ION SERIES AND THE PHYSICAL PROPERTIES OF PROTEINS. I

1. This paper contains experiments on the influence of acids and alkalies on the osmotic pressure of solutions of crystalline egg albumin and of gelatin, and on the viscosity of solutions of gelatin. 2. It was found in all cases that there is no difference in the effects of HCl, HBr, HNO₃, acetic, mono-, di-, and trichloracetic, succinic, tartaric, citric, and phosphoric acids upon these physical properties when the solutions of the protein with these different acids have the same pH and the same concentration of originally isoelectric protein. 3. It was possible to show that in all the protein-acid salts named the anion in combination with the protein is monovalent. 4. The strong dibasic acid H₂SO₄ forms protein-acid salts with a divalent anion SO₄ and the solutions of protein sulfate have an osmotic pressure and a viscosity of only half or less than that of a protein chloride solution of the same pH and the same concentration of originally isoelectric protein. Oxalic acid behaves essentially like a weak dibasic acid though it seems that a small part of the acid combines with the protein in the form of divalent anions. 5. It was found that the osmotic pressure and viscosity of solutions of Li, Na, K, and NH₄ salts of a protein are the same at the same pH and the same concentration of originally isoelectric protein. 6. Ca(OH)₂ and Ba(OH)₂ form salts with proteins in which the cation is divalent and the osmotic pressure and viscosity of solutions of these two metal proteinates are only one-half or less than half of that of Na proteinate of the same pH and the same concentration of originally isoelectric gelatin. 7. These results exclude the possibility of expressing the effect of different acids and alkalies on the osmotic pressure of solutions of gelatin and egg albumin and on the viscosity of solutions of gelatin in the form of ion series. The different results of former workers were probably chiefly due to the fact that the effects of acids and alkalies on these proteins were compared for the same quantity of acid and alkali instead of for the same pH.     

THE MECHANISM BY WHICH TRIVALENT AND TETRAVALENT IONS PRODUCE AN ELECTRICAL CHARGE ON ISOELECTRIC PROTEIN

1. Experiments on anomalous osmosis suggested that salts with trivalent cations, e.g. LaCl₃, caused isoelectric gelatin to be positively charged, and salts with tetravalent anions, e.g. Na₄Fe(CN)₆, caused isoelectric gelatin to be negatively charged. In this paper direct measurements of the P.D. between gels of isoelectric gelatin and an aqueous solution as well as between solutions of isoelectric gelatin in a collodion bag and an aqueous solution are published which show that this suggestion was correct. 2. Experiments on anomalous osmosis suggested that salts like MgCl₂, CaCl₂, NaCl, LiCl, or Na₂SO₄ produce no charge on isoelectric gelatin and it is shown in this paper that direct measurements of the P.D. support this suggestion. 3. The question arose as to the nature of the mechanism by which trivalent and tetravalent ions cause the charge of isoelectric proteins. It is shown that salts with such ions act on isoelectric gelatin in a way similar to that in which acids or alkalies act, inasmuch as in low concentrations the positive charge of isoelectric gelatin increases with the concentration of the LaCl₃ solution until a maximum is reached at a concentration of LaCl₃ of about M/8,000; from then on a further increase in the concentration of LaCl₃ diminishes the charge again. It is shown that the same is true for the action of Na₄Fe(CN)₆. From this it is inferred that the charge of the isoelectric gelatin under the influence of LaCl₃ and Na₄Fe(CN)₆ at the isoelectric point is due to an ionization of the isoelectric protein by the trivalent or tetravalent ions. 4. This ionization might be due to a change of the pH of the solution, but experiments are reported which show that in addition to this influence on pH, LaCl₃ causes an ionization of the protein in some other way, possibly by the formation of a complex cation, gelatin-La. Na₄Fe(CN)₆ might probably cause the formation of a complex anion of the type gelatin-Fe(CN)₆. Isoelectric gelatin seems not to form such compounds with Ca, Na, Cl, or SO₄. 5. Solutions of LaCl₃ and Na₄Fe(CN)₆ influence the osmotic pressure of solutions of isoelectric gelatin in a similar way as they influence the P.D., inasmuch as in lower concentrations they raise the osmotic pressure of the gelatin solution until a maximum is reached at a concentration of about M/2,048 LaCl₃ and M/4,096 Na₄Fe(CN)₆. A further increase of the concentration of the salt depresses the osmotic pressure again. NaCl, LiCl, MgCl₂, CaCl₂, and Na₂SO₄ do not act in this way. 6. Solutions of LaCl₃ have only a depressing effect on the P.D. and osmotic pressure of gelatin chloride solutions of pH 3.0 and this depressing effect is quantitatively identical with that of solutions of CaCl₂ and NaCl of the same concentration of Cl.     

