2001
DOI: 10.1081/css-120000280
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Comparison of soluble P in soil water extracts determined by ion chromatography, colorimetric, and inductively coupled plasma techniques in PPB range

Abstract: The determination of soil solution phosphate ions at trace levels is questionable with colorimetric method due to both limit of sensitivity and possible hydrolysis of organic soluble phosphate (P). A simple procedure was developed to determine orthophosphate at trace levels in soil solutions by single-column, suppressed-ion chromatography with conductivity detection without prior sample concentration. The procedure requires column capacity selection and use of a 500-mL injection loop. The method shows a detect… Show more

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Cited by 25 publications
(16 citation statements)
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“…Several researchers have documented differences between P measured colorimetrically and P measured by ICP (Khiari et al 2000;Masson et al 2001;Nathan et al 2002). Generally ICP P values are greater due to the presence of organic P (Nathan et al 2002) or other complexed forms of P in soil extracts.…”
Section: Tablementioning
confidence: 97%
“…Several researchers have documented differences between P measured colorimetrically and P measured by ICP (Khiari et al 2000;Masson et al 2001;Nathan et al 2002). Generally ICP P values are greater due to the presence of organic P (Nathan et al 2002) or other complexed forms of P in soil extracts.…”
Section: Tablementioning
confidence: 97%
“…Once a redox couple on the superficial surface is achieved, a constant and reproducible time-independent potential signal is provided. Moreover, this reference electrode has inherent advantages such as low cost, easy handling, and great in-soil stability (Masson et al 2001).…”
Section: Soil Phosphorus Probementioning
confidence: 99%
“…[21][22][23][24][25] During the 5-30 min contact period with the Mehlich 1 solution each of these P sources begins to approach an equilibrium state in the soil solution. [21][22][23][24][25] During the 5-30 min contact period with the Mehlich 1 solution each of these P sources begins to approach an equilibrium state in the soil solution.…”
Section: Reprintsmentioning
confidence: 99%