Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-28T07:17:35.842Z Has data issue: false hasContentIssue false

Influence of pH, Concentration, and Chelating Power of Organic Anions on the Synthesis of Aluminum Hydroxides and Oxyhydroxides

Published online by Cambridge University Press:  01 July 2024

A. Violante
Affiliation:
Istituto di Chimica Agraria dell’ Università di Napoli, 80055, Portici, Italy
P. Violante
Affiliation:
Istituto di Chimica Agraria dell’ Università di Napoli, 80055, Portici, Italy
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Chelating organic acids hampered the hydrolytic reactions of Al and affected the nature of the crystalline aluminum hydroxides. Chemical composition, structure, size, nature of functional groups, and concentration of each organic anion, as well as the pH of the system, controlled the rate of Al(OH)3 crystallization. The order of effectiveness of the various acids was: glutaric < succinic = phthalic < glycine < malonic < glutamic < aspartic < oxalic < salicylic = malic < citric < tartaric. An increase in the stability of complexes formed between the organic ligands and Al decreased the rate of crystallization and changed the final aluminous products from bayerite to nordstrandite and/or gibbsite and then to pseudoboehmite and/or amorphous material. In the presence of anions with a great affinity for Al, particularly at pH equal to or less than 9.0, the reaction products were commonly poorly crystalline or structurally distorted. In the range of pH 8.0 to 10.0 moderately or strongly chelating anions acted to retard or prevent olation and facilitated the formation of stable pseudoboehmite or X-ray-amorphous products. The stronger the chelating power or the higher the concentration of organic anions, the easier was the formation of pseudoboehmite or amorphous material.

Резюме

Резюме

Хелатообразующие органические кислоты препятствовали гидролитическим реакциям А1 и влияли на природу кристаллических гидроокисей алюминия. Скорость кристаллизации контролировалась химическим составом, структурой, размером, природой функциональных групп и концентрацией каждого органического аниона, а также рН системы. Порядок эффективности различных кислот был следующий: глутаровоя < янтарная = фталевая < аминоуксусная < малоновая < глутаминовая < аминоянтарная < щавелевая < салициловая = оксиянтарная < лимонная < винная. Увеличение стабильности комплексов, формированных между органическими аддендами и А1, уменьшало скорость кристаллизации и изменяло конечные алюминиевые продукты от байерита до нордстрандита и/или гиббсита потом до псевдобемита и/или аморфного материала. В присутствии анионов, которые имеют большое химическое сродстве с А1, особенно для рН равного или меньшего чем 9,0, продукты реакции были обычно плохо выкристаллизированы или структурно искаженные. В диапазоне рН от 8,0 до 10,0 умеренно или сильно хелатообразующие анионы задерживали или предупреждали олацию и облегчали образование стабильного псевдобемита или рентгеновско-аморфных продуктов. Чем сильнее была хелатообразующая способность или чем большая была концентрация органических анионов, тем легче была образование псевдобемита или аморфных материалов. [Е.С.]

Resümee

Resümee

Chelatkomplex-bildende organische Säuren verhindern die hydrolytischen Reaktionen von aluminium und beeinflussen die Art der kristallinen Aluminiumhydroxide. Die chemische Zusammensetzung, die Struktur, die Größe, die Art der funktionellen Gruppen, und die Konzentration jedes einzelnen organischen Anions sowie der pH-Wert des Systems bestimmen die Kristallisationsgeschwindigkeit von Al(OH)3. Die Reihenfolge der Wirksamkeit der verschiedenen Säuren war: Glutarsäure < Bernsteinsäure = Phthalsäure < Glycinsäure < Malonsäure < Glutaminsäure < Asparaginsäure < Oxalsäure < Salicylsäure = Monohydroxibernsteinsäure < Zitronensäure < Weinsäure. Eine Stabilitätszunahme der Komplexe aus den organischen Liganden mit dem Aluminium verringerte die Kristallisationsgeschwindigkeit und veränderte die Aluminium-Endprodukte von Bayerit nach Nordstrandit und/oder Gibbsit und danach zu Pseudoboehmit und/oder amorphe Substanz. In der Gegenwart von Anionen mit einer großen Affinität für Aluminium waren die Reaktionsprodukte, vor allem bei pH-Werten gleich oder kleiner 9,0, im allgemeinen schlecht kristallisiert oder hatten eine verzerrte Struktur. Im pH-Bereich von 8,0 bis 10,0 wirkten mässig oder stark Chelatkomplex-bildende Anion verzögernd oder verhindernd auf die Olation und begünstigten die Bildung von stabilem Pseudoboehmit oder von röntgenamorphen Substanzen. Je größer die Komplexierungsfähigkeit oder je höher die Konzentration an organischen Anionen war, umso leichter war die Bildung von Pseudoboehmit oder amorphem Material. [U.W.]

