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Characterization of Clay of the Benin Used in Ruminale Feeding. Complete Determination of the Smectites Contained in These Clays

机译:反刍动物饲料中使用的贝宁粘土的表征。完全测定这些粘土中所含的蒙脱石

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In this work, by the use of several physico-chemical complementary methods for the characterization of soil (diffraction of x-rays, chemical analysis, density, cationic exchange capacity, specific sur faces, m?ssbauer, granulometry, etc.), the smectite of the three clayey localities of Benin (Gbédji-Kotovi, Massi-Sèhouè and Zogbodomey) was notably studied. Thus, these three sites principally contain principally smectite, kaolinite and quartz in variable proportion. This smectite is a beidellite. Its chemical formula is proposed. The specific surfaces and the cationic exchange capacity of the samples are determined. For these samples, the fraction lower than 2 μm is practically beidellitic for Gbédji-Kotovi and Massi-Sèhouè (more than 82% of beidellite) and practically kaolinitic (70% of kaolinite) for Zogbodomey. So, used as additive food to ruminant, the clay of Gbédji-Kotovi and Massi-Sèhouè will induce an enteric reduction of methane more than clay of Zogbodomey.
机译:在这项工作中,通过使用几种物理化学补充方法来表征土壤(X射线衍射,化学分析,密度,阳离子交换容量,比表面,msssbauer,粒度分析等),贝宁的三个黏土的蒙脱石(Gbédji-Kotovi,Massi-Sèhouè和Zogbodomey)得到了显着研究。因此,这三个部位主要包含变比例的蒙脱石,高岭石和石英。该蒙脱石是贝得石。提出了其化学式。确定样品的比表面积和阳离子交换容量。对于这些样品,对于Gbédji-Kotovi和Massi-Sèhouè(低于贝得石的82%),实际上小于2μm的贝氏体,对于Zogbodomey,实际上是高岭石(70%的高岭石)。因此,Gbédji-Kotovi和Massi-Sèhouè的黏土用作反刍动物的添加食品,比Zogbodomey的黏土更能引起肠溶性甲烷的减少。

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