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1.
Adv Space Res ; 34(7): 1546-51, 2004.
Article in English | MEDLINE | ID: mdl-15846884

ABSTRACT

A major challenge of designing a bioregenerative life support system for Mars is the reduction of the mass, volume, power, thermal and crew-time requirements. Structural mass of the greenhouse could be saved by operating the greenhouse at low atmospheric pressure. This paper investigates the feasibility of this concept. The method of equivalent system mass is used to compare greenhouses operated at high atmospheric pressure to greenhouses operated at low pressure for three different lighting methods: natural, artificial and hybrid lighting.


Subject(s)
Ecological Systems, Closed , Life Support Systems , Lighting , Mars , Air Conditioning , Atmospheric Pressure , Facility Design and Construction , Hot Temperature , Light , Plants, Edible/growth & development , Radiation Protection , Sunlight
2.
Agron J ; 92(2): 353-60, 2000.
Article in English | MEDLINE | ID: mdl-11543523

ABSTRACT

Hydroponic culture has traditionally been used for controlled environment life support systems (CELSS) because the optimal environment for roots supports high growth rates. Recent developments in zeoponic substrate and microporous tube irrigation (ZPT) also offer high control of the root environment. This study compared the effect of differences in water and nutrient status of ZPT or hydroponic culture on growth and yield of wheat (Triticum aestivum L. cv. USU-Apogee). In a side-by-side test in a controlled environment, wheat was grown in ZPT and recirculating hydroponics to maturity. Water use by plants grown in both culture systems peaked at 15 to 20 L m-2 d-1 up to Day 40, after which it declined more rapidly for plants grown in ZPT culture due to earlier senescence of leaves. No consistent differences in water status were noted between plants grown in the two culture systems. Although yield was similar, harvest index was 28% lower for plants grown in ZPT than in hydroponic culture. Sterile green tillers made up 12 and 0% of the biomass of plants grown in ZPT and hydroponic culture, respectively. Differences in biomass partitioning were attributed primarily to NH4-N nutrition of plants grown in ZPT compared with NO3-N in hydroponic nutrient solution. It is probable that NH4-N-induced Ca deficiency produced excess tillering and lower harvest index for plants grown in ZPT culture. These results suggest that further refinements in zeoponic substrate would make ZPT culture a viable alternative for achieving high productivity in a CELSS.


Subject(s)
Culture Media/metabolism , Hydroponics , Triticum/growth & development , Water/metabolism , Zeolites/metabolism , Biomass , Calcium/deficiency , Culture Media/pharmacokinetics , Ecological Systems, Closed , Environment, Controlled , Fertilizers , Germination , Life Support Systems , Nutritional Requirements , Quaternary Ammonium Compounds/pharmacokinetics , Triticum/metabolism , Zeolites/pharmacokinetics
3.
Adv Space Res ; 20(10): 1861-7, 1997.
Article in English | MEDLINE | ID: mdl-11542562

ABSTRACT

The variable pressure growth chamber (VPGC) was used in a 34-day functional test to grow a wheat crop using reduced pressure (70 kPa) episodes totalling 131 hours. Primary goals of the test were to verify facility and subsystem performance at 70 kPa and to determine responses of a wheat stand to reduced pressure and modified partial pressures of carbon dioxide and oxygen. Operation and maintenance of the chamber at 70 kpa involved continuous evacuation of the chamber atmosphere, leading to CO2 influx and efflux. A model for calculating CO2-exchange rates (net photosynthesis and dark respiration) was developed and tested and involved measurements of chamber leakage to determine appropriate corrections. Measurement of chamber leakage was based on the rate of pressure change over a small pressure increment (70.3 to 72.3 kPa) with the pump disabled. Leakage values were used to correct decreases and increases in chamber CO2 concentration resulting from net photosynthesis (Ps) and dark respiration (DR), respectively. Composite leakage corrections (influx and efflux) at day 7 of the test were 9% and 19% of the changes measured for Ps and DR, respectively. On day 33, composite corrections were only 3% for Ps and 4% for DR. During the test, the chamber became progressively tighter; the leak rate at 70.3 kPa decreasing from 2.36 chamber volumes/day pretest, to 1.71 volumes/day at the beginning of the test, and 1.16 volumes/day at the end of the test. Verification of the short-term leakage tests (rate of pressure rise) were made by testing CO2 leakage with the vacuum pump enabled and disabled. Results demonstrate the suitability of the VPGC or conducting gas exhange measurements of a crop stand at reduced pressure.


