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Soil phosphorus fractions after seven decades of fertilizer application in the Rengen Grassland Experiment
Author(s) -
Pätzold Stefan,
Hejcman Michal,
Barej Julia,
Schellberg Jürgen
Publication year - 2013
Publication title -
journal of plant nutrition and soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 1436-8730
DOI - 10.1002/jpln.201300152
Subject(s) - fertilizer , fractionation , chemistry , phosphorus , cambisol , lime , zoology , nutrient , grassland , composition (language) , environmental chemistry , agronomy , soil water , geology , soil science , biology , organic chemistry , paleontology , linguistics , philosophy
Declining global P reserves require a better understanding of P cycling in soil and related plant uptake. On managed grasslands, application of lime and fertilizer affects not only soil nutrient status, but also plant‐species composition of the sward. We examined the P fractionation in the Rengen Grassland Experiment (RGE) on a naturally acid Stagnic Cambisol in the Eifel Mts. (Germany) 69 y after the setup of the experiment. A modified sequential Hedley fractionation was carried out for samples from 30 plots at 0–10 cm depth. Application of inorganic phosphorus fertilizer had diverse effects on inorganic (P i ) and organic P (P o ) fractions. Resin‐P i , NaHCO 3 ‐P i , NaHCO 3 ‐P o , NaOH‐P i , HCl dil ‐P i , HCl conc ‐P i , and HCl conc ‐P o contents increased, while NaOH‐P o significantly decreased and residual‐P remained unaffected. Strongest enrichment occurred in the HCl dil ‐P i fraction, probably due to the chemical nature of the basic Thomas slag applied as P fertilizer. Without P fertilization, all fractions except residual‐P were more or less depleted. Strong P limitation of the vegetation in the limed treatments without P led to lowered contents also for NaOH‐P i and NaOH‐P o . However, NaOH‐P o was largest in the Control and even exceeded the respective content in the treatments with P. It remained unclear why species adapted to a low soil P status did not access this P fraction though being P‐limited. Published theory on the availability of Hedley P fractions does neither match P exploitation nor P nutritional status of the vegetation in the RGE. Regarding NaOH‐P o as stable and HCl dil ‐P i as moderately labile led to a more realistic evaluation of plant P uptake. Evaluation of P availability on the basis of chemical extractions alone is questionable for conditions like in the RGE. On long‐term grassland, plant‐species composition has to be taken into account to estimate access of plants to soil P.