Heavy metals alter the electrokinetic properties of bacteria, yeasts, and clay minerals.

The electrokinetic patterns of four bacterial species (Bacillus subtilis, Bacillus megaterium, Pseudomonas aeruginosa, and Agrobacterium radiobacter), two yeasts (Saccharomyces cerevisiae and Candida albicans), and two clay minerals (montmorillonite and kaolinite) in the presence of the chloride salts of the heavy metals, Cd, Cr, Cu, Hg, Ni, Pb, and Zn, and of Na and Mg were determined by microelectrophoresis. The cells and kaolinite were net negatively charged at pH values above their isoelectric points (pI) in the presence of Na, Mg, Hg, and Pb at an ionic strength (mu) of 3 x 10(-4); montmorillonite has no pI and was net negatively charged at all pH values in the presence of these metals. However, the charge of some bacteria, S. cerevisiae, and kaolinite changed to a net positive charge (charge reversal) in the presence of Cd, Cr, Cu, Ni, and Zn at pH values above 5.0 (the pH at which charge reversal occurred differed with the metal) and then, at higher pH values, again became negative. The charge of the bacteria and S. cerevisiae also reversed in solutions of Cu and Ni with a mu of greater than 3 x 10(-4), whereas there was no reversal in solutions with a mu of less than 3 x 10(-4). The clays became net positively charged when the mu of Cu was greater than 3 x 10(-4) and that of Ni was greater than 1.5 x 10(-4). The charge of the cells and clays also reversed in solutions containing both Mg and Ni or both Cu and Ni (except montmorillonite) but not in solutions containing both Mg and Cu (except kaolinite) (mu = 3 x 10(-4)). The pIs of the cells in the presence of the heavy metals were at either higher or lower pH values than in the presence of Na and Mg. Exposure of the cells to the various metals at pH values from 2 to 9 for the short times (ca. 10 min) required to measure the electrophoretic mobility did not affect their viability. The specific adsorption on the cells and clays of the hydrolyzed species of some of the heavy metals that formed at higher pH values was probably responsible for the charge reversal. These results suggest that the toxicity of some heavy metals to microorganisms varies with pH because the hydrolyzed speciation forms of these metals, which occur at higher pH values, bind on the cell surface and alter the net charge of the cell.(ABSTRACT TRUNCATED AT 400 WORDS)     

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.     

Cationic specificity of a Ca2+-accumulating system in smooth muscle cell mitochondria

In the experiments conducted with application of an isotopic technique (45Ca2+) on the myometrium cells suspension treated by digitonin solution (0.1 mg/ml) some properties of Ca ions accumulation system in the mitochondria--cationic and substrate specificity as well as effects of Mg2+ and some other bivalent metals ions on the Ca2+ accumulation velocity have been estimated. Ca ions accumulation from the incubation medium containing 3 mM sodium succinate Na, 2 mM Pi (as potassium K(+)-phosphate buffer, pH 7.4 at 37 degrees C), 0.01 mM (40CaCl2 + 45CaCl2) and 100 nM thapsigargin--selective inhibiting agent of endoplasmatic reticulum calcium pump were demonstrated as detected just only in presence of Mg, while not Ni, Co or Cu ions. The increase of Mg2+ concentration from 1 x 10(-6) to 10(-3) M induced the ATP dependent transport activation in the myometrium mitochondria. Under [Mg2+] increase till 40 mM this cation essentially decreased Ca2+ accumulation (by 65% from the maximal value). The optimum for Ca2+ transport in the myometrium cells suspension is Mg2+ 10 mM concentration. Ka activation apparent constant along Mg2+ value (in presence 3 mM ATP and 3 mM sodium succinate) is 4.27 mM. The above listed bivalent metals decreased Mg2+, ATP-dependent accumulation of calcium, values of inhibition apparent constants for ions Co2+, Ni2+ and Cu2+ were--2.9 x 10(-4) M, 5.1 x 10(-5) M and 4.2 x 10(-6) M respectively. For Mg2+, ATP-dependent Ca2+ transport in the uterus myocytes mitocondria a high substrate specificity is a characteristic phenomenon in elation to ATP: GTP, CTP and UTP practically fail to provide for Ca accumulation process.     