Subject(s)
Atmospheric Pressure , Carbon Dioxide/metabolism , Environment, Controlled , Triticum/growth & development , Air Conditioning , Cell Respiration , Darkness , Evaluation Studies as Topic , Oxygen , Partial Pressure , Photosynthesis , Triticum/metabolism
4.
Adv Space Res ; 20(10): 1869-77, 1997.
Article in English | MEDLINE | ID: mdl-11542563

ABSTRACT

A 34-day functional test was conducted in Johnson Space Center's Variable Pressure Growth Chamber (VPGC) to determine responses of a wheat stand to reduced pressure (70 kPa) and modified partial pressures of carbon dioxide and oxygen. Reduced pressure episodes were generally six to seven hours in duration, were conducted at reduced ppO2 (14.7 kPa), and were interrupted with longer durations of ambient pressure (101 kPa). Daily measurements of stand net photosynthesis (Pn) and dark respiration (DR) were made at both pressures using a ppCO2 of 121 Pa. Corrections derived from leakage tests were applied to reduced pressure measurements. Rates of Pn at reduced pressure averaged over the complete test were 14.6% higher than at ambient pressure, but rates of DR were unaffected. Further reductions in ppO2 were achieved with a molecular sieve and were used to determine if Pn was enhanced by lowered O2 or by lowered pressure. Decreased ppO2 resulted in enhanced rates of Pn, regardless of pressure, but the actual response was dependent on the ratio of ppO2/ppCO2. Over the range of ppO2/ppCO2 of 80 to 200, the rate of Pn declined linearly. Rate of DR was unaffected over the same range and by dissolved O2 levels down to 3.1 ppm, suggesting that normal rhizosphere and canopy respiration occur at atmospheric ppO2 levels as low as 11 kPa. Partial separation of effects attributable to oxygen and those related to reduced pressure (e.g. enhanced diffusion of CO2) was achieved from analysis of a CO2 drawdown experiment. Results will be used for design and implementation of studies involving complete crop growth tests at reduced pressure.


Subject(s)
Atmospheric Pressure , Carbon Dioxide/metabolism , Environment, Controlled , Oxygen/metabolism , Photosynthesis/physiology , Triticum/metabolism , Biomass , Cell Respiration , Darkness , Humans , Life Support Systems , Partial Pressure , Plant Transpiration , Triticum/growth & development
5.
Plant Cell Environ ; 20(12): 1506-16, 1997 Dec.
Article in English | MEDLINE | ID: mdl-11541524

ABSTRACT

Water transport through a microporous tube-soil-plant system was investigated by measuring the response of soil and plant water status to step change reductions in the water pressure within the tubes. Soybeans were germinated and grown in a porous ceramic 'soil' at a porous tube water pressure of -0.5 kpa for 28 d. During this time, the soil matric potential was nearly in equilibrium with tube water pressure. Water pressure in the porous tubes was then reduced to either -1.0, -1.5 or -2.0 kPa. Sap flow rates, leaf conductance and soil, root and leaf water potentials were measured before and after this change. A reduction in porous tube water pressure from -0.5 to -1.0 or -1.5 kPa did not result in any significant change in soil or plant water status. A reduction in porous tube water pressure to -2.0 kPa resulted in significant reductions in sap flow, leaf conductance, and soil, root and leaf water potentials. Hydraulic conductance, calculated as the transpiration rate/delta psi between two points in the water transport pathway, was used to analyse water transport through the tube-soil-plant continuum. At porous tube water pressures of -0.5 to-1.5 kPa soil moisture was readily available and hydraulic conductance of the plant limited water transport. At -2.0 kPa, hydraulic conductance of the bulk soil was the dominant factor in water movement.


Subject(s)
Glycine max/metabolism , Hydroponics/methods , Plant Transpiration/physiology , Soil , Water/metabolism , Biological Transport , Biomass , Ceramics , Hydroponics/instrumentation , Hydrostatic Pressure , Osmosis , Particle Size , Plant Leaves/growth & development , Plant Leaves/metabolism , Plant Leaves/physiology , Plant Roots/growth & development , Plant Roots/metabolism , Plant Roots/physiology , Glycine max/growth & development , Glycine max/physiology
6.
Adv Space Res ; 18(1-2): 211-21, 1996.
Article in English | MEDLINE | ID: mdl-11538966

