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ÓÉͼ2¿ÉÖª£¬ÑùÆ·Ö»ÓÐÔÚ712 cm-1ºÍ876 cm-1´¦ÓÐÇ¿ÎüÊշ壬ÕâÓë·½½âʯµÄÌØÕ÷·åλ (712 cm-1¡¢876 cm-1)ÏàÎǺϡ£Í¨¹ýͼ3¿ÉÖª³öÏÖµÄÌØÕ÷ÑÜÉä·åλÖÃ(2¦È=23.0¡ã¡¢29.4¡ã¡¢39.4¡ã¡¢47.5¡ã)£¬Óë±ê×¼PDF¿¨(¿¨ºÅ£º05-0586)¶ÔÕÕ£¬·Ö±ð¹éÊô·½½âʯµÄ(012)¡¢(104)¡¢(113)¡¢(018)¾§Ã棬½øÒ»²½Ö¤Êµ²úÎïΪµ¥Ò»·½½âʯ£¬ÕâÓëÆäFT-IR±íÕ÷½á¹ûÏàÎǺϡ£´Óͼ4¿ÉÒÔ¿´³öÔÚ´¿Ë®ÌåϵÖÐCaCO3ÒÔ¹æÔòµÄ²ã×´½á¹¹¾Û¼¯ÔÚÒ»Æð£¬³ÊÁ¢·½ÌåÐÎ×´£¬¶øÇÒÆäÁ£¾¶±ß³¤Îª3-6 ¦Ìm£¬·Ö²¼½ÏΪ¾ùÔÈ¡£×ÛÉϱíÃ÷£ºÔÚ´¿Ë®ÌåϵÖÐÉú³ÉµÄ̼Ëá¸Æ¾ùΪµ¥Ò»µÄ·½½âʯ¡£ ´Óͼ5¿É¼ûÔÚ712 cm-1¡¢745 cm-1¡¢ºÍ876 cm-1¾ùÓгö·å£¬ÕâÓë·½½âÊ¯ÌØÕ÷ÑÜÉä·åºÍÇòö±Ê¯ÌØÕ÷ÑÜÉä·å (745 cm-1¡¢876 cm-1)ÏàÎǺϡ£¸÷ÌõÆ×Ïß·åµÄÇ¿¶È²»Í¬£¬¿ÉÄÜÊÇÓÉÓÚ²»Í¬pHÖµÌõ¼þÏÂÐγÉÇòö±Ê¯º¬Á¿²»Í¬ÒýÆðµÄ¡£±íÃ÷²»Í¬pHÖµÌåϵÏÂËùµÃµÄ̼Ëá¸Æº¬Óз½½âʯºÍÇòö±Ê¯¾§ÐÍ£¬ÇÒÇòö±Ê¯µÄº¬Á¿¿ÉÄܲ»Í¬¡£ |
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hookhans
Ìú¸Ëľ³æ (ÖøÃûдÊÖ)
Farmer
- ·ÒëEPI: 263
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- ×¢²á: 2013-01-25
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°®ÓëÓêÏÂ: ½ð±Ò+1 2013-03-25 19:22:41
°®ÓëÓêÏÂ: ½ð±Ò+1 2013-03-25 19:22:41
| The FSEM images of the calcium carbonate aged for different times are shown in (Fig 10. It can be seen that the calcium carbonate was still in the growth state with irregular morphologies when the aging time was 0 h (image 10a) and 0.5 h(image 10c). When the aging time is 1 h, spherical like calcium carbonate with regular morphology was obtained. With the increase of the aging time to 6 h, the spherical like vaterite became to dissolve and show irregular surface. Further increase the aging time would result in the crystallization of the dissolved vaterite to cubic calcite. When the aging time reached to 12 h, the morphology of the calcium carbonate tended to be stabilized, and the content of the vaterite could be as high as 86.2%. In summary, with the increase of the aging time, the content of the vaterite in the sample decreases, and part of the vaterite became to dissolve and transfer to calcite. |

2Â¥2013-03-25 16:07:06
X1213655221
Òø³æ (³õÈëÎÄ̳)
- Ó¦Öú: 2 (Ó×¶ùÔ°)
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3Â¥2013-03-25 16:49:22
hookhans
Ìú¸Ëľ³æ (ÖøÃûдÊÖ)
Farmer
- ·ÒëEPI: 263
- Ó¦Öú: 186 (¸ßÖÐÉú)
- ¹ó±ö: 0.142
- ½ð±Ò: 7967.5
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- ºì»¨: 51
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¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï
°®ÓëÓêÏÂ: ½ð±Ò+1 2013-03-25 19:22:52
X1213655221: ½ð±Ò+50, ·ÒëEPI+1, ¡ï¡ï¡ïºÜÓаïÖú 2013-03-26 09:31:50
°®ÓëÓêÏÂ: ½ð±Ò+1 2013-03-25 19:22:52
X1213655221: ½ð±Ò+50, ·ÒëEPI+1, ¡ï¡ï¡ïºÜÓаïÖú 2013-03-26 09:31:50
|
ref. only. As shown in Fig. 2, the sample shows strong absorption peaks only at 712 cm- and 876 cm-1, which is in accordance with the characteristic peaks of calcite ((712 cm-1 and 876 cm-1). Comparison with the PDF standard card (card number: 05-0586) indicates that the diffraction peaks appeared in Fig. 3 (2¦È=23.0¡ã¡¢29.4¡ã¡¢39.4¡ã¡¢47.5¡ã) can be assigned to (012), (104), (113) and (018) facet of the calcite. This further demonstrates the product is pure calcite, consistent with the results of the FTIR. Fig. 4 shows that CaCO3 agglomerates in regular layer structure in pure water system, homogeneously distributed as cubic shape with grain size of ca. 3-6 nm. In summary, calcium carbonate forms pure calcite in pure water system. Fig. 5 shows peaks at 712 cm-1, 745 cm-1, and 876 cm-1, which is consistent with the absorption peaks of calcite and vaterite ((745 cm-1¡¢876 cm-1). The intensity difference of these peaks might be due to the content of the vaterite synthesized at different pH conditions. This demonstrates that the calcium carbonate synthesized at different pH conditions has both calcite and vaterite crystal forms , but the content of the latter might be different. |

4Â¥2013-03-25 17:59:34
hookhans
Ìú¸Ëľ³æ (ÖøÃûдÊÖ)
Farmer
- ·ÒëEPI: 263
- Ó¦Öú: 186 (¸ßÖÐÉú)
- ¹ó±ö: 0.142
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- ºì»¨: 51
- Ìû×Ó: 2088
- ÔÚÏß: 401.2Сʱ
- ³æºÅ: 2260260
- ×¢²á: 2013-01-25
- רҵ: ´ß»¯»¯Ñ§

5Â¥2013-03-25 21:49:25
X1213655221
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6Â¥2013-03-26 09:32:20














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