Adsorption of reovirus to clay minerals: effects of cation-exchange capacity, cation saturation, and surface area

The adsorption of reovirus to clay minerals has been reported by several investigators, but the mechanisms defining this association have been studied only minimally. The purpose of this investigation was to elucidate the mechanisms involved with this interaction. More reovirus type 3 was adsorbed, in both distilled and synthetic estuarine water, by low concentrations of montmorillonite than by comparable concentrations of kaolinite containing a mixed complement of cations on the exchange complex. Adsorption to the clays was essentially immediate and was correlated with the cation-exchange capacity of the clays, indicating that adsorption was primarily to negatively charged sites on the clays. Adsorption was greater with low concentrations of clays in estuarine water than in distilled water, as the higher ionic strength of the estuarine water reduced the electrokinetic potential of both clay and virus particles. The addition of cations (as chloride salts) to distilled water enhanced adsorption, with divalent cations being more effective than monovalent cations and 10(-2) M resulting in more adsorption than 10(-3) M. Potassium ions suppressed reovirus adsorption to montmorillonite, probably by collapsing the clay lattices and preventing the expression of the interlayer-derived cation-exchange capacity. More virus was adsorbed by montmorillonite made homoionic to various mono-, di-, and trivalent cations (except by montmorillonite homoionic to potassium) than by comparable concentrations of kaolinite homoionic to the same cations. The sequence of the amount of adsorption to homoionic montmorillonite was Al greater than Ca greater than Mg greater than Na greater than K; the sequence of adsorption to kaolinite was Na greater than Al greater than Ca greater than Mg greater than K. The constant partition-type adsorption isotherms obtained when the clay concentration was maintained constant and the virus concentration was varied indicated that a fixed proportion of the added virus population was adsorbed, regardless of the concentration of infectious particles. A heterogeneity within the reovirus population was indicated.     

Adsorption of reovirus to clay minerals: effects of cation-exchange capacity, cation saturation, and surface area.

The adsorption of reovirus to clay minerals has been reported by several investigators, but the mechanisms defining this association have been studied only minimally. The purpose of this investigation was to elucidate the mechanisms involved with this interaction. More reovirus type 3 was adsorbed, in both distilled and synthetic estuarine water, by low concentrations of montmorillonite than by comparable concentrations of kaolinite containing a mixed complement of cations on the exchange complex. Adsorption to the clays was essentially immediate and was correlated with the cation-exchange capacity of the clays, indicating that adsorption was primarily to negatively charged sites on the clays. Adsorption was greater with low concentrations of clays in estuarine water than in distilled water, as the higher ionic strength of the estuarine water reduced the electrokinetic potential of both clay and virus particles. The addition of cations (as chloride salts) to distilled water enhanced adsorption, with divalent cations being more effective than monovalent cations and 10(-2) M resulting in more adsorption than 10(-3) M. Potassium ions suppressed reovirus adsorption to montmorillonite, probably by collapsing the clay lattices and preventing the expression of the interlayer-derived cation-exchange capacity. More virus was adsorbed by montmorillonite made homoionic to various mono-, di-, and trivalent cations (except by montmorillonite homoionic to potassium) than by comparable concentrations of kaolinite homoionic to the same cations. The sequence of the amount of adsorption to homoionic montmorillonite was Al greater than Ca greater than Mg greater than Na greater than K; the sequence of adsorption to kaolinite was Na greater than Al greater than Ca greater than Mg greater than K. The constant partition-type adsorption isotherms obtained when the clay concentration was maintained constant and the virus concentration was varied indicated that a fixed proportion of the added virus population was adsorbed, regardless of the concentration of infectious particles. A heterogeneity within the reovirus population was indicated.     

The effects of eight trace metals in acid soft water on survival, mineral uptake and skeletal calcium deposition in yolk-sac fry of brown trout, Salmo trutta L.

