Phosphate supplying power of rock phosphates in an oxisol

Summary The P-supplying power of triple superphosphate, three apatitic rock phospates and a calcined aluminum rock phosphate were tested by measuring the quantities of fertilizer P recovered in soybean and in four chemical extractants, after 3-day and 75-day periods of contact between soil and fertilizer.The triple superphosphate supplied the highest amounts of P, but it lost efficiency during the longer incubation period. The rock phosphates maintained their original efficiencies, probably as a result of a balance between P released from the fertilizer and P converted into non-labile forms.The following coefficients of correlation between P uptake by soybean from an acid oxisol and P extracted by chemical extractants, after the two incubation periods, were found: 0.902^** for 0.01M CaCl₂; 0.823^** for anion-exchange resin; 0.720^** for 0.03N NH₄F+0.025N HCl; –0.037 (n.s.) for 0.025N H₂SO₄+0.050N HCl.The acid NH₄F solubilized residual calcined aluminum phosphate particles, and double acid extracted P from residual apatite particles, thus accounting for their poorer performances in predicting availability of fertilizer P.The relative efficiencies of the rock phosphates could largely be predicted after an incubation period of only three days. This finding attests to the presence in these rock phosphates of an easily soluble fraction of P which is not indicative of the degree of reactiveness of the phosphate as a whole.on leave at the Agricultural University during 1977.     

Biosolubilization of poorly soluble rock phosphates by Aspergillus tubingensis and Aspergillus niger

Three isolates of Aspergillus tubingensis and two isolates of Aspergillus niger isolated from rhizospheric soils were tested on solubilization of different rock phosphates. All the isolates of Aspergillus were capable of solubilizing all the natural rock phosphates. A. tubingensis (AT1) showed maximum percent solubilization in all the rock phosphates tested in this study when compared to other isolates. This isolate also showed highest phosphorus (P) solubilization when grown in the presence of 2% of rock phosphate. A. tubingensis (AT1) seems to be more efficient in solubilization of rock phosphates compared to other isolates reported elsewhere. This is the first report of rock phosphate solubilization by A. tubingensis and might provide an efficient large scale biosolubilization of rock phosphates intended for P fertilizer.     

Phosphorus transformations from rock phosphates in acid soils and measures for increasing their efficiency for growing rice (Oryza sativa L.)

Summary Laboratory incubation experiments showed that addition of rock phosphate to P-deficient acid red and laterite soils resulted in an increase in Al–P or/and Fe–P, with a consequent decrease in Ca–P during 15 days, of moist aerobic incubation. The transformations of P from Gafsa, Jordan, North Carolina and Florida rock phosphates were more than those from Tennessee, Missouri and Udaipur. Studies with North Carolina, Gafsa, and Udaipur rock phosphates showed that application of the former two to moist aerobic P-deficient acid soils 2 weeks prior to flooding and transplanting rice gave higher content of Al–P, Fe–P and Bray-P, compared to when these were applied at flooding. The grain yields obtained with the former two treatments were also at par with that obtained with the addition of superphosphate at comparable rate (100 ppm) of P application, compared to when the, rock phosphates were applied at flooding, where the grain yields were lower than the superphosphate treatment, indicating that some of these rock phosphates could be made as efficient as superphosphate for growing rice on acid soils by their application to moist aerobic soil, 2–3 weeks prior to flooding and transplanting rice and thus conserve some amount of sulphur required for the manufacture of water soluble phosphates.     

