The relative content of manganese in plants

Summary Oats, vetch, and rye were grown as successive crops in pots of a manganese-deficient soil to which -MnO₂ had been added in increasing amounts. Manganese deficiency of oats was overcome with 32 ppm of added manganese. Additions of 10, 18 and 32 ppm caused a decrease in concentration of maganese in the plants. Vetch and rye were unaffected by manganese deficiency and kept on accumulating manganese with increasing additions to the soil. Of the three plants vetch showed the greatest uptake of manganese, both with and without added manganese.     

Ethylenediamine uptake and metabolism in the cyanobacterium Anabaena variabilis

The cyanobacterium Anabaena variabilis showed a pH dependent uptake of ethylenediamine. No uptake of ethylenediamine was detected at pH 7.0. At higher pH values (e.g. pH 8.0 and pH 9.0) accumulation did occur and was attributed to diffusion of uncharged ethylenediamine in response to a pH gradient. A biphasic pattern of uptake was observed at these higher pH values. Treatment with l-methionine-d,l-sulphoximine (MSX) to inactivate glutamine synthetase (GS) inhibited the second slower phase of uptake without any significant alteration of the initial uptake. Therefore for sustained uptake, metabolism of ethylenediamine via GS was required. NH ₄ ⁺ did not alter the uptake of ethylenediamine. Ethylenediamine was converted in the second phase of uptake to an analogue of glutamine which could not be detected in uptake experiments at pH 7.0 or in uptake experiments at pH 9.0 following pretreatment of cells with MSX. Ethylenediamine treatment inhibited nitrogenase activity and this inhibition was greatest at high pH values.Abbreviations EDA 1,2-diaminoethane (ethylenediamine) - GS glutamine synthetase - HEPES 4-(2-hydroxyethyl)-1 piperazine ethanesulphonic acid - MSX l-methionine-dl-sulphoximine - membrane potential - Tricine N-tris(hydroxymethyl) methylglycine     

The effect of liming a neutral soil on the cycle of manganese

Summary A manganese-deficient soil was mixed at pH 7 and pH 8, both moist and dry with (a) -MnO₂ and (b) MnSO₄. The amounts of bivalent manganese were determined after incubating for varying times. With the moist soils more bivalent manganese was released at pH 8 than at pH 7. However, after long air-drying much more bivalent manganese was released than from the moist soils and more was released at pH 7 than at pH 8.     

Measurement of internal pH in the coccolithophoreEmiliania huxleyi using 2′,7′-bis-(2-carboxyethyl)-5(and-6)carboxyfluorescein acetoxymethylester and digital imaging microscopy

Internal pH (pH_i) was determined inEmiliania huxleyi (Lohmann) using the probe 2,7-bis-(2-carboxyethyl)-5(and-6)carboxyfluoresceinacetoxymethylester (BCEF-AM) and digital imaging microscopy. The probe BCECF-AM was taken up and hydrolysed to the free acid by the cells. A linear relationship was established between pH_i and the 490/450 fluorescence ratio of BCECF-AM over the pH range 6.0 to 8.0 using the ionophore nigericin. Two distinct pH domains were identified within the cell, the cytoplasmic domain (approx. pH 7.0) and the chloroplast domain (approx. pH 8.0). The average pH_i was 7.29 (±0.11) for cells in the presence of 2 mM HCO ₃ ^– . In the absence of HCO ₃ ^– the pH_i was decreased by 0.8 pH unit. The importance of these changes in pH_i is considered in relation to inorganic-carbon uptake.Abbreviations AM acetoxymethylester - BCECF 2,7-bis-(2-carboxyethyl)-5(and-6)carboxyfluorescein - Hepes 4-(2-hydroxyethyl)-1-piperazine ethanesulfonic acid - pH_i intracellular pH     

