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Adsorption Characteristics of Starch Digested with Alkali on Fine Hematite Particles

机译:碱在细赤铁矿颗粒上消化碱的吸附特性

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In this paper, the influence of alkali on the flocculation of starch on fine hematite was investigated through a series of tests, like turbidities, paste titration, adsorption, conductance, scanning electron microscope (SEM) measurement, and Fourier transforms infrared spectroscopic analysis (FTIR) as well. The results pointed out that alkali concentration has a strong influence on physicochemical changes of starch granules, inducing different adsorption densities on mineral surfaces. A maximum amount of adsorption density on mineral particles was harvested for the starch digested with sodium hydroxide at a concentration of 0.4 N/g starch. It is worthy to note that starch is not fully digested in the presence of alkali at a concentration of less than 0.4 N/g starch. Higher concentration of hydroxide ions, however, tends to obtain less adsorption density of starch on hematite because too small remnants in the starch gel have inverse effects on adsorption capacity.
机译:本文通过一系列试验研究了碱对淀粉絮凝物对细赤铁矿絮凝的影响,如浊度,糊状滴定,吸附,电导,扫描电子显微镜(SEM)测量,傅里叶变换红外光谱分析(FTIR )也是如此。 结果指出,碱浓度对淀粉颗粒的物理化学变化产生强烈影响,诱导矿物表面上的不同吸附密度。 收获最大量的矿物颗粒的吸附密度,以0.4n / g淀粉的浓度用氢氧化钠消化的淀粉。 值得注意的是,淀粉在碱存在下不完全消化,浓度小于0.4n / g淀粉。 然而,较高浓度的氢氧化浓度倾向于在赤铁矿上获得较少的吸附密度,因为淀粉凝胶中的微小残余物具有对吸附能力的反效果。

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