Adsorption/Desorption of toluene on clay minerals

Adsorption/desorption of toluene on montmorillonite, illite, and kaolinite was studied using the batch equilibrium method. The isotherms measured fit the Freundlich equation (r² >0.95). Montmorillonite adsorbed more toluene than illite or kaolinite; the adsorption of toluene on illite and kaolinite was not significantly different. Adsorption of toluene by montmorillonite showed an exponential increase as the ratio of toluene to clay was increased from 5 to 100. The rate studies showed that 62% of the adsorption was completed within 6 h. A rapid desorption was observed initially, followed by slow desorption after 1 h. The desorption rate decreased as the time of adsorption was increased. Almost all of the adsorbed toluene was extracted with water from the clay when the adsorption time was 0.1 h, but only 61% of the toluene could be desorbed when the adsorption time was 24 h.     

Michaelis constant (K m ) of acid phospatase as affected by montmorillonite,illite, and kaolinite clay minerals

The influence of Ca homoionic clay minerals (montmorillonite, illite, and kaolinite) on the activity,K _m , andV _m values of acid phosphatase was examined in model experiments. At each substrate (p-nitrophenyl phosphate) level tested, the addition of increasing amounts of clays (50, 100, and 150 mg, respectively) decreased the activity and increased theK _m value from 1.43×10^–3 m PNP (in the soluble state) to 82.3×10^–3M (montmorillonite), 8.02×10^–3 m (kaolinite), and 7.65×10^–3 m (illite) at the 150 mg level. The maximum enzyme reaction velocity (V _m ) remained nearly constant at different amounts of kaolinite and illite, but increased remarkably with rising quantities of montmorillonite. Apparently, the substrate affinity of sorbed acid phosphatase is significantly lower with montmorillonite than with kaolinite or illite. This may be ascribed to an intensive sorption of both substrate and enzyme to the surface as well as to interlattice sites of montmorillonite.     

The role of particles on the biogeochemical cycling of domoic acid and its isomers in natural water matrices

The adsorption of dissolved domoic acid (DA) and its geometrical isomers was assessed in aqueous solutions containing various types of particles. In one series of experiments carried out in coastal seawater, detectable net adsorption of 100 nM DA occurred only onto natural seawater particles (unfiltered seawater) and 0.5 g L⁻¹ chromatographic silica (18%) in 0.2 μm-filtered seawater. Some net adsorption (<5%) also occurred in the 0.5 g L⁻¹ suspension of estuarine sediment and 0.5 g L⁻¹ solution of humic acid in filtered seawater. No losses were seen in 0.5 g L⁻¹ suspensions of illite, kaolinite, montmorillonite, and silica sand. Biological degradation accounted for small losses (8–10%) in filtered seawater without particles. A second series of experiments using organic-free, <5 μm fractions of kaolinite and montmorillonite in deionized water (DIW) demonstrated that 70% of DA adsorbed onto kaolinite, but only 5% onto montmorillonite. Geometrical isomers of DA (iso-DA D, E, and F) showed negligible adsorption (0–8%) onto a variety of particles in filtered seawater, suggesting that major ions in seawater neutralize electrostatic attractions between particles and DA isomers. These results suggest that DA and its isomers are relatively hydrophilic and not particle reactive. Our data suggest that photochemical and biological degradation of dissolved DA and its isomers appears to occur in bulk surface seawater and its transport to bottom sediments must be mainly biologically driven.     

Influence of clay minerals on sorption of bacteriolytic enzymes

Myxobacteria presumably produce extracellular bacteriolytic enzymes when they are growing in soil. In order to study their ecological significance, adsorption experiments were performed with lytic enzymes produced byMyxococcus virescens in casitone media. Different soils as well as montmorillonite and kaolinite can rapidly adsorb the bacteriolytic but not the proteolytic enzymes. About 1 gm of montmorillonite per liter of cell-free culture solution is enough for the adsorption of 97% of the bacteriolytic enzymes. The adsorption per unit weight is about 100 times greater on montmorillonite than on kaolinite. About 40% of the adsorbed enzymes can be eluted with solutions of high pH or high ionic strength. The only desorbed bacteriolytic enzyme is the alanyl-∈-N-lysine endopeptidase.     

