Instrument Information |
|
IDENTIFIER | urn:nasa:pds:context:instrument:lr2.vl2::1.0 |
NAME |
LABELED RELEASE |
TYPE |
REGOLITH PROPERTIES |
DESCRIPTION |
Instrument Overview =================== Each Viking Lander had identical Labeled Release (LR) instruments that used two solid-state beta detectors (Geiger counters) to measure the release of radioactive gas from samples of martian soil that had been inoculated with an aqueous nutrient solution. The instrument contained additional sensors to measure headspace (i.e, the volume of test chamber above the sample) and detector temperatures. Heaters were also included in the LR instrument for the detectors and test chambers. A number of published papers describe the characteristics and performance of the LR instrument. The scientific rationale and early design of the instrument are described in LEVIN1972 and a detailed description of the flight module is given in LEVIN&STRAAT1976A. A summary of the information from these papers is given here as a high-level description of the LR instrument and its operation. The Labeled Release instrument was part of a package of three biology experiments on the Viking Landers [KLEIN1974]. Science Objectives ================== The major scientific objectives of the Viking Lander biology investigation were to detect the plausibility and/or presence of life on Mars. In particular, the LR experiment was designed to detect microbial life in the martian soil. The Labeled Release experiment tested for heterotrophic metabolism by monitoring the release of radioactive gases from a soil sample inoculated with carbon-14 labeled organic substrates. The experiment also was designed to analyze control samples that were heat sterilized. Several assumptions were used in the design and operation of the Labeled Release experiment. These assumptions included the following: A) life on Mars was carbon based; B) one or more of the nutrient compounds would be metabolized by possible microbial life; and C) one end product of metabolism would be a carbon based gas. LR Detailed Description ======================= The Labeled Release instrument contained four incubation test cells mounted on a carousel. Each test cell could be rotated and sealed beneath an assembly that contained a heater, plumbing terminals for nutrient delivery and gas removal, and a tube leading to the beta detectors. Gas and nutrient moving through the plumbing system were controlled by eight miniaturized solenoid valves. The headspace was connected to the two solid-state beta detectors through a tube bent at several spots. The connecting tube was bent to prevent radioactive particles from reaching the detectors from the test cell. The instrument also had two temperature sensors. One sensor measured the temperature of the detectors and the other measured the temperature of the headspace within the test cell. For a schematic and photographs of the Labeled Release instrument see LEVIN&STRAAT1976A. The Labeled Release nutrient was stored in a sealed glass ampoule within a reservoir. The reservoir, in turn, was connected to the test cells by the instrument plumbing system. The ampoule containing the nutrient was broken by a mechanical striker driven by high pressure helium shortly after the spacecraft landed on the surface of Mars. Low pressure helium was then bubbled through the nutrient in the reservoir for several hours in order to degas the nutrient. At the start of an analysis cycle high pressure helium was used to route a portion of the nutrient into a sealed test cell. Testing prior to launch indicated that 0.115 cc +/- 8% of nutrient was delivered during each injection. The pressure in the test cell headspace was kept above Mars ambient atmospheric pressure with helium from the plumbing system to prevent boiling of the nutrient. The total pressure at the start of an analysis cycle was about 9200 Pa (92 millibar). At the end of an analysis cycle, radioactive gas was purged from the test cell through the plumbing system. The LR instrument had two identical solid-state beta detectors (Geiger counters) to monitor the evolved radioactive gas from the soil sample. There were two detectors as a contingency against failure of one detector. The detectors continuously counted gaseous radioactivity as it evolved from the test cell. The instrument could be commanded to count with either one or both detectors. Detectors were referred to as the right and left channels. The Viking Landers were powered by radioisotope thermoelectric generators (RTGs), which provided background radiation to the detectors. As a result, this background signal had to be determined by monitoring the detectors for one to several Mars days before nutrient was injected into a test cell. The test cell heaters were used in a number of ways. Samples could be heated in the test cell prior to nutrient injections to provide sterilized control samples. During an analysis cycle the test cell was heated to prevent the temperature from falling below 9-10 degree C during the martian night. The heater was also used at the end of an analysis cycle to dry the sample. The Labeled Release instrument shared common support services with the other biology instruments. This included the sample delivery system [KLEIN1974]. Martian soil samples were collected by the Viking Lander surface sampler arm [MOOREETAL1987; CROUCH1977]. Soil from the sampler arm was dumped into a hopper on top of the lander. The hopper contained a sieve that only allowed particles less than 2 mm in size to enter the instrument test cells. The sieved samples entered a distribution assembly that automatically delivered measured volumes of soil to each biology experiment [KLEIN1974]. The