An investigation of the distribution of phosphorus between free and mineral associated soil organic matter, using density fractionation
| Autor: | Edward Tipping, John Quinton, Jessica Adams, S.A. Thacker |
|---|---|
| Jazyk: | angličtina |
| Rok vydání: | 2018 |
| Předmět: |
010504 meteorology & atmospheric sciences
Soil Science chemistry.chemical_element Plant Science Fractionation 01 natural sciences Pasture Ecology and Environment chemistry.chemical_compound 0105 earth and related environmental sciences Total organic carbon geography geography.geographical_feature_category Chemistry Soil organic matter Phosphorus fungi food and beverages 04 agricultural and veterinary sciences Environmental chemistry Soil water 040103 agronomy & agriculture Earth Sciences 0401 agriculture forestry and fisheries Sodium polytungstate Specific gravity |
| DOI: | 10.1007/s11104-017-3478-4 |
| Popis: | Aims: We investigated whether density fractionation can be used to determine the distribution of organic phosphorus (OP) between free and mineral-associated soil organic matter (SOM). Methods: We performed density fractionations using sodium polytungstate solution (specific gravity 1.6 g cm−3) on 20 soils from UK semi-natural and pasture ecosystems, to obtain a light fraction (LF) and a heavy fraction (HF) for each soil. The fractions were quantified by weight, and analysed for organic carbon (OC), total N (TN), total P (TP), inorganic P (IP), and OP (by difference). Results: Good recoveries of soil mass (96%), OC and TN (both ~ 90%) were obtained, but recovery of OP only averaged 56%. The average P:C ratio of HF SOM exceeded that of LF SOM by a factor of six, greater than the factor of two obtained for TN:OC. For the soils studied, the elements of SOM were predominantly in the HF, with averages of 75% for C, 82% for N, and 90% for P. Conclusions: The incomplete recovery of OP demands further work. Nonetheless, the results show that HF SOM is much richer in P than LF SOM. |
| Databáze: | OpenAIRE |
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