The heterogeneous nature of microbial products as shown by solid-state13C CP/MAS NMR spectroscopy

Homoionic Na-, Ca-, and Al-clays were prepared from the <2 m fractions of Georgia kaolinite and Wyoming bentonite and mixed with sand to give artificial soils with 5, and 25% clay. The artificial soils were inoculated with microbes from a natural soil before incubation. Unlabelled and uniformly¹³C-labelled (99.9% atom) glucose were incorporated into the artificial soils to study the effects of clay types, exchangeable cations and clay contents on the mineralization of glucose-carbon and glucose-derived organic materials. Chemical transformation of glucose-carbon upon incorporation into microbial products and metabolites, was followed using solid-state¹³C CP/MAS NMR spectroscopy.There was a significant influence of exchangeable cations on the mineralization of glucose-carbon over a period of 33 days. At 25% clay content, mineralization of glucose-carbon was highest in Ca-soils and lowest in Al-soils. The influence of exchangeable cations on mineralization of glucose-carbon was more pronounced in soils with bentonite clay than those with kaolinite clay. Statistical analysis of data showed no overall effect of clay type on mineralization of glucose-carbon. However, the interactions of clay type with clay content and clay type with clay content and exchangeable cations were highly significant. At 25% clay content, the mineralization of glucose-carbon was significantly lower in Na- and Al-soils with Wyoming bentonite compared with Na- and Al-soils with Georgia kaolinite. For Ca-soils this difference was not significant. Due to the increased osmotic tension induced by the added glucose, mineralization of glucose-carbon was slower in soils with 5% clay than soils with 25% clay.Despite the differences in the chemical and physical characteristics of soils with Ca-, Na- and Al-clays, the chemical composition of organic materials synthesised in these soils were similar in nature. Assuming CP/MAS is quantitative, incorporation of uniformly¹³C-labelled glucose (99.9% atom) in these soils resulted in distribution of carbon in alkyl (24–25%), O-alkyl (56–63%), carbonyl (11–15%) and small amounts of aromatic and olefinic carbon (2–4%). However, as decomposition proceeded, the chemistry of synthesised material showed some changes with time. In the Ca- and Na-soils, the proportions of alkyl and carbonyl carbon decreased and that of O-alkyl carbon increased with time of incubation. However, the opposite trend was found for the Al-soil.Proton-spin relaxation editing (PSRE) subspectra clearly showed heterogeneity within the microbial products. Subspectra of the slowly-relaxing (long T₁(H)) domains were dominated by alkyl carbon in long- and short-chain structures. The signals due to N-alkyl (55 ppm) and carbonyl carbon were also strong in these subspectra. These subspectra were very similar to those obtained for microbial and fungal materials and were probably microbial tissues attached to clay surfaces by polysaccharide extracellular mucilage. Subspectra of fast-relaxing (short T₁(H)) domains comprised mostly O-alkyl and carbonyl carbon and were probably microbial metabolites released as neutral and acidic sugars into the extracellular environment, and strongly sorbed by clay surfaces.     