Recently hatched fry of brown trout were exposed to each of eight trace metals (Al, Cd, Cu, Fe, Mn, Ni, Pb, Zn) and to a mixture of all eight, at concentrations typical of soft acid waters, in flowing artificial soft water medium at pH 4·5 and 6·5, for 30 days. At pH 4·5, in the absence of trace metals, net uptake of Ca, Na and K and skeletal calcification were impaired but mortalities were low (10%). At pH 4·5, in the presence of Al, Cu, Pb and Zn individually and the mixture, mortalities were high (87–100%). Cd, Fe, Mn and Ni at pH 4·5 each caused some mortalities (17–43%) and impaired skeletal calcification. At pH 6·5, each of Al, Cd, Cu, Fe, Mn, Pb and the mixture of metals impaired net Ca uptake and (except Al, Fe and Pb) skeletal calcification. Net K uptake was impaired by Al and by the mixture, and less severely by Cu and by Fe. Net Na uptake was impaired by Al and by the mixture, and less severely by Fe and by Mn. The role of trace metals other than Al in fisheries'decline in soft acid waters is discussed.     

Heavy Metal Resistance of the Extreme Acidotolerant Filamentous Fungus Bispora sp

To obtain information on the importance of membrane and zeta potentials as repelling or facilitating forces during the uptake of cationic trace elements, the heavy metal content and the growth resistance of the acidotolerant fungus Bispora. sp. to heavy metals were compared at pH 1.0 and pH 7.0. Cu, Co, Ni, Cd, Cr, and La contents of the fungus were significantly lower at pH 1.0 than at pH 7.0. A similar pH effect occurred with cationic macro elements such as Na, Mg, Ca, Fe, and Mn. Only K and Zn exhibited higher levels at pH 1.0 in the fungus than at pH 7.0. Macro and micro elements present in the medium in anionic form (sulfate, chloride) showed the opposite pattern to cations: Contents were higher at pH 1.0 than at pH 7.0. Minerals present at pH 1.0 predominantly in the electrical neutral, protonated form (phosphate, borate) exhibited a similar cell content at both acid and neutral pH (P) or a higher content at neutral pH than at acid pH (B). The resistance of fungal growth to the cations Cu, Zn, Ni, Co, Cr, and Cd was significantly higher at pH 1.0 than at pH 7.0. Such a difference was not observed with Hg, present in the medium at both pH values as electrically silent HgCl₂. The anionic tungstate exhibited the opposite pattern to cationic heavy metals: The resistance of growth was higher at pH 7.0 than at pH 1.0. A greater growth resistance to heavy metals was correlated with a lower uptake of these elements, and vice versa; Uptake of heavy metals correlated with a lower resistance of fungal growth to these elements. The results are in agreement with the hypothesis that membrane and zeta potentials of the fungus are important factors controlling the uptake of heavy metals and thereby the resistance of growth to these elements: At pH 1.0 positive potentials of fungal hyphae impede the uptake of cationic heavy metals, but facilitate the uptake of anionic species. At neutral pH values the negative potentials facilitate the uptake of cations, but impede the uptake of anions.     

Physicochemical interaction of Escherichia coli cell envelopes and Bacillus subtilis cell walls with two clays and ability of the composite to immobilize heavy metals from solution

Isolated Escherichia coli K-12 cell envelopes or Bacillus subtilis 168 cell walls were reacted with smectite or kaolinite clay in distilled deionized water (pH 6.0); unbound envelopes or walls were separated by sucrose density gradient centrifugation, and the extent of adsorption was calculated. At saturation, both clays adsorbed approximately 1.0 mg (dry weight) of envelopes or walls per mg (dry weight) of clay. Clays showed a preference for edge-on orientation with both walls and envelopes, which was indicative of an aluminum polynuclear bridging mechanism between the wall or envelope surface and the clay edge. The addition of heavy metals increased the incidence of planar surface orientations, which suggested that multivalent metal cation bridging was coming into play and was of increasing importance. The metal-binding capacity of isolated envelopes, walls, clays, and envelope-clay or wall-clay mixtures was determined by atomic absorption spectroscopy after exposure to aqueous 5.0 mM Ag+, Cu2+, Cd2+, Ni2+, Pb2+, Zn2+, and Cr3+ nitrate salt solutions at pHs determined by the buffering capacity of wall, envelope, clay, or composite system. The order of metal uptake was walls greater than envelopes greater than smectite clay greater than kaolinite clay for the individual components, and walls plus smectite greater than walls plus kaolinite greater than envelopes plus smectite greater than envelopes plus kaolinite for the mixtures. On a dry-weight basis, the envelope-clay and wall-clay mixtures bound 20 to 90% less metal than equal amounts of the individual components did.(ABSTRACT TRUNCATED AT 250 WORDS)     

