1141 Notes WOLIN, E. A., M. J. WOLIN, AND R. S. WOLFE. iology of a Methanobacterium Microbial. 11 l(3): 199-206. 1963. Formation of methane by bacterial extracts. J. Biol. Chem. 238: 2882-2886. ZEHNDER, A. J., AND K. WUHRMANN. 1977. Phys- Limnol. Oceanogr., 24(6), 1979,1141-1145 Society of Limnology @ 1979, by the American A modified respiration and Oceanography, strain AZ. Arch. Submitted: 1 March 1979 Accepted: 22 May 1979 Inc. procedure for determining [‘“C]CO, in water or sediment samples’ produced by strate incubated with sediment or water samples is displaced from the sample by acidification and trapped in 2-phenylethylamine (PEA) absorbed on a small strip of filter paper suspended over the sample. Respired [l”C]CO, is then determined by liquid scintillation counting of the filter strip in toluene scintillation Organic materials labeled with 14C fluid. All the evolved CO, was absorbed have been used by many workers to de- by PEA (Hobbie and Crawford 1969), but termine heterotrophic activity and sub- only 82% of the [14C]C0, evolved could strate turnover times in soils, sediments, be accounted for by scintillation counting and natural waters. Initial experiments after correcting for counting efficiency on the kinetics of substrate uptake by nat- with an internal standard. Christian and ural populations of heterotrophs took no Weibe (1978) observed even lower recovaccount of carbon lost as [14C]C0, by res- ery (60%) when using a scintillation fluid piration and consequently the results containing Triton X-100 to estimate consistently underestimated the total [14C]C0, evolved from soils although turnover of substrate (Wright and Hobbie they did not give sufficient experimental 1965; Vaccaro and Jannasch 1967; Vac- detail to conclude unequivocally that all care 1969; Hobbie et al. 1968). Respirathe [r4C]C0, was absorbed by the traption losses of substrate were a large ping agent. Harrison et al. (1971) and source of error in these early studies with Griffiths et al. (1974) have shown that substrates such as acetate, glucose, and PEA not absorbed on filter paper quanamino acids, for which respiration can be titatively traps C02, and Hobbie and the major metabolic fate. However, HobCrawford (1969) established by wet oxibie and Crawford (1969) devised a simple dizing their filter paper strips and countand reasonably effective means of traping the absorbed [14C]C0, in an ion ping and quantifying respired [ 14C]C0, chamber that complete trapping had ocwhich has achieved widespread popularcurred. Hobbie and Crawford concluded ity (see Christian and Hall 1977; Wright that the lower level of radioactivity mea1973) in kinetic studies of substrate utisured in the strips by liquid scintillation lization in natural systems. counting was a result of masking effects According to Hobbie and Crawford’s by the paper. Because the complex of (1969) procedure, [ l”C]CO, produced by PEA with CO, (2-phenylethylammonium respiration of 14C-labeled organic sub- phenylethylcarbamate) is not very soluble in toluene (Rapkin 1969) it remains r The work was carried out at the Central Elecassociated with the filter paper strip and tricity Research Laboratories and the paper is pubdoes not dissolve appreciably in the scinlished by permission of the Central Electricity Gentillation cocktail. Thus beta-absorption erating Board. Abstract-Poor recovery of radioactivity when determining [14C]C0, respired by microbes can be overcome by substituting 2-ethanolamine for 2-phenylethylamine to absorb [14C]C0, and by increasing the solubility of solution absorbed [‘“C]CO, in the scintillation with 2-ethoxyethanol. 1142 Notes by the paper and by the complex (selfabsorption) may almost entirely account for the low recovery of radioactivity. Heterogeneous counting on filter paper has been reviewed by Long et al. (1976) in connection with 3H counting, and their remarks are partly applicable to more energetic beta-emitters such as r4C. Beta-absorption occurs when the radioisotope is not homogeneously distributed within the scintillation cocktail. Some beta particles emitted inside an aggregate of sample or within the filter matrix are absorbed without producing measurable excitation of the solvent, resulting in a reduction of the potential counting rate. Because the amount of beta-absorption is in part related to the quantity of material on the filter (self-absorption) the observed counting rate also depends on the total amount of CO, absorbed. Beta particles emitted in the bulk of