THE INFLUENCE OF THE CHEMICAL NATURE OF SOLID PARTICLES ON THEIR CATAPHORETIC P.D. IN AQUEOUS SOLUTIONS

1. The effect of eight salts, NaCl, Na₂SO₄, Na₄Fe(CN)₆, CaCl₂, LaCl₃, ThCl₄, and basic and acid fuchsin on the cataphoretic P.D. between solid particles and aqueous solutions was measured near the point of neutrality of water (pH 5.8). It was found that without the addition of electrolyte the cataphoretic P.D. between particles and water is very minute near the point of neutrality (pH 5.8), often less than 10 millivolts, if care is taken that the solutions are free from impurities. Particles which in the absence of salts have a positive charge in water near the point of neutrality (pH 5.8) are termed positive colloids and particles which have a negative charge under these conditions are termed negative colloids. 2. If care is taken that the addition of the salt does not change the hydrogen ion concentration of the solution (which in these experiments was generally pH 5.8) it can be said in general, that as long as the concentration of salts is not too high, the anions of the salt have the tendency to make the particles more negative (or less positive) and that cations have the opposite effect; and that both effects increase with the increasing valency of the ions. As soon as a maximal P.D. is reached, which varies for each salt and for each type of particles, a further addition of salt depresses the P.D. again. Aside from this general tendency the effects of salts on the P.D. are typically different for positive and negative colloids. 3. Negative colloids (collodion, mastic, Acheson''s graphite, gold, and metal proteinates) are rendered more negative by low concentrations of salts with monovalent cation (e.g. Na) the higher the valency of the anion, though the difference in the maximal P.D. is slight for the monovalent Cl and the tetravalent Fe(CN)₆ ions. Low concentrations of CaCl₂ also make negative colloids more negative but the maximal P.D. is less than for NaCl; even LaCl₃ increases the P.D. of negative particles slightly in low concentrations. ThCl₄ and basic fuchsin, however, seem to make the negative particles positive even in very low concentrations. 4. Positive colloids (ferric hydroxide, calcium oxalate, casein chloride—the latter at pH 4.0) are practically not affected by NaCl, are rendered slightly negative by high concentrations of Na₂SO₄, and are rendered more negative by Na₄Fe(CN)₆ and acid dyes. Low concentrations of CaCl₂ and LaCl₃ increase the positive charge of the particles until a maximum is reached after which the addition of more salt depresses the P.D. again. 5. It is shown that alkalies (NaOH) act on the cataphoretic P.D. of both negative and positive particles as Na₄Fe(CN)₆ does at the point of neutrality. 6. Low concentrations of HCl raise the cataphoretic P.D. of particles of collodion, mastic, graphite, and gold until a maximum is reached, after which the P.D. is depressed by a further increase in the concentration of the acid. No reversal in the sign of charge of the particle occurs in the case of collodion, while if a reversal occurs in the case of mastic, gold, and graphite, the P.D. is never more than a few millivolts. When HCl changes the chemical nature of the colloid, e.g. when HCl is added to particles of amphoteric electrolytes like sodium gelatinate, a marked reversal will occur, on account of the transformation of the metal proteinate into a protein-acid salt. 7. A real reversal in the sign of charge of positive particles occurs, however, at neutrality if Na₄Fe(CN)₆ or an acid dye is added; and in the case of negative colloids when low concentrations of basic dyes or minute traces of ThCl₄ are added. 8. Flocculation of the suspensions by salts occurs when the cataphoretic P.D. reaches a critical value which is about 14 millivolts for particles of graphite, gold, or mastic or denatured egg albumin; while for collodion particles it was about 16 millivolts. A critical P.D. of about 15 millivolts was also observed by Northrop and De Kruif for the flocculation of certain bacteria.     

