Results 211 to 220 of about 6,443 (255)
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Isotopic Exchange Reactions between Phosphorus Trichloride and Phosphorus Pentachloride1

Journal of the American Chemical Society, 1957
A measurable exchange of isotoplcally labeled phosphorus and chlorine has been observed between phosphorus trichloride and phosphorus pentachloride in carbon tetrachloride solution. The exchange rates are the same within experimental error and the reaction is first order in phosphorus pentachloride and zero order in phosphorus trichloride.
Warren E. Becker, Rowland E. Johnson
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Phosphorus in caves : Oxygen isotopes in phosphate as a novel speleothem palaeothermometer [PDF]

open access: possible, 2022
Speleothems are key archives for palaeoclimatological study, yet current methods for palaeotemperature records are often affected by processes independent to temperature. Phosphorus is a ubiquitous component of speleothem calcite in caves, yet its efficacy as a palaeothermometer has not yet been fully explored.
Morgan, Alistair   +3 more
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Phosphorus in Urban Sewage Sludges as Assessed by Isotopic Exchange

Soil Science Society of America Journal, 1996
Abstract Sewage sludges have been used for years as fertilizers but little information exists on the availability of P in these complex materials. Isotopically exchangeable P was measured in 12 urban sewage sludges using the isotopic exchange kinetics method.
Frossard, E., Sinaj, S., Dufour, P.
openaire   +2 more sources

Identification of phosphorus sources in the East Creek using isotope signatures of the residual phosphorus pool

2021
Phosphorus (P) is often the limiting nutrient contributing to phytoplankton blooms and deteriorating water quality. It is imperative to identify key sources of P in watersheds, especially in areas where P has accumulated in the soil and created a potential source of long-term releases into water bodies. The existing limitation of analytical methods for
openaire   +2 more sources

Effects of Soil Properties on Plant‐Available Phosphorus Determined by the Isotopic Dilution Phosphorus‐32 Method

Soil Science Society of America Journal, 1988
Abstract A procedure using 32 P isotopic exchange kinetics was suggested to characterize the availability of soil P. The ratio of the radioactivity remaining in the solution over the total radioactivity ( r 1 /
T. Sen Tran, M. Giroux, J. C. Fardeau
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Phosphorus Transformations and Availability under Cropping and Fertilization Assessed by Isotopic Exchange

Soil Science Society of America Journal, 1994
Abstract In fertilized agricultural soils, both fertilizer and soil P are partly depleted by crop export, while residual fertilizer P reacts with the soil. As a result, P availability changes in complex ways that cannot be described by an available P pool.
Morel, Christian   +3 more
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Process‐Based Assessment of Phosphorus Availability in a Low Phosphorus Sorbing Forest Soil using Isotopic Dilution Methods

Soil Science Society of America Journal, 2009
Our objective was to evaluate the relative contribution of physicochemical (diffusion) and biological (mineralization) processes to the supply of ionic P (iP) in solution and potential P availability to plants in a low P sorbing forest soil.
Achat, David   +2 more
openaire   +3 more sources

Synthesis of nucleoside 5'-triphosphates labelled with radioactive phosphorus isotopes

Russian Chemical Reviews, 1995
The review presents an analysis of the chemical chemicoenzymic, and enzymic methods of synthesis of nucleoside 5'-triphosphates labelled with phosphorus isotopes ( 32P and 33P) in the α- and γ-positions. The major part of the review is devoted to enzymic methods of synthesis, because they have undoubted advantages. The enzymatic reactions are described
Yurii S Skoblov   +2 more
openaire   +1 more source

Evaluation of Phosphorus Enrichment in Groundwater by Legacy Phosphorus in Orchard Soils with High Phosphorus Adsorption Capacity Using Phosphate Oxygen Isotope Analysis

Environmental Science & Technology
Long-term phosphorus (P) fertilization results in P accumulation in agricultural soil and increases the risk of P leaching into water bodies. However, evaluating P leaching into groundwater is challenging, especially in clay soil with a high P sorption capacity.
Takuya Ishida   +7 more
openaire   +2 more sources

Reactivity of Phosphorus in Northeastern Brazilian Soils Assessed by Isotopic Dilution

Soil Science Society of America Journal, 1991
Abstract To diagnose fertilizer requirements in regions of high soil variability where P‐fixing capacities can vary 100‐fold, single‐extraction P tests must be complemented by an evaluation of P sorption. The isotopic‐dilution kinetics of 32 P was tested for its potential to
I. H. Salcedo   +2 more
openaire   +1 more source

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