Application of 31P and 27Al MAS NMR for phosphate speciation studies in soil and aluminium hydroxides:: promises and constraints

被引:83
作者
Lookman, R
Grobet, P
Merckx, R
Van Riemsdijk, WH
机构
[1] Lab Soil Fertil & Soil Biol, B-3001 Heverlee, Belgium
[2] Ctr Surface Chem & Catalysis, B-3001 Heverlee, Belgium
[3] Wageningen Univ Agr, NL-6700 EC Wageningen, Netherlands
关键词
MAS NMR; phosphate; speciation; aluminium hydroxides; soil;
D O I
10.1016/S0016-7061(97)00061-X
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Magic angle spinning (MAS) nuclear magnetic resonance (NMR) was used to investigate the chemical environment of P in soil and soil components. P-31 and Al-27 MAS NMR spectra are presented of synthetic aluminium hydroxides (amorphous aluminium hydroxide and gibbsite), reacted with P under different conditions of P concentration, temperature and pH. The reaction product is amorphous octahedral aluminium phosphate, which transforms (partly reversibly) to tetrahedral aluminium phosphate upon drying. Results of several experiments on excessively fertilized sandy soil material are discussed. The soil particle fraction smaller than 50 mu m was used for NMR analysis. P-31 and Al-27 MAS NMR spectra show a Ca-P pool and an Al-P pool. A six-fold water extraction removes part of both P pools. Oxalate extraction removes all Ca-P and Al-P from the sample. Removal of the labile P pool by the HFO-DMT long-term P desorption technique, does not drastically change the P-31 MAS NMR spectrum. The formerly mentioned Ca-P and AI-P are thus stable P pools. The H-1-P-31 cross-polarization (CP) spectrum of the original soil sample revealed a third chemical environment, which was identified as labile Ca-P: this P pool does not appear in the H-1-P-31 CP spectrum of the soil sample from which the fast P pool had been removed. The combination of MAS and CP MAS NMR can thus reveal at least three different P species in soil, of which two pools were identified as stable, and one as labile. (C) 1997 Elsevier Science B.V.
引用
收藏
页码:369 / 388
页数:20
相关论文
共 45 条
[1]   ALUMINIUM + IRON PHOSPHATE STUDIES RELATING TO SOILS .2. REACTIONS BETWEEN PHOSPHATE + HYDROUS OXIDES [J].
BACHE, BW .
JOURNAL OF SOIL SCIENCE, 1964, 15 (01) :110-&
[2]  
BARROW NJ, 1985, ADV AGRON, V40, P183
[3]  
Bleam W. F., 1991, ADV AGRON, V46, P119
[4]   P-31 AND AL-27 SOLID-STATE NUCLEAR MAGNETIC-RESONANCE STUDY OF TARANAKITE [J].
BLEAM, WF ;
PFEFFER, PE ;
FRYE, JS .
PHYSICS AND CHEMISTRY OF MINERALS, 1989, 16 (08) :809-816
[5]   A P-31 SOLID-STATE NUCLEAR-MAGNETIC-RESONANCE STUDY OF PHOSPHATE ADSORPTION AT THE BOEHMITE AQUEOUS-SOLUTION INTERFACE [J].
BLEAM, WF ;
PFEFFER, PE ;
GOLDBERG, S ;
TAYLOR, RW ;
DUDLEY, R .
LANGMUIR, 1991, 7 (08) :1702-1712
[6]  
BLEAM WF, 1989, PHYS CHEM MINER, V16, P455, DOI 10.1007/BF00197015
[7]   DESCRIBING THE EFFECT OF TIME ON SORPTION OF PHOSPHATE BY IRON AND ALUMINUM HYDROXIDES [J].
BOLAN, NS ;
BARROW, NJ ;
POSNER, AM .
JOURNAL OF SOIL SCIENCE, 1985, 36 (02) :187-197
[8]   MODELING THE EFFECT OF ADSORPTION OF PHOSPHATE AND OTHER ANIONS ON THE SURFACE-CHARGE OF VARIABLE CHARGE OXIDES [J].
BOLAN, NS ;
BARROW, NJ .
JOURNAL OF SOIL SCIENCE, 1984, 35 (02) :273-281
[9]  
Dzomback D.A., 1990, Surface Complexation Modelling: Hydrous Ferric Oxide
[10]  
ENGELHARDT TG, 1987, HIGH RESOLUTION SOLI