TEMPERATURE ACTIVATION OF THE UREASE-UREA SYSTEM USING CRUDE AND CRYSTALLINE UREASE

1. The hydrolysis of urea catalyzed by jack bean meal has been followed by determining colorimetrically after Nesslerization the ammonia nitrogen, and volumetrically the carbon dioxide liberated at successive intervals during the reaction. During the early part of hydrolysis the rate of ammonia or carbon dioxide liberation is constant for all the urease solutions which were used. 2. When log rate of NH₃ or CO₂ formation was plotted against 1/T, the points fell along a straight line, the slope of which corresponded to an activation energy of either 8,700 or 11,700 calories per gram mol. Frequently urease, when dissolved in sulfite solution, was characterized by an activation energy of 11,700 below and 8,700 above the critical temperature of about 23°C. At high temperatures the plotted points fell off from the curve due to temperature inactivation. 3. Essentially the same results on temperature activation were obtained with crude jack bean meal, Arlco urease, crystalline urease not recrystallized, and crystalline urease once recrystallized. The temperature characteristic which was obtained depended in part upon the composition of the medium. When dissolved in water, or aqueous solutions of glycerine, KCN, Na₂S₂O₂, cystine, Na₂SO₄, and K₄Fe(CN)₆, the temperature characteristic or µ of urease is 8,700. On the other hand, when urease is dissolved in solutions of K₃Fe(CN)₆ or H₂O₂ the µ value is 11,700. When dissolved in a solution containing Na₂SO₃ and NaHSO₃ the µ value may be either 8,700 or 11,700 over the whole temperature range, or 11,700 below and 8,700 above 23°C. 4. When crystalline urease is dissolved in varying mixtures of K₄Fe(CN)₆ and K₃Fe(CN)₆, the temperature characteristic depends upon the oxidation-reduction potential of the digest. When E_h is greater than +0.46 volt µ = 11,700, when less than +0.42 volt µ = 8,700, when between +0.42 – +0.46 µ = 11,700 below and 8,700 above the critical temperature. 5. It is suggested that in reducing or in indifferent solutions the configuration of the urease molecule (as determined especially by SH groups present) is such that the activation energy is 8,700 calories. In oxidizing solutions the urease molecule has been so altered (perhaps by the oxidation of the SH groups) as to be partly inactivated and now has an activation energy of 11,700. Such changes in the urease molecule are reversible (unless oxidation has proceeded too far) and are accompanied by a corresponding change in the activation energy.     

The Effect of Various Carbonate Sources on the Survival of Escherichia coli in Dairy Cattle Manure

Manure slurries (n = 3) prepared from the feces and urine of lactating dairy cattle (1 part urine, 2.2 parts feces, and 6.8 parts distilled water) had an initial pH of 8.6 ± 0.1; dissolved carbonate concentrations of 48 ± 4 mm, and Escherichia coli counts of 5.9 ± 0.7 logs per ml slurry. The pH of untreated slurries declined to pH 7.0 ± 0.1 by the 10th day of incubation, and the E. coli count increased approximately 10-fold (P < 0.05). When slurries were treated with Na₂CO₃, K₂CO₃, NaHCO₃ or Na₂CO₃·NaHCO₃ (0 to 16 g/kg slurry), the dissolved carbonates increased in a linear fashion, but only Na₂CO₃ and K₂CO₃ (8 g/kg or greater) or Na₂CO₃·NaHCO₃ (16 g/kg) ensured an alkaline pH. Even relatively low concentrations of Na₂CO₃ or K₂CO₃ (8 or 12 g/kg) caused a decrease in E. coli viability (P < 0.05), and E. coli could not be detected if 16 g/kg was added (day 5 or 10 of incubation). Na₂CO₃·NaHCO₃ also caused a decrease in E. coli viability, (P < 0.05), but some E. coli (approximately 10⁴ cells per g) were detected on day 10 even if the concentration was 16 g/kg. NaHCO₃ did not prevent the decrease in pH or cause a decrease in E. coli numbers (P > 0.05). Calculations based on the Henderson-Hasselbalch equation (pH and dissolved carbonates) indicated that little E. coli killing was noted until the dissolved carbonate anion concentrations (CO₃ ⁻²) were greater than 1 mm, but bicarbonate anion (HCO₃ ⁻) concentrations as high as 180 mm did not affect E. coli viability. These results are consistent with the idea that carbonate anion has antimicrobial properties and can kill E. coli in dairy cattle manure. Received: 20 December 2000 / Accepted: 7 February 2001     

Na2CO3 Influence on DNA Double Helix Stability: Strong Anion Destabilizing Effect