The uptake and metabolism of methylamine by N2-fixing cyanobacteria

The cyanobacteria Anabaena variabilis and Nostoc CAN showed a biphasic pattern of ¹⁴CH₃NH ₃ ⁺ uptake at external pH values of 7.0 and 9.0. The initial phase of uptake, which was independent of metabolism of ¹⁴CH₃NH ₃ ⁺ , was attributed to uptake via a CH₃NH ₃ ⁺ (NH ₄ ⁺ ) transport system at pH 7.0 and probably to passive diffusion of uncharged CH₃NH₂ and trapping by protonation at pH 9.0. The second slower phase of uptake was attributed to metabolism of CH₃NH ₃ ⁺ via glutamine synthetase to form -methylglutamine which accumulates. Anabaena cylindrica showed an initial rapid uptake at pH 7.0 and pH 9.0 but metabolism of ¹⁴CH₃NH ₃ ⁺ was undetectable at pH 7.0 and was barely detectable at pH 9.0. Pretreatment of A. variabilis with l-methionine-d,l-sulphoximine to inactivate glutamine synthetase, inhibited the second phase of ¹⁴CH₃NH ₃ ⁺ uptake at both pH 7.0 and pH 9.0 and the accumulation of -methylglutamine but had no effect on the first phase of uptake. Following transfer of A. variabilis to darkness the initial phase of ¹⁴CH₃NH ₃ ⁺ uptake at pH 7.0 and 9.0 was unaffected but the subsequent metabolism via glutamine synthetase was inhibited.Abbreviations MSX l-methionine-d,l-sulphoximine - GS glutamine synthetase     

Manganese deficiency of sugar beet in organic soils

Summary The manganese content of sugar beet grown in pots of organic soils taken from fields where crops regularly show symptoms of manganese deficiency, and the effects on it of foliar sprays of manganous sulphate and of manganous oxide or manganese silicate frit applied to the soil, of changing the soil pH, air-drying the soil, and growing the plants either in the glasshouse or outside were determined. All the manganese treatments increased the concentration of manganese in the plants and decreased deficiency symptoms, but increased the dry matter yield only slightly. Increasing the pH by liming greatly increased symptoms and decreased the manganese concentration in the dry matter; air-drying the soil before cropping had the opposite effect. Plants grown in pots of the same soil in the glasshouse or outdoors showed similar symptoms and had similar manganese content.The concentration of manganese in the leaves was related to the percentage of plants with deficiency symptoms and to the concentration of active soil manganese. Leaves usually had symptoms when the concentration of manganese in the dried leaves was less than 30 ppm, and always had severe symptoms when they contained less than 15 ppm Mn. The soil analyses suggest that sugar beet grown in organic soil with pH greater than 7.0 and containing less than 40 ppm active soil manganese is likely to show deficiency symptoms.     

Studies on the Pentose Isomerases of Lactic Acid Bacteria

Production of d-xylose and l-arabinose isomerases by lactic acid bacteria was greatly promoted by the addition of manganese ions in cultural medium. Effective concentration of the ions was 5 × 1O^-3 m. Ferrous ions were also effective for the production of d-xylose isomerase and cobaltous ions were somewhat effective for the production of l-arabinose isomerase. Zinc and cadmium ions inhibited bacterial growth. It was possible to increase the production of isomerase by changing MnSO₄ concentration to 5× 10^-3 m (0.l1 %) in place of 0.001 per cent in the normal medium.

Column chromatographic procedures for the purification of pentose isomerases were carried out. Cation and anion exchange resins were not suitable because of their low exchange capacities and instability of the enzyme at acidic pH range. But the isomerases were successfully purified by DEAE-cellulose column chromatography with high recovery (85~90%). Using a Tris buffer, KCl concentration was increased in gradient. d-Xylose isomerase was eluted at pH 7.0 at 0~0.2 m KCl, and l-arabinose isomerase at pH 8.0 at 0~0.4 m KCl. The purified isomerases, d-xylose isomerase and l-arabinose isomerase, both required manganese ions specifically for their activities.

D-Xylose isomerase and l-arabinose isomerase are different enzymes which can be separated from each other with acetone fractionation at pH 4.8~5.0, heat treatment or chromatography on a colnmn of DEAE-cellulose. In DEAE-cellulose chromatography with a linear gradient elution method, d-xylose isomerase is recovered in the first peak at pH 7.0 (Tris bnffer) with 0~0.2 m KCl, and l-arabinose isomerase is eluted in the second peak at pH 8.0 (Tris buffer) with a larger ionic strength.     