Optimizations of particle size and pulp density for solubilization of rock phosphate by a microbial consortium from activated sludge

Microbial solubilization of rock phosphate is getting more and more attention recently. However, the microorganisms used in previous studies were mostly single or known species, and seldom studies focused on the mixed microorganisms or microbial consortia from natural environments. In this study, a microbial consortium taken from activated sludge was used to solubilize two different mid-low-grade rock phosphates. The results showed that the microbial consortium could effectively solubilize the rock phosphates in National Botanical Research Institute’s phosphate growth medium and released soluble phosphorus in the broth. The biomass increased gradually, whereas the pH decreased sharply during the solubilizing process. The maximum phosphorus solubilization was recorded at particle size of 150?µm. Higher or lower than this optimal particle size, the phosphorus solubilization decreased. The phosphorus solubilization gradually decreased with a larger pulp density from 1 to 5%, and the optimal pulp density was 1%. The solubilization level of microbial consortium varied with different rock phosphates. The results revealed that the soluble phosphorus released from high-silicon ore was higher than which from high-magnesium ore. A strong positive correlation between biomass and phosphorus solubilization in the broth was observed from regression analysis results, and the phosphorus solubilization also had a significant negative correlation with pH in the broth.     

An evaluation of plant-borne factors promoting the solubilization of alkaline rock phosphates

Summary Four experiments are described in which the uptake patterns of various crop species were shown to enhance the solubilization of alkaline rock phosphates. In most cases, such enhancements resulted from soil acidification brought about by the alkaline uptake patterns. In one case, the enhancement may have stemmed primarily from a high Ca-uptake rate, which might be responsible for a shift in mass-action equilibria favoring the solubilization of rock phosphates. High uptake of Ca is expected to serve two purposes: 1. it acts in creating alkaline uptake patterns causing a decline in soil pH, and 2. it promotes a shift in mass-action equilibria.     

Phosphate solubilization potential and stress tolerance of Eupenicillium parvum from tea soil

Eupenicillium parvum was recorded for first time during isolation of phosphate-solubilizing microorganisms from the tea rhizosphere. The fungus developed a phosphate solubilization zone on modified Pikovskaya agar, supplemented with tricalcium phosphate. Quantitative estimation of phosphate solubilization in Pikovskaya broth showed high solubilization of tricalcium phosphate and aluminium phosphate. The fungus also solubilized North Carolina rock phosphate and Mussoorie rock phosphate, and exhibited high levels of tolerance against desiccation, acidity, salinity, aluminium, and iron. Solubilization of inorganic phosphates by the fungus was also observed under high stress levels of aluminium, iron, and desiccation, though the significant decline in phosphate solubilization was marked in the presence of aluminium than iron. The fungal isolate showed 100 % identity with E. parvum strain NRRL 2095 ITS 1, 5.8S rRNA gene and ITS 2, complete sequence; and 28S rRNA gene, partial sequence.     

Synthesis and properties of photolabile (caged) phosphotriester derivatives of dinucleoside phosphates

Dinucleoside phosphates that harbor phosphate groups transiently blocked (caged) byo-nitrobenzyl oro-nitroveratryl residues were synthesized. It was shown that the conditions of the UV-induced deprotection largely depend on the nature of the protective group. The phosphotriesters obtained were resistant toward snake venom phosphodiesterase and nucleases of the cellular extract. The synthesis of the dinucleoside phosphates containing a photolabile group preceeded the incorporation of the modified blocks into extended oligonucleotides by the phosphoramidite method.     

Absence of phosphates from the myosin heavy chains of striated muscles

This work aimed to determine whether the heavy chains of myosin from different striated muscle were phosphorylated. Myosin and its heavy chains were prepared from cardiac and skeletal muscles of rats injected in vivo with radioactive phosphates.The results for radioactive phosphate localization indicate the absence of phosphate from pure heavy chains and from any of their purified fragments, whatever the striated muscle used. In addition, phosphates are present in the myosin phosphorylated light chain and in a contaminating protein closely associated to the myosin heavy chain.     

Rock phosphate solubilization under alkaline conditions byAspergillus japonicus andA. foetidus

Aspergillus japonicus andA. foetidus were found to solubilize, five types of Indian rock phosphates at pH 8 and 9. Solubilization was higher in the presence of pyrite than in controls lacking either pyrite or fungal, inoculum. Both the aspergilli were found to be good pyrite solubilizers and could grow over a wide pH range. Solubilization of rock phosphates was the result of organic acid release and pyrite oxidation.     

