DNA adsorption on synthetic and natural allophanes

被引:46
作者
Saeki, Kazutoshi [1 ]
Sakai, Masao [2 ]
Wada, Shin-Ichiro [3 ]
机构
[1] Kyushu Univ, Biotron Inst, Higashi Ku, Fukuoka 8128581, Japan
[2] Kagoshima Univ, Fac Agr, Kagoshima 8900065, Japan
[3] Kyushu Univ, Grad Sch Bioresource & Bioenvironm Sci, Higashi Ku, Fukuoka 8128581, Japan
基金
日本学术振兴会;
关键词
DNA adsorption; Allophane; pH; Ionic strength; SELENITE ADSORPTION; BACILLUS-SUBTILIS; MONTMORILLONITE; TRANSFORMATION; KAOLINITE; GIBBSITE; BINDING; SILICA; CLAY; SOIL;
D O I
10.1016/j.clay.2010.09.015
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The adsorption of DNA on natural and synthetic samples of allophane which is a primary clay mineral of andosols was investigated with respect to the DNA concentration pH ionic strength in the sample solution and competition between DNA molecules and phosphate ions for adsorption to understand the behavior of extracellular DNA molecules in andosols The relationships between DNA adsorption and the final concentrations were significantly fitted to a simple linear Langmuir equation DNA adsorption decreased considerably with increasing suspension pH in the range between 3 and 9 The adsorption was less affected by the ionic strength of the suspension from 0 1 to 05 mol L-1 Under the same experimental conditions DNA adsorption on allophanes was relatively higher than that on montmorillonite and silica but relatively lower than that on gibbsite and goethite DNA adsorption on allophanes decreased on the addition of phosphate indicating that there was a competition between DNA molecules and phosphate ions for adsorption on the minerals These results suggested that DNA adsorption on allophanes occurred via two mechanisms direct bonding of the phosphate group at the end of the DNA molecule to the OH groups of the Al-oxide layer on allophane and the association of DNA molecules with the surface of negatively charged allophane via a bridging of inorganic ations (C) 2010 Elsevier B V All rights reserved
引用
收藏
页码:493 / 497
页数:5
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