Investigating the drying behaviour of clay-containing slurries

IF 5.3 2区 地球科学 Q2 CHEMISTRY, PHYSICAL Applied Clay Science Pub Date : 2024-08-12 DOI:10.1016/j.clay.2024.107500
Nadia Kashif , Boris Albijanic , Jing Jing Xu , Teresa McGrath , Muhammad Kashif Nazir , Michael Hitch , Bogale Tadesse
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Abstract

Managing clay-containing slurries during drying process remains a persistent challenge in various industries. Despite challenges of drying clay-containing-slurries, limited information is available. The aim of this study is to explore the drying performance of slurries containing kaolin and bentonite and gain insights into the underlying drying mechanisms. The research presented integrates drying experiments, rheology measurements, settling experiments, zeta potential measurements, FTIR, TGA/DTA, and SEM analysis. Bentonite-containing slurries retained more moisture due to their high-water adsorption capacity, with higher bentonite percentages extending drying times. The addition of Ca2+ ions reduced moisture content by replacing Na+ ions with smaller Ca2+ ions, making the slurries less viscous. The addition of Ca2+ disrupted the gel-like structure of bentonite as confirmed by SEM and FTIR. In contrast, kaolin-containing slurries maintain lower moisture levels owing to the non-swelling structure of kaolinite. SEM showed the formation of agglomerates for kaolin when Ca2+ was added The addition of Ca2+ ions had a subtle impact on drying rates, despite a slight increase in slurry viscosity probably due to the agglomeration of kaolinite particles. Both slurries exhibited three drying phases: rapid drying due to high moisture, a moderate phase with reduced rates, and a final phase of slowed drying as tightly bound moisture was harder to remove. This paper demonstrated the significance of understanding the drying processes of clay-containing slurries to enhance the overall drying efficiency.

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研究含粘土泥浆的干燥行为
在干燥过程中管理含粘土泥浆仍然是各行各业面临的一项长期挑战。尽管含粘土泥浆的干燥过程充满挑战,但可用的信息却很有限。本研究旨在探索含高岭土和膨润土泥浆的干燥性能,并深入了解其潜在的干燥机制。本研究综合了干燥实验、流变学测量、沉降实验、zeta 电位测量、傅立叶变换红外光谱、TGA/DTA 和扫描电镜分析。由于膨润土的高吸水能力,含膨润土的泥浆保留了更多水分,膨润土比例越高,干燥时间越长。加入 Ca2+ 离子后,较小的 Ca2+ 离子取代了 Na+ 离子,使泥浆粘度降低,从而减少了水分含量。经扫描电镜和傅立叶变换红外光谱证实,Ca2+ 的加入破坏了膨润土的凝胶状结构。相比之下,由于高岭石的非膨胀结构,含高岭土的泥浆能保持较低的湿度。扫描电镜显示,添加 Ca2+ 后,高岭土形成了团聚体。尽管泥浆粘度略有增加,但添加 Ca2+ 离子对干燥速率的影响微乎其微,这可能是由于高岭石颗粒团聚所致。两种泥浆都表现出三个干燥阶段:高水分导致的快速干燥阶段、速率降低的中等干燥阶段以及最后的缓慢干燥阶段,因为紧密结合的水分更难去除。本文表明,了解含粘土泥浆的干燥过程对于提高整体干燥效率具有重要意义。
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来源期刊
Applied Clay Science
Applied Clay Science 地学-矿物学
CiteScore
10.30
自引率
10.70%
发文量
289
审稿时长
39 days
期刊介绍: Applied Clay Science aims to be an international journal attracting high quality scientific papers on clays and clay minerals, including research papers, reviews, and technical notes. The journal covers typical subjects of Fundamental and Applied Clay Science such as: • Synthesis and purification • Structural, crystallographic and mineralogical properties of clays and clay minerals • Thermal properties of clays and clay minerals • Physico-chemical properties including i) surface and interface properties; ii) thermodynamic properties; iii) mechanical properties • Interaction with water, with polar and apolar molecules • Colloidal properties and rheology • Adsorption, Intercalation, Ionic exchange • Genesis and deposits of clay minerals • Geology and geochemistry of clays • Modification of clays and clay minerals properties by thermal and physical treatments • Modification by chemical treatments with organic and inorganic molecules(organoclays, pillared clays) • Modification by biological microorganisms. etc...
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