Abstract

Addition of Na₂CO₃ to almost salt-free DNA solution (5·10^?5M EDTA, pH=5.7, Tm=26.5 °C) elevates both pH and the DNA melting temperature (Tm) if Na₂CO₃ concentration is less than 0.004M. For 0.004M Na₂CO₃, Tm=58 °C is maximal and pH=10.56. Further increase in concentration gives rise to a monotonous decrease in Tm to 37 °C for 1M N₂CO₃ (pH=10.57). Increase in pH is also not monotonous. The highest pH=10.87 is reached at 0.04M Na₂CO₃ (Tm=48.3 °C). To reveal the cause of this DNA destabilization, which happens in a narrow pH interval (10.56÷10.87) and a wide Na₂CO₃ concentration interval (0.004÷1M), a procedure has been developed for determining the separate influences on Tm of Na⁺, pH, and anions formed by Na₂CO₃ (HCO₃ ^? and CO₃ ^2-). Comparison of influence of anions formed by Na₂CO₃ on DNA stability with Cl^? (anion inert to DNA stability), ClO₄ ^? (strong DNA destabilizing “chaotropic” anion) and OH^? has been carried out. It has been shown that only Na⁺ and pH influence Tm in Na₂CO₃ solution at concentrations lower than 0.001M. However, the Tm decrease with concentration for [Na₂CO₃]≥0.004M is only partly caused by high pH≈10.7. Na₂CO₃ anions also exert a strong destabilizing influence at these concentrations. For 0.1M Na₂CO₃ (pH=10.84, [Na⁺]=0.2M, Tm=42.7 °C), the anion destabilizing effect is higher 20 °C. For NaClO₄ (ClO₄ ^? is a strong “chaotropic” anion), an equal anion effect occurs at much higher concentrations ～3M. This means that Na₂CO₃ gives rise to a much stronger anion effect than other salts. The effect is pH dependent. It decreases fivefold at neutral pH after addition of HCl to 0.1M Na₂CO₃ as well as after addition of NaOH for pH>11.2.     

Production of Alkaline Lipase by Corynebacterium paurometabolum, MTCC 6841 Isolated from Lake Naukuchiatal, Uttaranchal State, India

A moderately psychrophilic bacterium Corynebacterium paurometabolum MTCC 6841 (gram positive, short rod type) producing extracellular alkaline lipase was isolated from Lake Naukuchiatal, Uttaranchal, India. The bacterium was able to grow within a broad range of pH (5–10). Soyabean oil and olive oil served as the best carbon sources for lipase production. The bacterium preferred inorganic nitrogenous compounds, NaNO₃ and KNO₃, over organic nitrogenous compound for its growth. Maximum lipase production occurred at 25°C and 8.5 pH. The enzyme activity was found to be maximum at the same values of temperature and pH. The enzyme was reasonably stable in the presence of various organic solvents. No significant effect of Ca⁺, Cu⁺⁺, Fe⁺⁺, Na⁺, K⁺, Mg⁺⁺, Mn⁺, NH4⁺, Co⁺⁺ ions over enzyme activity was detected. Treatment with EDTA reduced the activity to nearly one half.     

模拟酸沉降对鼎湖山季风常绿阔叶林地表径流水化学特征的影响

通过模拟酸沉降实验,研究了旱季期间(10-3月份)鼎湖山季风常绿阔叶林在4种不同pH模拟酸雨处理(对照、pH 4.0、pH 3.5、pH 3.0)下地表径流水化学输出特征.结果显示:(1)地表径流pH随酸处理强度增强呈“U”型变化模式,酸沉降对地表径流pH的影响不显著(P＞0.05),表明模拟酸沉降尚未引起地表水的酸化.(2)地表径流中NO3-、SO24-浓度随酸处理强度增强略有增加;HCO3-浓度的变化模式与地表径流pH类似.酸根离子浓度与地表径流pH相关性分析表明,SO24-、HCO3-有助于提高地表水抗酸化能力而NO3-则有助于促进地表水酸化.(3)地表径流中盐基离子对酸沉降的响应不尽相同.pH 3.0处理显著提高地表径流中Ca2+、Na+浓度;Mg2+浓度具有随酸处理梯度增强而增加的趋势;K+受模拟酸度的影响小.表明强酸(pH3.0)处理将导致土壤Na+、Ca2+、Mg2+盐基离子流失.(4)酸沉降具有诱发土壤可溶性有机碳(DOC)流失的倾向,增加地表水受有机污染的风险.     

THE COMBINATION OF GELATIN WITH HYDROCHLORIC ACID : II. NEW DETERMINATIONS OF THE ISOELECTRIC POINT AND COMBINING CAPACITY OF A PURIFIED GELATIN.

