Abstract

Phosphorus (P) limits plant growth especially where agriculture is performed on older soils. Predictions indicate that rock-P mining peaks within 35 years with severe impacts on global food production1. Several studies have been made to completely understand fate and cycle of P in soils but knowledge in this field remains limited. Therefore we aim in our physicochemical/ecological research to elucidate overall speciation and sorption mechanisms of organic P in environmental matrices ranging from boreal to African soils and even water systems. Our aim is to develop solution and solid state 31P-NMR techniques to identify P-species in soils and water; information ideal for correlating different organic P-species to plant and soil processes2. NMR studies on soil P have consequently suffered from serious line broadening caused by paramagnetic ions. We developed a new approach to avoid paramagnetic line broadening by physically removing them. using sulfide precipitation which reduces and removes Fe and Mn ions without affecting P-composition, we could see a dramatic reduction in NMR line widths from over 100 Hz down to 2 Hz on soil extracts. This resolution allowed application of 2D 1H, 31P-NMR to resolve the crowded spectral region where abundant monoester P appears.3 By exploiting 2D 1H-31P correlations in the NMR spectra of soil extracts we were able to identify unambiguously individual organic P species by combining 31P and 1H chemical shifts and coupling constants, an approach even suitable for a structural characterization of unknown P-components3, 4. Applications on boreal4 and tropical soil are underway, where tropical soils from Burkina Faso can be studied in greater detail using the new protocols. Studies using passive sampling with ion-exchange resin analyzed with solid state 31P-MAS NMR have the potential to analyze organic P-species in aquatic systems.

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