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USDA Agricultural Research Service, New England Plant, Soil, and Water Lab., Univ. of Maine, Orono, ME 04469
* Corresponding author (zhe{at}maine.edu)
Received for publication December 8, 2000.
| ABSTRACT |
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Abbreviations: NMR, nuclear magnetic resonance P-a and P+a, orthophosphate determined after samples were incubated in the absence and presence of alkaline phosphatase P-w and P+w, orthophosphate determined after samples were incubated in the absence and presence of wheat phytase
| INTRODUCTION |
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Phosphorus-31 nuclear magnetic resonance (NMR) offers another way to identify and quantify the relative amount of organic P. The procedure was first applied to 0.5 M NaOH soil extracts in 1980 (Newman and Tate, 1980). This method has identified structural features of alkali-soluble P mainly as orthophosphate, monoester P, diester P, and pyrophosphate (Condron et al., 1985; Hawkes et al., 1984; Leinweber et al., 1997; Newman and Tate, 1980; Rubaek et al., 1999). Identification of more specific P forms by 31P NMR, such as glucose-6-phosphate and teichoic acid in NaOH extract, has been reported recently (Guggenberger et al., 1996; Pant et al., 1999). To our knowledge, no study has been reported that correlates the P data obtained from 31P NMR to that taken from sequential fractionation.
In nature, phosphatases catalyze chemical reactions that release orthophosphate from various types of organic phosphorus compounds. Those enzymes provide a possibility to enzymatically identify and quantify organic P forms in manure. That is, if a manure sample is incubated with a specific phosphatase, the resulting inorganic phosphate concentration will represent the corresponding type of organic P and its amount in the sample. Phosphatases (acid and alkaline) and phytase have been used to release organic phosphorus compounds in soil solutions (Hayes et al., 2000; Pant et al., 1994; Shand and Smith, 1997). Bishop et al. (1994) reported enzymatic mineralization of organic phosphorus in a volcanic soil in Chile in which soil samples were incubated with four phosphate-releasing enzymes, and then 31P NMR analysis of both untreated and treated 1 M NaOH soil extracts was used to show the change in soil organic phosphorus. To our knowledge, no such biological or enzymatic approaches have been used in the characterization of organic P in animal manure.
The objective of this study was to evaluate an enzymatic approach for quantifying manure-derived organic P compounds. As a first step in exploring this novel enzymatic approach, we examined the release of orthophosphate from pig and cattle manure by several commercially available phosphatases.
| MATERIALS AND METHODS |
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Sequential Fractionation of Manure Phosphorus
A modification of the method presented by Sui et al. (1999) was used in this study (Fig. 1). Duplicate samples were fractionated. Each manure sample (0.25 g) was placed in a centrifuge tube with 30 mL of distilled water. The tubes were set horizontally on the platform of an orbital shaker (250 rpm) for 16 h at room temperature (22°C). The samples were then centrifuged at 2800 x g for 30 min at 4°C, and the supernatant was decanted and saved. The residues were then suspended in 10 mL of water. The suspension was shaken for 1 h (250 rpm on the orbital shaker) and the residues were spun down in the same way as above. The two supernatants were pooled and used for the P assay. The same procedure was repeated for fractionation by 0.5 M NaHCO3, 0.1 M NaOH, and 0.1 M HCl (Fig. 1). Those fractions were neutralized to pH 7.0 by appropriate amounts of 2 M HCl or NaOH.
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Release of Organic Phosphorus from Manure Extraction Fractions
A portion of each fraction (250 µL in a total 500-µL reaction mixture) was incubated for 30 min in the presence or absence of wheat phytase (0.1 U mL-1) at 55°C or alkaline phosphatase (1 U mL-1) at room temperature. The reaction mixture for the phytase reaction was 100 mM potassium acetate (pH 5.0). The reaction mixture for the alkaline phosphatase reaction was 100 mM Tris-HCl buffer (pH 9.0) with 1 mM MgCl2 and 0.1 mM ZnCl2. Total P was released by H2SO4H2O2 digestion (Thomas et al., 1967). Orthophosphate in these mixtures was then assayed by a molybdate blue method modified by the inclusion of citratearsenate reagent to minimize the interference of labile organic and inorganic phosphorus (Dick and Tabatabai, 1977).