1. Cooper''s gelatin purified according to Northrop and Kunitz exhibited a minimum of osmotic pressure and a maximum of opacity at pH 5.05 ±0.05. The pH of solutions of this gelatin in water was also close to this value. It is inferred that such gelatin is isoelectric at this pH and not at pH 4.70. 2. Hydrogen electrode measurements with KCl-agar junctions were made with concentrated solutions of this gelatin in HCl up to 0.1 M. The combination curve calculated from these data is quite exactly horizontal between pH 2 and 1, indicating that 1 gm. of this gelatin can combine with a maximum of 9.35 x 10^–4 equivalents of H⁺. 3. Conductivity titrations of this gelatin with HCl gave an endpoint at 9.41 (±0.05) x 10^–4 equivalents of HCl per gram gelatin. 4. E.M.F. measurements of the cell without liquid junction, Ag, AgCl, HCl + gelatin, H₂, lead to the conclusion that this gelatin in 0.1 M HCl combines with a maximum of 9.4 x 10^–4 equivalents of H⁺ and 1.7 x 10^–4 equivalents of Cl^- per gram gelatin.     

Analysis of feeding mechanism in a pitcher ofNepenthes hybrida

The process of digestion of captured feeds in a pitcher, an insect-trapping organ, ofNepenthes was studied. Changes in bacterial population, pH and NH₄ ⁺ concentrations in pitcher juice were examined. Strong activities of both acid- and alkaline phosphatase, phosphoamidase, esterase C4 and esterase C8 were found in the pitcher juice. Optimum pH of proteases in the juice and those secreted from bacteria showed pH 3.0 and pH 8.0–9.0, respectively. Twenty six strains of bacteria were isolated from 4 pitchers: 10 strains were gram positive, 16 strains were gram negative (10 strains had casein hydrolase activity). A proton excretion was induced by NH₄ ⁺ released from the added solutions, and accordingly, the pH of the solutions fell. As a simulation model of the digestion process of feeds in pitcher juice and polypeptone solution was added into the washed pitcher. A good correlation was found among the NH₄ ⁺ concentration, pH and bacterial cell titer.     

ION SERIES AND THE PHYSICAL PROPERTIES OF PROTEINS. II

1. Our results show clearly that the Hofmeister series is not the correct expression of the relative effect of ions on the swelling of gelatin, and that it is not true that chlorides, bromides, and nitrates have "hydrating," and acetates, tartrates, citrates, and phosphates "dehydrating," effects. If the pH of the gelatin is taken into considertion, it is found that for the same pH the effect on swelling is the same for gelatin chloride, nitrate, trichloracetate, tartrate, succinate, oxalate, citrate, and phosphate, while the swelling is considerably less for gelatin sulfate. This is exactly what we should expect on the basis of the combining ratios of the corresponding acids with gelatin since the weak dibasic and tribasic acids combine with gelatin in molecular proportions while the strong dibasic acid H₂SO₄ combines with gelatin in equivalent proportions. In the case of the weak dibasic acids he anion in combination with gelatin is therefore monovalent and in the case of the strong H₂SO₄ it is bivalent. Hence it is only the valency and not the nature of the ion in combination with gelatin which affects the degree of swelling. 2. This is corroborated in the experiments with alkalies which show that LiOH, NaOH, KOH, and NH₄OH cause the same degree of swelling at the same pH of the gelatin solution and that this swelling is considerably higher than that caused by Ca(OH)₂ and Ba(OH)₂ for the same pH. This agrees with the results of the titration experiments which prove that Ca(OH)₂ and Ba(OH)₂ combine with gelatin in equivalent proportions and that hence the cation in combination with the gelatin salt with these two latter bases is bivalent. 3. The fact that proteins combine with acids and alkalies on the basis of the forces of primary valency is therefore not only in full agreement with the influence of ions on the physical properties of proteins but allows us to predict this influence qualitatively and quantitatively. 4. What has been stated in regard to the influence of ions on the swelling of the different gelatin salts is also true in regard to the influence of ions on the relative solubility of gelatin in alcohol-water mixtures. 5. Conductivity measurements of solutions of gelatin salts do not support the theory that the drop in the curves for swelling, osmotic pressure, or viscosity, which occurs at a pH 3.3 or a little less, is due to a drop in the concentration of ionized protein in the solution; nor do they suggest that the difference between the physical properties of gelatin sulfate and gelatin chloride is due to differences in the degree of ionization of these two salts.     

