Continuous monitoring of rhizosphere respiration after labelling of plant shoots with 14CO2

The present work describes an original method to follow rate of ¹⁴CO₂ and total CO₂ production from rhizosphere respiration after plant shoots had been pulse-labelled with ¹⁴CO₂. We used a radioactivity detector equipped with a plastic cell for flow detection of beta radiation by solid scintillation counting. The radioactivity detector was coupled with an infrared gas analyser. The flow detection of ¹⁴CO₂ was compared to trapping of ¹⁴CO₂ in NaOH and counting by liquid scintillation. First, we demonstrated that NaOH (1 M) trapped 95% of the CO₂ of a gaseous sample. Then, we determined that the counting efficiency of the radioactivity flow cell was 41% of the activity of gaseous samples as determined by trapping in NaOH (1 M) and by counting by static liquid scintillation. The sensitivity of the ¹⁴CO₂- flow detection was 0.08 Bq mL⁻¹ air and the precision was 2.9% of the activity measured compared to 0.9% for NaOH trapping method. We presented two applications which illustrate the relevance of ¹⁴CO₂-flow detection to investigations using 14C to trace photoassimilates within the plant-soil system. First, we examined the kinetics of 14CO₂ production when concentrated acid is added to NaH¹⁴CO₃. This method is the most commonly used to label photoassimilates with ¹⁴C. Then, we monitored ¹⁴CO₂ activity in rhizosphere respiration of 5-week old maize cultivated in soil and whose shoots had been pulse-labelled with ¹⁴CO₂. We conclude that alkali traps should be used for a cumulative determination of ¹⁴CO₂ because they are cheap and accurate. On the other hand, we demonstrated that the flow detection of ¹⁴CO₂ had a finer temporal resolution and was consequently a relevant tool to study C dynamics in the rhizosphere at a short time scale. This revised version was published online in June 2006 with corrections to the Cover Date.     

Agarose-DTNB column for binding sulfhydryl-containing proteins and peptides.

The counting rate of [1-¹⁴C]trichloroacetic acid (TCA) was not stable in a standard toluene/Triton X-100 liquid scintillation solution because this compound becomes partially degraded to ¹⁴CO₂ and CHCl₃. Both toluene and Triton were contributing factors in causing this degradation. The NCS solubilizer added to the toluene/Triton scintillation solution trapped ¹⁴CO₂ and stabilized counting rates of [1-¹⁴C]TCA. When [2-¹⁴C]TCA was used, ¹⁴CHCl₃ remained in the scintillation solution resulting in stable counting rates without the addition of NCS.     

Methodological Modifications for Accurate and Efficient Determination of Contaminant Biodegradation in Unsaturated Calcareous Soils

Many techniques for quantifying microbial biodegradation of ¹⁴C-labeled compounds use soil-water slurries and trap mineralization-derived ¹⁴CO₂ in solution wells suspended within the incubation flasks. These methods are not satisfactory for studies of arid-region soils that are highly calcareous and unsaturated because (i) slurries do not simulate unsaturated conditions and (ii) the amount of CO₂ released from calcareous soils exceeds the capacity of the suspended well. This report describes simple, inexpensive methodological modifications for quantifying microbial degradation of [¹⁴C]benzene and 1,2-dichloro[U-¹⁴C]ethane in calcareous soils under unsaturated conditions. Soils at 50% water holding capacity were incubated with labeled contaminants for periods up to 10 weeks, followed by acidification of the soil and trapping of the evolved CO₂ in a separate container of 2 N NaOH. The CO₂ was transferred from the incubation flask to the trap solution by a gas transfer shunt containing activated charcoal to remove any volatilized labeled organics. The amount of ¹⁴CO₂ in the trap solution was measured by scintillation counting (disintegrations per minute). The method was tested by using two regional unamended surface soils, a sandy aridisol and a clay-rich riparian soil. The results demonstrated that both [¹⁴C]benzene and 1,2-dichloro[U-¹⁴C]ethane were mineralized to release substantial amounts of ¹⁴CO₂ within 10 weeks. Levels of mineralization varied with contaminant type, soil type, and aeration status (anaerobic vs. aerobic); no significant degradation was observed in abiotic control samples. Methodological refinements of this technique resulted in total ¹⁴CO₂ recovery efficiency of approximately 90%.     

