Effect of proteins on reovirus adsorption to clay minerals

Organic matter in sewage, soil, and aquatic systems may enhance or inhibit the infectivity of viruses associated with particulates (e.g., clay minerals, sediments). The purpose of this investigation was to identify the mechanisms whereby organic matter, in the form of defined proteins, affects the adsorption of reovirus to the clay minerals kaolinite and montmorillonite and its subsequent infectivity. Chymotrypsin and ovalbumin reduced the adsorption of reovirus to kaolinite and montmorillonite homoionic to sodium. Lysozyme did not reduce the adsorption of the virus to kaolinite, but it did reduce adsorption to montmorillonite. The proteins apparently competed with the reovirus for sites on the clay. As lysozyme does not adsorb to kaolinite by cation exchange, it did not inhibit the adsorption of reovirus to this clay. The amount of reovirus desorbed from lysozyme-coated montmorillonite was approximately 38% less (compared with the input population) than that from uncoated or chymotrypsin-coated montmorillonite after six washings with sterile distilled water. Chymotrypsin and lysozyme markedly decreased reovirus infectivity in distilled water, whereas infectivity of the virus was enhanced after recovery from an ovalbumin-distilled water-reovirus suspension (i.e., from the immiscible pelleted fraction plus supernatant). The results of these studies indicate that the persistence of reovirus in terrestrial and aquatic environments may vary with the type of organic matter and clay mineral with which the virus comes in contact.     

Effect of dietary phosphate intake on phosphate transport by isolated rat renal brush-border vesicles

Renal brush-border membrane vesicles isolated from rats kept for 6-8 weeks on a low-phosphate diet (0.15% of dry matter) showed a markedly faster Na(+)-dependent phosphate uptake than did membrane vesicles isolated from animals kept on a high-phosphate diet (2% of dry matter). Phosphate-uptake rate by brush-border membrane vesicles isolated from animals on a low-phosphate diet remained significantly increased after acute parathyroidectomy. Dietary adaptation was also observed in animals that had been parathyroidectomized before exposure to the different diets. In animals on the low-phosphate diet parathyrin administration inhibited phosphate uptake by brush-border vesicles only if the animals were repleted with P(i) (5ml of 20mm-NaH(2)PO(4)) 1h before being killed. After acute phosphate loading and parathyrin administration the difference in the transport rate between the two dietary groups remained statistically significant. The results suggest that the adaptation of proximal-tubule phosphate transport to dietary intake of phosphate is reflected in the Na(+)/phosphate co-transport system located in the luminal membrane of the proximal-tubule cell. Since the dietary effects on phosphate transport by brush-border membranes are only partially reversed by acute changes in parathyrin concentration and are also observed in chronically parathyroidectomized animals, the adaptation of the Na(+)/phosphate co-transport system to dietary phosphate intake seems to involve an additional mechanism independent of parathyrin.     

Effect of proteins on reovirus adsorption to clay minerals.

Organic matter in sewage, soil, and aquatic systems may enhance or inhibit the infectivity of viruses associated with particulates (e.g., clay minerals, sediments). The purpose of this investigation was to identify the mechanisms whereby organic matter, in the form of defined proteins, affects the adsorption of reovirus to the clay minerals kaolinite and montmorillonite and its subsequent infectivity. Chymotrypsin and ovalbumin reduced the adsorption of reovirus to kaolinite and montmorillonite homoionic to sodium. Lysozyme did not reduce the adsorption of the virus to kaolinite, but it did reduce adsorption to montmorillonite. The proteins apparently competed with the reovirus for sites on the clay. As lysozyme does not adsorb to kaolinite by cation exchange, it did not inhibit the adsorption of reovirus to this clay. The amount of reovirus desorbed from lysozyme-coated montmorillonite was approximately 38% less (compared with the input population) than that from uncoated or chymotrypsin-coated montmorillonite after six washings with sterile distilled water. Chymotrypsin and lysozyme markedly decreased reovirus infectivity in distilled water, whereas infectivity of the virus was enhanced after recovery from an ovalbumin-distilled water-reovirus suspension (i.e., from the immiscible pelleted fraction plus supernatant). The results of these studies indicate that the persistence of reovirus in terrestrial and aquatic environments may vary with the type of organic matter and clay mineral with which the virus comes in contact.     