Sorption and desorption of copper by and from clay minerals

Summary The sorption of Cu by different clay minerals from dilute CuSO₄ solutions was studied as a function of pH. It was found that Cu sorption increased with increasing the equilibrium pH. The low sorption at low pH values was attributed to the competition effect of H⁺ ions and the release of octahedral Mg, Fe and Al from the 2: 1 minerals in acid solutions. The higher sorption of copper at higher pH values was related to the absence of H⁺ ions and to the increase in the pH-dependent negative charge in kaolinite and gibbsite.The desorption of copper using solutions of 1 N NaCl at different pH values indicated that kaolinite and montmorillonite released large amounts of their adsorbed Cu even at high pH values. Vermiculite, on the other hand, exhibited a strong retention of Cu against extraction with NaCl. Oven-drying had no significant effect on the desorption characteristics of the Cu-saturated clays.The Ca-Cu exchange isotherms on montmorillonite were studied at two different pH values. The isotherms indicated a preference of Ca at the lower pH (pH 3.5), with K = 0.931 and G = +41.0 cal./mole. At the higher pH (5.2) the isotherms indicated a preference of Cu with K = 1.282 and G = –141.0 cal./mole. The difference was attributed to the competition of H⁺ at low pH.     

Factors affecting the growth form of Aspergillus terreus NRRL 1960 in relation to itaconic acid fermentation

The effect of medium composition on the growth form of Aspergillus terreus NRRL 1960 in relation to itaconic acid fermentation has been studied. Four types of mycelial pellets were obtained under the conditions used and may be classified as (a) frayed and loose with 0.1–0.5 mm diameter (b) compact with 0.1–0.5 mm diameter (c) loose with 0.5–2.0 mm diameter and (d) compact with 0.5–2.0 mm diameter. Their respective maximum specific rates of formation and yields of itaconic acid, based on 100 g sucrose supplied, were (a) 1.25 mol mg^–1h^–1 and 55–59 g, (b) 0.27–0.43 mol mg^–1 h^–1 and 26–38 g, (c) 0.75–0.90 mol mg^–1 h^–1 and 45–51 g and (d) 0.12 mol mg^–1 h^–1 and 10 g. The presence of Ca²⁺, Zn²⁺ and Fe²⁺ in the basal medium at concentrations of 23.3 mg/100 ml, 0.01 mg/100 ml and 0.006 mg/100 ml respectively were found to be adequate and crucial in obtaining the desired outgrowth for both high production rates and consistent yields of itaconic acid. The further addition of either commercial plaster of Paris or analytical-reagent-grade CaSO₄, especially when activated by heating to 530°C and present in excess of solubility, results in small and frayed pellets, which lead to itaconic acid yields of 55–59 g acid/100 g sugar supplied.     

Effect of Mineral and Organic Soil Constituents on Microbial Mineralization of Organic Compounds in a Natural Soil

This research addressed the effect of mineral and organic soil constituents on the fate of organic compounds in soils. Specifically, it sought to determine how the associations between organic chemicals and different soil constituents affect their subsequent biodegradation in soil. Four ¹⁴C-labeled surfactants were aseptically adsorbed to montmorillonite, kaolinite, illite, sand, and humic acids. These complexes were mixed with a woodlot soil, and ¹⁴CO₂ production was measured over time. The mineralization data were fitted to various production models by nonlinear regression, and a mixed (3/2)-order model was found to most accurately describe the mineralization patterns. Different mineralization patterns were observed as a function of the chemical and soil constituents. Surfactants that had been preadsorbed to sand or kaolinite usually showed similar mineralization kinetics to the control treatments, in which the surfactants were added to the soil as an aqueous solution. Surfactants that had been bound to illite or montmorillonite were typically degraded to lesser extents than the other forms, while surfactant-humic acid complexes were degraded more slowly than the other forms. The desorption coefficients (K_d) of the soil constituent-bound surfactants were negatively correlated with the initial rates of degradation (k₁) and estimates of ¹⁴CO₂ yield (P_o) as well as actual total yields of ¹⁴CO₂. However, there was no relationship between K_d and second-stage zero-order rates of mineralization (k_o). Microbial community characteristics (biomass and activity) were not correlated with any of the mineralization kinetic parameters. Overall, this study showed that environmental form had a profound effect on the ultimate fate of biodegradable chemicals in soil. This form is defined by the physicochemical characteristics of the chemical, the composition and mineralogy of the soil, and the mode of entry of the chemical into the soil environment.     