the scintillation cocktail are quenched to a different extent than those emitted from the surface of the filter; therefore internal standards cannot be used to correct for the effects of beta-absorption. For the same reason, quench correction cannot be made by using an external standard ratio (ESR) method, and the sample channels ratio (SCR) technique is of doubtful value because SCR does not change in accordance with increasing beta-absorption. Another disadvantage of heterogeneous counting on filter paper is the dependence of counting rate upon the orientation of the paper strip within the vial, a consequence of which is to increase the variability between replicate samples. Because of this effect, and also because of the reduction in counting rate caused by beta-adsorption, the precision of measurements obtained by the technique is likely to be lower than with a system in which radioactivity is homogeneously distributed throughout the cocktail, even when correction factors are applied to compensate for an apparently constant reduction in efficiency caused by betaabsorption. These difficulties can all be minimized by ensuring that the absorbed [14C]C0, is dissolved in the scintillation cocktail. I here describe such a modification. [‘“C]CO, was generated in a system slightly different from that described by Hobbie and Crawford (1969), but because complete absorption of CO, was observed, these minor differences do not influence the validity of the conclusions drawn regarding counting conditions for the absorption strip. Carrier-free [14C]NaHC03 (0.065 &i) (Radiochem. Centre, Amersham, U.K.) in 50 ~1 of distilled water was added to 25-ml screwcap bottles containing up to 500 ~1 of 0.5% (wt/vol) NaHCO, solution and the total volume of liquid adjusted to 550 ~1 with distilled water. The bottles were sealed with rubber suba-seals. [14C]C0, was absorbed by accordian-folded strips (25 x 51 mm) of Whatman No. 1 filter paper moistened with 200 ~1 of trapping solution and contained in small plastic cups suspended (by means of bent paper clips) from the suba-seals. Gas was generated by injecting 0.5 ml of 1 M H,SO, into the liquid. The bottles were incubated overnight at 4°C to allow the strips to absorb all the evolved CO,. After the bottles were opened, the strips were placed in plastic scintillation vials, either empty or containing 5 ml of 2-ethoxyethanol (EE). Strips placed in these latter vials were allowed to soak for up to 10 min with occasional gentle agitation. All the strips were counted at 6°C in scintillation fluid (10 ml) containing 2-(4’-t-butylphenyl)-4(4”-biphenylyl)-1,3,4-oxadiazole (butylPBD), 7 g-liter-l, in toluene in an Intertechnique SL33 automatic scintillation spectrometer having a 22”Ra external standard source. Vials were placed in the instrument 30 min before counting to allow thermal equilibration and the decay of chemiluminescence before determining radioactivity with the preset discriminator settings for 3H, 14C, and 3H + 14C. Samples were counted until at least lo5 cpm had been recorded in the 3H + 14C channel. SCR and ESR were determined automatically. Chemicals used for scintillation counting were “scintillation” Notes 1143 Table 1. Effect of different trapping solutions and scintillation systems on recovery of [14C]C0,. [14C]C0, was released from a solution of 0.5% NaHCO,, 500 ~1, containing 70,250 k 2,458 dpm [‘“C]NaHCO,, and absorbed in 0.2 ml of trapping solution on Whatman No. 1 paper as described in text. Radioactivity of carrier-free [r4C]NaHC03 determined by counting aliquots of the solution in toluene scintillation fluid, 10 ml, with 5.2 ml of EA/EE. A filter paper strip was placed in each vial and cpm corrected for quenching by internal standardization with [14C1]-n-hexadecane. As discussed in text, internal standardization is valid only when most of the 14C is dissolved in scintillation fluid. Figures for dpm are means of three replicate determinations k SD. Soluble Trapping agent SEE1 EA/EE (Modified PEA Yes procedure) No Yes No (Standard H-C) Complete system dpm Recovery % dp111 62,645 + 314 70,755 IL 240 101 62,181 k 952 88 9,100 k 677 60,690 k 2,911 27,472 2 3,012 86 39 22,227 k 1,873 3,793 k 58 grade (Fisons, Loughborough, U.K.); all other chemicals were of AR grade. Because the insolubility in toluene of the complex of 2-phenylethylamine with CO, is the cause of inefficient counting of radioactivity and other problems resulting from beta-absorption, the amount of soluble [14C]C02 was increased