Amiloride-sensitive Na+ transport in human red cells: Evidence for a Na/H exchange system

Summary The role of transmembrane pH gradients on the ouabain, bumetanide and phloretin-resistant Na⁺ transport was studied in human red cells. Proton equilibration through the Jacobs-Stewart cycle was inhibited by the use of DIDS (125 m) and methazolamide (400 m). Red cells with different internal pH (pH _i =6.4, 7.0 and 7.8) were prepared and Na⁺ influx was measured at different external pH (pH _o =6.0, 7.0, 8.0). Na⁺ influx into acid-loaded cells (pH _i =6.4) markedly increased when pH _o was raised from 6.0 to 8.0. Amiloride, a well-known inhibitor of Na⁺/H⁺ exchange systems blocked about 60% of the H⁺-induced Na⁺ entry, while showing small inhibitory effects in the absence of pH gradients. When pH₀ was kept at 8.0, the amiloride-sensitive Na⁺ entry was abolished as pH _i was increased from 6.4 to 7.8. Moreover, measurements of H⁺ efflux into lightly buffered media indicated that the imposition of an inward Na⁺ gradient stimulated a net H⁺ efflux which was sensitive to the amiloride analog 5-N-methyl-N-butyl-amiloride. Furthermore, in the absence of a chemical gradient for Na⁺ (Na _i ⁺ =Na ₀ ⁺ =15mm,Em=+6.7 mV), an outward H⁺ gradient (pH _i =6.4, pH₀=8.0) promoted a net amiloride-sensitive Na⁺ uptake which was abolished at an external pH of 6.0. These findings are consistent with the presence of an amiloride-sensitive Na⁺/H⁺ exchange system in human red cells.     

Bauxite residue sand has the capacity to rapidly decrease availability of added manganese

Bauxite residue sand, even though a poor substrate for plant growth because of very high pH, salinity and sodicity, is required to be revegetated. Manganese deficiency is observed in residue-grown plants because broadcast applications of manganese fertiliser to the surface of residue deposits have a low residual value. In a laboratory experiment, manganese (as MnSO₄) was added to fresh and 4-year-old residue sand and a sequential fractionation procedure performed at 0, 1, 4, 8 and 24 h and 6, 14, 21, 43, 73, 103 and 130 d. Extraction with DTPA estimated plant-available Mn, while sequential fractionation with various extractants yielded the following fractions: readily soluble [Ca(NO₃)₂]; weakly adsorbed [CaDTPA-B₄O₇]; carbonate-bound [HNO₃]; and oxide-bound [NH₂OHHCl]. Residual Mn was calculated as a difference between the sum of all these forms and total Mn in residue sand. Transformation of manganese from the initially dominant readily soluble form to the less-available forms was very rapid (< 24 h). A change to fertilisation strategies is required if better efficiency of manganese application and uptake is to be achieved for plants growing on bauxite residue.     

Effect of the manganese ion on human α3/4 fucosyltransferase III activity

The effect of manganese and other divalent cations on the activity of a soluble recombinant form of human 3/4 fucosyltransferase III (SFT3) expressed in Spodoptera frugiperda (Sf9) insect cells was studied. SFT3 was active in the absence of divalent cations with an optimum pH of 4.5. In the absence of Mn²⁺ increasing the pH from 4.5 to 7.0 caused a decrease in the affinity of SFT3 for the acceptor Gal3GlcNAcO(CH₂)₃NHCO(CH₂)₅NH-biotin, as monitored by the 4-fold increase in the apparent K_M value (0.9 to 3.3 mM). At pH 7.0, the addition of Mn²⁺ activated the enzyme and caused an increase in the affinity of SFT3 for the acceptor, as monitored by the 5-fold decrease of the apparent K_M value (3.3 to 0.7 mM). In solution, a complex between GDP-Fuc donor and the divalent cation Mn²⁺ was observed by electrospray ionization mass spectrometry, in a 1:1 stoichiometry. These results indicated that Mn²⁺ bound the enzyme and increased its affinity for the acceptor; one possible functional role of manganese in catalysis could be as an electrophilic catalyst, co-ordinating the negative charges of the phosphate groups of the GDP-Fuc donor and promoting Fuc transfer. At low pH values such role would be played by the proton.     