ABSTRACT

The Regenerative Life Support Systems (RLSS) Test Bed at NASA's Johnson Space Center is an atmospherically closed, controlled environment facility for human testing of regenerative life support systems using higher plants in conjunction with physicochemical life support systems. The facility supports NASA's Advanced Life Support (ALS) Program. The facility is comprised of two large scale plant growth chambers, each with approximately 11 m2 growing area. The root zone in each chamber is configurable for hydroponic or solid media plant culture systems. One of the two chambers, the Variable Pressure Growth Chamber (VPGC), is capable of operating at lower atmospheric pressures to evaluate a range of environments that may be used in a planetary surface habitat; the other chamber, the Ambient Pressure Growth Chamber (APGC) operates at ambient atmospheric pressure. The air lock of the VPGC is currently being outfitted for short duration (1 to 15 day) human habitation at ambient pressures. Testing with and without human subjects will focus on 1) integration of biological and physicochemical air and water revitalization systems; 2) effect of atmospheric pressure on system performance; 3) planetary resource utilization for ALS systems, in which solid substrates (simulated planetary soils or manufactured soils) are used in selected crop growth studies; 4) environmental microbiology and toxicology; 5) monitoring and control strategies; and 6) plant growth systems design. Included are descriptions of the overall design of the test facility, including discussions of the atmospheric conditioning, thermal control, lighting, and nutrient delivery systems.


Subject(s)
Ecological Systems, Closed , Environment, Controlled , Life Support Systems/instrumentation , Plant Development , Atmospheric Pressure , Computer Systems , Equipment Design , Evaluation Studies as Topic , Facility Design and Construction , Humans , Hydroponics/instrumentation , Light , Space Simulation , Systems Integration , United States , United States National Aeronautics and Space Administration
7.
Adv Space Res ; 18(1-2): 223-32, 1996.
Article in English | MEDLINE | ID: mdl-11538967

ABSTRACT

Future NASA missions to explore the solar system will be long-duration missions, requiring human life support systems which must operate with very high reliability over long periods of time. Such systems must be highly regenerative, requiring minimum resupply, to enable the crews to be largely self-sufficient. These regenerative life support systems will use a combination of higher plants, microorganisms, and physicochemical processes to recycle air and water, produce food, and process wastes. A key step in the development of these systems is establishment of a human-rated test facility specifically tailored to evaluation of closed, regenerative life supports systems--one in which long-duration, large-scale testing involving human test crews can be performed. Construction of such a facility, the Advanced Life Support Program's (ALS) Human-Rated Test Facility (HRTF), has begun at NASA's Johnson Space Center, and definition of systems and development of initial outfitting concepts for the facility are underway. This paper will provide an overview of the HRTF project plan, an explanation of baseline configurations, and descriptive illustrations of facility outfitting concepts.


Subject(s)
Ecological Systems, Closed , Environment, Controlled , Ergonomics , Facility Design and Construction , Life Support Systems , Program Evaluation , Air Conditioning , Electronic Data Processing , Evaluation Studies as Topic , Humans , Systems Integration , United States , United States National Aeronautics and Space Administration , Waste Management , Water
8.
Soil Sci Soc Am J ; 59(1): 248-55, 1995.
Article in English | MEDLINE | ID: mdl-11539131

ABSTRACT

Nutrient release in clinoptilolite-phosphate rock (Cp-PR) systems occurs through dissolution and cation-exchange reactions. Investigating the kinetics of these reactions expands our understanding of nutrient release processes. Research was conducted to model transport kinetics of nutrient release in Cp-PR systems. The objectives were to identify empirical models that best describe NH4, K, and P release and define diffusion-controlling processes. Materials included a Texas clinoptilolite (Cp) and North Carolina phosphate rock (PR). A continuous-flow thin-disk technique was used. Models evaluated included zero order, first order, second order, parabolic diffusion, simplified Elovich, Elovich, and power function. The power-function, Elovich, and parabolic-diffusion models adequately described NH4, K, and P release. The power-function model was preferred because of its simplicity. Models indicated nutrient release was diffusion controlled. Primary transport processes controlling nutrient release for the time span observed were probably the result of a combination of several interacting transport mechanisms.


Subject(s)
Nitrogen/chemistry , Soil/analysis , Zeolites/chemistry , Calcium/chemistry , Cation Exchange Resins , Crops, Agricultural , Culture Media , Diffusion , Fertilizers , Geological Phenomena , Geology , Models, Chemical , Phosphates/chemistry , Potassium/chemistry , Quaternary Ammonium Compounds/chemistry
9.
Adv Space Res ; 14(11): 403-10, 1994 Nov.
Article in English | MEDLINE | ID: mdl-11540213

ABSTRACT

Human exploration of the solar system will include missions lasting years at a time. Such missions mandate extensive regeneration of life support consumables with efficient utilization of local planetary resources. As mission durations extend beyond one or two years, regenerable human life support systems which supply food and recycle air, water, and wastes become feasible; resupply of large volumes and masses of food, water, and atmospheric gases become unrealistic. Additionally, reduced dependency on resupply or self sufficiency can be an added benefit to human crews in hostile environments far from the security of Earth. Comparisons of resupply and regeneration will be discussed along with possible scenarios for developing and implementing human life support systems on the Moon and Mars.


