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 ที่มา:33rd Congress on Science and Technology of Thailandหัวเรื่อง:แร่เคโอลิไนต์ในดินนาประเทศไทย |
ที่มา:Geodermaหัวเรื่อง:Surface charge properties of kaolinite from Thai soils |
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ผลงานตีพิมพ์ในวารสารวิชาการImpedimetric detection of 2,4,6-trinitrotoluene using surface-functionalized halloysite nanotubesผู้แต่ง: Pattaweepaiboon, S., Pimpakoon, V., Phongzitthiganna, N.,  Mr.WEEKIT SIRISAKSOONTORN, Associate Professor , Dr.Kannika Jeamjumnunja, Assistant Professor , Dr.Chaiya Prasittichai, Assistant Professor, วารสาร: 
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การประชุมวิชาการComposition and microstructure of fly ash geopolymer containing metakaolinผู้แต่ง:Pimraksa, K., Mr.Thanudkij Chareerat, Lecturer, Chindaprasirt, P., Mishima, N., Hatanaka, S., การประชุมวิชาการ: |
 หัวเรื่อง:การกระจายของแร่ดินเหนียวเคโอลิไนต์ อิลไลต์ และมอนต์มอริลโลไนต์ในขนาดอนุภาคดินเหนียวชนิดหยาบ และชนิดละเอียดของดินตะกอนน้ำพาบางชนิด ผู้เขียน:Kannica yoothong, Mitri Pukamphol, Ampawan Hutspardol สื่อสิ่งพิมพ์:pdf Abstract Seven selected soil profiles of alluvial soils from various parts of Thailand were used in the study of the distribution of clay minerals – kaolinite, illite and montmorillonite in coarse and the find clay fractions. The clay fraction of soils was first separated into coarse and fine fractions between 2.0 to 0.2 micron and smaller than 0.2 micron, respectively. The mineralogical composition of both fractions was determined by X-ray diffraction technique. The results reveal that the clay mineralogy of the alluvial soils consists mainly of kaolinite, montmorillonite and illite with kaolinite yielding the biggest proportion in most of the soils studied. Interstratified clay minerals, vermiculite, chlorite, goethite and quartz are also present in small quantities in some soil series. The distribution of kaolinite in the two fractions are nearly the same, slightly more in the coarse clay fraction (2.0 to 0.2 micron) in some soils, however slightly more in the fine clay fraction (<0.2 micron) is also observed. Montmorillonite is found in both fractions of most soils, more in the fine clay fraction than in the coarse clay fraction. Illite segregates largely in th coarse clay fraction and is found in the fine clay fraction in minor amount or does not present in some soils. Other minerals from these alluvial soils such as vermiculite, quartz and chlorite are found only in the coarse clay fraction and the interstratified clay minerals and goethite are presented in both clay fractions. From the reasons that many minerals do not segregate largely in either coarse or fine clay fraction, in general practice, it is not necessary to separate the clay fraction into coarse and fine fractions prior to X-ray diffraction examination of minerals. Separation of the clay fraction < 2 micron is satisfactory. |
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