Interactions of glycolate-, HCO 3 - -, Cl--, and H+-balance of Scenedesmus obliquus

Excretion and absorption of glycolate by young cells of Scenedesmus obliquus (Turp.) Krüger strain D₃ grown synchronously with 2% CO₂ was compared after no pretreatment with air (CO₂-adapted) or after a 2 h adaptation to normal air (0.03% CO₂) (air-adapted). At 21% O₂, excretion occurred only from CO₂-adapted cells at high pH (pH 8.0). Under conditions where no excretion occurred, external glycolate (0.2 mM) was taken up by both air-and CO₂-adapted cells at a much faster rate at pH 5 than at pH 8. The uptake was accompanied by an apparent stoichiometric uptake of H⁺. CO₂-adapted algae exhibited high uptake rates that were even higher in the dark than in the light. Air-adapted algae showed high uptake rates in the light but only minimal uptake in the dark. The uptake rate was decreased to about 1/3 with 5% CO₂, except with CO₂-adapted cells in the light, in which a slight stimulation occurred. Cl^- ions inhibited glycolate uptake by air-adapted cells in the light; conversely, light-stimulated Cl^- uptake of these cells was inhibited by glycolate. A hypothesis is discussed according to which the internal pH regulates the uptake and release of Cl^-, HCO ₃ ^- , and glycolate.Abbreviations DCMU 3-(3,4 dichlorophenyl)-1, 1-dimethyl urea - FCCP carbonyl cyanide p-trifluoro-methoxyphenylhydrazone - HEPES 2-(4-(2-hydroxyethyl)-piperazinyl) ethanesulfonic acid - HPMS -hydroxypyridinemethanesulfonate - MES 2-morpholinoethanesulfonic acid - PCV packed cell volume     

Kinetic and Structural Properties of NADP-Malic Enzyme from Sugarcane Leaves

Oligomeric structure and kinetic properties of NADP-malic enzyme, purified from sugarcane (Saccharam officinarum L.) leaves, were determined at either pH 7.0 and 8.0. Size exclusion chromatography showed the existence of an equilibrium between the dimeric and the tetrameric forms. At pH 7.0 the enzyme was found preferentially as a 125 kilodalton homodimer, whereas the tetramer was the major form found at pH 8.0. Although free forms of l-malate, NADP⁺, and Mg²⁺ were determined as the true substrates and cofactors for the enzyme at the two conditions, the kinetic properties of the malic enzyme were quite different depending on pH. Higher affinity for l-malate (K_m = 58 micromolar), but also inhibition by high substrate (K_i = 4.95 millimolar) were observed at pH 7.0. l-Malate saturation isotherms at pH 8.0 followed hyperbolic kinetics (K_m = 120 micromolar). At both pH conditions, activity response to NADP⁺ exhibited Michaelis-Menten behavior with K_m values of 7.1 and 4.6 micromolar at pH 7.0 and 8.0, respectively. Negative cooperativity detected in the binding of Mg²⁺ suggested the presence of at least two Mg²⁺ - binding sites with different affinity. The K_a values for Mg²⁺ obtained at pH 7.0 (9 and 750 micromolar) were significantly higher than those calculated at pH 8.0 (1 and 84 micromolar). The results suggest that changes in pH and Mg²⁺ levels could be important for the physiological regulation of NADP-malic enzyme.     