Phosphate transport in intestinal brush-border membrane

In the small intestine of the rabbit the process of Na⁺-dependent uptake of phosphate occurs only at the brush-border of duodenal enterocytes. Li⁺ can replace Na⁺. The process is activated when either K⁺, Cs⁺, Rb⁺, or choline is present in the intravesicular space. The presence of membrane-permeable anions is essential for maximum rates of phosphate transport. We conclude that the mechanism of the phosphate carrier is electrogenic at pH 6–8, probably two Na⁺ moving with each H₂PO ₄ ^– . This. will lead to the development of a positive charge within the vesicle. The variation of theK _m for H₂PO ₄ ^– with pH is thought to be the consequence of the affinity of the carrier protein for H₂PO ₄ ^– increasing as the pH increases. Polyclonal antibodies against membrane vesicles isolated from rabbit duodenum, jejunum, and ileum were prepared. The antibodies raised against the ileum and jejunum both activated the phosphate transport process, while the anti-duodenum antibody preparation inhibited phosphate transport.     

Forest soil solutions: Acid/base chemistry and response to calcite treatment

Soil solution chemistry was investigated at a forested watershed draining into Woods Lake. N.Y. as part of the Experimental Watershed Liming Study (EWLS). The objective of this study was to assess the response of soil water to watershed treatment of calcite (CaCO₃). This material was applied in an effort to mitigate the effects of acidic atmospheric deposition. Soil solutions draining Oa and Bs horizons in reference subcatchments were characterized by low pH and acid neutralizing capacity (ANC) due to elevated concentrations of SO ₄ ^2– , NO ₃ ^– and organic anions relative to the sum of base cation (C_B Ca²⁺, Mg²⁺, Na⁺, K⁺) concentrations. Seasonal and spatial variation of pH andANC in soil solutions appeared to belargely controlled by variations in the concentrations of dissolved organic acids which, in turn, were regulated by reactions of Al with soil organic matter. Nitrate was positively correlated and SO²⁺ was negatively correlated with Ca²⁺ and Al concentrations in reference soil solutions, indicating that changes in NO ₃ ^– influences spatial and seasonal variations in Ca²⁺ and Al concentrations. On this basis, NO ₃ ^– appears to be important in soil acidification and the dynamics of drainage water acidity. Comparison of our results with historical data for the site showed declines in concentrations of SO ₄ ^2– , which are consistent with decreases in emissions of SO₄, in the eastern U.S. and atmospheric deposition of SO ₄ ^2– , to the Adirondack region. Mineral soil solutions have shown large increases in concentrations of NO ₃ ^– . Declines in concentrations of C_B and increases in concentrations of Al have occurred over the last ten years, suggesting depletion of soil pools of exchangeable basic cations and increased sensitivity to acidic deposition. Calcite (CaCO₃) treatment of 6.89 Mg/ha resulted in a significant increase of Ca²⁺, ANC and pH in both Oa and Bs horizon soil solutions. Soil water response to CaCO₃ addition was most evident during the first year after treatment, apparently due to macropore transport of particulate and dissolved CaCO₃ However, increases in ANC and pH in the mineral soil waters were not sustained and appeared insufficient to result in substantial improvement in surface water quality over the 43 month study period.     

Effects of abscisic acid on sequestration and exchange of Na+ by barley roots

Excised Na⁺-starved barley roots were suspended in solutions of Na⁺ in combination with NO ₃ ^- , Cl^-, and SO ₄ ^2- , and effects of the added phytohormone, abscisic acid (ABA), to the medium were determined. Abscisic acid increased the rate of Na⁺ (²²Na⁺) accumulation and the amount of Na⁺ deposited in the vacuoles. These stimulating effects of ABA were modified by anions following the sequence NO ₃ ^- >Cl^->SO ₄ ^2- . Testing whether the magnitude of the pH gradient across the plasmalemma of the cells of the root cortex affects rates of Na⁺ accumulation and their dependence upon ABA, we observed that, in the pH range from 4 to 8, the ABA-induced stimulation was strongest at pH 5.8, and least at pH 4. Changes in pH during the experiment caused changes in the rates of Na⁺ accumulation in agreement with experiments performed at constant pH values. Simultaneously with ABA-enhanced accumulation, loss of Na⁺ occurred. Loss of Na⁺ was strongest at pH 4 and was affected by anions, being greatest with SO ₄ ^2- and following the sequence SO ₄ ^2- >Cl^->NO ₃ ^- . On the basis of the finding that initial acceleration of uptake as well as loss of Na⁺ depended on the pH of the medium we suggest that, in barley roots, ABA stimulates an exchange of Na⁺ for H⁺ at the plasmalemma of the cortical cells. The results indicate that ABA-stimulated expulsion of Na⁺, in combination with ABA-stimulated sequestration in the vacuoles, constitutes one of the mechanisms which enable barley plants to tolerate higher than normal levels of Na⁺.Abbreviations ABA abscisic acid - FW fresh weight     

