Partitioning soil phosphorus into three discrete pools of differing availability

被引:66
作者
Guo, FM [1 ]
Yost, RS [1 ]
机构
[1] Univ Hawaii, Dept Agron & Soil Sci, Honolulu, HI 96822 USA
关键词
phosphorus; pools; fractionation; highly weathered soils;
D O I
10.1097/00010694-199810000-00006
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The Hedley phosphorus (P) fractionation procedure provides an alternative for characterizing soil P availability without qualifying the component P species. Interpretation of results involving all fractions is complicated and offers Little practical utility. The objective of this study was to group P fractions of similar availability into three functional pools according to the plant availability of the P fractions. These grouped pools may simplify practical use of fractionation data and provide insights into differences in availability and cycling of added P in diverse soils. Eight soils in the greenhouse were treated with four levels of P and planted with 14 consecutive crops. Soils were fractionated using a modified Hedley method. The seven fractions were then grouped into three discrete pools of decreasing availability: the readily available, the reversibly available, and the sparingly available. Phosphorus extracted by the iron-impregnated filter paper strips (Strip P) and inorganic P extracted by 0.5 M NaHCO3 (NaHCO3-P-i) were readily available in all soils. The reversibly available P fractions differed between the slightly weathered and the highly weathered soils. In the slightly weathered soils, the reversibly available P included the organic P (P-o) (NaHCO3- and NaOH-P-o), NaOH-P-i, HCl-P, and residual P, In the highly weathered soils, NaOH-P-i and organic P were considered reversibly available. No P fractions appeared to be sparingly available in the three slightly weathered soils. The residual P was the sparingly available P in the highly weathered soils. The results suggest quantitatively that P availability was greater when added to slightly weathered soils than when added to highly weathered soils.
引用
收藏
页码:822 / 833
页数:12
相关论文
共 39 条
[1]   PHOSPHORUS TRANSFORMATIONS IN A TOPOSEQUENCE OF LITHOSOLS AND CAMBISOLS FROM SEMIARID NORTHEASTERN BRAZIL [J].
AGBENIN, JO ;
TIESSEN, H .
GEODERMA, 1994, 62 (04) :345-362
[2]  
American Public Health Association, 1995, STAND METH EX WAT WA, P4
[3]  
Barrow N.J., 1980, Role Phosphorus Agric, P333, DOI DOI 10.2134/1980.ROLEOFPHOSPHORUS.C14
[4]   SOIL-PHOSPHORUS FRACTION DYNAMICS DURING 18 YEARS OF CULTIVATION ON A TYPIC PALEUDULT [J].
BECK, MA ;
SANCHEZ, PA .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1994, 58 (05) :1424-1431
[5]  
CHANG S. C., 1957, SOIL SCI, V84, P133, DOI 10.1097/00010694-195708000-00005
[6]   RESIDUAL AVAILABLE PHOSPHORUS IN NEAR-NEUTRAL AND ALKALINE SOILS .2. PERSISTENCE AND QUANTITATIVE ESTIMATION [J].
FIXEN, PE ;
LUDWICK, AE .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1982, 46 (02) :335-338
[7]  
FOX R L, 1970, Soil Science Society of America Proceedings, V34, P902
[8]   ON THE MECHANISM OF SPECIFIC PHOSPHATE - ADSORPTION BY HYDROXYLATED MINERAL SURFACES - A REVIEW [J].
GOLDBERG, S ;
SPOSITO, G .
COMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS, 1985, 16 (08) :801-821
[9]  
GUO F, 1998, IN PRESS SOIL SCI SO
[10]   Evaluating iron-impregnated paper strips for assessing available soil phosphorus [J].
Guo, FM ;
Yost, RS ;
Jones, RC .
COMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS, 1996, 27 (11-12) :2561-2590