Active transport of proline into washed cells of Rhodopseudomonas sphaeroides f. sp. denitrificans grown with nitrate

Washed cells of Rhodopseudomonas sphaeroides f. sp. denitrificans, prepared from cultures grown anaerobically in light with NO ₃ ^- as the terminal acceptor, readily incorporated [¹⁴C]-proline both in light and in the dark. The proline uptake was coupled to the reduction of either NO ₃ ^- , NO ₂ ^- , N₂O or O₂. Light stimulated the accumulation of proline in these cells. The addition of NO ₃ ^- to washed cells in light decreased the K _m for proline from 40 M to 5.7 M. Proline transport was inhibited by antimycin A, 2-n-heptyl-4-hydroxyquinoline-N-oxide both in light and in the dark with nitrate indicating that electron transfer from both denitrification and photosynthesis are involved in this uptake. Inhibition by carbonyl cyanide-m-chlorophenyl hydrazone and 2.4-dinitrophenol indicate that proline transport is energy dependent. The H⁺/proline stoichiometry increased from 1 to 2.5 when the external pH was increased from 6.0 to 8.0. Under these conditions pro increased but p decreased markedly above pH 7.0.Abbreviations TPP⁺ Tetraphenylphosphonium bromide - EDTA ethylenediamine-tetra-acetic acid - CCCP carbonyl cyanide-m-chlorophenyl hydrazone - DNP 2,4-dinitrophenol - HOQNO 2-n-heptyl-4-hydroxyquinoline-N-oxide - DBMIB dibromo-methyl-isopropyl-p-benzoquinone - DCCD N,N-dicyclohexylcarbodiimide     

Evidence for the contribution of pseudocyclic photophosphorylation to the energy requirement of the mechanism for concentrating inorganic carbon in Chlamydomonas

Mass-spectrometric measurements of ¹⁶O₂ and ¹⁸O₂ were made to compare the rates of light-dependent O₂ evolution and uptake by Chlamydomonas reinhardtii Dang. grown in air (0.035% CO₂; low-C_i cells) or CO₂-enriched air (5% CO₂; high-C_i cells) at pH 5.5 and 8.0. While at pH 5.5, no differences were observed in the isotopic O₂-gas exchange of high- and low-C_i cells, at pH 8.0 the rates of true O₂ evolution and uptake were considerably higher in low-C_i than in high-C_i cells. The enhanced rates of O₂ uptake and evolution by low-C_i cells were completely inducible within 6 h after transferring high-C_i cells to ambient air. At pH 8.0, O₂ uptake in the light was inhibited by 2 M 3-(3,4-dichlorophenyl)-1,1 dimethylurea in both types of alga, but this effect was more pronounced in low-C_i than in high-C_i cells.When the cells were grown at pH 5.5 the activities of the superoxide-radical-degrading enzymes, superoxide dismutase, ascorbate peroxidase, monodehydroascorbate reductase, dehydroascorbate reductase and glutathione reductase, were similar regardless of the CO₂ concentration provided during growth. At pH 8.0, however, the activities of these enzymes were 4 to 20 times higher in low-C_i than in high-C_i cells. When high-C_i cells were allowed to acclimate to ambient air for 6 h at pH 8.0, the activities of superoxide dismutase, ascorbate peroxidase and monodehydroascorbate dehydrogenase increased to more than 50% of the level observed with low-C_i cells. These results are consistent with an enhanced operation of O₂ photoreduction which could provide energy to the inorganic-carbon-concentrating mechanism via pseudo-cyclic photophosphorylation.     

Xylanolytic anaerobic thermophiles from Icelandic hot-springs

Anaerobic enrichment cultures inoculated with neutral and alkaline (pH 7.0–9.0) sediment and biomat samples from hot-springs in Hveragerdi and Fluir, Iceland, were screened for growth on beech xylan from pH 8.0 to 10.0 at 68° C: no growth occured in cultures above pH 8.4. Five anaerobic xylanolytic bacteria were isolated from enrichment cultures at pH 8.4; all five microbes were Gram-positive rods with terminal spores, and produced CO₂, H₂, acetate, lactate and ethanol from xylan and xylose. One of the isolates, strain A2, grew from 50 to 75° C, with optimum growth near 68° C, and from pH 5.2 to 9.0 with an optimum between 6.8 and 7.4. Taxonomically, strain A2 was most similar to Clostridium thermohydrosulfuricum. At pH 7.0, the supernatant xylanases of strain A2 had a temperature range from 50 to 78° C with an optimum between 68 and 78° C. At 68° C, xylanase activity occurred from pH 4.9 to 9.1, with an optimum from pH 5.0 to 6.6. At pH 7.0 and 68° C, the K _m of the supernatant xylanases was 2.75 g xylan/l and the V _max was 2.65 × 10^–6 kat/l culture supernatant. When grown on xylose, xylanase production was as high as when grown on xylan. Correspondence to: B. K. Ahring     

