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Diazotrophic Klebsiella oxytoca VN 13 was able to lyse pectate, but the lytic activity of cultures grown on non-selective media was weak, and the enzyme was located mainly inside the cells. A small fraction of the population (10-6 to 10-5) was able to grow in a selective medium with sodium polygalacturonate as sole carbon source, and produced increased amounts of the pectinolytic enzyme pectate lyase. When wheat seeds were inoculated with these bacteria, increased levels of this enzyme correlated with a higher rate of internal colonization of wheat roots and with stimulation of wheat growth resulting in higher biomass. This suggests that colonization occurs via lyzed pectin layers.

Endosymbionts from the Ethiopian highland acacia species Acacia abyssinica, A. negrii and A. etbaica, and the lowland species A. nilotica, A. prasinata, A.senegal, A. seyal, A. tortilis and Faidherbia (Acacia) albida were isolated and characterized. Seven tree species were found to be nodulated by species of both Rhizobium and Bradyrhizobium. F. (Acacia) albida and A. senegal were nodulated by only Bradyrhizobium or Rhizobium, respectively. In A. abyssinica, both genera were isolated from the same nodule, whereas in A. nilotica and A. tortilis, both strains were isolated from different nodules of the same plant. The nitrogen fixation (acetylene reduction) activities varied considerably and showed no correlation with the nitrogen content of the plant. Highland species were as effective as lowland plants, thus demonstrating good potential for soil reclamation. The endosymbionts isolated proved rather promiscuous, efficiently nodulating other Acacia spp. and some tropical grain legumes, but did not nodulate temperate legumes.

Continuous culture studies have been carried out on a strain ofA. brasilense to study ammonia excretion, dinitrogen fixation and ammonia assimilatory enzymes (glutamate-ammonia ligase and glutamate synthase (NADPH)) in encysted conditions. High glutamate synthase (NADPH) and low ammonia excretion was observed at the time of induction of cyst formation. Low and oscillating nitrogenase activity was observed throughout the experiment.

African yam bean (Sphenostylis stenocarpa), which is widely cultivated in Africa because of its growth capability on marginal soils, was nodulated by an endosymbiont (characterized and designed Bradyrhizobium sp. AUEB20) isolated from the Ethiopian tree Erythrina brucei with the formation of a small number of large, indeterminate N2-fixing nodules. In contrast, 24 other isolates from Ethiopian woody legumes were ineffective. Strain AUEB20 promiscuously nodulated a number of tropical legumes, but none out of five European crop plants tested.

Both the changes in the activities of nitrogenase, glutamine synthetase and glutamate dehydrogenase and in the extracellular and intracellular NH4+ concentrations were investigated during the transition from an NH4+ free medium to one containing NH4+ ions for a continuous culture of Azotobacter vinelandii. If added in amounts causing 80-100% repression of nitrogenase, ammonium acetate, lactate and phosphate are absorbed completely, whereas chloride, sulfate and citrate are only taken up to about 80%. After about 1-2 hrs the NH4+ remaining in the medium is absorbed too, indicating the induction or activation of a new NH4+ transport system. One of the new permeases allows the uptake of citrate in the presence of sucrose. Addition of inorganic NH4+ level leads to a reversible rise in the glutamine synthetase activity which is not prevented by chloramphenicol, and to a reversible decrease in nitrogenase activity. During these measurements glutamate dehydrogenase activity remains close to zero. The intracellular NH4+ level of about 0.6 mM does not change when extracellular NH4+ is taken up and repression of nitrogenase starts.

A method is described which allows the quantitative determination of small ammonia concentrations in the culture of nitrogen-fixing microorganisms. With this method the ammonia concentration range was estimated in which repression of nitrogenase synthesis in Azotobacter vinelandii occurs. Both in batch and continuous cultures there was no repression below 10 μM, whereas nitrogenase synthesis stopped completely if the ammonia concentration in the medium exceeded 25 μM.