Comparison of photomixotrophic and heterotrophic callus and suspension cultures of Pinus elliottii. 1. Photosynthetic properties and ultrastructural evidence for coexistence of starch granules and secondary metabolites

Photomixotrophic callus and suspension cultures of salsh pine (Pinus elliottii var. elliottii Engelm.) have been established. Callus tissues contained up to 2.76 g chlorophyll mg^-1 dry wt and suspensions 2.98 g chlorophyll mg^-1 dry wt. Maximum photosynthetic oxygen evolution was 25–32 mol O₂ h^-1 mg^-1 chlorophyll for callus and 35–39 mol O₂h^-1 mg^-1 chlorophyll for suspension, respectively. Photomixotrophic callus was friable with a high moisture content during early and exponential growth, but evolved into a compact and dense tissue during the latter stage of growth. Compact photomixotrophic callus accumulated and deposited secondary metabolites in the central vacuole and developed large starch granules in the chloroplasts. Secondary metabolites were not observed in photomixotrophic suspensions or in heterotrophic calli and suspensions. Photomixotrophic callus contained numerous mitochondria closely associated with well-developed chloroplasts containing 2–6 thylakoids per granum. Heterotrophic callus was characterized by a poorly developed cytoplasm and cup-shaped mitochondria.     

Immobilisation of lipases by adsorption and deposition: high protein loading gives lower water activity optimum

Two different immobilisation techniques for lipases were investigated: adsorption on to Accurel EP-100 and deposition on to Celite. The specific activities were in the same order of magnitude, 2.9 (mol min^–1 mg protein) when Celite was used as support and 2.3 (mol min^–1 mg^–1 protein) when Accurel EP-100 was used as support, even if the amount of lipase loaded differed by 2 orders of magnitude. Immobilisation on Accurel EP-100 was the preferred technique since 40–100 times more protein can be loaded/per g carrier, thus yielding a more active catalyst. The water activity profiles in lipase catalysed esterification were influenced by the amount of protein adsorbed to Accurel EP-100. Higher protein loading (40 mg g^–1) resulted in a bell-shaped water activity profile with highest specific activity (6.1 mol min^–1 mg^–1 protein) at a _w=0.11, while an enzyme preparation with low protein loading (4 mg g^–1) showed highest specific activity at a _w=0.75.     

Some aspects of the chemistry of lithium in soils

Summary A method for the determination of exchangeable lithium using 0.5M NH₄Cl is described. The range of exchangeable Li in the fifty Papua New Guinea (PNG) soils analyzed was 0.002 to 0.409 gg^–1 in contrast to five Australian soils which ranged from 0.032 to 0.830 gg^–1. The PNG soils were divided into hill and alluvial soils with average exchangeable Li contents of 0.062 and 0.263 gg^–1 respectively. No significant correlation between total and exchangeable Li was found in either group of soils althoughr=0.67 for the comined data and was significant at the 5% level. From the analysis of three profiles exchangeable Li was found to be at least twice as high (0.27 gg^–1) in surface soils as in subsurface samples (0.10 gg^–1). The average value of the deeper subsoil samples was 0.18 ppm.R mode cluster analysis of the data for village garden soils collected on a sampling grid showed that exchangeable Li was more strongly assoicated with Ca and Mg than with pH, 0.05M EDTA soluble Zn, 0.5M NaHCO₃ soluble P or exchangeable Na and K. Computer constructed isographs using the analyses of grid samples from a garden illustrated the association between Li, Ca and Mg and the inverse association with Na.The correlation coefficient between Ca and Li in the ash of three food plants (Gnetum gnemon, Hibiscus abelmoschus andStenochlaena plustris) while not significant on an individual basis, was significant when the data was combined suggesting that the association between these elements in the soil may reflect an association in the ash returned to the soil when the garden was cleared. The correlation coefficient between soil exchangeable Li and Li in plant ash was positive, but not significant.Adsorption experiments over a five-day period demonstrated that Li was strongly adsorbed from solution. On average 63–75% of the adsorbed Li was fixed in a form which was not exchangeable with 0.5M NH₄Cl or soluble in 0.05M EDTA.     