Nucleoside phosphorylation by phosphate minerals

In the presence of formamide, crystal phosphate minerals may act as phosphate donors to nucleosides, yielding both 5'- and, to a lesser extent, 3'-phosphorylated forms. With the mineral Libethenite the formation of 5'-AMP can be as high as 6% of the adenosine input and last for at least 10(3) h. At high concentrations, soluble non-mineral phosphate donors (KH(2)PO(4) or 5'-CMP) afford 2'- and 2':3'-cyclic AMP in addition to 5'-and 3'-AMP. The phosphate minerals analyzed were Herderite Ca[BePO(4)F], Hureaulite Mn(2+)(5)(PO(3)(OH)(2)(PO(4))(2)(H(2)O)(4), Libethenite Cu(2+)(2)(PO(4))(OH), Pyromorphite Pb(5)(PO(4))(3)Cl, Turquoise Cu(2+)Al(6)(PO(4))(4)(OH)(8)(H(2)O)(4), Fluorapatite Ca(5)(PO(4))(3)F, Hydroxylapatite Ca(5)(PO(4))(3)OH, Vivianite Fe(2+)(3)(PO(4))(2)(H(2)O)(8), Cornetite Cu(2+)(3)(PO(4))(OH)(3), Pseudomalachite Cu(2+)(5)(PO(4))(2)(OH)(4), Reichenbachite Cu(2+)(5)(PO(4))(2)(OH)(4), and Ludjibaite Cu(2+)(5)(PO(4))(2)(OH)(4)). Based on their behavior in the formamide-driven nucleoside phosphorylation reaction, these minerals can be characterized as: 1) inactive, 2) low level phosphorylating agents, or 3) active phosphorylating agents. Instances were detected (Libethenite and Hydroxylapatite) in which phosphorylation occurs on the mineral surface, followed by release of the phosphorylated compounds. Libethenite and Cornetite markedly protect the beta-glycosidic bond. Thus, activated nucleic monomers can form in a liquid non-aqueous environment in conditions compatible with the thermodynamics of polymerization, providing a solution to the standard-state Gibbs free energy change (DeltaG degrees ') problem, the major obstacle for polymerizations in the liquid phase in plausible prebiotic scenarios.     

Effect of bacteria on the inactivation and adsorption on clay minerals of reovirus

This investigation studied the antiviral activity of, and the utilization of viruses as substrates by, bacteria. Reovirus type 3 and bacterial species representative of those endemic to sewage, aquatic, and terrestrial habitats were used in the model systems. Culture supernatants from Bacillus subtilis maintained for 5 days in a minimal salts medium displayed antiviral activity, but supernatants from Escherichia coli or Serratia marcescens did not. Both live and toluene-killed cells reduced the inactivation of reovirus during 4 days of incubation at 23 +/- 2 degrees C. This protective effect was more pronounced with killed than with live cells of B. subtilis, confirming the presence of an antiviral component(s) in this species and indicating that the component(s) was metabolic in origin. When reovirus was presented to these bacteria as a sole source of carbon, some growth (determined spectrophotometrically) of B. subtilis and S. marcescens occurred with reovirus concentrations of 3.1 X 10(6) and 8.2 X 10(6) mean tissue culture infective dose-fifty X mL-1, respectively. Growth of S. marcescens did not occur with a reovirus concentration of 8.0 X 10(4) mean tissue culture infective dose-fifty X mL-1, nor did that of E. coli with any virus concentration used in this study. Adsorption of reovirus on kaolinite was enhanced by the culture supernatant from S. marcescens and on montmorillonite, albeit to a lesser extent, by that from E. coli. The effect of culture supernatants from B. subtilis on the adsorption of reovirus on clay minerals could not be determined, as a result of the antiviral component produced by these cells. The virus was not adsorbed on the bacteria.     

