in Mission 1a and 1b because it is wind-pollinated, and there was no wind inside the structure. This and other species-specific behaviors could increase the accuracy as well as the educational potential of SIMOC.
• Include some metric of human wellness besides simple survival. Some of the difference in plant productivity between Missions 1 and 2 can be attributed to crew energy levels and morale. Taking into account nutrition, workload, variety of diet, etc. and giving an overall indication of crew’s well-being will be useful in optimizing these systems, and for making the simulations more engaging.

Despite this imprecision, the measured system-level behaviors of the B2 missions are observable in the simulation. By making adjustments the base configurations, users can also observe the following phenomena:

• Plant growth can be increased by adding supplemental lighting (at the cost of increased electric consumption), or decreased by reducing CO2 setpoint to <700ppm.
• Crop layouts can be adjusted to add higher-yield crops, or crops which transpire and photosynthesize at different rates, affecting overall gas balances.
• The starting concrete carbonation rate can be adjusted, which affects the rate at which it consumes CO2. This is also affected by the ambient CO2 levels, with lower rates of carbonation when CO2 levels are lower.
• Adjusting the areas of each biome impacts (1) the size of the air sink, and therefore the overall changes in concentrations, (2) O2 and CO2 exchanges, as each biome has a different rate.

In completion of a seven months development endeavor, a simulation of the original and second missions at Biosphere 2 are now incorporated into SIMOC and available for free from the National Geographic Society’s educational web portal.

The intent of SIMOC is to provide a model of Biological Life Support Systems for human space exploration. SIMOC was originally built around an ideal plant growth scenario (NASA CELSS growth chamber experiments and the NASA BVAD document), and was calibrated so that the simulation reproduced similar outcomes as given in published NASA experiments. The reality of a Moon or Mars habitat will be less than ideal, where the original Biosphere 2 missions are likely a closer approximation to how things might actually play out.

SIMOC B2 adds new degrees of freedom to the plant model (light response, planting density, crop management) as well as other new agents (concrete, biomes) such that the model reproduces experimental data from both NASA CELSS and the original Biosphere 2 missions with a single model. We attribute the large differences in plant productivity (up to 10x) and validate the system-level outputs against experimental B2 data.

By calibrating the model to these two extremes, we’re granting researchers, students and citizen scientists greater insight into the historical data from both and an opportunity to evaluate and compare a wider range of different BLSS scenarios with higher accuracy.

by Grant Hawkins, lead developer for SIMOC B2 at Over the Sun, LLC

The final step of integrating Biosphere 2 into SIMOC was building the configuration files, which specify how many of each agent to include in a simulation, their starting resource balances, etc. Our aim was to replicate the real-life Biosphere 2 experiments: Mission 1 (September 26, 1991 to September 26, 1993) and Mission 2 (March 6, 1994 to September 7, 1994).

There was a major non-linearity in Mission 1 of course, which was the extra oxygen added to the habitat, beginning on January 12, 1993, 475 days into Mission 1. Some other changes were made throughout the experiment, such as adjusting the planting areas of different crops to maximize calorie-production and CO2-sequestration. To account for this, we split Mission 1 into two configurations: Mission 1a for before the O2 was added, and Mission 1b for after O2 was added. The configuration of 1b starts with the final atmosphere and concrete carbonation of Mission 1a, and includes an O2 resupply system and modified greenhouse layout.

The feature of significance for Mission 2 was improved plant productivity. We spoke with Tilak Mahato, one of the crew member on Mission 2 usually credited with improving output, and currently a researcher of Controlled Environment Agriculture at the University of Arizona. He described several specific practices that improved output:

• Removing pests immediately. Because pest populations grow so quickly, catching and remediating an infestation early has an outsized impact.
• Taking care not spread pests, fungi or diseases via contaminated tools.
  Washing diseased leaves with soap and water.
• Protect seedling growing areas from roaches and other pests.
• Pollinating plants by hand. During Mission 1, the entire corn crop had failed to produce food because there was no wind to spread pollen from the (male) tassels to the (female) silk. Other plants’ pollen had been washed away by overhead irrigation.

There was no ‘primary’ factor, according to Tilak, to which the improvements in productivity could be attributed. For this reason, we added a simple field to SIMOC, ‘Improved Crop Management’, which increases productivity of the plants by 50%, and describe the specific processes above in the SIMOC web app.

The result of these 3 configurations is encouraging so far!

by Grant Hawkins, lead developer for SIMOC B2 at Over the Sun, LLC

Storytelling is a core part of SIMOC, especially when it comes to the educational components. As we integrate Biosphere 2 into SIMOC, we’re focused on telling one story in particular: how the soil and concrete conspired to crash O2 levels during Mission 1.