Phosphate sorption isotherms for evaluating phosphorus requirement of wetland rice soils

Summary Phosphate sorption isotherms were developed for five Philippine wetland rice soils using the conventional technique and a modified one. In the conventional method, P requirements of soils varied between 280 and 810 g P/g soil. In the modified method, they varied from 160 to 540 g P/g soil at 0.2 ppm P in solution. Soils with high P-sorption capacities had vermiculite and halloysite as the dominant clay minerals. Soil reduction by flooding decreased P-sorption by 28–70 percent at 0.2 ppm P in solution. The decrease in P-sorption due to soil reduction was greatest in a crystalline soil with vermiculite and halloysite as the dominant clay minerals and least in a soil with dominant X-ray amorphous silicates in the clay fraction.Desorption of freshly adsorbed P under reduction was greater in HCO ₃ ^– solution than in CaCl₂ and it increased with level of applied P. Desorption patterns of freshly adsorbed P were similar to adsorption patterns but values of P in solution were lower at desorption. Soils varied with respect to desorption of freshly sorbed P. Desorption studies indicate that soils vary in intensity factor with respect to P and thus influence P availability to plants. Use of P-sorption and P-desorption data obtained under reduced soil condition was proposed for detecting P needs of submerged rice soils.Results of a pot study with IR36 at different levels of solution P (reduced) in one soil indicated a high degree of correlation between adjusted P levels and the measured growth parameters. About 0.12 ppm P in the soil solution or 0.46 ppm P desorbed in HCO ₃ ^– solution (equivalent to 100 mg P/kg soil) was adequate for near-maximum plant height, tiller production, total dry matter yield, plant P content, and total P uptake.     

Uptake of selenite,selenomethionine and selenate by brush border membrane vesicles isolated from rat small intestine

The uptake of selenite, selenate and selenomethionine (SeMet) was performed with brush border membrane vesicles (BBMV) prepared from rats fed selenium-deficient and supplemented diets. At equilibrium (60 min), the uptake of ⁷⁵Se from [⁷⁵Se]selenite ranged from 16.5 to 18.9 nmol mg^-1 protein. There was a curvilinear relationship in the uptake of selenite over a concentration range of 10–1000 m. About 2 nmol mg^-1 protein was obtained with selenomethionine (SeMet) which occurred between 90 and 180 s. In contrast to selenite, there was a linear relationship in the initial uptake of SeMet over a concentration range of 10–1000 m. The uptake of selenate was approximately 50-fold lower than selenite, reaching 350 pmol mg^-1 protein. Dietary selenium level had no effect on the rate of ⁷⁵Se accumulation by BBMV. Dramatic differences are found in the uptake and binding of selenium by BBMV incubated with different selenocompounds.     

Short-term effects of biological and physical forces on aggregate formation in soils with different clay mineralogy

