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首页> 外文期刊>Applied clay science >Exfoliation/delamination of kaolinite by low-temperature washing of kaolinite-urea intercalates
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Exfoliation/delamination of kaolinite by low-temperature washing of kaolinite-urea intercalates

机译:通过低温洗涤高岭石-尿素插层对高岭石的剥落/分层

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The effects of short milling (2 x 10 min) of two fractions of kaolinite (<5 μm (S5) and 5-45 μm (S)), previously expanded by intercalation with 20 wt.% and 40 wt.% urea (U) and exfoliated/delaminated using low-temperature procedures, were studied. Untreated and treated kaolinite samples were examined by X-ray powder diffraction (XRPD), and their specific surface area (SSA), particle size distribution (PSD) and Fourier-transform infrared (FTIR) spectra were measured and interpreted. Samples intercalated with different concentrations of urea and subsequently exfoliated during thermal or low-temperature washing exhibit a variable intensity of the 001 diffractions of kaolinite (K) and interstratified intermediate kaolinite (H) with randomly interstratified layers of grafted urea and water. Low-temperature washing procedures yield H structures interstratified with layers grafted with urea and water with a mean d_(001) = 8.168(50) A. After thermal washing procedures, H structures form with a mean d_(001) = 8.322(60) A, apparently as a result of prevailing interstratifications of water over grafted layers of urea. The H/K peak intensity ratio for exfoliated/delaminated samples S and S5 previously intercalated with 20% U is significantly higher than for those intercalated with 40% U. After all washing procedures, fine fraction S5 increases its SSA from 20.2 m~2/g to 25-35 m~2/g, whereas the grain-size diameter remains approximately constant, with a mean M_D = 2.80(20) μm. Exfoliated/delaminated coarse kaolinite of the S fraction not only increases its SSA from 9.4 m~2/g to SSA between 12.5 m~2/g and 20.5 m~2/g, but also decreases its M_D from 12 μm to between 8.73 μm and 5.60 μm due to the breaking of particles. This procedure is quicker than milling and thermal washing operations reported and used so far, and, moreover, it yields SSA values comparable to those obtained for exfoliated/delaminated kaolinite.
机译:短暂研磨(2 x 10分钟)的两部分高岭石(<5μm(S5)和5-45μm(S))的效果,事先通过插入20 wt%和40 wt%的尿素(U ),并使用低温程序对角质层/角质层进行了研究。通过X射线粉末衍射(XRPD)检查未处理和处理过的高岭石样品,并测量和解释其比表面积(SSA),粒度分布(PSD)和傅立叶变换红外(FTIR)光谱。插有不同浓度尿素并随后在热或低温洗涤过程中剥离的样品显示出高岭石(K)和层间化中间高岭石(H)的001衍射强度可变,其中层间接枝的尿素和水随机分层。低温洗涤程序产生的H结构与尿素和水接枝的层互层,平均d_(001)= 8.168(50)A。热洗涤程序后,H结构形成,平均d_(001)= 8.322(60) A,显然是由于水在尿素的接枝层上普遍存在的分层作用的结果。预先插入20%U的剥落/分层样品S和S5的H / K峰强度比明显高于插入40%U的剥落/分层样品S和S5的H / K峰强度比。在所有洗涤程序后,细级分S5的SSA从20.2 m〜2 /增加g到25-35 m〜2 / g,而晶粒直径保持大致恒定,平均M_D = 2.80(20)μm。 S级分的剥落/分层的粗高岭石不仅将其SSA从9.4 m〜2 / g增加到12.5 m〜2 / g至20.5 m〜2 / g的SSA,而且还将其M_D从12μm降低到8.73μm和5.60μm由于颗粒破裂。该方法比迄今为止报道和使用的研磨和热洗操作要快,而且,其SSA值可与剥离/分层高岭石的SSA值相媲美。

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