This story was first told in a research paper from January 1994, Oxygen Loss in Biosphere 2. Over the course of Mission 1, the O2 level in the habitat fell quickly, but the CO2 levels didn’t show the expected corresponding rise. The obvious hypothesis is that there was an unaccounted-for O2 consumer. The paper showed that in fact two separate processes were more active than was expected: soil respiration, which consumed O2 and produced CO2, and concrete carbonation, which consumed CO2. The combined effect of both of these was the observed ‘O2 consumer’. We created 5 new agents in SIMOC – 1 concrete and 4 soil-containing biomes – and calibrated them to the measurements in the research paper.

The concrete agent models the process of carbonation. Each step of the simulation, carbonation occurs based on a diffusion rate and a saturation point. The saturation point is heavily dependent on the current CO2 concentration in the atmosphere, however, more than 10x higher under extreme conditions like those at Biosphere 2, which accounted for the unexpected difference in total uptake. We corresponded by email with Bill Dempster, an author of the paper above, about the problem and our approach to it.

The biomes model the combined effect of the soil and ground vegetation in the rainforest, savannah, desert and intensive agriculture biome (farm). A paper from 1999 measured the net productivity of the rainforest and desert biomes, and the Oxygen Loss in Biosphere 2 paper gives the habitat-wide soil respiration.

If all goes according to plan, the net effect of the humans, plants, concrete and biomes will be the drop in O2 observed in real life. This then becomes a story we can tell in SIMOC: the oxygen levels fall much faster than carbon dioxide rises, and the user can discover that it’s being ‘caused’ by the concrete and biomes.

by Grant Hawkins, lead developer for SIMOC B2 at Over the Sun, LLC

In mid-2022, our team took on the challenge of modeling Biosphere 2 (B2) in SIMOC. Beyond simply describing the outcomes and making sure that they match the published data, we also had to make sure that — The system and sub-systems responded correctly to changes in the configuration. When a user changes the area of sweet potatoes or the CO2 scrubber activation threshold, other agents are responding appropriately to those changes.

The sub-systems remain accurate on the original SIMOC validation data, the NASA CELSS growth-chamber experiments. There, plants were grown in highly-controlled environments in order to maximize their food productivity. For certain plants, the production rate in kg/m2-day was as much as 10x greater at CELSS than in Biosphere 2.

Light was found to be the biggest contributing factor to the differences in plant productivity. At CELSS, plants received constant-output electric lighting at an optimal level for an optimal number of hours per day. These ranged from 1.4 Mol/m2-h for 12 hours/day for rice, to 3.53 Mol/m2-h for 20 hours/day for wheat. At B2, the plants received whatever sunlight passed through the B2 windows and structural frame. Our approach was to use the CELSS data as the baseline for SIMOC plant consumption and production, and

The first step toward implementing SIMOC-B2 was to add a ‘light-response’ mechanism to the SIMOC plant agent. We added a new variable, ‘par_factor’, which scales the rate of biomass accumulation to the species-specific, hourly light requirement. The other functions of the plant (photosynthesis) are scaled to its total accumulated biomass, so the light response will be applied to those exchanges as well.

So this was a big step forward for the accuracy and flexibility of our plant growth model, but that wasn’t all. Some of the deeper changes to how exchange values are calculated led to a major reduction in memory footprint – more than 80% for simulations with more than one plant – which is great news for our cloud computing budget 🙂

The SIMOC development team has for the past six months been hard at work in developing two new versions of SIMOC: SIMOC B2 and SIMOC Live. SIMOC B2 is a new kind of simulation, a model of the first and second missions at Biosphere 2 in order to present citizen scientists with the tools to understand the challenges faced by the world’s largest and longest running human-in-the-loop bioregenerative experiment. SIMOC Live enables the real-time monitoring and capture of data from sensor arrays, such as those used to monitor carbon dioxide or oxygen levels, and other air quality measures.

We apologize for the lack of updates to this forum, but promise to catch-up (and back date) several stories soon!

This month brings new features and performance improvements. The migration to Vite is now complete, which has decreased startup time from around a minute to less than a second. A basic Kiosk mode is also now functional, and is being fine tuned.

Progress has been made on the Biosphere 2 simulation mode too, with new menus being developed such that a user can choose between whether they want to run a Mars simulation or a Biosphere 2 simulation, with corresponding visuals for each mode. New features are also being integrated into SIMOC’s model in order to account for factors that made the two Biosphere 2 experiments challenging, such as low light levels due to shadows cast by space frame and a year of heavy cloud cover in southern Arizona. The effect of pests and their role in the actual Biosphere 2 experiment are included, as well as a new agent to represent the concrete and associated carbon dioxide uptake.