The mechanisms resulting in the binding of primary soil particles into stable aggregates vary with soil parent material, climate, vegetation, and management practices. In this study, we investigated short-term effects of: (i) nutrient addition (Hoagland's solution), (ii) organic carbon (OC) input (wheat residue), (iii) drying and wetting action, and (iv) root growth, with or without dry–wet cycles, on aggregate formation and stabilization in three soils differing in weathering status and clay mineralogy. These soils included a young, slightly weathered temperate soil dominated by 2:1 (illite and chlorite) clay minerals; a moderately weathered soil with mixed [2:1 (vermiculite) and 1:1 (kaolinite)] clay mineralogy and oxides; and a highly weathered tropical soil dominated by 1:1 (kaolinite) clay minerals and oxides. Air-dried soil was dry sieved through a 250 m sieve to break up all macroaggregates and 100 g-subsamples were brought to field capacity and incubated for 42 days. After 14 and 42 days, aggregate stability was measured on field moist and air-dried soil, to determine unstable and stable aggregation respectively. In control treatments (i.e., without nutrient or organic matter addition, without roots and at constant moisture), the formation of unstable and stable macroaggregates (> 250 m) increased in the order: 2:1 clay soil < mixed clay soil < 1:1 clay soil. After 42 days of incubation, nutrient addition significantly increased both unstable and stable macroaggregates in the 2:1 and 1:1 clay soils. In all soils, additional OC input increased both unstable and stable macroaggregate formation. The increase in macroaggregation with OC input was highest for the mixed clay soil and lowest for the 1:1 clay soil. In general, drying and wetting cycles had a positive effect on the formation of macroaggregates. Root growth caused a decrease in unstable macroaggregates in all soils. Larger amounts of macroaggregates were found in the mixed clay and oxides soil when plants were grown under 50% compared to 100% field capacity conditions. We concluded that soils dominated by variable charge clay minerals (1:1 clays and oxides) have higher potential to form stable aggregates when OC concentrations are low. With additional OC inputs, the greatest response in stable macroaggregate formation occurred in soils with mixed mineralogy, which is probably a result of different binding mechanisms occurring: i.e., electrostatic bindings between 2:1 clays, 1:1 clays and oxides (i.e. mineral-mineral bindings), in addition to OM functioning as a binding agent between 2:1 and 1:1 clays.     

Production of thermostable α-galactosidase from thermophilic fungusHumicola sp

The thermophilic fungus,Humicola sp isolated from soil, secreted extracellular -galactosidase in a medium cotaining wheat bran extract and yeast extract. Maximum enzyme production was found in a medium containing 5% wheat bran extract as a carbon source and 0.5% beef extract as a carbon and nitrogen source. Enzyme secretion was strongly inhibited by the presence of Cu²⁺, Ni²⁺ and Hg²⁺ (1mM) in the fermentation medium. Production of enzyme under stationary conditions resulted in 10-fold higher activity than under shaking conditions. The temperature range for production of the enzyme was 37° C to 55°C, with maximum activity (5.54 U ml^–1) at 45°C. Optimum pH and temperature for enzyme activity were 5.0 and 60° C respectively. One hundred per cent of the original activity was retained after heating the enzyme at 60°C for 1 h. At 5mM Hg²⁺ strongly inhibited enzyme activity. TheK _m andV _max forp-nitrophenyl--d-galactopyranoside were 60M and 33.6 mol min^–1 mg^–1, respectively, while for raffinose those values were 10.52 mM and 1.8 mol min^–1 mg^–1, respectively.     

Physiological energetics of a midge,Chironomus riparius Meigen (Insecta,Diptera): normoxic heat output over the whole life cycle and response of larva to hypoxia and anoxia