Na-Stimulation of Photosynthesis in the Cyanobacterium Synechococcus UTEX 625 Grown on High Levels of Inorganic Carbon

Photosynthesis of washed cells of Synechococcus UTEX 625 grown on 5% CO₂ was markedly stimulated (647 ± 50%) at pH 8.0 by the addition of low concentrations of NaCl (concentration required for half-maximal response, K_½, = 18 micromolar). Studies with KCl and Na₂SO₄ showed that the stimulation was due to Na⁺. Photosynthesis at pH 6.1 was only slightly stimulated by Na⁺. The response of photosynthesis at pH 8.0 to [Na⁺] was strongly sigmoidal for dissolved inorganic carbon ([DIC] ≤ 500 micromolar). Cells grown with high total [DIC], but air-levels of CO₂, at pH 9.6 showed the same response to low [Na⁺]. The absence of Na⁺ could be partially, but not completely overcome, by higher [DIC]. Various methods for examining CO₂ or HCO₃⁻ use (K_½^CO₂ determination; isotopic disequilibrium; and consideration of HCO₃⁻ dehydration rate) were consistent with CO₂ use by the cells, but HCO₃⁻ use could not be ruled out. Isotopic disequilibrium studies showed that CO₂ use was stimulated by Na⁺. Cells grown on 5% CO₂ accumulated DIC against a concentration gradient by a process (or processes) dependent on Na⁺. No evidence for uptake of Na⁺ concomitant with DIC uptake could be found. The lack of O₂ evolution during the initial and most rapid period of DIC accumulation suggested that the required energy was obtained from cyclic photophosphorylation.     

Extension of sperm motility leads to increased rates of fertilization and hatching in curimba,Prochilodus lineatus

The objective of this study was to evaluate the effects of six activating solutions on duration of sperm motility, fertilization rate (FR), and hatching rate (HR) of Prochilodus lineatus (Valenciennes, 1837). The activating solutions (SA) used were: SA₀ (199 mOsm kg^?1, pH 8.5), SA₁ (138 mOsm kg^?1, pH 7.5), SA₂ (256 mOsm kg^?1, pH 7.5), SA₃ (131 mOsm kg^?1, pH 10), NaCl (92 mOsm kg^?1, pH 7.5) and distilled water (32 mOsm kg^?1, pH 7.5). SA₁ induced the highest motility, FR and HR, compared with the other activating solutions. The lowest motility was obtained with SA₀, with no fertilization or hatching, whereas motility was zero with SA₂ and SA₃. It is possible to conclude that the solution SA₁ can be used for the activation of gametes during fertilization in induced reproduction of curimba to achieve higher fertilization and hatching rates. Thus, it was found that the osmolality and pH of activating solutions, probably with the participation of dissolved substances therein, are the main factors acting on semen motility after activation.     

Counterion binding and hydration of hyaluronate and chondroitin in solution: An 17O, 23Na,and 25Mg nuclear-magnetic-relaxation study

Nuclear magnetic relaxation rates of H₂¹⁷O, ²³Na⁺, and ²⁵Mg²⁺ have been measured in aqueous hyaluronate solutions. The dependence on solution pH of the relaxation rates has been investigated, as well as the competition behavior of Na⁺ with Ca²⁺ and Mg²⁺. H₂¹⁷O and ²³Na⁺ relaxation rates in chondroitin and hyaluronate solutions have been compared in the interval, 2 ? pH ? 12.5. The ion binding of hyaluronate can be fully accounted for by Coulomb interactions, with no need to involve chemical specificity. The hydration is only slighly pH dependent, and is comparable in magnitude to hydration of synthetic polyelectrolytes and monosaccharides. Ion-binding and hydration properties of hyaluronate and chondroitin are quite similar, except at elevated pH. At alkaline pH, an increase in charge density with pH is seen in hyaluronate and, to a much lesser degree, in chondroitin, possibly due to the titration of hydroxy groups. H₂¹⁷O data indicate an alkali-induced transition in both glycosaminoglycans.     

Interaction of Calcium Ion with Bovine Caseins

In order to clarify the interaction of calcium ion with casein, the volume change associated with the interaction was measured by dilatometric procedures. When CaCl₂ was added to the casein solutions at neutral pH, a volume increase occurred and reached a constant saturated value of about 700 ml per 10⁶ g protein with increasing CaCl₂ concentrations for whole-, α_s- and β-casein solutions, but there was no volume change for κ-casein solution. On the other hand, the binding of calcium ion to the casein fractions was determined by a gel filtration procedure at pH 6.0 to 9.0. The number of Ca²⁺ ions bound to the caseins increased with the CaCl₂ concentration and pH value, and the relative order of binding capacities for the caseins was: α_s-casein > whole-casein > β-casein > κ-casein.