Labeled Release instrument typically received 0.5 cc of soil. The Biology common support services and the Labeled Release instrument held enough nutrient and helium to conduct up to two injections on four soil samples. Testing prior to launch showed that after proper drying of a soil sample and purging of gases from a test cell that the cell could be used a second time by adding more soil and nutrient. One of the test cells on Viking Lander 2 was used a second time. Nutrient Description ==================== Considerable effort went into selecting, preparing, and testing the nutrients for the Label Release experiment [LEVIN&STRAAT1976A]. Selection criteria were partially based on the assumption that life evolved similarly on Mars as on Earth. There were several criteria used in selecting compounds for the nutrient that included: A) Compounds that were likely to be produced on Mars; B) Compounds that primitive organisms were likely to use in metabolism based on terrestrial analogs; and C) Compounds that were unlikely to have nonbiological reactions with martian soil. In addition, each compound in the nutrient was tested to show that it produced a rapid response in a variety of terrestrial soils and in cultures of several types of organisms. The stability of the materials was also considered given that the nutrient was stored for about 2 years from the time it was prepared until it was used on Mars. The storage period included the nearly one year cruise phase of the spacecraft on its journey to Mars. Nutrient material also had to undergo sterilization of the biology module (54 hr at 120 degree C) and the entire spacecraft (20 hr at 100 degree C). It was expected that some decomposition (<1%) of the nutrient would occur due to the long storage time and sterilization. Any radioactive carbon dioxide produced by the nutrient decomposition was removed by flushing the nutrient reservoir with helium before the first injection. A complete list of nutrient compounds is given in LEVIN&STRAAT1976A. The nutrient included sodium formate, calcium glycolate, glycine, D- and L-alanine, sodium D-lactate and sodium L-lactate. The concentrations of each nutrient component were dilute in case any particular compound was toxic to possible martian organisms. Each compound in the nutrient was labeled with a precise amount of radioactive carbon-14. Operation and Sampling Modes ============================ The basic analysis cycle for the Labeled Release experiment was to have a sample of martian soil delivered to a test cell and to be moistened with an aqueous solution of carbon-14 labeled organic media. A second nutrient injection was typically done about 7-8 Mars days after the first injection. The headspace above the sample was monitored continuously for evolved radioactive gas as evidence for metabolism. Viking Lander 1 completed four cycles, whereas Viking Lander 2 completed five cycles for a total of nine cycles between the two landers. VL2 cycle 5 was performed in a previously used test cell using a stored portion of the cycle 4 soil sample. Eight of the cycles received two injections of nutrient. VL1 cycle 3 received three injections of nutrient. Three of the analysis cycles were control cycles where the soil sample was heated for several hours before nutrient injection. The control cycle for Viking Lander 1 was heated to 160 degree C. After receiving highly attenuated results from Viking Lander 1, Viking Lander 2 control cycles were modified to be 50 degree C. Radioactivity was counted for 16-minute intervals during an analysis cycle, except for several hours around the time of nutrient injection where intervals of 2- to 4-minutes were used. Background levels were determined by measuring the test cell for several Mars days prior to nutrient injection. The headspace and detector temperatures were measured every 16 minutes throughout an analysis cycle. At the end of the cycle, the radioactive gas was removed by purging and the soil was dried by brief heating to prevent evaporation upon opening the cell. A fresh test cell was then rotated beneath the head end assembly and a three-hour cleanup was accomplished by heating both the head assembly and detectors during continuous helium purging. After cooling, trapped nutrient was vented from the system. The instrument was fairly automated with preprogrammed sequences. Commands could be sent from the ground to change the preprogrammed sequences to perform nutrient injections, to select active or control sequences, to select a fresh soil sample, and to initiate or terminate an analysis cycle. Commands could be sent to conduct single or double channel counting. Principal Investigator ====================== The principal investigator for the Viking Lander Labeled Release experiment was Dr. Gilbert V. Levin of Biospherics, Inc. Much of the work on selecting the nutrient was directed by Co-Investigator Dr. Patricia Ann Straat. |
MODEL IDENTIFIER | |
NAIF INSTRUMENT IDENTIFIER |
not applicable |
SERIAL NUMBER |
not applicable |
REFERENCES |
Crouch, D.S., Mars Viking surface sampler subsystem, Proc. 25th Conf.
Remote Sens. Tech., The American Nuclear Society, Anniverssary issue,
141-152, 1977. Klein H.P., Automated life-detection experiments for the Viking Mission to Mars, Origins of Life, 5, 431-441, 1974. Levin, G. V., and P.A. Straat, Labeled Release - An experiment in radiorespirometry, Origins of Life, 7, 293-311, 1976. Levin, G.V., Detection of Metabolically produced labeled gas: The Viking Mars Lander, Icarus, 16,153-166, 1972. Moore, H.J., R.E. Hutton, G.D. Clow, and C.R. Spitzer, Physical properties of the surface materials at the Viking landings sites on Mars, USGS Professional Paper 1389, 1987. |