Radiorespirometry and metabolism of cultured cells attached to petri dishes

A radiorespirometer was constructed for continuous quantitation of ¹⁴CO₂ released from specifically labeled substrates by intact cultured cells attached to plastic petri dishes. An airtight chamber is created by sealing the petri dish with a specially designed cover inside a thermostated holder. Rapid equilibration of released ¹⁴CO₂ with a 5% $\text{CO}{}_2\text{95\%}$ air carrier gas is achieved by bubbling the carrier gas under the surface of the growth medium. Labeled CO₂ is removed from the carrier gas by trapping in an organic base and quantitated by liquid scintillation counting. Additions to or sampling of the growth medium may be performed during a run and the carrier gas may be modified to test the effects of anesthetics and different O₂ levels. The ability to continuously monitor ¹⁴CO₂ release can provide valuable information concerning the metabolic pathways of substrate oxidation which cannot be obtained from single ¹⁴CO₂ determinations. A capacity of 12 culture plates enormously increases the amount of data that can be collected in a given time. The use of liquid scintillation counting increases the sensitivity and resolution over the ion chamber and Geiger counter methods, and permits utilization of the procedure in a much wider range of laboratories. Data obtained for the oxidation of specifically ¹⁴C-labeled glucose and pyruvate by neonatal rat heart cells in culture, in both the presence and absence of oxygen, are provided as examples of the utility of the method.     

Determination of low levels of 14C radioactivity in cell exudates by means of ultraviolet photooxidation and a rapid 14CO2-collection technique

The low levels of ¹⁴C radioactivity found in many biological samples, such as cell exudates of marine algae, can be determined conveniently by uv photooxidation of the ¹⁴C-labeled compounds. The acid distillation of the resultant ¹⁴CO₂ and its rapid absorption (cf. 15 min) by a quaternary amine in a closed recirculating system prior to liquid scintillation counting provides a means of concentrating the ¹⁴C activity by up to 10 times. Quench problems are thus reduced to that of one compound, namely ¹⁴CO₂. The kinetics of photooxidation of various ¹⁴C-labeled compounds in seawater are complex but similar in form for the several different classes of compounds tested. The role of the nature and concentration of the oxidant, sample pH, and the source of uv irradiation during photooxidation are discussed.     

Occurrence and activity of iron- and sulfur-oxidizing microorganisms in alkaline coal strip mine spoils

Spoils samples collected from a coal strip mine in southeastern Montana were examined for populations and activities of iron- and sulfur-oxidizing bacteria. Spoils examined were of three types: (a) acidic pyrite-rich waste coal, (b) oxidation halo material, and (c) alkaline material, which was the most widespread type. Bacterial numbers, sulfur oxidation, and¹⁴CO₂ uptake activity declined to low levels in the summer when spoils were dry. Even in wetter spring months pyritic spoils contained relatively low numbers of acidophilic iron- and sulfur-oxidizing bacteria, probably indicative of water stress since the same spoils incubated with excess water or dilute mineral salts showed considerably greater bacterial numbers and activity. Certain wells in coal and spoils aquifers contained substantial populations of iron-oxidizing acidophilic bacteria. However, these wells were always of alkaline or neutral pH, indicating that bacterial pyrite oxidation occurred where groundwaters contacted either replaced spoils or coal that contained pyrite or other metal sulfides. Bacterial activity may contribute to trace metal and sulfate leaching in the area.     

Improvements in and Environmental Applications of Double-Vial Radiorespirometry for the Study of Microbial Mineralization

Several variations in the scintillation mixture and the filter paper arrangements for double-vial radiorespirometry were compared. Improved efficiencies (44%) and shorter response times were found by adding wetting agents and methanolic NaOH to the scintillation mixture in the filter paper. The scintillation chemicals used did not contain dioxane and were found to be nontoxic to the test microbiota in this system. Covering the inner reaction vial with aluminum foil minimized the reduction in counting efficiency when testing colored or dense environmental samples. Mineralization rates were determined with ¹⁴C-labeled glucose, acetate, and glutamate and [¹⁴C]cellulose- and [¹⁴C]lignin-labeled lignocellulose for composting cow manure, forest soil, and arctic lake sediment microbiota. This improved method can be used in a variety of procedures involving the measurement of microbial mineralizations of organic compounds. Since no liquid scintillation cocktail is used for counting, the radioactive wastes are aqueous or can be incinerated, making disposal easy.     

Method for simultaneous measurement of total and radioactive carbon in soils,soil extracts and plant materials

Summary A rapid procedure is proposed for simultaneous measurement of total and radioactive carbon in soils, soil extracts and plant materials. The procedure involves dry or wet combustion of the sample, total carbon determination with an automatic analyser and C¹⁴O₂ absorbtion in a liquid for scintillation measurement. The use of methyl-cellosolve plus mono-ethanolamine as a CO₂ absorber allows measurements of weakly labelled materials. This method is suitable for fast routine analysis. re]19750929     

The use of tritiated cellulose in screening for cellulolytic microorganisms

Summary Phosphoric acid swollen cellulose has been reduced with³H-KBH₄ and the resulting radioactive amorphous cellulose is broken down by a number of cellulolytic bacteria and fungi with accumulation of radioactive label in the culture filtrate. This is detected by scintillation counting. Non-cellulolytic microorganisms do not behave in a similar manner.     