The rate of metabolism of laboratory reared Chironomus riparius was monitored by direct calorimetry over the entire life cycle from egg to adult stage. The metabolic response of the fourth instar larva to decreasing oxygen concentrations and anoxia was also measured. Normoxic measurements were carried out at 20°C and the hypoxic-anoxic experiments at 10°C. In larvae with body sizes ranging from 0.0028 to 0.645 mg ash-free dry mass (afdm), the rate of heat dissipation was related to body mass by a power function, with a mass exponent of 0.71±0.02 corresponding to an exponent of -0.29 for the relationship between mass-specific metabolic rate and body mass. However, the allometric equations applicable to larvae would not predict the metabolic rates of eggs, pupae and adults. Single egg batches used in the experiments consisted of 354±90 eggs, the individual egg with a mass of 0.99±0.01 g (mean±SD). The mass-specific rate of heat dissipation of the egg (13.7±1.8 W mg^-1 afdm) was considerably lower than that of the first and second instar larvae (44–53 W mg^-1) but equal to that of fourth instar larvae (13.1±3.9 W mg^-1). Heat dissipation by a pupa shortly before adult emergence was high (14.8±1.8 W mg^-1), probably due to high metabolism during metamorphosis. Emergence of the adult in the calorimeter was indicated by a short but intense burst of heat. The newly emerged imago had a ca. 20–35% higher metabolic rate than the pupa. In response to reduced O₂ partial pressure the fourth instar larva of C. riparius displayed metabolic regulation. In continuously declining oxygen partial pressure, the fourth instar larva maintained its aerobic energy metabolism (4.2 W mg^-1) with only a small decrease down to 0.8 kPa, corresponding to an oxygen concentration of 0.42 mg O₂l^-1 H₂O. Below this critical oxygen concentration (P_c), the rate of heat dissipation decreased rapidly down to the anoxic level which was only 14–17% of the normoxic level. The high relative reduction of metabolic rate under anoxia gives a wrong impression of short-term tolerance of C. riparius to anoxia. The absolute energetic costs of C. riparius associated with anaerobic energy metabolism (0.64±0.11 W mg^-1) are almost 6 times higher than those of more anoxia tolerant invertebrates such as sphaeriid bivalves.     

Distribution of sulphur forms in soils from beech and spruce forests of Mont Lozère (France)

From a quantitative inventory of sulphur forms and sulphur budget, the relation between the distribution of the various sulphur forms and the sulphate fluxes in three soil profiles has been addressed. These profiles are located in two forested watersheds at Mont Lozère. One has been sampled in a beech forest and the other two in a spruce forest and in a harvested plot of this spruce forest, respectively. The mean annual input-output budgets showed a sulphur immobilization in the soil cover of the three plots. In the preserved spruce forest plot, because of larger dry depositions, the sulphur immobilization is much greater than in other plots and occurs essentially in the B horizons. In the other two profiles, the dominant immobilization occurs in the parent material.The total sulphur content is very high in the forest floor reaching 2065 g S g^-1 in the litter of one of the soils under spruce. In the organo-mineral horizons of soils under spruce, the total sulphur content decreases with depth and ranges from 310 to 520 g S g^-1 in the A horizons to 100–200 g S g^-1 in the parent material. In the profile under beech, the total sulphur content is lower except in the parent material. In all cases, the organic sulphur is the major part of sulphur often representing more than 90% of total sulphur. In organo-mineral soil horizons of the spruce forest, the part of the sulphateesters is more important than in the soil of the beech forest, probably related to the different nature of the microbial activity in the spruce forest. In contrast, the humification processes are more efficient in the soil under beech, which can be due to the greater input of organic sulphur by litterfall. It appears that the dominant organic sulphur form varies as a function of microbial ecology and sulphate flux. The maximum of the inorganic sulphate is located at the base of the B horizons in the soil of the spruce forest and in the parent material of the soil under beech. In these horizons, the high content of inorganic sulphate can be related to the higher amounts of amorphous Fe and Al phases.     

Response of Rhizobium leguminosarum to nickel stress

Rhizobium leguminosarum strain P-5 biovar viciae was sensitive to Ni²⁺ (MIC, 75 M) and showed concentration-dependent Ni²⁺ uptake in a wide concentration range (50–500 M). Ni²⁺ uptake up to a certain threshold limit also increased thiol content (66 nmol mg^–1 protein), proline content (10.85 nmol mg^–1 protein) and urease specific activity (500 nmol min^–1 mg^–1 protein) maximum corresponding to 100 M Ni²⁺ as the external concentration or 151 nmol Ni²⁺ mg^–1 protein as the intracellular buildup. Proline synthesis was stimulated most even at much lower Ni²⁺ concentration (25 M). Higher intracellular Ni²⁺ load neither favoured thiol nor proline biosynthesis nor urease activity. Ni²⁺ requirement of urease was ascertained by using EDTA-grown cells and the addition of bicarbonate (NaHCO₃, 100 mM) to the crude extract. The induction of thiol or proline by Ni²⁺, therefore, reflects the possible strategies adopted by bacterial cells to overcome the environmental stress.     