Amplification of DNA bound on clay minerals

DNA adsorbs and binds on clay minerals, which provides protection to the DNA against degradation by nucleases but does not eliminate the ability of bound DNA to transform cells. These observations support the concept that 'cryptic genes' can persist in the environment when bound on particles and that the genes could subsequently be expressed if an appropriate host was transformed. The polymerase chain reaction (PCR) was used to amplify free and bound DNA from Bacillus subtilis and calf thymus. DNA bound on montmorillonite, but not on kaolinite, was amplified. However, amplification occurred when kaolinite was pretreated with sodium metaphosphate. DNA was not released from the clays during the amplification procedure. The type of clay (e.g. its structure and charges) affected amplification. Because DNA bound on clay is protected against biodegradation, the ability to amplify DNA bound on clay by the PCR has palaeontological, archaeological, and anthropological implications for the detection of 'ancient' DNA, as well as for monitoring the persistence of recombinant DNA introduced to the environment in genetically modified organisms.     

乙酸对土壤胶体矿物吸附酸性磷酸酶的影响

研究了不同pH值、不同浓度乙酸对酸性磷酸酶在土壤胶体和矿物表面吸附的影响,结果表明,在pH2～8的乙酸体系中,酶在胶体矿物表面的最大吸附pH一般出现在蛋白的等电点和矿物的零电荷点(PZC)之间,各土壤胶体和粘粒矿物对酶的吸附量大小顺序为针铁矿》黄棕壤>砖红壤>高岭石>二氧化锰,乙酸浓度对酶在胶体矿物表面的吸附量和吸附结合能具有较显著影响,在0～200mmol·L^-1范围内,随着乙酸浓度的增加,酶吸附量呈现先升高、后降低、再稳定的趋势,而吸附结合能的变化与此相反,并就乙酸对酶在胶体矿物表面吸附影响的可能机理进行了初步探讨。     

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.     

Effect of the clay minerals montmorillonite and kaolinite on the genetic transformation of competentBacillus subtilis cells

The effect of the clay minerals montmorillonite and kaolinite on the transformation of competentBacillus subtilis cells with chromosomal DNA was studied. Clay particles were found to substantially increase the transformation frequency of competent cells, as well as the rate of their spontaneous chromosomal and plasmid transformation. The effect was ascribed to the adsorption of bacterial cells on the surface of mineral particles.     

Transformation of clay minerals caused by an alkaliphilic cyanobacterial community

Transformation of clay minerals (smectite-zeolite, illite, kaolinite, and bentonite) and admixtures of iron oxides (hydroxides) under the action of an alkaline cyanobacterial community was studied. The results demonstrate that the processes of transformation of clay minerals such as intensification of removal of exchange bases and dissolution of silicates and iron oxides occurred in the presence of the alkaliphilic cyanobacterial community. The main factor that determines resistance of a mineral to biochemical weathering is its composition. Transformations of clay minerals in the course of active cyanobacterial photosynthesis (up to 14 days) and at decomposition of organic matter (OM) (28–60 days) are different. For smectite-zeolite and illite, these processes are dissolution of silicates and oxides (removal of Si and Fe) and removal of exchange bases (K), which were observed at both the of biomass production and OM destruction stages. For two other clays, the processes of neosynthesis are more typical: formation of carbonates (most probably siderite for bentonite clay and Mg-calcite for kaolin clay) and transformation of ferrihydrite into the more thermodynamically stable goethite.     

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.     

Growth inhibition of the rumen bacterium Selenomonas ruminantium by ammonium salts

Summary The objective of this study was to determine the maximum ammonium source concentration tolerated by Selenomonas ruminantium and its metabolic response to high ammonium source concentrations. The ammonia-nitrogen half-inhibition constant (K _i) in defined basal medium was 239 mabetm for NH₄Cl, 173 mabetm for NH₄OH, 153 mabetm for (NH₄)₂SO₄ and 110 mabetm for NH₄HCO₃. Reduction in continuous culture maximal growth rate was similar to the reduction in the batch culture logarithmic growth rate for the respective NH₄Cl concentrations. Cell yield when expressed as Y _ATP decreased for 150 and 200 mabetm NH₄C1. the NH₃-N K _i estimates are in line with inhibiting concentrations observed for other bacteria and suggest that energy efficiency is reduced when the NH₃-N concentration is increased. Offprint requests to: S. C. Ricke     

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.     

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.