Measurement of CO(2) Assimilation in Soils: an Experiment for the Biological Exploration of Mars

A method is described for the measurement of ¹⁴CO₂ assimilation by microorganisms in soils. A determination involves exposing soil to ¹⁴CO₂, pyrolyzing the exposed soil, trapping the organic pyrolysis products on a column of firebrick coated with CuO, combusting the trapped organics by heating, and measuring the radioactivity in the CO₂ produced in the combustion. The detection of significant levels of ¹⁴C in the trapped organic fraction appears to be an unambiguous indication of biological activity. The ¹⁴CO₂ which is adsorbed or exchanged into soils by nonbiological processes does not interfere. The method easily detects the ¹⁴CO₂ fixed by 10² to 10³ algae after light exposure for 3 to 24 hr. Assimilation of ¹⁴C is also demonstrable in dark-exposed soils containing 10⁵ to 10⁶ heterotrophic bacteria. Possible applications of the method in the biological exploration of Mars are discussed.     

Automatic collector of expired 14CO2 for liquid scintillation counting

A filtration technique was employed to trap ¹⁴CO₂ continuously for liquid scintillation counting. Devices for delivering scintillator and ethanolamine solutions were combined symmetrically with two fritted-glass aspirators for altenating operation. The collector was regulated by a fraction collector timer. Trial and animal tests indicated that the described method was efficient, reliable, and more convenient for frequent collection over long periods than alternative methods. The automatic collector was used for metabolic studies of [1-¹⁴C] arachidonic acid in rats kept in metabolic cages and the results were processed by multicompartmental analysis.     

Preparation of 14C-labeled algal samples for liquid scintillation counting

Four commonly used techniques for preparation of ¹⁴C-labeled algal samples on membranes for liquid scintillation counting were compared and a simple technique for apparent net assimilation measurement from aqueous samples was introduced. All four techniques yielded similar radioactivities from the test cultures and are thus suitable for measurements of ¹⁴C algal samples. The possibly carcinogenic solvent dioxane was not necessary with PCS scintillation cocktail for dissolving radioactivity from algae on filters.     

Mineralization of 2,4-dichlorophenoxyacetic acid in soil previously enriched with organic substrates

Samples of chernozem soil were enriched with vanillic acid, protocatechuic acid glucose, a mixture of glucose and (NH₄)₂SO₄ (C∶N = 5∶1), ethanol and 2,4-dichlorophenoxyacetic acid (2,4-D). After a 6-d (with 2,4-D 35-d) incubation during which primary oxidation of the introduced substrates occurred, the soil was supplied with a solution of 2-¹⁴C-2,4-D (50ppm; 6.7kBq) and production of¹⁴CO₂ (product of microbial degradation of 2,4-D) was measured. Previously enriched samples exhibited a higher degradation rate; both the lag phase and doubling time of mineralization activity in the exponential phase of the process were markedly higher. This reflected an overall proliferation of bacteria and the increased relative proportion of bacterial strains capable of mineralizing 2,4-D in enriched samples. The stimulation of 2,4-D degradation may involve specific adaptation and selection mechanisms (as in the case with samples previously enriched with 2,4-D or its structural analogues—aromatic monomers, ethanol) as well as nonspecific mechanisms. The extent of mineralization of 2,4-D was not affected by soil pretreatment, about 1/3 of introduced radioactive carbon being invariably transformed to¹⁴CO₂.     

Measurement of photorespiration in algae

The rates of true and apparent photosynthesis of two unicellular green algae, one diatom and four blue-green algae were measured in buffer at pH 8.0 at subsaturating concentrations of dissolved inorganic carbon (13-27 micromolar). Initial rates of depletion from the medium of inorganic carbon and ¹⁴C activity caused by the algae in a closed system were measured by gas chromatography and by liquid scintillation counting, respectively. The rate of photorespiration was calculated as the difference between the rates of apparent and true photosynthesis. The three eucaryotic algae and two blue-green algae had photorespiratory rates of 10 to 28% that of true photosynthesis at air levels of O₂. Reduction of the O₂ level to 2% caused a 52 to 91% reduction in photorespiratory rate. Two other blue-green algae displayed low photorespiratory rates, 2.4 to 6.2% that of true photosynthesis at air levels of O₂, and reduction of the O₂ concentration had no effect on these rates.     

A rapid, hygienic method for the preparation of fecal samples for liquid scintillation counting.