Phosphoinositides and inositol phosphates in growth and photoconidiation ofTrichoderma viride

Incorporation of³H-inositol and³²P into the mycelium ofTrichoderma viride shows that this fungus contains phosphoinositides (PI) and inositol phosphates (IP). Under conditions suitable for the induction of photoconidiation, a pulse of light did not elicit a change in the incorporation of³²P but decreased the incorporation of³H-inositol into PI. The incorporation of³H-inositol into IP was unaffected by light. Inhibitors of PI metabolism, Li⁺ and neomycin, inhibited more effectively photoconidiation than vegetative growth. The distribution of the³H-inositol label in inositol phosphates was not changed by the light pulse.     

Minor nucleosides in RNA: Optical studies of dinucleoside phosphates containing dihydrouridine

Photoreduction with NaBH₄ was used to reduce the dinucleoside phosphates ApU, UpA, and GpU to the corresponding molecules containing dihydrouridine (H). Also obtained from this reaction are dinucleoside phosphates containing (β-N-ribosyl) ureido-propanol, an open ring form of dihydrouridine. The results of CD and ultraviolet absorption studies with these compounds imply that HpA is strongly stacked, but that ApH and GpH are only slightly stacked. The temperature dependence of the CD suggests that the stacking in HpA is unusual. The results with compounds containing open ring forms of dihydrouridine indicate that there is more intramolecular interaction when the ring is open than when it is closed.     

Flocculation of kaolin by waxy maize starch phosphates

Waxy maize starch phosphates were tested as flocculants in order to determine if they have the potential to replace petroleum-based polymer flocculants currently used commercially. Phosphorylation was carried out by dry heating of starches and sodium orthophosphates at 140 °C for 4 h. Native and phosphorylated waxy maize starches were ineffective as flocculants for kaolin in deionized water. However, in the presence of small amounts of Ca²⁺ (1–4 mM), starch phosphates were effective flocculants of kaolin at concentrations as low at 3–4 ppm. The optimal degree of substitution (DS) for flocculation was 0.024 but the effect of DS was rather small over the range DS 0.007–0.08. Although a common synthetic polymer flocculant (polyacrylamide-co-acrylic acid) was effective at 1 ppm, the lower cost of starches should make them economically competitive.     

Amplified luminometric assays of alkaline phosphatase using riboflavin phosphates

An asasy for alkaline phosphatase is described which is based on the hydrolysis of riboflavin phosphates (5′FMN or 4′FMN) to produce riboflavin. This is converted to 5′FMN using riboflavin kinase, and then asayed using the bacterial bioluminescent system from Vibrio harveyi or V. Fischeri. The most sensitive assay is obtained using 4′FMN, which can measure less than 20 amol after a 1-hour incubation.     

Distributional changes of P-labeled acid-soluble phosphates and phospholipids among subcellular fractions during early vertebrate embryonic development

Early developing embryos of the toad Bufo arenarum Hensel were employed to study the content and in vivo labeling with ³²P of the acid-soluble phosphates and phospholipids at the subcellular level. The radionuclide was administered to the female toad along with the pituitary extract used to induce the ovulation.Most of the total phospholipids (68%) and proteins (84%) are confined to the yolk platelet fractions. Up to the heart beat stage (130 h of development) there are no significant changes detectable in protein and phospholipid content.The total P content in trichloroacetic acid-soluble fraction was distributed mainly between postmitochondrial supernatant (58%) and yolk platelet fraction (37%) in the unfertilized oocyte. As development proceeds an increase was observed in the former and a decrease in the latter. The acid-solube phosphates in the mitochondrial fraction only amount to 4% of the total embryo throughout the examined stages.The unfertilized oocyte contains about 98% of acid-soluble phosphates labeled with ³²P in the postmitochondrial supernatant and as development proceeds a striking decrease was found to occur while the radioactivity in the acid-soluble phosphates of mitochondrial and yolk platelet fractions increases significantly during the studied stages. About 11.5% of the lost radioactivity from the acid-soluble phosphates was found to be used to label the phospholipids.     

