{'fraction_non_alphanumeric': 0.03484513274336283, 'fraction_numerical': 0.02157079646017699, 'mean_word_length': 5.259515570934256, 'pattern_counts': {'":': 0, '<': 0, '<?xml version=': 0, '>': 0, 'https://': 0, 'lorem ipsum': 0, 'www.': 0, 'xml': 0}, 'pii_count': 0, 'substrings_counts': 0, 'word_list_counts': {'cursed_substrings.json': 0, 'profanity_word_list.json': 0, 'sexual_word_list.json': 0, 'zh_pornsignals.json': 0}}
Characterisation of organic phosphorus in overland flow from grassland plots using 31P nuclear magnetic resonance spectroscopy

Grazing animals are known to change the characteristics of agricultural grasslands as a source of and pathway for phosphorus (P) loss to water. Previous work, using physico‐chemical analysis of the overland flow revealed that the presence of grazing animals increased the overall quantity of P being lost, in particular the unreactive and particulate P fractions. The aim of this study was to characterise the organic P (Po) fraction in overland flow from grazed and non‐grazed grassland small plots using phosphorus‐31 nuclear magnetic resonance (31P NMR) spectroscopy to give greater insight into P loss to water under simulated rainfall. The effect of the grazing animal was most pronounced in the dissolved unreactive P (DUP) and particulate unreactive P (PUP) fractions measured in overland flow from the grazed plots, over four times higher than from the non‐grazed plots. Five distinct classes of P compounds were detected in the 31P NMR spectra, inorganic orthophosphate (δ = 6.83 ppm), orthophosphate monoesters (δ = 4.95–5.69 ppm), orthophosphate diesters (δ = 1.89 ppm), phosphonates (δ = 19.38 ppm), and pyrophosphates (δ = −3.26 ppm). Distinct signals at 5.69, 5.37, 5.10, and 4.95 ppm in the overland flow extracts from the plots indicated significant concentrations of myo‐inositol hexakisphosphate in the orthophosphate monoester region. Orthophosphate diesters (assigned to phospholipids) and phosphonates were also only detected in overland flow collected from the grazed plot. These results indicate that normal grazing management practices may not only affect the concentrations of Po but also the forms of Po being transferred from grassland systems to water.