A method for the preparation of fecal samples for liquid scintillation counting is described which is rapid, hygienic, and inexpensive. By the use of a novel type of homogenizer, fecal samples can be homogenized while totally enclosed within a sealed, plastic bag, so reducing the possible risk of infection. The subsequent preparation of a clear solution suitable for liquid seintillation counting is performed using an “in-vial” digestion technique which enables any ¹⁴CO₂ released during digestion to be trapped within the vial.     

Potential Sources of Error in the Measurement of Low Rates of Planktonic Photosynthesis and Excretion

THE introduction of liquid scintillation counting techniques to the study of aquatic productivity^1–3 has stimulated interest in the accurate determination of low rates of algal photosynthesis, such as occur in tropical waters or in deep living phytoplankton populations. Attention is also being directed to the measurement of soluble extracellular products of photosynthesis⁴. Our studies have revealed some potential sources of interference in the widely used ¹⁴C technique when used to study low rates: (1) retention of NaH¹⁴C0₃ by filters; (2) passive adsorption of radioactivity by filters and/or seston and (3) soluble and insoluble radioactive impurities in commercially available NaH¹⁴C0₃.     

Method for Simultaneous Measurement of Radioactive and Inactive CO(2) Evolved from Soil Samples During Incubation with Labeled Substrates

An apparatus is described which allows the simultaneous, continuous, and highly sensitive analysis of inactive and radioactive CO₂ evolved from ¹⁴C-supplemented soils or other materials. The apparatus consists of a control unit, a commercially available conductometric CO₂ analyzer, and fraction collector. A number of model experiments were conducted to demonstrate the potentials of the apparatus. These included analysis of the time course of priming action, when ¹⁴C-glucose was added to soil, separation of CO₂ respiration peaks caused by simultaneous degradation of radioactive and inactive soil supplements, and study of the effects of a fungicide, Benomyl, on degradation of ¹⁴C-labeled glucose. In the last experiment, partial degradation of the fungicide could also be followed.     

Method for Simultaneous Measurement of Radioactive and Inactive CO2 Evolved from Soil Samples During Incubation with Labeled Substrates

An apparatus is described which allows the simultaneous, continuous, and highly sensitive analysis of inactive and radioactive CO₂ evolved from ¹⁴C-supplemented soils or other materials. The apparatus consists of a control unit, a commercially available conductometric CO₂ analyzer, and fraction collector. A number of model experiments were conducted to demonstrate the potentials of the apparatus. These included analysis of the time course of priming action, when ¹⁴C-glucose was added to soil, separation of CO₂ respiration peaks caused by simultaneous degradation of radioactive and inactive soil supplements, and study of the effects of a fungicide, Benomyl, on degradation of ¹⁴C-labeled glucose. In the last experiment, partial degradation of the fungicide could also be followed.     

Sequence of Formation of Phosphoglycolate and Glycolate in Photosynthesizing Chlorella pyrenoidosa

In Chlorella pyrenoidosa which have been photosynthesizing in either 1.5% ¹⁴CO₂ or 0.05% ¹⁴CO₂ in air, gassing with 100% O₂ results in rapid formation of phosphoglycolate which is apparently converted to glycolate. However, only about one-third to one-half of the rate of glycolate formation can be accounted for by this route. The remaining glycolate formation may be the result of the oxidation of sugar monophosphates. The rates of formation of both glycolate and phosphoglycolate are about four times greater with algae that have been photosynthesizing in 1.5% ¹⁴CO₂ than with algae which have been photosynthesizing with air, when the algae are then gassed with 100% O₂.     

Comparison of linoleate,palmitate and acetate metabolism in rat ventral prostate

Rat ventral prostate incorporated (1-¹⁴C)acetate, (1-¹⁴C)palmitate and (1-¹⁴C)linoleate into different phospholipids in a time-dependent process. The rate of incorporation into total phospholipids was higher with linoleate (10.0 nmol/g) than with either palmitate (5.8 nmol/g) or acetate (4.7 nmol/g). Predominant labelling with all the radioactive substrates assayed was found in choline glycerophospholipids (PC). The radioactive profiles for linoleate in the other ventral prostate phospholipids differed from those obtained with palmitate and acetate. Specifically linoleate was incorporated into inositol glycerophospholipids plus lysoethanolamine glycerophospholipids (PI+LPE) and not into sphingomyelin (SM), while palmitate and acetate incorporated into SM but not into PI+LPE. Acetate showed the highest oxidation to CO₂ whereas no differences were observed in the radioactivity incorporated into CO₂ from a saturated (palmitate) or an essential unsaturated fatty acid (linoleate). These studies also show zinc-dependence by the acetate to CO₂ oxidation.Abbreviations PL total phospholipids - PC choline glycerophospholipids - PE ethanolamine glycerophospholipids - PI+LPE inositol glycerophospholipids plus lysoethanolamine glycerophospholipids - PS serine glycerophospholipids - SM sphingomyelin