Résumé

Résumé

Des acides organiques chélatants ont rendu plus difficiles les réactions hydrolitiques d'Al et affecté la nature des hydroxides d'aluminium cristallins. La composition chimique, la structure, la taille, la nature des groupes fonctionnels, et la concentration de chaque anion organique, ainsi que le pH du système ont contrôlé l'allure de la cristallisation d'Al(OH)3. L'ordre d'efficacité des acides variés était le suivant: glutarique < succinique = phthalique < glycine < malonique < glutamique < aspartique < oxalique < salicylique = malique < citrique < tartarique. Un accroissement de la stabilité des complexes formés par les liants organiques et Al a diminué l'allure de cristallisation et changé les produits alumineux finaux de bayerite en nordstrandite et/ou gibbsite et ensuite en pseudobohémite et/ou matériel amorphe. En présence d'anions ayant une grande affinité pour Al, particulièrement à un pH égal à ou inférieur à 9, les produits de réaction étaient souvent pauvrement cristallins ou structuralement dérangés. Dans la gamme de pH de 8 à 10, des anions modérément ou très chélatants ont agi de façon à retarder ou empêcher l'olation et ont facilité la formation de pseudobohémite stable ou de produits amorphes aux rayons-X. Plus le pouvoir de chélation des anions organiques était grand, ou plus leur concentration était haute, plus la formation de pseudobohémite ou de matériel amorphe était facile. [D.J.]

Type
Research Article
Copyright
Copyright © Clay Minerals Society 1980

Footnotes

1

This work was supported in part by the CNR research grant CT79.01978.06.

