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关注：1
2013-05-23 12:21
求翻译：The wollastonite powder was additionally characterized by FTIR spectroscopy. The FTIR spectrum in the range from 400 to 2000 cm1 is shown in Fig. 3. The high-frequency peaks in the spectral range 800–1250 cm1 were assigned to asymmetric Si–O stretching modes within a SiO4 tetrahedron [32]. The mid-frequency ones at 6是什么意思？ 待解决
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- 离问题结束还有
The wollastonite powder was additionally characterized by FTIR spectroscopy. The FTIR spectrum in the range from 400 to 2000 cm1 is shown in Fig. 3. The high-frequency peaks in the spectral range 800–1250 cm1 were assigned to asymmetric Si–O stretching modes within a SiO4 tetrahedron [32]. The mid-frequency ones at 6
问题补充： |
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2013-05-23 12:21:38
硅灰石粉末附加特征红外光谱。
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2013-05-23 12:23:18
正在翻译，请等待...
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2013-05-23 12:24:58
wollastonite粉末描绘的是另外为FTIR分光学。 FTIR光谱在范围从400到2000 cm 1显示在。 3. 高频率峰顶在鬼范围800-1250 cm 1在SiO4四面体32之内的被分配了到不对称的SiO舒展 (方式)。 而那些在lowfrequency范围400-600 cm 1起源于舒展方式的OSiO弯曲和Ca-O中频一个在600-800 cm 1可以 (归因于Si OSi) 债券弯曲和舒展振动的相称SiO。
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2013-05-23 12:26:38
硅灰石粉体的红外光谱的特点是另外。红外光谱在 400 至 2000 厘米 1 范围如图 3 所示。高频率峰值的光谱范围在 800 — — 1250年厘米 1 被分配到不对称硅 — — O 拉伸模式内 SiO4 四面体 [32]。中频部分在 600 — — 800 厘米 1 可以归因于寺 — — O — — 债券弯曲和对称寺 — — O 伸缩振动，而那些在低频范围 (400-600 厘米 1) 起源于 O — — Si — — O 弯曲和 Ca — — O 拉伸模式。
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2013-05-23 12:28:18
wollastonite 粉此外被 FTIR spectroscopy 描绘。The FTIR spectrum in the range from 400 to 2000 cm1 is shown in Fig.3.The high-frequency peaks in the spectral range 800-1250 cm1 were assigned to asymmetric Si-O stretching modes within a SiO4 tetrahedron (32).The mid-frequency ones at 600-800 cm1 can be at
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