G. Batdemberel, S. Chadraabal, P. Jargalbat, D. Sangaa, B. Namjildorj
{"title":"蒙古天然沸石晶体结构研究","authors":"G. Batdemberel, S. Chadraabal, P. Jargalbat, D. Sangaa, B. Namjildorj","doi":"10.1109/IFOST.2010.5667928","DOIUrl":null,"url":null,"abstract":"We have studied zeolitic rocks discovered in Mongolia using electron microscopy (SEM), X-ray fluorescence (XRF), X-ray diffraction (XRD) methods. SEM, XRF and XRD measurements were carried out in the Max Plank Institute of Stuttgart, Germany. Our samples are collected from Mongolian deposits: Tsagaan tsav, Tushig uul, Urgun deposit, Bayan Zurkh Black Mountain and Mandal ovoo. Firstly, we have made chemical element analysis by using X-ray fluorescence spectroscopy which gives chemical contents of samples from all zeolite deposits. Comparing contents of above 5 deposits samples shows us that zeolite of Tushig Mountain, Dornogobi, is has the highest content of potassium and can be identified in potassium clinoptilolite- K (2.56 at %), others belong to clinoptilolite- Na. The main cations are K,Na,Ca,Mg,Fe,Ti for all the samples from the above mentioned deposits. Also, the (Si Al)/O ratio shows that the Mongolian zeolites have comparatively good qualities. We made X-ray phase analysis study on X-ray powder diffractometer Bruker-Axes D8 and refined the X-ray diffraction spectra by using ≪Match! Crystal Impact≫ program. As a result, we established that these zeolites are Na and K type of clinoptilolite with monoclinic symmetry (C2/m). Finally, the exact crystallochemical formula of clinoptilolites can be written as the next: • (Na<inf>2.02</inf>, K<inf>1.81</inf>, Mg<inf>0.49</inf>, Ca<inf>0.46</inf>, Fe<inf>0.36</inf>)(Al<inf>6.28</inf>O<inf>30.45</inf>) (Si<inf>28.47</inf>O<inf>30.45</inf>)·z·H<inf>2</inf>O for Tsagaan tsav sample. • (K<inf>2.56</inf>, Na<inf>1.69</inf>, Mg<inf>0.64</inf>, Ca<inf>0.47</inf>, Fe<inf>0.78</inf>)(Al<inf>6.39</inf>O<inf>28.15</inf>) (Si<inf>31.17</inf>O<inf>28.15</inf>)·z·H<inf>2</inf>O for Tushig Mountain sample. • (Na<inf>2.34</inf>, K<inf>1.48</inf>, Mg<inf>0.86</inf>, Ca<inf>0.57</inf>, Fe<inf>0.62</inf>)(Al<inf>7</inf>O<inf>29.03</inf>) (Si<inf>29.07</inf>O<inf>29.03</inf>)·z·H<inf>2</inf>O for Urgun deposit sample. • (Na<inf>2.14</inf>, K<inf>1.64</inf>, Mg<inf>0.53</inf>, Fe<inf>0.64</inf>, Ti<inf>0.19</inf>)(Al<inf>6.38</inf>O<inf>28.95</inf>) (Si<inf>30.59</inf>O<inf>28.95</inf>)·z·H<inf>2</inf>O for Bayan Zurh Black Mountain sample. • (Na<inf>3.59</inf>, K<inf>1.17</inf>, Ca<inf>1.17</inf>, Mg<inf>0.68</inf>, Fe<inf>0.30</inf>)(Al<inf>6.58</inf>O<inf>28.90</inf>) (Si<inf>28.65</inf>O<inf>28.90</inf>)·z·H<inf>2</inf>O for Mandalovoo sample.","PeriodicalId":379676,"journal":{"name":"International Forum on Strategic Technology 2010","volume":"26 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2010-12-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Crystal structural investigations of Mongolian natural zeolites\",\"authors\":\"G. Batdemberel, S. Chadraabal, P. Jargalbat, D. Sangaa, B. Namjildorj\",\"doi\":\"10.1109/IFOST.2010.5667928\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"We have studied zeolitic rocks discovered in Mongolia using electron microscopy (SEM), X-ray fluorescence (XRF), X-ray diffraction (XRD) methods. SEM, XRF and XRD measurements were carried out in the Max Plank Institute of Stuttgart, Germany. Our samples are collected from Mongolian deposits: Tsagaan tsav, Tushig uul, Urgun deposit, Bayan Zurkh Black Mountain and Mandal ovoo. Firstly, we have made chemical element analysis by using X-ray fluorescence spectroscopy which gives chemical contents of samples from all zeolite deposits. Comparing contents of above 5 deposits samples shows us that zeolite of Tushig Mountain, Dornogobi, is has the highest content of potassium and can be identified in potassium clinoptilolite- K (2.56 at %), others belong to clinoptilolite- Na. The main cations are K,Na,Ca,Mg,Fe,Ti for all the samples from the above mentioned deposits. Also, the (Si Al)/O ratio