Temperature-dependent properties of dinucleoside phosphates

The optical rotatory dispersion, hypochromism, and proton magnetic resonance were measured for a number of dinucleoside phosphates in both dilute salt solutions and in 25.2% LiCl (which freezes below ?70°C.) as a function of temperature. Two models for the “disordering” of dinucleoside phosphates: the two-state model and the oscillating dimer model, are used to analyze the data. Both models fit some of the data, but neither are completely satisfactory. Evidence is given for a dynamic structure of dinucleoside phosphates, in which the bases oscillate with respect to one another, remaining parallel to one another with no solvent in between, even at high temperatures. Implications of this model to the structures of single-strand sections of RNA's are discussed.     

Inositol phosphates in the environment

The inositol phosphates are a group of organic phosphorus compounds found widely in the natural environment, but that represent the greatest gap in our understanding of the global phosphorus cycle. They exist as inositols in various states of phosphorylation (bound to between one and six phosphate groups) and isomeric forms (e.g. myo, D-chiro, scyllo, neo), although myo-inositol hexakisphosphate is by far the most prevalent form in nature. In terrestrial environments, inositol phosphates are principally derived from plants and accumulate in soils to become the dominant class of organic phosphorus compounds. Inositol phosphates are also present in large amounts in aquatic environments, where they may contribute to eutrophication. Despite the prevalence of inositol phosphates in the environment, their cycling, mobility and bioavailability are poorly understood. This is largely related to analytical difficulties associated with the extraction, separation and detection of inositol phosphates in environmental samples. This review summarizes the current knowledge of inositol phosphates in the environment and the analytical techniques currently available for their detection in environmental samples. Recent advances in technology, such as the development of suitable chromatographic and capillary electrophoresis separation techniques, should help to elucidate some of the more pertinent questions regarding inositol phosphates in the natural environment.     

The metabolic significance of octulose phosphates in the photosynthetic carbon reduction cycle in spinach

¹⁴C-Labelled octulose phosphates were formed during photosynthetic ¹⁴CO₂ fixation and were measured in spinach leaves and chloroplasts. Because mono- and bisphosphates of d-glycero- d-ido-octulose are the active 8-carbon ketosugar intermediates of the L-type pentose pathway, it was proposed that they may also be reactants in a modified Calvin–Benson–Bassham pathway reaction scheme. This investigation therefore initially focussed only on the ido-epimer of the octulose phosphates even though ¹⁴C-labelled d-glycero- d-altro-octulose mono- and bisphosphates were also identified in chloroplasts and leaves. ¹⁴CO₂ predominantly labelled positions 5 and 6 of d-glycero- d-ido-octulose 1,8-P₂ consistent with labelling predictions of the modified scheme. The kinetics of ¹⁴CO₂ incorporation into ido-octulose was similar to its incorporation into some traditional intermediates of the path of carbon, while subsequent exposure to ¹²CO₂ rapidly displaced the ¹⁴C isotope label from octulose with the same kinetics of label loss as some of the confirmed Calvin pathway intermediates. This is consistent with octulose phosphates having the role of cyclic intermediates rather than synthesized storage products. (Storage products don’t rapidly exchange isotopically labelled carbons with unlabelled CO₂.) A spinach chloroplast extract, designated stromal enzyme preparation (SEP), catalysed and was used to measure rates of CO₂ assimilation with Calvin cycle intermediates and octulose and arabinose phosphates. Only pentose (but not arabinose) phosphates and sedoheptulose 7-phosphate supported CO₂ fixation at rates in excess of 120 μmol h⁻¹ mg⁻¹ Chl. Rates for octulose, sedoheptulose and fructose bisphosphates, octulose, hexose and triose monophosphates were all notably less than the above rate and arabinose 5-phosphate was inactive. Altro-octulose phosphates were more active than phosphate esters of the ido-epimer. The modified scheme proposed a specific phosphotransferase and SEP unequivocally catalysed reversible phosphate transfer between sedoheptulose bisphosphate and d-glycero- d-ido-octulose 8-phosphate. It was also initially hypothesized that arabinose 5-phosphate, an L-Type pentose pathway reactant, may have a role in a modified Calvin pathway. Arabinose 5-phosphate is present in spinach chloroplasts and leaves. Radiochromatography showed that ¹⁴C-arabinose 5-phosphate with SEP, but only in the presence of an excess of unlabelled ribose 5-phosphate, lightly labelled ribulose 5-phosphate and more heavily labelled hexose and sedoheptulose mono- and bisphosphates. However, failure to demonstrate any CO₂ fixation by arabinose 5-phosphate as sole substrate suggested that the above labelling may have no metabolic significance. Despite this arabinose and ribose 5-phosphates are shown to exhibit active roles as enzyme co-factors in transaldolase and aldolase exchange reactions that catalyse the epimeric interconversions of the phosphate esters of ido- and altro-octulose. Arabinose 5-phosphate is presented as playing this role in a New Reaction Scheme for the path of carbon, where it is concluded that slow reacting ido-octulose 1,8 bisphosphate has no role. The more reactive altro-octulose phosphates, which are independent of the need for phosphotransferase processing, are presented as intermediates in the new scheme. Moreover, using the estimates of phosphotransferase activity with altro-octulose monophosphate as substrate allowed calculation of the contributions of the new scheme, that ranged from 11% based on the intact chloroplast carboxylation rate to 80% using the carboxylation rate required for the support of octulose phosphate synthesis and its role in the phosphotransferase reaction.     

