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首页> 外文期刊>Applied and Environmental Microbiology >Precipitation of Metallic Cations by the Acidic Exopolysaccharides from Bradyrhizobium japonicum and Bradyrhizobium (Chamaecytisus) Strain BGA-1
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Precipitation of Metallic Cations by the Acidic Exopolysaccharides from Bradyrhizobium japonicum and Bradyrhizobium (Chamaecytisus) Strain BGA-1

机译:日本根瘤菌和根瘤菌(Chamaecytisus)菌株BGA-1的酸性胞外多糖沉淀金属阳离子

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摘要

The interaction between the acidic exopolysaccharides produced by two Bradyrhizobium strains and several metal cations has been studied. Aqueous solutions in the millimolar range of Fe3+ but not of Fe2+ precipitated the exopolysaccharides from Bradyrhizobium (Chamaecytisus) strain BGA-1 and, to a lesser extent, Bradyrhizobium japonicum USDA 110. The precipitation was pH dependent, with a maximum around pH 3. The precipitate was redissolved by changing the pH and by Fe3+ reduction or chelation. Deacetylation of B. japonicum polysaccharide increased its precipitation by Fe3+. At pH near neutrality, the polysaccharide from Bradyrhizobium (Chamaecytisus) strain BGA-1 stabilized Fe3+ solutions, despite the insolubility of Fe(OH)3. Aluminum precipitated Bradyrhizobium (Chamaecytisus) polysaccharide but not the polysaccharide produced by B. japonicum. The precipitation showed a maximum at about pH 4.8, and the precipitate was redissolved after Al3+ chelation with EDTA. Precipitation was inhibited by increases in the ionic strength over 10 mM. Bradyrhizobium (Chamaecytisus) polysaccharide was also precipitated by Th4+, Sn2+, Mn2+, and Co2+. The presence of Fe3+ increased the exopolysaccharide precipitation by aluminum. No precipitation, gelation, or increase in turbidity of polysaccharide solutions occurred when K+, Na+, Ca2+, Mg2+, Cu2+, Cd2+, Pb2+, Zn2+, Hg2+, or U6+ was added at several pH values. The results suggest that the precipitation is based on the interaction between carboxylate groups from different polysaccharide chains and the partially hydrolyzed aquoions of Fe3+, Al3+, Th4+, and Sn2+.
机译:已经研究了由两个根瘤菌菌株产生的酸性胞外多糖与几种金属阳离子之间的相互作用。毫摩尔范围的Fe3 +而不是Fe2 +的水溶液会沉淀出Bradyrhizobium(Chamaecytisus)菌株BGA-1的胞外多糖,并在较小程度上沉淀了日本Bradyrhizobium japonicum USDA 110的沉淀。沉淀是pH依赖性的,最大pH约为3。改变pH值,并通过Fe3 +还原或螯合将沉淀重新溶解。日本芽孢杆菌多糖的脱乙酰作用增加了其Fe3 +的沉淀。在pH接近中性的条件下,尽管Fe(OH)3不溶,但Bradyrhizobium(Chamaecytisus)BGA-1菌株的多糖稳定了Fe3 +溶液。铝沉淀的缓生根瘤菌(Chamaecytisus)多糖,但不是日本芽孢杆菌产生的多糖。 Al3 +与EDTA螯合后,沉淀在约pH 4.8处显示最大值,沉淀重新溶解。离子强度增加超过10 mM可以抑制沉淀。缓生根瘤菌(Chamaecytisus)多糖也被Th4 +,Sn2 +,Mn2 +和Co2 +沉淀。 Fe3 +的存在增加了铝的胞外多糖沉淀。当在多个pH值下添加K +,Na +,Ca2 +,Mg2 +,Cu2 +,Cd2 +,Pb2 +,Zn2 +,Hg2 +或U6 +时,多糖溶液未发生沉淀,凝胶化或浊度增加。结果表明,沉淀是基于来自不同多糖链的羧酸酯基团与部分水解的Fe3 +,Al3 +,Th4 +和Sn2 +的水族基之间的相互作用。

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