Abstract
Phosphorus (P) is one of the most important nutrients for all life forms irrespective of physiological uptake mechanism or metabolic pathway. Soils and sediments contain a variety of organic P compounds that may undergo active transformation into inorganic P and vice versa. Phosphate oxygen isotope ratios have increasingly been applied to better understand the physico-chemical and biological pathways of P cycling and its fate in agricultural and nonagricultural soils. For example, the fractionation factors during hydrolysis of structurally-similar organic P compounds studied thus far are often distinct. Therefore compound-specific isotopic composition could be a powerful tool for differentiating transformation of different P compounds, tracking their origin and fate, and ultimately to develop an integrated and quantitative understanding of P cycling in both extant and fossil ecosystems. This chapter reviews biochemical reaction mechanisms and the current state of knowledge on compound-specific isotopic effects during hydrolysis of organic P compounds. While this research is still in its infancy, a new paradigm has emerged and it is hoped that the future expansion of this research will allow development of a holistic approach to integrate transformation of organic and inorganic P over time and space in different ecosystems.
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Authors would like to thank editors for the invitation to contribute this chapter. This work was supported by research grants from the US Department of Agriculture (NIFA awards 2012-67019-19320 and 2013-67019-21373) and ACS-PRF (53469-DNI2) to DPJ, and National Science Foundation (OCE 0928247) to REB.
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Jaisi, D.P., Blake, R.E., Liang, Y., Chang, S.J. (2014). Investigation of Compound-Specific Organic-Inorganic Phosphorus Transformation Using Stable Isotope Ratios in Phosphate. In: He, Z., Zhang, H. (eds) Applied Manure and Nutrient Chemistry for Sustainable Agriculture and Environment. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-8807-6_13
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