16O2/18O2 analysis of oxygen exchange in Dunaliella tertiolecta. Evidence for the inhibition of mitochondrial respiration in the light

A mass spectrometric ¹⁶O₂/¹⁸O₂-isotope technique was used to analyse the rates of gross O₂ evolution, net O₂ evolution and gross O₂ uptake in relation to photon fluence rate by Dunaliella tertiolecta adapted to 0.5, 1.0, 1.5, 2.0 and 2.5 M NaCl at 25°C and pH 7.0.At concentrations of dissolved inorganic carbon saturating for photosynthesis (200 M) gross O₂ evolution and net O₂ evolution increased with increasing salinity as well as with photon fluence rate. Light compensation was also enhanced with increased salinities. Light saturation of net O₂ evolution was reached at about 1000 mol m^-2s^-1 for all salt concentrations tested. Gross O₂ uptake in the light was increased in relation to the NaCl concentration but it was decreased with increasing photon fluence rate for almost all salinities, although an enhanced flow of light generated electrons was simultaneously observed. In addition, a comparison between gross O₂ uptake at 1000 mol photons m^-2s^-1, dark respiration before illumination and immediately after darkening of each experiment showed that gross O₂ uptake in the light paralleled but was lower than mitochondrial O₂ consumption in the dark.From these results it is suggested that O₂ uptake by Dunaliella tertiolecta in the light is mainly influenced by mitochondrial O₂ uptake. Therefore, it appears that the light dependent inhibition of gross O₂ uptake is caused by a reduction in mitochondrial O₂ consumption by light.Abbreviations DCMU 3-(3, 4-dichlorophenyl)-1, 1-dimethylurea - DHAP dihydroxy-acetonephosphate - DIC dissolved inorganic carbon - DR_a rate of dark respiration immediately after illumination - DR_b rate of dark respiration before illumination - E₀ rate of gross oxygen evolution in the light - NET rate of net oxygen evolution in the light - PFR photon fluence rate - RubP rubulose-1,5-bisphosphate - SHAM salicyl hydroxamic acid - U₀ rate of gross oxygen uptake in the light     

Production of biosurfactant “Biosur-Pm” by Pseudomonas maltophila CSV89: characterization and role in hydrocarbon uptake

Pseudomonas maltophilia CSV89, a soil bacterium, produces an extracellular biosurfactant, Biosur-Pm. The partially purified product is nondialyzable and chemically composed of 50% protein and 12–15% sugar, which indicates the complex nature of Biosur-Pm. It reduces the surface tension of water from 73 to 53×10^-3 N m^-1 and has a critical micellar concentration of 80 mg/l. Compared to aliphatic hydrocarbons, Biosur-Pm shows good activity against aromatic hydrocarbons. The emulsion formed is stable and does not require any metal ions for emulsification. The kinetics of Biosur-Pm production suggest that its synthesis is a growth-associated and pH-dependent process. At pH 7.0, cells produced more Biosur-Pm with less cell surface hydrophobicity. At pH 8.0, however, the cells produced less Biosur-Pm with more cell surface hydrophobicity and showed a twofold higher affinity for aromatic hydrocarbons compared to the cells grown at pH 7.0. The Biosur-Pm showed a pH-dependent release, stimulated growth of the producer strain on mineral salts medium with 1-naphthoic acid when added externally, and facilitated the conversion of salicylate to catechol. All these results suggest that Biosur-Pm is probably a cell-wall component and helps in hydrocarbon assimilation/uptake.     