by changing the solubility of the recovered CO, absorbed in PEA and by using other absorption agents. Hyamine hydroxide (p-di-isobutylcresoxyethoxyethyldimethylbenzylammonium hydroxide, 1 M in methanol) has been used to trap [14C]C02 before liquid scintillation counting (Snyder and Godfrey 1961; Edwards and Kitchener 1965), but although it forms a toluene-soluble complex with C02, it has the disadvantages of being a severe quenching agent and of low trapping capacity per unit cost (Rapkin 1969). Ethanolamine (EA) is also able to completely trap CO, (Jeffay and Alvarez 1961; Kadota et al. 1966), but its high viscosity makes accurate pipetting difficult and the salt formed with CO, is not appreciably soluble in toluene. However, these problems can be overcome by diluting EA with EE, which reduces its viscosity and dissolves the EA-CO, complex. Unlike PEA, EA does not darken appreciably on storage and therefore does not quench as severely as some batches of PEA. EA was used as a trapping agent % 89 13 32 5.4 for these experiments, mixed with an equal volume of EE. The low viscosity of the mixture permitted accurate dispensing, and 200-4 aliquots of the mixture were applied to filter paper strips for absorption of [14C]C0,. The capacity of the EA/EE mixture to absorb CO, is not appreciably different from that of an equal volume of PEA, because the higher molecular weight of the latter compound (121) is compensated by the dilution of EA (mol wt 61). In all the experiments described here, ~2% of the absorption capacity of the trapping agent was utilized by the evolved CO,. The recovery of radioactivity absorbed on filter strips moistened with PEA and then placed in toluene scintillation fluid for counting (referred to as standard H-C) is compared in Table 1 with recovery of radioactivity from filter strips moistened with EA/EE. This table also shows the effect of adding EE (5 ml) to the scintillation system on recovery of radioactivity. Soluble counts were determined by replacing the original filter paper strips with nonradioactive strips of similar dimensions and recounting. The standard H-C procedure gave the lowest recovery of radioactivity, although recovery was more than doubled by adding 5 ml of EE. However, even without additional EE, recovery was better using EA/EE as trapping agent than the standard H-C procedure, and, when Notes I 100 I I I 200 300 400 CARRIER NaHCO, SOLUTION,pt I 500 Fig. 1. Effect of CO2 concentration on recovery of fixed amount of [14C]C0,. [14C]C0, was liberated in presence of various amounts of 0.5% NaHCO, carrier from [14C]NaHC0, at total activity of 63,000 cpm (see text). Absorbed radioactivity determined by standard H-C procedure (0) or by the modified procedure described here (0). [14C]C02 was trapped with EA/EE and additional EE was included in the scintillation cocktail, recovery of radioactivity was complete. The increase in recovery of radioactivity obtained by using EA/ EE as trapping agent and counting in the presence of additional EE (referred to as modified procedure) over the standard H-C procedure is paralleled by a large increase in dissolved counts, from 5.4% soluble with the standard H-C procedure to over 89% soluble in the modified system. An overall counting efficiency of 95.5% was determined for the modified procedure with an internal standard of [ 14CJ-n -hexadecane. Chemical quenching in the modified procedure by the filter paper strips resulted in small but significant (P = 0.01) reductions of ESR and SCR, of 1.56 and 6.50%, compared with control vials in which filter paper had been omitted and to which [14C]NaHC03 and 200 ~1 of EA/ EE were added directly to the cocktail. The P-energy spectrum was slightly displaced toward the lower energy (3H) range, but no significant difference in 3H + 14C channel counts could be detected between vials containing paper strips and the controls. The orientation of the paper strips did not affect 3H + 14C count rate, ESR, or SCR, and these parameters were effectively constant between vials in which the filter strips were pressed against the bottom of the vessel and those in which the strips were allowed to stand upright. Figure 1 shows the effect of increasing the amount of absorbed CO, on recovery of radioactivity from a constant amount of [14C]C02. The maximum amount of CO, released in these experiments (57 pmol of CO, from 500 ,ul of 0.5% NaHCO,) is similar to that liberated after acidification of l-2 ml of hard freshwater or seawater samples, although