2016
DOI: 10.2136/sssaj2015.09.0340
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Soil Phosphorus Forms from Organic and Conventional Forage Fields

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Cited by 91 publications
(83 citation statements)
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“…The NMR delay times were determined based on the ratio of concentrations of P/(Fe + Mn) within the extracts, for example, higher concentrations of paramagnetic ions (e.g. Corrections were made to account for orthophosphate diester degradation by summing the peak areas associated with degradation products (α-and β-glycerophosphate and mononucleotides, degraded from phospholipids and RNA respectively), subtracting this sum from the total monester area, and adding it to the total diester area (Young et al, 2013;Schneider et al, 2016). A temperature of 21 C and a 45 pulse were used, with a pulse delay of 4.5 s. Acquisition time was 0.5 s and 2800-5830 scans (~4-8 h) were collected.…”
Section: Solution 31 P-nmrmentioning
confidence: 99%
“…The NMR delay times were determined based on the ratio of concentrations of P/(Fe + Mn) within the extracts, for example, higher concentrations of paramagnetic ions (e.g. Corrections were made to account for orthophosphate diester degradation by summing the peak areas associated with degradation products (α-and β-glycerophosphate and mononucleotides, degraded from phospholipids and RNA respectively), subtracting this sum from the total monester area, and adding it to the total diester area (Young et al, 2013;Schneider et al, 2016). A temperature of 21 C and a 45 pulse were used, with a pulse delay of 4.5 s. Acquisition time was 0.5 s and 2800-5830 scans (~4-8 h) were collected.…”
Section: Solution 31 P-nmrmentioning
confidence: 99%
“…And researchers indicated that the mineralization and degradation of organic matter can cause OP release from soil and sediment. But the mobilization of OP may take longer than Fe-P and result in a lower quantity of P exchange in the short-term, and also the procession was affected by many factors, such as DO and pH (McGill and Cole, 1981;Suzumura and Kamatani, 1995;Rydin 2000;Kraal et al, 2013;Schneider et al, 2016).…”
Section: Sediment P Pollution and P Fraction In Different Riversmentioning
confidence: 99%
“…It is generally now agreed that α-and β-glycerophosphates are degradation products from phospholipids, while most mononucleotides (e.g. adenosine monophosphate) originate from RNA [29,[34][35][36][37]. There has long been an interest in quantifying total orthophosphate monoesters and total orthophosphate diesters in soil; diesters are thought to be more labile, while many monoesters are more recalcitrant due to strong sorption to mineral surfaces [4].…”
Section: P-nmr Spectroscopymentioning
confidence: 99%
“…In addition, activities of the soil enzymes acid monoesterase, alkaline monoesterase and diesterase are commonly measured [4], and linked back to total orthophosphate monoester and diester concentrations in models [e.g., 38]. However, if corrections are not made for degradation products, the M:D and models are of questionable value for predicting mineralization of organic P forms [37].…”
Section: P-nmr Spectroscopymentioning
confidence: 99%
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