Designation of Phosphorus Forms
Simple monoester P in a given sample was calculated from the difference in orthophosphate contents determined after incubation in the presence and absence of alkaline phosphatase (P+a - P-a in Fig. 3). Phytate-like P was calculated from the difference in orthophosphate released with phytase and alkaline phosphatase (P+w - P+a in Fig. 3). DNA-like P was the difference of orthophosphate content in a given sample preincubated with or without nuclease P1 (Pnu - P+w in Fig. 4). Organic pyrophosphates were calculated from the difference in orthophosphate content in a given sample preincubated with or without nucleotide pyrophosphatase (Ppy - P+w in Fig. 4). Total organic P was determined by the difference in P from an H2SO4H2O2 digested sample and inorganic P (undigested sample). Inorganic P was calculated as the average P contents measured at pH 5.0 and at pH 9.0 without enzymatic incubation (P-a and P-w).
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| RESULTS AND DISCUSSION |
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Phosphorus Distribution in Fractions of Sequential Treatments
Two types of animal manure, one from monogastric pigs and one from polygastric cattle, were used in this study. The specific activity of crude wheat phytase from the supplier was very low (0.03 unit per mg solid), compared with 2745 units per mg of protein for the alkaline phosphatase reagent. In other words, the purchased phytase preparation contained many impurities. In addition, precipitates were observed during orthophosphate determination by the modified molybdate-blue method when the enzyme was used at a concentration of 1 unit per mL in the P-releasing incubation. To reduce interference, the concentration of wheat phytase was changed to 0.1 unit per mL of reaction mixture, and the incubation temperature was increased from room temperature to 55°C (at which the activity was increased by about five- or sixfold). The activity of wheat phytase under such conditions was still far more than the amount required to release relevant organic P from the samples.
Total P and inorganic P were 3875 ± 9 and 1959 ± 60 mg per kg of dry pig manure and 3450 ± 187 and 1946 ± 78 mg per mg of dry cattle manure, respectively (Fig. 3). The data indicated that about 49% of P in pig manure was in organic forms, and about 44% of P in the cattle manure was present as organic P.
Organic phosphorus mainly distributed in H2O, Na-HCO3, and NaOH fractions. Treatment of these fractions with the two enzymes did provide information about P forms found in the sequential fractions, in addition to the conventionally determined values for inorganic P and total P (Fig. 3).
In H2O fractions of both manures, P-a was about 5 to 8% greater than P-w (Fig. 3). This might be caused by measurement interference or by decomposition of some organic P at pH 9.0. In the pig manure fraction, 4% more orthophosphate was observed after treatment with alkaline phosphatase. Treatment with wheat phytase released 33% more P than observed for untreated controls in pig manure, and 20% more in cattle manure. The substrate specificity in Fig. 2 suggested that the inability of alkaline phosphatase acting on phytate is the cause of the difference. Pant et al. (1994) reported that phytase released nearly twice as much P as acid and alkaline phosphatases did in water extracts of soil. The authors suggested that a significant part of the inositol-type material was unavailable, either "hidden" or protected from the two more general phosphatases. In fact, we believe that characterizing the difference as phytate seems more convenient and easier to understand.
The P forms in NaHCO3 fractions seem to be similar in both manure samples (Fig. 3). In the NaHCO3 fraction, enzymatic treatments increased orthophosphate by only 6.3 and 1.9% for pig and cattle manure, respectively, still leaving 96 and 98% of the organic P forms unknown. Hayes et al. (2000) reported that only a small proportion (19%) of NaHCO3extracted organic P in three soil samples was hydrolyzable by wheat phytase. Otani and Ae (1999) also reported a negligible amount of organic P in NaHCO3 extracts from a range of soils. Our data indicated that most NaHCO3extractable organic P from animal manure was also unhydrolyzable by phytase and alkaline phosphatase. This supports the claim by Hayes et al. (2000) that the common supposition that considers NaHCO3extracted organic P to be labile may not be true.