Physicochemical interaction of Escherichia coli cell envelopes and Bacillus subtilis cell walls with two clays and ability of the composite to immobilize heavy metals from solution.

Isolated Escherichia coli K-12 cell envelopes or Bacillus subtilis 168 cell walls were reacted with smectite or kaolinite clay in distilled deionized water (pH 6.0); unbound envelopes or walls were separated by sucrose density gradient centrifugation, and the extent of adsorption was calculated. At saturation, both clays adsorbed approximately 1.0 mg (dry weight) of envelopes or walls per mg (dry weight) of clay. Clays showed a preference for edge-on orientation with both walls and envelopes, which was indicative of an aluminum polynuclear bridging mechanism between the wall or envelope surface and the clay edge. The addition of heavy metals increased the incidence of planar surface orientations, which suggested that multivalent metal cation bridging was coming into play and was of increasing importance. The metal-binding capacity of isolated envelopes, walls, clays, and envelope-clay or wall-clay mixtures was determined by atomic absorption spectroscopy after exposure to aqueous 5.0 mM Ag+, Cu2+, Cd2+, Ni2+, Pb2+, Zn2+, and Cr3+ nitrate salt solutions at pHs determined by the buffering capacity of wall, envelope, clay, or composite system. The order of metal uptake was walls greater than envelopes greater than smectite clay greater than kaolinite clay for the individual components, and walls plus smectite greater than walls plus kaolinite greater than envelopes plus smectite greater than envelopes plus kaolinite for the mixtures. On a dry-weight basis, the envelope-clay and wall-clay mixtures bound 20 to 90% less metal than equal amounts of the individual components did.(ABSTRACT TRUNCATED AT 250 WORDS)     

Expression, purification, and characterization of recombinant amorpha-4,11-diene synthase from Artemisia annua L

A cDNA clone encoding amorpha-4,11-diene synthase from Artemisia annua was subcloned into a bacterial expression vector in frame with a His6-tag. Recombinant amorpha-4,11-diene synthase was produced in Escherichia coli and purified to apparent homogeneity. The enzyme showed pH optimum at pH 6.5, and a minimum at pH 7.5. Substantial activity was observed in the presence of Mg2+, Mn2+ or Co2+ as cofactor. The enzyme exhibits a low activity in the presence of Ni2+ and essentially no activity with Cu2+ or Zn2+. The sesquiterpenoids produced from farnesyl diphosphate in the presence of Mg2+ were analyzed by GC-MS. In addition to amorpha-4,11-diene, 15 sesquiterpenoids were produced. Only small quantitative differences in product pattern were observed at pH 6.5, 7.5, or 9.5. Amorpha-4,11-diene synthase showed significant increased product selectivity in the presence of Mn2+ or Co2+. Km for farnesyl diphosphate was 3.3, 8.0, and 0.7 microM in the presence of Mg2+, Mn2+ or Co2+, respectively. The corresponding kcat-values were 6.8, 15.0, and 1.3 x 10(-3) s(-1), respectively. Km and kcat for geranyl diphosphate were 16.9 microM and 7.0 x 10(-4) s(-1), respectively, at pH 6.5, in the presence of Mn2+.     

