A NEW APPROACH TO THE DETERMINATION OF PHOSPHATE ROCK DISSOLUTION IN ORGANIC SOILS USING GRAPHITE-FURNACE ATOMIC-ABSORPTION SPECTROPHOTOMETRY

Citation
Mm. Hanafi et al., A NEW APPROACH TO THE DETERMINATION OF PHOSPHATE ROCK DISSOLUTION IN ORGANIC SOILS USING GRAPHITE-FURNACE ATOMIC-ABSORPTION SPECTROPHOTOMETRY, Communications in soil science and plant analysis, 27(5-8), 1996, pp. 1479-1499
Citations number
21
Categorie Soggetti
Agriculture Soil Science","Plant Sciences","Chemistry Analytical
ISSN journal
00103624
Volume
27
Issue
5-8
Year of publication
1996
Pages
1479 - 1499
Database
ISI
SICI code
0010-3624(1996)27:5-8<1479:ANATTD>2.0.ZU;2-8
Abstract
The determination of phosphorus (P) in 0.5 M NaOH extracting solution following the dissolution of phosphate rock (PR) materials in mineral soils is frequently done using a molybdenum blue method. For organic s oils, 0.5 M NaOH soil extracts usually give dark color solutions. This dark color solution reduces the intensity of light in spectrophotomet er, thus, underestimating the dissolution of PR in organic soils compa red to mineral soils. A sew approach using a graphite furnace atomic a bsorption spectrophotometer (GFAAS) was evaluated for measuring P in p ure solutions; and this was used for measuring the dissolution of PR i norganic soils. The P standard solutions prepared in distilled water, 1% humic acid, 1% fulvic acid, 0.5 M NaOH, 0.5 M NaOH+1% humic acid, a nd 0.5 M NaOH+1% fulvic acid were used for establishing the standard c urve and the selection of matrix modifier. The organic soils at differ ent degree of decomposition (saprist, hemist, and fibrist) were incuba ted with gafsa phosphate rock (GPR), Christmas Island A-grade phosphat e rock (CIPR), and triple superphosphate (TSP) each at a rate of 0, 50 0, and 1000 mg P/kg soil. The dissolution of PR was measured using 0.5 M NaOH-extractable P and 0.5 M BaCl2/TEA-extractable Ca. The measurem ent of peak area gave the highest sensitivity reading (p = 0.01) compa red to peak height; and lanthanum nitrate was the most suitable matrix modifier for determination of P in distilled water, 1% humic acid, 1% fulvic acid, 0.5 M NaOH, 0.5 M NaOH+1% humic acid, and 0.5 M NaOH+1% fulvic acid. The dissolution of PR as measured by 0.5 M NaOH decreases in the following sequence: Sapric (B) > Hemic > Fibric > Sapric (D). Absolute amounts of P increased with increasing levels of P addition; and TSP gave the highest dissolution value followed by GPR, and CIPR. The dissolution of PR in organic soils using 0.5 M NaOH extracting sol ution can be accurately determined by GFAAS method.