Phosphorus stocks and speciation in soil profiles of a long-term fertilizer experiment: Evidence from sequential fractionation, P K-edge XANES, and 31P NMR spectroscopy

被引:95
|
作者
Koch, Maximilian [1 ]
Kruse, Jens [2 ]
Eichler-Loebermann, Bettina [3 ]
Zimmer, Dana [4 ]
Willbold, Sabine [5 ]
Leinweber, Peter [4 ]
Siebers, Nina [1 ]
机构
[1] Forschungszentrum Julich, Agrosphere, Inst Bio & Geosci IBG 3, D-52425 Julich, Germany
[2] Univ Bonn, Inst Crop Sci & Resource Conservat INRES Soil Sci, Nussallee 11, D-53115 Bonn, Germany
[3] Univ Rostock, Agron & Crop Sci, Justus von Liebig Weg 6, D-18051 Rostock, Germany
[4] Univ Rostock, Soil Sci, Justus von Liebig Weg 6, D-18051 Rostock, Germany
[5] Forschungszentrum Julich, Cent Inst Engn Elect & Analyt, Analyt ZEA 3, D-52425 Julich, Germany
基金
加拿大健康研究院; 加拿大自然科学与工程研究理事会; 加拿大创新基金会;
关键词
Triple superphosphate TSP; Organic fertilizer; Topsoil; Subsoil; NEXAFS; NUCLEAR-MAGNETIC-RESONANCE; ORGANIC PHOSPHORUS; INORGANIC P; MYOINOSITOL HEXAKISPHOSPHATE; LEACHING LOSSES; SORPTION; PHOSPHATE; FORMS; EXTRACTION; AMENDMENTS;
D O I
10.1016/j.geoderma.2017.12.003
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Agricultural productivity depends on the use of phosphorus (P) of which not only the topsoil, but also the subsoil, can hold immense stocks. To assess their importance for plant nutrition, we compared the P status of Stagnic Cambisol profiles in experimental plots that received different P fertilizer applications for 16 years. Sequential fractionation was combined with P K-edge X-ray absorption near edge structure (XANES) spectroscopy and liquid P-31 nuclear magnetic resonance (NMR) spectroscopy to identify the chemical P speciation. Fertilized topsoils showed P stocks larger by a factor of 1.2 to 1.4, and subsoil stocks larger by a factor of 1.3 to 1.5 than the control. P-XANES revealed the predominance of mainly inorganic P species, such as moderately labile Fe- (46 to 92%), Al- (0 to 40%) and Ca- (0 to 21%) P compounds besides organic P (0 to 12%). This was supported by 31P NMR with decreasing proportions of orthophosphate monoesters from topsoil (20 to 28%) towards the second subsoil layer (7 to 13%). In summary, fertilizer application maintained or increased P stocks but only slightly altered the P speciation throughout the profiles. The kind of fertilizers had no significant effect on soil P, only affecting the inorganic P pools. Our findings proved that subsoil P stocks are potentially important contributors to plant nutrition, but their accessibility must be assessed for improved soil P tests and reduced fertilizer recommendations.
引用
收藏
页码:115 / 126
页数:12
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