Interaction between ATP,metal ions,glycine, and several minerals

Summary The adsorption of ATP and ADP on montmorillonite, kaolinite, and A1(OH)₃ was studied as a funtion of pH and, for montmorillonite and kaolinite, as a funtion of the ionic composition of the system. The three minerals exhibit different adsorption charcteristics. Mg²⁺- and Zn²⁺-montmorillonite adsorb ATP and ADP more than Na⁺-montmorillonite, presumably because of complex formation. In kaolinite, the effect of these divalent cations is small. Pure ATP decomposes upon heating, and the rate of the decomposition is accelerated by the presence of glycine. Drying and heating glycine to 70°C under vacuum in the presence of ATP results in abiotic peptide formation with yields up to 0.25%. This peptide formation also occurs when kaolinite or montmorillonite is added to the system. The presence of kaolinite, Mg²⁺-or Zn²⁺-koalinite, or Mg²⁺-montmorillonite results in a reduction in the rate of the ATP decomposition in the abiotic peptide synthesizing system. These results suggest that one role for clays and metal ions in chemical evolution may have been the stabilization of nucleotides during prebiotic peptide synthesis.On Leave from the Hebrew University of Jerusalem, Israel     

Binding of metals by cell walls of Cunninghamella blakesleeana grown in the presence of copper or cobalt

Summary The binding of metals by cell walls isolated from Cunninghamella blakesleeana grown in the presence of inhibitory concentration of Cu or Co and which had altered chemical compositions was compared with the binding by control cell walls. The Co-cell walls, which had higher contents of phosphate and chitosan, bound more Cu and Co. Although the V _max for Cu and Co differed with each of the cell walls, the K _m values for the binding of Cu (6.3x10^-3 M) and Co (2.1x10^-3 M) were the same for all three types of cell walls. The cell walls also differed in their quantitative binding of various metals; control cell walls: Zn> Fe> Mn> Cd> Ca> Ni> Cu> Ag> Co> Mg; Cu-cellwalls: Zn> Fe> Mn> Cu> Ni> Cd> Ag> Ca> Co> Mg; and Co-cell walls: Fe> Zn> Cu> Mn> Cd> Ag> Ca> Ni=Co> Mg. The binding of Cu was temperature-dependent and had an optimum pH. The binding of Co was inhibited by Cu, but the binding of Cu was not inhibited by Co, and Cd totally suppressed the binding of Co but not of Cu, suggesting two binding sites on the cell walls, one exclusively for Cu and the other common to both metals but with a higher affinity for Co. The cell walls did not bind Mg. The Cu-or Co-loaded cell walls eluted with 5 mM ethylenediaminetetraacetate (EDTA) rebound these metals to the same or greater extent as the original walls, but walls eluted with 0.5 N HCl bound only 50% of that bound originally.     

豚草叶片和果实气体交换特性与11种土壤重金属相关性

对10个样地中Cu、Pb、Zn、Mn、Cr、Co、Ni、Cd、As、Sb和Hg11种土壤重金属含量及样地内豚草叶片和果实气体交换特性进行测定.结果表明,样地内豚草叶片的净光合速率在1·88~9·41μmol·m-2·s-1,而果实的净光合速率最高可达2·81μmol·m-2·s-1.叶片的呼吸速率、气孔导度、光合速率和水分利用效率的平均值分别为1·81μmol·m-2·s-1、75·7mmol·m-2·s-1、6·05μmol·m-2·s-1和4·72μmol·mmol-1,分别是果实的5·26、0·64、1·31和1·69倍,说明非同化器官幼嫩果实具有与叶片相当,甚至更强的呼吸、光合能力和水分利用效率;研究地点重金属Ni达到轻微污染水平,其它重金属含量都接近或者显著低于重金属污染的阈值.相关分析和多元回归分析显示,大部分土壤重金属(如Cu、Pb、Zn、Cd、As、Sb和Hg)含量的高低对豚草气体交换特性没有显著影响,仅部分重金属含量与豚草的叶片、果实气体交换特性密切相关,如Ni和Cr对豚草叶片、果实的气孔导度及水分利用效率显著相关;Cr与豚草叶片饱和光合速率显著相关;而As与豚草果实的气孔导度显著相关.表明大部分土壤重金属对叶片和球果的气体交换没有直接影响,而Ni、Cr和As可以在轻微污染甚至没有达到污染水平时影响豚草的气体交换特性.     