Activation of immunoglobulin control elements in trasgenic mice

To assess the role interleukins and mitogens play in regulating immunoglobulin (Ig) gene expression via the Ig enhancer and promoter, transgenic mice carrying two different Ig gene regulatory regions were generated. One, EkCAT, contains the Ig heavy chain enhancer (E) and the light chain promoter driving the chloramphenicol acetyltransferase (CAT) gene. In the other, EkCAT, CAT is under the control of the promoter alone. E and relative activity were assessed by CAT assay. In EkCAT mice, low CAT expression was consistently found in spleen, bone marrow, mesenteric lymph node, and thymus but not in brain, lung, or kidney. In EkCAT mice, CAT expression was detectable just above background in lymphoid tissues, suggesting a basic level of tissue specificity in the absence of the enhancer. Whole spleen cell cultures prepared from the mice were treated with lymphokines and mitogens. Lipopolysaccharide (LPS), concanavilin A (Con A), interleukin 6 (IL-6), and interferon- (IFN-) increased CAT expression to varying extents in cells derived from EkCAT mice but not in spleen cells prepared from EkCAT mice. Thus, the presence of E, in addition to the promoter, is essential for the stimulation of CAT expression mediated by these factors. B cells from EkCAT mice were separated by density into populations of small and large cells. In untreated small B cells, no CAT expression was detected and only addition of LPS resulted in an increase in CAT expression. In large B cells, CAT was expressed at a low level without addition of exogenous factors. Incubation with LPS, IL-6, Con A and IFN- caused CAT expression to increase several-fold. This transgenic system provides a means to identify exogenous factors that activate Ig enhancers and promoters.This work has been submitted in partial fulfillment of the requirements for the doctoral degree from the George Washington University.     

Composition and mean residence time of molecular weight fractions of organic matter extracted from two soils under different forest species

The organic matter extracted from various mineral horizons of two forest soils, one under silver fir (Abies alba Mill.), the other under European beech (Fagus sylvatica L.), was fractionated by dialysis into three fractions, 100–1000, 1000–8000, and >8000Da. On a C basis, in all horizons the recovered organic matter amounted to less than a half of the total and was mainly composed of molecules >8000Da. The 100–1000Da fraction had a principal elemental composition profoundly different from the other two fractions, which, instead differed from each other significantly only for the S content and the molar ratio of C with N. No significant difference in this regard was found between soils. The richness in O and some typical absorption bands in the FT-IR spectra indicated that the 100–1000Da fraction had a lot of carboxyl moieties. The spectroscopic (¹³C NMR) investigation showed that the 1000–8000 and >8000Da fractions had a prevalently aliphatic nature and signals attributable to polysaccharides (O-alkyl C) revealed overall a high presence of non-humic biopolymers. These latter were significantly more abundant, suggesting a lower degree of humification, in the >8000Da fraction than in the 1000–8000Da fraction. Comparing soils, that under beech appeared significantly richer in O-alkyl C than that under fir. The organics extracted from the A horizon of both soils had positive ¹⁴C values, indicating recent synthesis mainly due to the present forest cover. The mean residence time (MRT) of the combined 100–1000Da and 1000–8000Da fractions and the >8000Da fraction increased with depth, even to about 5000 years in the more than 1-m deep BC horizons under beech. In some cases, and especially in the soil under fir, despite higher values of ¹³C denoting stronger microbial decomposition, the 100–8000Da fraction showed a higher MRT than that of the >8000Da fraction, perhaps due to its ascertained lower content of non-humic biopolymers.