Subject(s)
Conservation of Natural Resources , Ecological Systems, Closed , Life Support Systems/instrumentation , Space Flight/economics , Air Conditioning/methods , Facility Design and Construction , Humans , Life Support Systems/economics , Mars , Moon , Space Flight/instrumentation , Spacecraft/instrumentation , Waste Management/methods
10.
Adv Space Res ; 14(11): 435-43, 1994.
Article in English | MEDLINE | ID: mdl-11538023

ABSTRACT

Regenerative Life Support Systems (RLSS) will be required to regenerate air, water, and wastes, and to produce food for human consumption during long-duration missions to the Moon and Mars. It may be possible to supplement some of the materials needed for a lunar RLSS from resources on the Moon. Natural materials at the lunar surface may be used for a variety of lunar RLSS needs, including (i) soils or solid-support substrates for plant growth, (ii) sources for extraction of essential, plant-growth nutrients, (iii) substrates for microbial populations in the degradation of wastes, (iv) sources of O2 and H2, which may be used to manufacture water, (v) feed stock materials for the synthesis of useful minerals (e.g., molecular sieves), and (vi) shielding materials surrounding the outpost structure to protect humans, plants, and microorganisms from harmful radiation. Use of indigenous lunar regolith as a terrestrial-like soil for plant growth could offer a solid support substrate, buffering capacity, nutrient source/storage/retention capabilities, and should be relatively easy to maintain. The lunar regolith could, with a suitable microbial population, play a role in waste renovation; much like terrestrial waste application directly on soils. Issues associated with potentially toxic elements, pH, nutrient availability, air and fluid movement parameters, and cation exchange capacity of lunar regolith need to be addressed before lunar materials can be used effectively as soils for plant growth.


Subject(s)
Agriculture/trends , Ecological Systems, Closed , Life Support Systems , Moon , Soil/analysis , Agriculture/methods , Extraterrestrial Environment , Fertilizers , Forecasting , Geological Phenomena , Geology , Minerals/analysis , Plant Development , Soil Microbiology
11.
Soil Sci Soc Am J ; 57(5): 1368-74, 1993.
Article in English | MEDLINE | ID: mdl-11537990

ABSTRACT

Mixtures of zeolite and phosphate rock (PR) have the potential to provide slow-release fertilization of plants in synthetic soils by dissolution and ion-exchange reactions. This study was conducted to examine solubility and cation-exchange relationships in mixtures of PR and NH4- and K-saturated clinoptilolite (Cp). Batch-equilibration experiments were designed to investigate the effect of PR source, the proportion of exchangeable K and NH4, and the Cp to PR ratio on solution N, P, K, and Ca concentrations. The dissolution and cation-exchange reactions that occurred after mixing NH4- and K-saturated Cp with PR increased the solubility of the PR and simultaneously released NH4 and K into solution. The more reactive North Carolina (NC) PR rendered higher solution concentrations of NH4 and K when mixed with Cp than did Tennessee (TN) PR. Solution P concentrations for the Cp-NC PR mixture and the Cp-TN PR mixture were similar. Solution concentrations of N, P, K, and Ca and the ratios of these nutrients in solution varied predictably with the type of PR, the Cp/PR ratio, and the proportions of exchangeable K and NH4 on the Cp. Our research indicated that slow-release fertilization using Cp/PR media may provide adequate levels of N, P, and K to support plant growth. Solution Ca concentrations were lower than optimum for plant growth.


Subject(s)
Cation Exchange Resins/chemistry , Phosphates/chemistry , Quaternary Ammonium Compounds/chemistry , Zeolites/chemistry , Calcium/chemistry , Fertilizers/analysis , Nitrogen/chemistry , Nutritional Requirements , Phosphorus/chemistry , Plant Development , Potassium/chemistry , Soil/analysis , Solubility , Time Factors
12.
Endeavour ; 15(2): 79-85, 1991.
Article in English | MEDLINE | ID: mdl-11537088

ABSTRACT

America's long-term commitment to a new Space Exploration Initiative has focused attention on the basic requirements for establishing a permanently manned lunar outpost and, ultimately, a martian one. High among these is the development of Regenerative Life Support Systems--with lunar agriculture an essential component--to provide a high level of self-sufficiency.


Subject(s)
Ecological Systems, Closed , Extraterrestrial Environment , Moon , Plants, Edible/growth & development , Space Flight/trends , Agriculture/trends , Environment Design , Forecasting , Humans , Life Support Systems , Minerals , Soil/analysis , Space Flight/instrumentation , United States , United States National Aeronautics and Space Administration
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