SO2 and NO2 effects on microbial activity in an acid forest soil

The rate of glucose decomposition and the pH fell in a forest soil (initial pH 4.06) exposed to 1.0 ppm SO₂. No such effect was noted if the soil was exposed to 1.0 ppm nitrogen dioxide (NO₂). Nitrite but not bisulfite (5g N or S/g of soil) inhibited O₂ consumption and CO₂ evolution in the glucose-amended forest soil, and nitrite and bisulfite acted synergistically in inhibiting these processes. Iron and manganese were solubilized when the soil was exposed to 10 ppm SO₂, but NO₂ caused no such change.     

Soil phosphorus levels needed for equal P uptake from four soils with different water contents at the same water potential

Soil volumetric water contents, , at –33 kPa potential may vary with soil from 0.06 to 0.70. Because P diffusion depends on , most economic P fertilizer rates required for different soils may require adjusting according to their soil-water relationships. The objective of this study was, after experimentally verifying a mechanistic nutrient uptake model on a series of soils varying in at –33 kPa potential, to use the model to predict labile P levels needed for each of these soils to achieve equal P uptake by maize (Zae mays L.) and verify these predictions. Maize was grown in a pot experiment using four soils having of 0.13, 0.20, 0.26, and 0.40 at –33 kPa each at 0, 200, and 400 mg kg^-1 of added P. When root parameters obtained experimentally were used, predicted P uptake with the uptake model agreed with observed P uptake, y=0.99x+9.08 (r²=0.98). When P uptake was plotted vs. soil solution P, C_li, the relation varied with soil. The higher the the lower the C_li needed for equal P uptake. A similar relation was found between P uptake and diffusible soil P, C_si. Differences between the two plots occurred because of differences among soils in buffer power, C_si/C_li. The C_si vs. P added relation was used to calculate differences among soils in the C_si needed to obtain equal P uptake. The C_si values ranged from 1.3 to 4.0 mmol kg^–1. The calculated values were used in a second pot experiments to verify the predictions. No significant difference (=0.05) in P uptake occurred. The results of this research indicate that the mechanistic nutrient uptake model can be used to predict the degree of adjustments in C_si needed to obtain the most economic P fertilizer rates among soils varying in .Journal Paper No. 13072. Purdue Univ. Agric. Exp. Stn., West Lafayette, IN 47907.     

The influence of metal cations and pH on the heat sensitivity of photosynthetic oxygen evolution and chlorophyll fluorescence in spinach chloroplasts

The heat-sensitivity of photosynthetic oxygen evolution of thylakoids isolated from spinach increases by increasing the pH above neutral value. The temperature for inactivation (transition temperature) is lowered from about 45° C (pH 6.0–7.4) to 33°C (pH 8.5). Similar results are obtained with intact chloroplasts. At pH 7.0 the transition temperature of washed thylakoids decreases by lowering the salt concentration below 20 mM with monovalent cations (Li⁺, Na⁺, K⁺) and below 3–4 mM with divalent cations (Mg²⁺, Ca²⁺, Sr²⁺). Illumination decreases the heat-sensitivity of oxygen evolution in intact chloroplasts, but even increases the heat-sensitivity in uncoupled chloroplasts. In intact chloroplasts the transition temperature of the heat-induced rise in chlorophyll fluorescence yield (F_o; see Schreiber and Armond 1978) decreases from 44° C to 38° C when the pH of the suspending medium is increased from 6.5 to 8.5. At 20° C, F_o is almost insensitive to pH (6.0–8.5). At 40° C, however, F_o is constant between 6.0 and 7.0, but strongly increases by increasing the pH above neutral value. The results are discussed in terms of a close relation between electrostatic forces at the thylakoid membrane and thermal sensitivity of photosynthetic apparatus. It is suggested that the heat-sensitivity of the photosystem II complex partially depends on the ionization state of fixed groups having alkaline pK. The packed volume of thylakoids suspended in a low salt medium increases when the temperature is increased above 30° C (pH 7.0) and above 20° C (pH 8.0), respectively. This result suggests a heat-induced increase in surface charge density of the thylakoid membrane.Abbreviations HEPES N-2-hydroxyethylpiperazine-N-2-ethane sulfonic acid - MES morpholinoethane sulfonic acid - MOPS 2-N-morpholinopropane sulfonic acid - TRICIN N-[tris(hydroxymethyl)-methyl] glycine