References

Aldcroft, D. Bye, G. C. and Hughes, C. A., (1969) Crystallization process in aluminum hydroxide gels. IV. Factors influencing the formation of the crystalline trihydroxides J. Appl. Chem. 19 167172.CrossRefGoogle Scholar
Bailar, J. C., (1956) Chemistry of the Coordination Compounds New York Reinhold.Google Scholar
Bye, G. C. and Robinson, J. G., (1964) Crystallization process in aluminum hydroxide gels Kolloid Z. 198 5360.CrossRefGoogle Scholar
Cornell, R. M. and Schwertmann, U., (1979) The influence of organic anions on the crystallization of ferrihydrite Clays & Clay Minerals 27 402410.CrossRefGoogle Scholar
Das Sarma, B., (1956) The structures of copper monoglutamate J. Amer. Chem. Soc. 78 892894.CrossRefGoogle Scholar
Earl, K. D. Syers, J. K. and McLaughlin, J. R., (1979) Origin of the effects of citrate, tartrate and acetate on phosphate sorption by soils and synthetic gels Soil Sci. Soc. Amer. J. 43 674678.CrossRefGoogle Scholar
Hsu, Pa. H., (1967) Effect of salts on the formation of bay erite versus pseudoboehmite Soil Sci. 103 101110.CrossRefGoogle Scholar
Hsu, Pa. H., Dixon, J. B. and Weed, S. B., (1977) Aluminum hydroxides and oxyhydroxides Minerals in Soil Environments 99143.Google Scholar
Huang, W. H. and Keller, W. D., (1972) Organic acids as agent of chemical weathering of silicate minerals Nat. Phys. Sci. 239 149151.CrossRefGoogle Scholar
Huang, W. H. and Kiang, W. C., (1972) Laboratory dissolution of plagioclase feldspars in water and organic acids at room temperature Amer. Mineral. 57 18491859.Google Scholar
Keller, WD and Bradley, W. F., (1964) The origin of high alumina clay minerals Clays and Clay Minerals, Proc. 12th Nat. Conf., Atlanta, Georgia, 1963 New York Pergamon Press 129151.Google Scholar
Kinniburgh, D. G. Jackson, M. L. and Syers, J. K., (1976) Adsorption of alkaline earth, transition, and heavy metal cation by hydrous oxide gels of iron and aluminum Soil Sci. Soc. Amer. Proc. 40 796799.CrossRefGoogle Scholar
Kwong, Ng K and Huang, P. M., (1975) Influence of citric acid on the crystallization of aluminum hydroxides Clays & Clay Minerals 23 164165.CrossRefGoogle Scholar
Kwong, Ng K and Huang, P. M., (1977) Influence of citric acid on the hydrolytic reactions of aluminum Soil Sci. Soc. Amer. J. 41 692697.CrossRefGoogle Scholar
Kwong, Ng K Huang, P. M., Mortland, M. M. and Farmer, V. C., (1979) Nature of hydrolytic products of aluminum as influenced by low-molecular weight complexing organic acids Proc. Int. Clay Conf., Oxford, 1978 527536.Google Scholar
Kwong, Ng K and Huang, P. M., (1979) The relative influence of low-molecular weight, complexing organic acids on the hydrolysis and precipitation of aluminum Soil Sci. 128 337342.CrossRefGoogle Scholar
Lahodny-Sarc, O. D. Z. and Dosen-Sver, D., (1978) The influence of the activity of water on the phase composition of aluminum hydroxides formed by reaction of amalgamated aluminum with water Clays & Clay Minerals 26 153159.CrossRefGoogle Scholar
Lodding, W., (1961) Gibbsite vermiforms in the Pensouken Formation of New Jersey Amer. Mineral. 46 394401.Google Scholar
Luciuk, G. M. and Huang, P. M., (1974) Effect of monosilicic acid on hydrolytic reactions of aluminum Soil Sci. Soc. Amer. Proc. 38 235243.CrossRefGoogle Scholar
Murmann, R. K., (1969) Inorganic Complex Compounds New York Reinhold.Google Scholar
Parfitt, R. L., (1978) Anion adsorption by soils and soil materials Adv. Agron. 30 150.Google Scholar
Schoen, R. and Roberson, E. C., (1970) Structures of aluminum hydroxide and geochemical implication Amer. Mineral. 55 4377.Google Scholar
Souza Santos, P. Vallejo-Fraire, A. and Souza Santos, H. L., (1953) Electron microscope studies on the aging of amorphous colloidal aluminum hydroxide Kolloid Z. 133 101107.CrossRefGoogle Scholar
Struthers, P. H. and Sieling, D. H., (1950) Effect of organic anions on phosphate precipitation by Fe and Al as influenced by pH Soil Sci. 69 205213.CrossRefGoogle Scholar
Violante, A. Jackson, M. L., Mortland, M. M. and Farmer, V. C., (1979) Crystallization of nordstrandite in citrate systems and in the presence of mont-morillonite Proc. Int. Clay Conf, Oxford, 1978 Amsterdam Elsevier 517525.Google Scholar
Violante, A. and Violante, P., (1978) Influence of carboxylic acids on the stability of chlorite-like complexes and on the crystallization of Al(OH)3 polymorphs Agrochimica 22 335343.Google Scholar
Violante, A. and Jackson, M. L., (1980) Clay influence on the crystallization of Al(OH)3 polymorphs in the presence of citrate, sulfate, or chloride Geoderma .CrossRefGoogle Scholar