1983
DOI: 10.1002/j.1537-2197.1983.tb12474.x
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Use of the DCB Technique for Extraction of Hydrous Iron Oxides From Roots of Wetland Plants

Abstract: Replicate samples of Phragmites communis roots coated with hydrous iron oxide were analyzed for internal and external Fe using the dithionite‐citrate‐bicarbonate technique (hot DCB), a modified DCB technique (cold DCB), Ethylenediamine tetraacetic acid (EDTA), Diethylenetriamine pentaacetic acid (DTPA), and a total Fe analysis. EDTA and DTPA were found to be inefficient in extracting FeOOH while both DCB techniques were efficient. Concentrations of Fe extracted (8.93% and 9.37% by weight) and percent of total … Show more

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Cited by 233 publications
(72 citation statements)
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“…Roots were rinsed three times with deionized water that was added to the DCB extract. The resulting solution was made up to 50 ml with deionized water (Taylor and Crowder 1983). After DCB extraction, roots were oven dried at 70°C for 3 days and weighed.…”
Section: Dcb Extraction Of Iron Plaquementioning
confidence: 99%
“…Roots were rinsed three times with deionized water that was added to the DCB extract. The resulting solution was made up to 50 ml with deionized water (Taylor and Crowder 1983). After DCB extraction, roots were oven dried at 70°C for 3 days and weighed.…”
Section: Dcb Extraction Of Iron Plaquementioning
confidence: 99%
“…At harvest, rice roots with iron plaque were washed three time with deionized water, and then iron plaque was removed from the surface of the rice roots with 80 ml cold dithionite-citrate-bicarbonate (DCB) (0.03 M sodium citrate and 0.125 M sodium bicarbonate with 0.06 M sodium dithionite) for 60 min at room temperature (20-25°C) (Taylor and Crowder 1983). Roots were rinsed three times with deionized water, and the wash water was added to the DCB-extracts.…”
Section: Measurement Of Dcb Extraction Of Iron Plaque From Rootsmentioning
confidence: 99%
“…Under anaerobic conditions oxygen loss from rice roots induces iron and manganese deposits on the surface of the roots (Armstrong 1967). Iron plaque is commonly formed on the surfaces of roots of wetland plants, including Oryza sativa, Typha latifolia and Phragmites communis, and is mainly caused by the oxidation of ferrous iron and the precipitation of iron oxide on the root surface and rhizosphere (Armstrong 1964;Armstrong 1967;Chen et al 1980;Taylor and Crowder 1983;Taylor et al 1984).…”
Section: Introductionmentioning
confidence: 99%
“…Then the Fe and Mn plaques deposited on the root surface were extracted using the dithionite-citrate-carbonate (DCB) method of Taylor and Crowder (1983b) and McLaughlin et al (1985). The fresh roots were incubated for 3 h at 25°C in 45 mL of a solution (pH 6.5) containing 0.27 M sodium citrate (Na 3 C 6 H 5 O 7 Á2H 2 O) and 0.11 M sodium bicarbonate (NaHCO 3 ), with the addition of 3.0-g sodium dithionite (Na 2 S 2 O 4 ).…”
Section: Cs Treatmentsmentioning
confidence: 99%