shows that the Mongolian zeolites have comparatively good qualities. We made X-ray phase analysis study on X-ray powder diffractometer Bruker-Axes D8 and refined the X-ray diffraction spectra by using ≪Match! Crystal Impact≫ program. As a result, we established that these zeolites are Na and K type of clinoptilolite with monoclinic symmetry (C2/m). Finally, the exact crystallochemical formula of clinoptilolites can be written as the next: • (Na<inf>2.02</inf>, K<inf>1.81</inf>, Mg<inf>0.49</inf>, Ca<inf>0.46</inf>, Fe<inf>0.36</inf>)(Al<inf>6.28</inf>O<inf>30.45</inf>) (Si<inf>28.47</inf>O<inf>30.45</inf>)·z·H<inf>2</inf>O for Tsagaan tsav sample. • (K<inf>2.56</inf>, Na<inf>1.69</inf>, Mg<inf>0.64</inf>, Ca<inf>0.47</inf>, Fe<inf>0.78</inf>)(Al<inf>6.39</inf>O<inf>28.15</inf>) (Si<inf>31.17</inf>O<inf>28.15</inf>)·z·H<inf>2</inf>O for Tushig Mountain sample. • (Na<inf>2.34</inf>, K<inf>1.48</inf>, Mg<inf>0.86</inf>, Ca<inf>0.57</inf>, Fe<inf>0.62</inf>)(Al<inf>7</inf>O<inf>29.03</inf>) (Si<inf>29.07</inf>O<inf>29.03</inf>)·z·H<inf>2</inf>O for Urgun deposit sample. • (Na<inf>2.14</inf>, K<inf>1.64</inf>, Mg<inf>0.53</inf>, Fe<inf>0.64</inf>, Ti<inf>0.19</inf>)(Al<inf>6.38</inf>O<inf>28.95</inf>) (Si<inf>30.59</inf>O<inf>28.95</inf>)·z·H<inf>2</inf>O for Bayan Zurh Black Mountain sample. • (Na<inf>3.59</inf>, K<inf>1.17</inf>, Ca<inf>1.17</inf>, Mg<inf>0.68</inf>, Fe<inf>0.30</inf>)(Al<inf>6.58</inf>O<inf>28.90</inf>) (Si<inf>28.65</inf>O<inf>28.90</inf>)·z·H<inf>2</inf>O for Mandalovoo sample.\",\"PeriodicalId\":379676,\"journal\":{\"name\":\"International Forum on Strategic Technology 2010\",\"volume\":\"26 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2010-12-13\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"International Forum on Strategic Technology 2010\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/IFOST.2010.5667928\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Forum on Strategic Technology 2010","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/IFOST.2010.5667928","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Crystal structural investigations of Mongolian natural zeolites
We have studied zeolitic rocks discovered in Mongolia using electron microscopy (SEM), X-ray fluorescence (XRF), X-ray diffraction (XRD) methods. SEM, XRF and XRD measurements were carried out in the Max Plank Institute of Stuttgart, Germany. Our samples are collected from Mongolian deposits: Tsagaan tsav, Tushig uul, Urgun deposit, Bayan Zurkh Black Mountain and Mandal ovoo. Firstly, we have made chemical element analysis by using X-ray fluorescence spectroscopy which gives chemical contents of samples from all zeolite deposits. Comparing contents of above 5 deposits samples shows us that zeolite of Tushig Mountain, Dornogobi, is has the highest content of potassium and can be identified in potassium clinoptilolite- K (2.56 at %), others belong to clinoptilolite- Na. The main cations are K,Na,Ca,Mg,Fe,Ti for all the samples from the above mentioned deposits. Also, the (Si Al)/O ratio shows that the Mongolian zeolites have comparatively good qualities. We made X-ray phase analysis study on X-ray powder diffractometer Bruker-Axes D8 and refined the X-ray diffraction spectra by using ≪Match! Crystal Impact≫ program. As a result, we established that these zeolites are Na and K type of clinoptilolite with monoclinic symmetry (C2/m). Finally, the exact crystallochemical formula of clinoptilolites can be written as the next: • (Na2.02, K1.81, Mg0.49, Ca0.46, Fe0.36)(Al6.28O30.45) (Si28.47O30.45)·z·H2O for Tsagaan tsav sample. • (K2.56, Na1.69, Mg0.64, Ca0.47, Fe0.78)(Al6.39O28.15) (Si31.17O28.15)·z·H2O for Tushig Mountain sample. • (Na2.34, K1.48, Mg0.86, Ca0.57, Fe0.62)(Al7O29.03) (Si29.07O29.03)·z·H2O for Urgun deposit sample. • (Na2.14, K1.64, Mg0.53, Fe0.64, Ti0.19)(Al6.38O28.95) (Si30.59O28.95)·z·H2O for Bayan Zurh Black Mountain sample. • (Na3.59, K1.17, Ca1.17, Mg0.68, Fe0.30)(Al6.58O28.90) (Si28.65O28.90)·z·H2O for Mandalovoo sample.