Haloacetol phosphates as affinity labels for methylglyoxal synthase

3-Bromo- and 3-iodoacetol phosphates irreversibly inactivate methylglyoxal synthase. The substrate, dihydroxyacetone phosphate, and inorganic phosphate protect against the inhibition. Although the 3-chloro derivative does not inactivate the enzyme, it is a competitive inhibitor. Reduction of the enzyme-inactivator complex with [${}^3\text{H}$]-NaBH₄ indicates the incorporation of four haloacetol phosphates per mole of enzyme. These studies suggest the bromo- and iodoacetol phosphates inactivate the enzyme by reacting with a nucleophilic group located in the active center.     

Hydrolysis of organic phosphates by corn and soybean roots

Because of the importance of organic phosphates as sources of P for plants, this work was performed to study the hydrolysis of nine organic phosphates by sterile, intact corn (Zea mays L.) and soybean (Glycine max L.) roots. Results showed that the rates of hydrolysis ofp-nitrophenyl phosphate (PNP) in buffered solutions by roots of three varieties of corn and three varieties of soybean ranged from 13 to 22 μmol PO₄−P g⁻¹ root h⁻¹ and from 2.1 to 2.2 μmol PO₄−P 0.1 g⁻¹ root h⁻¹, respectively. The average rate of hydrolysis of PNP in nonbuffered solutions was 2- to 3-fold lower for corn roots and 6- to 10-fold lower for soybean roots as compared with those obtained with buffered solutions. The orthophosphate released from hydrolysis of organic P compounds in buffered solutions during a 48-h incubation of corn roots showed that the maximum rate of hydrolysis of PNP was 4 to 6 times greater than the commonly used substrates: α- and β-glycerophosphates, phenolphthalein diphosphate, and glucose-6-phosphate. The rates of hydrolysis of glucose-6-phosphate and glucose-1-phosphate were similar and about 6- to 12-fold lower than that of PNP. Phosphoethanolamine and phosphocholine were hydrolyzed slightly, ando-carboxyphenyl phosphate was not hydrolyzed. The rates of hydrolysis of organic P compounds in nonbuffered solutions by corn and soybean roots were 1 to 3 and 1 to 10 times lower than those in buffered solutions, respectively. The trends in rates of hydrolysis by soybean roots of buffered organic P substrates were similar to those observed with corn roots, with the exception of glucose-1-phosphate and phosphoethanolamine.