It was found that the volume changes obtained by the dilatometry were smaller than the calculated volume increases based on the assumption that these are caused by the binding of Ca²⁺ ion to the caseins. Therefore it is necessary to introduce another factor which reduces the volume increase due to the Ca²⁺ ion binding in order to reasonably explain the measured volume changes. At present it is presumed that there occurs the unfolding of peptide chain of casein molecule on Ca²⁺ ion binding, which has been known to decrease the volume of the protein solution.     

Thermostable Alkaline Protease from a Novel Marine Haloalkalophilic Bacillus Clausii Isolate

An oxidative and SDS-stable alkaline protease secreted by a marine haloalkalophilic Bacillus clausii isolated from the tidal mud flats of the Korean Yellow Sea near Inchon City was investigated in batch fermentation in shake flasks and in a bioreactor under a range of conditions. The isolate produced maximum protease yields (15,000 U ml⁻¹) under submerged fermentation conditions at 42 °C for 40 h with an aeration of 1.5 v/v/min and agitation of 400 rev/min in a formulated soybean—casein medium (pH 9.6) containing (w/v): soybean meal (2%), casein (1%), corn starch (0.5%), NH₄Cl (0.05%), NaCl (0.05%), KH₂PO₄(0.04%), K₂HPO₄(0.03%), MgSO₄(0.02%), yeast extract (0.01%) and Na₂CO₃(0.6%). The optimal pH and temperature of activity of the partially purified enzyme were 11.5 and 80 °C, respectively. The alkaline protease showed extreme stability towards SDS and oxidizing agents, retaining its activity above 96 and 75% on treatment for 72 h with 5% SDS and 5% H₂O₂, respectively. The inhibition profile exhibited by phenylmethanesulphonyl fluoride suggested that the protease from B. clausii belongs to the family of serine proteases.     

THE INFLUENCE OF ELECTROLYTES ON THE CATAPHORETIC CHARGE OF COLLOIDAL PARTICLES AND THE STABILITY OF THEIR SUSPENSIONS : II. EXPERIMENTS WITH PARTICLES OF GELATIN,CASEIN, AND DENATURED EGG ALBUMIN.

1. This paper gives measurements of the influence of various electrolytes on the cataphoretic P.D. of particles of collodion coated with gelatin, of particles of casein, and of particles of boiled egg albumin in water at different pH. The influence of the same electrolyte was about the same in all three proteins. 2. It was found that the salts can be divided into two groups according to their effect on the P.D. at the isoelectric point. The salts of the first group including salts of the type of NaCl, CaCl₂, and Na₂SO₄ affect the P.D. of proteins at the isoelectric point but little; the second group includes salts with a trivalent or tetravalent ion such as LaCl₃ or Na₄Fe(CN)₆. These latter salts produce a high P.D. on the isoelectric particles, LaCl₃ making them positively and Na₄Fe(CN)₆ making them negatively charged. This difference in the action of the two groups of salts agrees with the observations on the effect of the same salts on the anomalous osmosis through collodion membranes coated with gelatin. 3. At pH 4.0 the three proteins have a positive cataphoretic charge which is increased by LaCl₃ but not by NaCl or CaCl₂, and which is reversed by Na₄Fe(CN)₆, the latter salt making the cataphoretic charge of the particles strongly negative. 4. At pH 5.8 the protein particles have a negative cataphoretic charge which is strongly increased by Na₄Fe(CN)₆ but practically not at all by Na₂SO₄ or NaCl, and which is reversed by LaCl₃. the latter salt making the cataphoretic charge of the particles strongly positive. 5. The fact that electrolytes affect the cataphoretic P.D. of protein particles in the same way, no matter whether the protein is denatured egg albumin or a genuine protein like gelatin, furnishes proof that the solutions of genuine proteins such as crystalline egg albumin or gelatin are not diaphasic systems, since we shall show in a subsequent paper that proteins insoluble in water, e.g. denatured egg albumin, are precipitated when the cataphoretic P.D. falls below a certain critical value, while water-soluble proteins, e.g. genuine crystalline egg albumin or gelatin, stay in solution even if the P.D. of the particles falls below the critical P.D.