ADENINE, ADENOSINE, RIBOSE AND 5′-AMP ADSORPTION TO ALLOPHANE

dc.contributor.authorHashizume H.
dc.contributor.authorTheng B.K.G.
dc.date.accessioned2026-06-04T15:31:58Z
dc.date.issued2007
dc.description.abstractWe have investigated the adsorption of adenine, adenosine, ribose, and adenosine-5′-phosphate (5′-AMP) by allophane at pH 4, 6 and 8. Adenine, adenosine and ribose gave similar isotherms, i.e. adsorption increased regularly with solution concentration and decreased in the order: pH 8 > pH 6 > pH 4. Allophane had a greater affinity for 5′-AMP than for adenine, adenosine or ribose. Further, the extent of adsorption for 5′-AMP increased in the order: pH 8 ≪ pH 6 ≈ pH 4. The adsorption of 5′-AMP at pH 4 and pH 6 was about 60 times greater than at pH 8. The strong adsorption of 5′-AMP accords with the well known high phosphate-retention capacity of allophane and allophane-rich soils. The experimental data may be rationalized in terms of the pH-dependent charge characteristics of the organic solutes and allophane. The large propensity of allophane to retain 5′-AMP is ascribed to ligand exchange between the phosphate of 5′-AMP and the hydroxyl of (HO)Al(OH2) groups, exposed at perforations on the wall of allophane spherules, giving rise to a surface (chelation) complex. The high affinity of nucleotides for allophane has implications for the possible role of allophane in the abiotic formation of RNA-type polynucleotides although nucleotide ‘immobilization’ by surface complexation might hinder RNA oligomerization.
dc.identifierhttps://elibrary.ru/item.asp?id=51374809
dc.identifier.citationClays and Clay Minerals, 2007, 55, 6, 599-605
dc.identifier.doi10.1346/ccmn.2007.0550607
dc.identifier.issn0009-8604
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/53158
dc.subjectADENINE
dc.subjectADENOSINE
dc.subjectALLOPHANE
dc.subject5′-AMP
dc.subjectADSORPTION
dc.subjectRIBOSE
dc.titleADENINE, ADENOSINE, RIBOSE AND 5′-AMP ADSORPTION TO ALLOPHANE
dc.typeСтатья

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