1998
DOI: 10.1080/01904169809365448
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Elemental bioavailability in nutrient solutions in relation to complexation reactions

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1998
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Cited by 13 publications
(6 citation statements)
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“…It is surprising that the recommended potassium and phosphorus concentrations in the root environment are not between the supply and mean calculated drainage water concentrations. For these elements, it is not possible to explain this by dissociation, complexation or precipitation reactions in the nutrient solution [14].…”
Section: Characteristicmentioning
confidence: 99%
“…It is surprising that the recommended potassium and phosphorus concentrations in the root environment are not between the supply and mean calculated drainage water concentrations. For these elements, it is not possible to explain this by dissociation, complexation or precipitation reactions in the nutrient solution [14].…”
Section: Characteristicmentioning
confidence: 99%
“…At a pH above 8.3, Ca 2+ and Mg 2+ ions easily precipitate as carbonates by reacting with CO 3 2À . Also sulphate forms relatively strong complexes with Ca 2+ and Mg 2+ (De Rijck and Schrevens 1998). As pH increases from 2 to 9, the amount of SO 4 2À forming soluble complexes with Mg 2+ as MgSO 4 and with K + as KSO 4…”
Section: Nutrient Solution Propertiesmentioning
confidence: 99%
“…Also, as mentioned above, when the pH of the nutrient solution increases, the HPO 4 2-ion predominates, which precipitates with Ca 2+ when the product of the concentration of these ions is greater than 2.2, expressed in mol m -3 (Steiner, 1984). Sulphate also forms relatively strong complexes with Ca 2+ and Mg 2+ (De Rijck & Schrevens, 1998b). As pH increases from 2 to 9, the amount of SO 4 2-, forming soluble complexes with Mg 2+ as MgSO 4 and with K + as KSO 4 -increases (De Rijck & Schrevens, 1999).…”
Section: Nutrient Solutionmentioning
confidence: 97%