The method of proton magnetic resonance is used to determine the melting point of ice particles in the pores of monodisperse porous glasses ranging from 10 to 1000 A in radius.

Addition of ammonium salts to N2 fixing continuous cultures of Clostridium pasteurianum caused immediate stop of nitrogenase synthesis, while the levels of glutamine synthetase, glutamate dehydrogenase and asparagine synthetase remained constant. No evidence for an interconversion of the glutamine synthetase was found. The activities of glutamate synthase in crude extracts were inversely related to the nitrogenase levels. The intracellular glutamine pool rapidly expanded during nitrogenase repression and decreased as fast during derepression while the pool sizes of all other amino acids were not strongly related to the rate of nitrogenase formation. These investigations suggest glutamine as corepressor of nitrogenase synthesis.

When continuous cultures of Azotobacter vinelandii were supplied with ammonium or nitrate in amounts, which just repressed nitrogenase synthesis completely, both the intracellular glutamine level and the degree of adenylylation of the glutamine synthetase (GS) increased only slightly (from 0.45–0.50 mM and from 2 to 3 respectively), while the total GS level remained unaffected. Higher amounts of ammonium additionally inhibited the nitrogenase activity, caused a strong rise in the intracellular glutamine concentration and adenylylation of the GS, but caused no change in the ATP/ADP ratio. These results are considered as evidence that in A. vinelandii the regulation of nitrogenase synthesis is not linked to the adenylylation state of the GS and to the intracellular glutamine level, and that the inhibition of the nitrogenase activity as a consequence of a high extracellular ammonium level is not mediated via a change in the energy charge.

The purified Mo-Fe protein and Fe protein of nitrogenase from Azotobacter vinelandii have molecular weights (MW) of about 216000 and 64000, respectively. The Mo-Fe protein is composed of subunits of about 56000 MW, and the Fe protein has 2 equivalent subunits of about 33000 MW. The isoelectric point of the Mo-Fe protein is 5.2 and that of the Fe protein is 4.7. Amino acid compositions reflect the acidic nature of the proteins. The Mo-Fe protein yielded 24 atoms of Fe, 20 atoms of acid-labile sulfide and 1.54 atoms of Mo per molecule. Analysis of the Fe protein showed 3.45 atoms of Fe per molecule.

Based on the reduction of dimethylusulfoxide (DMSO) to dimethylsulfide (DMS) by microorganisms, a simple, rapid, sensitive and inexpensive method for the determination of microbial activity in soil samples was developed. When DMSO was added to samples, DMS appeared immediately in the gas phase, which was quantitatively analyzed by gas chromatography. The DMS liberation rate was constant for several hours. The reaction immediately starts and its linearity indicate that neither the physiological state nor the number of organisms were changed by the assay. DMSO reduction is widespread among microorganisms; out of 144 strains tested (both fungi and bacteria) only 5 were unable to carry out this reaction. The reaction in soil samples was strongly inhibited by toluene, cyanide, azide, or by fumigation, but was considerably stimulated by glucose. These findings demonstrate that the reaction was due to the activity of microorganisms. The DMSO reduction in different soil samples was significantly correlated with arginine ammonification and heat output (r>0.9). A good correlation was observed with the organic-matter content (r = 0.74), but not with microbial numbers, clay content, or the pH of the soil. Standard deviations of less than 10% were routinely found. Furthermore, the method is sufficiently sensitive to allow measurements of activity in very small samples (< 0.1 g). For example, a microbial activity profile can be established for a single soil aggregate, revealing marked differences in activity on the outside and in the interior.

Amendment of soils with arginine resulted in immediate liberation of ammonia. The rate was linear for several hours, and was strongly reduced by toluene treatment or under anaerobic conditions. Together with a strong stimulation of respiration by arginine these results demonstrate that arginine ammonification is due to living microorganisms. Arginine ammonification was strongly related to respiration and correlated significantly with the carbon content of the soil, but not or only poorly with soil pH, ammonia content, percentage clay or the number of microorganisms.