Phosphorus fractions and oxygen isotope composition of inorganic phosphate in typical agricultural soils

Chemosphere ◽  
2020 ◽  
Vol 239 ◽  
pp. 124622
Author(s):  
Liyan Tian ◽  
Qingjun Guo ◽  
Guirui Yu ◽  
Yongguan Zhu ◽  
Yunchao Lang ◽  
...  
2015 ◽  
Vol 12 (6) ◽  
pp. 5055-5077
Author(s):  
C. v. Sperber ◽  
F. Tamburini ◽  
B. Brunner ◽  
S. M. Bernasconi ◽  
E. Frossard

Abstract. Phosphorus (P) is an essential nutrient for living organisms. Under P-limiting conditions plants and microorganisms can exude extracellular phosphatases that release inorganic phosphate (Pi) from organic phosphorus compounds (Porg). Phytic acid (IP6) is an important form of Porg in many soils. The enzymatic hydrolysis of IP6 by phytase yields plant available inorganic phosphate (Pi) and less phosphorylated inositol derivates as products. The hydrolysis of organic P-compounds by phosphatases leaves an isotopic imprint on the oxygen isotope composition (δ18O) of released Pi, which might be used to trace P in the environment. This study aims at determining the effect of phytase on the oxygen isotope composition of released Pi. For this purpose, enzymatic assays with histidine acid phytases from wheat and Aspergillus niger were prepared using IP6, adenosine 5'monophosphate (AMP) and glycerophosphate (GPO4) as substrates. For a comparison to the δ18O of Pi released by other extracellular enzymes, enzymatic assays with acid phosphatases from potato and wheat germ with IP6 as substrate were prepared. During the hydrolysis of IP6 by phytase, four Pi are released, and one oxygen atom from water is incorporated into each Pi. This incorporation of oxygen from water into Pi is subject to an apparent inverse isotopic fractionation (ϵ ∼ 6 to 10‰), which is similar to that imparted by acid phosphatase from potato during the hydrolysis of IP6 (ϵ ∼ 7‰) where less than three Pi are released. The incorporation of oxygen from water into Pi during the hydrolysis of AMP and GPO4 by phytase yielded a normal isotopic fractionation (ϵ ∼ −12‰), again similar to values reported for acid phosphatases from potato and wheat germ. We attribute this similarity in ε to the same amino acid sequence motif (RHGXRXP) at the active site of these enzymes, which leads to similar reaction mechanisms. We suggest that the striking substrate-dependency of the isotopic fractionation could be attributed to a difference in the δ18O-values of the C-O-P bridging and non-bridging oxygen atoms in organic phosphate compounds.


2019 ◽  
Author(s):  
Catharina Simone Nisbeth ◽  
Federica Tamburini ◽  
Jacob Kidmose ◽  
Søren Jessen ◽  
David William O'Connell

Abstract. The ability to identify the origin of phosphorus is essential to effectively mitigate eutrophication of freshwater ecosystems. The oxygen isotope composition of orthophosphate (δ18Op) has been suggested to have a significant prospective as a tracer for P entering freshwater ecosystems. The δ18Op tracing method is, however, still in its preliminary stages and has proven challenging to implement for new practitioners. In order to achieve progress in developing the application of δ18Op signatures as a tracing tool, there is a need to eliminate the methodological challenges involved in accurately determining δ18Op. This technical note describes the various steps needed to concentrate and isolate orthophosphate in freshwater samples into an adequately pure analyte (Ag3PO4), without isotopic alteration during processing. The protocol compiles the disperse experiences from previous studies, combined with our own experience.


Geology ◽  
1993 ◽  
Vol 21 (3) ◽  
pp. 281 ◽  
Author(s):  
Gerald M. Friedman ◽  
R. P. Major ◽  
R. Michael Lloyd ◽  
F. Jerry Lucia

2007 ◽  
Vol 41 (6) ◽  
pp. 1870-1876 ◽  
Author(s):  
Jorge E. Spangenberg ◽  
Bernhard Dold ◽  
Marie-Louise Vogt ◽  
Hans-Rudolf Pfeifer

2011 ◽  
Vol 438 (1) ◽  
pp. 697-700
Author(s):  
N. S. Bortnikov ◽  
V. M. Novikov ◽  
E. O. Dubinina ◽  
A. D. Savko ◽  
A. G. Berketa ◽  
...  

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