基因工程菌大肠杆菌JM109富集废水中镍离子的研究

利用通过基因工程技术所构建的在细胞内同时表达出高特异性镍转运蛋白和金属硫蛋白的基因工程菌富集水体中的镍离子。菌体细胞对Ni²⁺的富集速率很快,富集过程满足Langmuir等温线模型。与原始宿主菌相比,经基因改造的基因工程菌不仅最大镍富集容量增加了5倍多,而且对pH值、离子强度的变化及其它共存重金属离子的影响都呈现出更强的适应性。相比而言,Na⁺、Ca²⁺、Cd²⁺、Pb²⁺的影响较小,但Mg²⁺、Hg²⁺和Cu²⁺所引起的负面效应较大。进一步的实验表明基因工程菌对Ni2+的富集行为不需要外加营养物质。     

Heavy metal contamination and health risk assessment in soil-rice system near Xinqiao mine in Tongling city,Anhui province,China

In this study, paddy soil and rice grain samples were collected from the vicinity around the Xinqiao mine in Tongling, China to test for the presence of heavy metals (Cd, Ni, Cr, Cu, Zn, and Pb) in soil-rice system. Results indicated that the soil samples were primarily contaminated with Cd and Cu and followed with Zn and Pb. In rice grains, Cd, Cu, and Cr concentrations exceeded recommended guidelines. However, the regional distribution of heavy metals in rice grains and soil was inconsistent. The bioaccumulation factor of heavy metals in rice grains decreased in the order of Cd > Zn > Cu > Ni > Cr > Pb. The BAF was significantly positively correlated with TCLP-extractable metals and significantly negatively correlated with soil pH. However, the relationship between soil organic matter and the BAF in rice grains was complex. Health risk assessment through rice intake showed that hazard quotients of Cu and Cd were greater than 1 and could pose a considerable non-cancer health risk to adults and children; meanwhile, Cr, Ni, and Cd could pose an unacceptable cancer risk. The results indicated that the government must take measures to reduce heavy metal contents in paddy soil and rice.     

Siderophores,NTA, and Citrate: Potential Soil Amendments to Enhance Heavy Metal Mobility in Phytoremediation

Phytoremediation of heavy metal-contaminated sites is often limited by the low bioavailability of the contaminants. Complexing agents can help to improve this technique by enhancing heavy metal solubility. We investigated the effect of three organic chelating agents, that is, the siderophore desferrioxamine B (DFOB), nitrilotriacetate (NTA), and citrate on binding of Cu, Zn, and Cd by either Namontmorillonite, kaolinite, or goethite. The different effects of the complexing agents on metal sorption can mainly be explained by the differences in stability constants and surface charge characteristics. In the presence of clay minerals, NTA was the most efficient ligand with respect to mobilization of heavy metals. In goethite suspensions, the effect of DFOB was more pronounced. In all systems, Cu proved to be the most affected element by the presence of the ligands. In batch experiments with heavy metal-contaminated soils from field sites, NTA was the most efficient metal mobilizer.     

The influence of phototrophic benthic biofilms on Cd, Cu, Ni, and Pb transport in permeable sediments

The effect of phototrophic biofilm activity on advective transport of cadmium (Cd), copper (Cu), nickel (Ni), and lead (Pb) in sandy sediments was examined using percolated columns. Cd and Ni in the effluent exhibited clear diel cycles in biofilm-containing columns, with concentrations at the end of dark periods exceeding those during illumination by up to 4.5- and 10-fold for Ni and Cd, respectively. Similar cycles were not observed for Pb or Cu. Breakthrough of the latter metals was greatly retarded and incomplete relative to Cd and Ni, and trends in biofilm treatments did not differ greatly from those in control columns. Inhibition of photosystem II by DCMU (3-(3,4-dichlorophenyl)-1,1-dimethylurea) proved that diel cycles of Cd and Ni were controlled by oxygenic photosynthesis, and microsensor measurements showed that metal cycles closely matched metabolic activity-driven pH variations. The sorption edge pH for the sand/biofilm substrate followed the order Ni > Cd > Cu > Pb, and for Ni and Cd, was within the pH 7?C10 range observed in the biofilm-containing column. Adsorption dynamics over the light periods matched pH increases, but desorption during dark periods was incomplete and slower than the rate of change of pH. Over a diel cycle, desorption was less than adsorption, resulting in net binding of dissolved metals due to the biofilm metabolic activity. Extraction with selective reagents indicated that the adsorbed metals were readily exchangeable, and potentially bioavailable. Thus, phototrophic benthic biofilms can control the transport of some metals across the sand?Cwater interface, and processes in this very thin surficial layer should be considered when evaluating chemical fluxes in permeable sediments.     

