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Some Physicochemical Properties Of A Clay Containing Smectite And Palygorskite

机译:绿土和坡缕石粘土的一些理化性质

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摘要

A sample of brown clay from the commercially mined Sungurlu deposit (Corum, Turkey) was examined in terms of its mineralogy, morphology and porosity by particle size analysis, X-ray diffraction, chemical analysis, cation exchange, Fourier transform infrared spectroscopy, Mossbauer spectroscopy, electron microscopy, thermal analysis, and nitrogen adsorption/desorption techniques. The fraction of particles with diameters < 2 μm in the aqueous dispersion was 83% (v,v). The moisture content and cation exchange capacity of the clay were 12.1 mass % and 0.85 eq/g, respectively. Total mass loss between 25-1000 ℃ was 22.1%. Two different recrystallization temperatures for the clay are 860 and 980 ℃. The sample contained iron rich calcium smectite (CaS), fibrous palygorskite (P), and quartz (Q). The specific values of surface area, micropore volume, mesopore volume, and micro-mesopore volume were 208 m~2 g~(-1), 0.074 cm~3 g~(-1), 0.158 cm~3 g~(-1), and 0.232 cm~3 g~(-1) respectively.
机译:通过粒度分析,X射线衍射,化学分析,阳离子交换,傅立叶变换红外光谱,Mossbauer光谱对来自商业开采的Sungurlu矿床(土耳其,Corum)的褐色粘土的矿物学,形态和孔隙度进行了检查,电子显微镜,热分析和氮吸附/解吸技术。在水分散体中直径<2μm的颗粒的比例为83%(v,v)。粘土的水分含量和阳离子交换容量分别为12.1质量%和0.85eq / g。 25-1000℃之间的总质量损失为22.1%。粘土的两种不同的重结晶温度分别为860和980℃。样品中含有富铁的蒙脱石钙(CaS),纤维坡缕石(P)和石英(Q)。表面积,微孔体积,中孔体积和微中孔体积的比值为208 m〜2 g〜(-1),0.074 cm〜3 g〜(-1),0.158 cm〜3 g〜(-1 )和0.232 cm〜3 g〜(-1)。

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