Unlike the H2O fractions, wheat phytase in NaOH fractions did not release more organic P than did alkaline phosphatase. Both enzymes were unable to release 44% of the total P in pig manure, and 49% of the total P in cattle manure. This observation suggests that phytate is not a major component of the NaOH fractions.
It is difficult to compare the results found in this study with the few data reported in other animal manure organic P investigations due to the different experimental approaches. The most similar investigation is the report by Leinweber et al. (1997). The investigators sequentially fractionated the P in liquid pig manure and chicken (Gallus gallus) manure to resin P (1129%), NaHCO3P (1013%), NaOH-P (310%), H2SO4P (1727%), and residual P (3941%). Leinweber et al. (1997) considered at least a portion of residual P to represent insoluble mineral phases.
In contrast, concentrations of HCl-P (47%) and residual P (less than 1%) were very low in our study. In soils, HCl- or H2SO4P was designated apatite P (Ca-associated), and residual P was considered occluded P (Hedley et al., 1982; Tiessen et al., 1983). There are two possible causes for the low P portion of the two fractions in our study. First, theoretically, most P in animal manure should be present as the products or residues of the biological processes of the animal itself or of microbes in its intestinal system. In other words, mineral apatite P or occluded P should not be major components of animal manure. Second, we discarded the manure materials too large to pass through a 0.991-mm sieve. This practice might have reduced the residual P content because these large feedstuff and litter materials may be expected to contain indigestible P that can only be released through H2O2acid treatment. Recently, Sharpley and Moyer (2000) reported that HCl-P varies from 1 to 33% in six types of animal manure, and residual P was less than 3% in five of six manures. Therefore, it is not uncommon that P forms present in animal manure vary widely depending on factors such as animal species, diet composition, and manure management. It may be speculated that optimal manure management may vary to the same extent as does manure P composition.
Further Exploration of the Unknown Phosphorus Forms
It was already shown in Fig. 2 that both alkaline phosphatase and wheat phytase were not active on NAD that contains nucleotide pyrophosphate bonds, nor on RNA and DNA that contain phosphodiester bonds. Two enzymes, a nucleotide pyrophosphatase that hydrolyzes NAD to nicotinamide mononucleotide (NMN) and adenosine monophosphate (AMP), and a nuclease P1 that cleaves RNA and DNA to produce 5'-phosphomonoesters, were used to test the presence of such P forms in both animal manures. As shown in Table 2, both enzymes acted on their own substrate only. Wheat phytase then released orthophosphate from their cleaved products. These results indicate that the two enzymes can be used to release the relevant P form when present in manure.
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Designation of Organic Phosphorus Forms in Manure Fractions
Although release of organic phosphorus in soil solutions has been investigated previously (Hayes et al., 2000; Pant et al., 1994; Shand and Smith, 1997), identification of specific phosphorus types in those soil solutions was not the purpose of these investigations. These investigators referred to phosphorus released by phytase, acid phosphatase, and alkaline phosphatase, generally as enzyme-labile (hydrolysable) P. We believe that it is reasonable to designate more specific P forms released by these enzymes based on the substrate specificity of the phosphate-releasing enzymes (Fig. 2 and Table 2). The difference in P in the presence and absence of alkaline phosphatase represents the content of simple or general phosphomonoesters (Table 3). The difference in P between phytase and alkaline phosphatase reflects the amount of phytate in a sample. The difference in P for manure incubated with phytase in the presence and absence of nuclease P1 was contributed by nucleotide-like phosphodiesters. The action of nucleotide pyrophosphatase revealed the content of organic pyrophosphate. Some negative figures in Table 3 were due to the result of the proteinmolybdate blue precipitation during P+w assay. We designated the percentage of the corresponding phosphorus form as zero.
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| CONCLUSIONS |
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| ACKNOWLEDGMENTS |
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| NOTES |
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| REFERENCES |
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