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首页> 外文期刊>Clays and clay minerals >ENHANCEMENT OF AMORPHOUS SILICA DISSOLUTION BY INTERACTION WITH SIX-MEMBERED RING HETEROCYCLIC COMPOUNDS
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ENHANCEMENT OF AMORPHOUS SILICA DISSOLUTION BY INTERACTION WITH SIX-MEMBERED RING HETEROCYCLIC COMPOUNDS

机译:通过与六元环杂环化合物的相互作用增强无定形二氧化硅溶解

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Abstract Six-membered ring heterocyclic compounds are widely present in the Earth's surface environments as biological organic molecules composed of soil organic matter including plant and microbial residues, while little is known about their effect on the dissolution of silicate minerals including amorphous silica. To evaluate the effect of these biological molecules on amorphous silica dissolution, dissolution experiments were carried out by the flow-through method using 0.1 g of amorphous silica and 0.1 mM NaCl electrolyte solutions containing 0.0, 0.1, 1.0, or 10.0 mM of the heterocyclic compounds, piperidine (pK = 11.12), pyridine (pK = 5.25), or pyridazine (pK = 2.33), at a pH of 6, 5, or 4. Additionally, adsorption experiments of the compounds on the amorphous silica surface were performed to confirm the adsorption affinity for the amorphous silica surface. The results demonstrated that these heterocyclic compounds enhance the dissolution rate of amorphous silica in the following order: piperidine > pyridine > pyridazine. When 10.0 mM solutions were used, the heterocyclic compounds enhanced greatly the dissolution rate up to enhancement factors of 6.0 to ~14.8, 5.0 to ~14.0, and 1.0 to ~2.6 through an interaction of piperidine, pyridine, and pyridazine, respectively, in the pH range of approximately 6 to ~ 4. The adsorption experiments indicated that the heterocyclic compounds exhibited significant adsorption affinity for the amorphous silica surface as follows: piperidine > pyridine > pyridazine, which was consistent with the order of their effects on the dissolution enhancement. The geochemical calculation revealed that this order of enhancement was in good agreement with the concentrations of cationic species of heterocyclic compounds at corresponding pH conditions. Consequently, the enhancement of amorphous silica dissolution is likely to be influenced by the electrostatic complexation of the cationic species of the heterocyclic compounds with the negative >SiO– sites on the amorphous silica surface.
机译:摘要六元环杂环化合物广泛存在于地球表面环境中,作为由包括植物和微生物残留物的土壤有机物质组成的生物有机分子,虽然对它们对包括无定形二氧化硅的硅酸盐矿物溶解的影响很少。为了评估这些生物分子对非晶二氧化硅溶解的影响,通过使用0.1g非晶二氧化硅和含有0.0,0.1,1.0或10.0mm的杂环化合物的0.1mM NaCl电解质溶液,通过流通方法进行溶解实验,哌啶(PK = 11.12),吡啶(PK = 5.25),或哒嗪(PK = 2.33),在6,5或4的pH下,进行无定形二氧化硅表面上的化合物的吸附实验以确认无定形二氧化硅表面的吸附亲和力。结果表明,这些杂环化合物以下列顺序提高无定形二氧化硅的溶出速率:哌啶>吡啶>吡啶啶。当使用100mM溶液时,通过分别在哌啶,吡啶和吡啶啶的相互作用中,杂环化合物提高了6.0至约14.8,5.0至约14.0和1.0至〜2.6的溶出速率。吸附实验的pH范围约为6至〜4。杂环化合物表现出对无定形二氧化硅表面的显着吸附亲和力,如下:哌啶>吡啶>哒嗪,其与它们对溶解增强的影响顺序一致。地球化学计算揭示了这种增强顺序与相应的pH条件下的杂环化合物的浓度很好。因此,可以通过在非晶二氧化硅表面上的阴性> SiO-位点的杂环化合物的阳离子种类的静电络合来影响非晶二氧化硅溶解的增强。

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