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.     

Interaction of Pseudomonas putida CZ1 with clays and ability of the composite to immobilize copper and zinc from solution

The present study was conducted to determine the abilities of the living and nonliving Pseudomonas putida CZ1 cells, clays (goethite, kaolinite, smectite and manganite) and their composites to accumulate copper and zinc from a liquid medium, and elucidate the role of microbes on the mobility of heavy metals. Various mixtures of bacteria and clays were exposed to solutions of 0.025 mM or 0.5mM Cu(II) and Zn(II) in 0.01M KNO(3) to differentiate between so-called "high-affinity" sites and "low-affinity" sites. Clays associated in an edge-on orientation to the cells was observed by electron microscope (EM) examination of these metal-treated bacteria-clay aggregates. Adsorption experiments and desorption with 1.0M CH(3)COOK solution indicated that clays contain more high-affinity copper binding sites and less high-affinity zinc binding sites than that of bacteria, however, bacteria are involved in more low-affinity heavy-metal-binding sites. Carboxyl group activity is more important at weak-binding sites than at strong-binding sites. TEM-EDS analysis confirmed that most of Zn removed from solution was associated with P. putida CZ1 in the composites. These results suggest that bacteria play an important role in regulating the mobility of heavy metals in the soil environment.     

Remobilization of toxic heavy metals adsorbed to bacterial wall-clay composites.

Significant quantities of Ag(I), Cu(II), and Cr(III) were bound to isolated Bacillus subtilis 168 walls, Escherichia coli K-12 envelopes, kaolinite and smectite clays, and the corresponding organic material-clay aggregates (1:1, wt/wt). These sorbed metals were leached with HNO3, Ca(NO3)2, EDTA, fulvic acid, and lysozyme at several concentrations over 48 h at room temperature. The remobilization of the sorbed metals depended on the physical properties of the organic and clay surfaces and on the character and concentration of the leaching agents. In general, the order of remobilization of metals was Cr much less than Ag less than Cu. Cr was very stable in the wall, clay, and composite systems; pH 3.0, 500 microM EDTA, 120-ppm [mg liter-1] fulvic acid, and 160-ppm Ca remobilized less than 32% (wt/wt) of sorbed Cr. Ag (45 to 87%) and Cu (up to 100%) were readily removed by these agents. Although each leaching agent was effective at mobilizing certain metals, elevated Ca or acidic pH produced the greatest overall mobility. The organic chelators were less effective. Lysozyme digestion of Bacillus walls remobilized Cu from walls and Cu-wall-kaolinite composites, but Ag, Cr, and smectite partially inhibited enzyme activity, and the metals remained insoluble. The extent of metal remobilization was not always dependent on increasing concentrations of leaching agents; for example, Ag mobility decreased with some clays and some composites treated with high fulvic acid, EDTA, and lysozyme concentrations. Sometimes the organic material-clay composites reacted in a manner distinctly different from that of their individual counterparts; e.g., 25% less Cu was remobilized from wall- and envelope-smectite composites than from walls, envelopes, or smectite individually in 500 microM EDTA. Alternatively, treatment with 160-ppm Ca removed 1.5 to 10 times more Ag from envelope-kaolinite composites than from the individual components. The particle size of the deposited metal may account for some of the stability changes; those metals that formed large, compact aggregates (Cr and Ag) as seen by transmission electron microscopy were less likely to be remobilized. In summary, it is apparent that remobilization of toxic heavy metals in sediments, soils, and the vadose zone is a complicated issue. Predictions based on single inorganic or organic component systems are too simplistic.