more would be released from carbonate-rich sediments. Because most of the recovered radioactivity in the standard H-C procedure remains associated with the filter strips (see Table I), apparent recovery is lowered when the amount of CO, absorbed is increased, even though a maximum of ~2% of the trapping agent’s capacity is utilized. In contrast to these results, complete recovery independent of the amount of CO, absorbed was recorded using the modified procedure because most of the radioactivity here was in free solution and therefore not subject to losses caused by self-absorption. It may be possible to use the modified technique described here with commercially prepared scintillation cocktails, if it is first established that EA-[‘4C]C02 complex dissolves in the fluid. This can be checked by measuring radioactivity in trial experimental vials with the filter paper strip in place and then again after its removal. Counting rate after removing the strip should not be appreciably less than in the complete system. Some scintillation cocktails containing solvents other than toluene (e.g. 1,4-dioxane) may not need the addition of EE to increase the solubility of the EA-CO, complex. Previous work using the standard H-C procedure did not necessarily underestimate respired [14C]C02 provided that an adequate correction factor was used to 1145 Notes compensate for beta-absorption losses and complete trapping of [‘4C]C02 was established. Because counting rate in the standard procedure depends partly on the total amount of CO, absorbed, correction factors must be determined for batches of samples which contain different amounts of total CO, or in which the endogenous rate of respiration varies, for example, in sediments or soils where biochemical activity may change greatly within a few centimeters depth. Keith A. Brown Research Central Electricity Laboratories Leatherhead Surrey KT22 7SE U.K. References CHRISTIAN, R. R., AND J. R. HALL. 1977. Experimental trends in sediment microbial heterotrophy: Radioisotopic techniques and analysis, p. 67-88. Zn B. C. Coull [ed.], Ecology of marine benthos, Univ. South Carolina. AND W. J. WEIBE. 1978. Anaerobic microbial community metabolism in Spartina altern$ora soils. Limnol. Oceanogr. 23: 328-336. EDWARDS, B., AND J. A. KITCHENER. 1965. A routine method for determination of 14C0, by liquid scintillation. Int. J. Appl. Radiat. Isot. 16: tion in lake sediments. Appl. AMicrobiol. 21: 698-702. HOBBIE, J. E., AND C. C. CRAWFORD. 1969. Respiration corrections for bacterial uptake of dissolved organic compounds in natural waters. Limnol. Oceanogr. 14: 528-532. -, AND K. L. WEBB. 1968. Amino acid -, flux in an estuary. Science 159: 1463-1464. JEFFAY, H., AND J. ALVAREZ. 1961. Liquid scintillation counting of carbon-14. Use of ethanolamine-ethylene glycol monomethyl ether-toluene. Anal. Chem. 33: 612-615. KADOTA, H., Y. HATA, AND H. MIYOSHI. 1966. A new method for estimating mineralization activity in lake water and sediment. Mem. Res. Inst. Food Sci. Kyota Univ. 27: 28-30. LONG, E., V. KOHLER, AND M. J. KELLY. 1976. Heterogeneous counting on filter support media, p. 47-68. Zn A. A. Noujaim et al. [eds.], Liquid scintillation science. Academic. RAPKIN, E. 1969. Sample preparation for liquid scintillation counting. No. 1. Solubilization techniques. Digitech. Tech. Rev. Publ. Intertech. Uxbridge, U.K. SNYDER, F., AND P. GODFREY. 1961. Collecting 14C0, in Warburg flasks for subsequent scintillation counting. J. Lipid Res. 2: 195. VACCARO, R. F. 1969. The response of natural microbial populations in seawater to organic enrichment. Limnol. Oceanogr. 14: 726-735. AND H. W. JANNASCH. 1967. Variations in -> uptake kinetics for glucose by natural populations in seawater. Limnol. Oceanogr. 12: 540- 542. WRIGHT, R. T. 1973. Some difficulties 445446. GRIFFITHS, R. P., F. J. HANUS, AND R. Y. MORITA. 1974. Effects of various water sample treatments on the apparent uptake of glutamic acid by natural marine microbial populations. Can. J. Microbial. 20: 1261-1266. HARRISON, M. J., R. T. WRIGHT, AND R. Y. MOFUTA. 1971. Methods for measuring mineraliza- -> using 14Corganic solutes to measure heterotrophic bacterial activity, p. 199-218. Zn L. H. Stevenson and R. R. Colwell [eds.], Estuarine microbial ecology. Univ. South Carolina. and J. E. Hobbie. 1965. The uptake of organic solutes in lake water. Limnol. Oceanogr. 10: 22-28. Submitted: 29 November Accepted: 24 March 1978 1979
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