利用SEM，XRD和FTIR研究四种化学预处理对楸木木屑酶解的影响

利用 NaOH ,Ca（OH）2,H2 SO4和 HCl 四种溶液对楸木木屑进行化学预处理,发现两种碱预处理均能显著提高楸木木屑的酶解效率。采用扫描电镜（SEM ）,X 射线衍射（XRD）和傅里叶红外光谱（FTIR）对四种化学预处理后的楸木木屑进行观察和分析。SEM 观察发现,四种化学预处理对楸木木屑的纤维表面均有不同程度的破坏与侵蚀,其中 Ca（OH）2的破坏效果最为明显。XRD 谱图表明,碱预处理对楸木木屑纤维素的非晶体结构产生破坏,导致其结晶度升高,而经过酸预处理后楸木木屑纤维素的结晶度没有明显变化。FTIR 谱图显示,酸碱预处理对楸木木屑中半纤维素和木质素的分子结构均有不同程度的破坏,碱预处理过程中木质素的高效溶出可能是楸木木屑酶解效率显著提高的主要原因。     

Characterization of diamond-like carbon films by SEM, XRD and Raman spectroscopy

Diamond-like carbon films were deposited by electrolysis of a water-ethanol solution on Cu at low voltages (60-100 V) at 2 mm interelectrode separation. The films were characterized by scanning electron microscopy (SEM), X-ray diffractometer (XRD) and Raman spectroscopy. The films were found to be continuous and compact with uniform grain distribution. Raman spectroscopy analysis revealed two broad bands at ∼1350 and ∼1580 cm⁻¹. The downshift of the G band of graphite is indicative of the presence of DLC. For XRD analysis, the three strong peaks located at 2θ values of 43.2°, 74.06° and 89.9° can be identified with reflections form (1 1 1), (2 2 0) and (3 1 1) plane of diamond.     

交联淀粉微球酶降解过程的FTIR和XRD分析

以可溶性淀粉为原料,N,N′-亚甲基双丙烯酰胺为交联剂,采用反相悬浮聚合得到了一种交联淀粉微球(CSM)。为了深入了解交联淀粉微球(CSM)的降解过程,利用傅里叶变换红外光谱(FTIR)和X射线粉末衍射(XRD) 等光谱分析手段,对可溶性淀粉、CSM及其CSM在模拟肠液中不同时间的降解产物进行了分析。FTIR和SEM的研究结果表明, CSM在消化液中3 h内可稳定维持其交联结构,降解后3和12 h之间1 090 cm-1处的C—O—C弯曲振动峰减弱,酰胺的Ⅰ带吸收峰和Ⅱ带吸收峰强度的减弱说明了淀粉分子链被降解, 交联结构开始解聚,12 h后酰胺的Ⅰ带吸收峰和Ⅱ带吸收峰完全消失,说明交联结构已完全被除去;XRD结果表明,CSM在消化液中降解12 h后的情况与可溶性淀粉的降解情况相似,非结晶性部分被分解,结晶度随降解过程的进行而提高,但是仍然小于可溶性淀粉的结晶度。     

酒石酸钠调控草酸钙晶体生长的SEM,XRD和FTIR研究

采用扫描电镜(SEM)、X射线衍射(XRD)和傅里叶红外光谱(FTIR)研究了凝胶体系中尿抑制剂酒石酸钠(Na₂tart)的浓度和结晶温度对草酸钙(CaOxa)晶体生长的影响。当Na₂tart浓度为0.01 mol·L-1时,体系中主要生成棱角尖锐的蔷薇花状一水草酸钙(COM)聚集体,二水草酸钙(COD)含量小于5％,此时XRD图谱上主要为归属于COM的(101),(020)和(202)晶面的衍射峰,FTIR光谱中COM晶体的羧基不对称伸缩振动ν_as(COO-)和对称伸缩振动ν_s(COO-)分别为1 618和1 317 cm-1。当Na₂tart浓度增加到0.10和0.50 mol·L-1时,COD百分含量分别增加至10％和50％,COM晶体的比表面积减小。COD含量增加后,XRD图谱上归属于COD的(200),(211),(411)和(213)晶面的衍射峰增强。环境温度的影响比浓度的影响更为显著。高温(＞47 ℃)有利于COM生成,而低温(＜27 ℃)有利于Na₂tart诱导COD。FTIR光谱中COD的ν_as(COO-)和ν_s(COO-)分别为1 647.6和1 327.7 cm-1。     

膨润土有机改性的FTIR和XRD研究

研究内容是制备有机膨润土以提高膨润土与有机相的相容性,同时观察膨润土的层状结构在有机化前后的变化情况。以钠基膨润土为原料,并用十八胺试剂作为有机插层剂取代膨润土层间的Na+,制得有机膨润土,且对其结构进行表征。FTIR和DTA-TG都证明有机插层剂已进入膨润土的层间;XRD表明膨润土的层间距由1.4增大到4.3 nm;从实验结果可知,钠化膨润土在各种指标上都比原钙基膨润土有显著的改善,如吸蓝量、膨胀容、胶质价、阳离子交换容量等。改性后的膨润土使其晶片层间的亲水环境改变为疏水环境以及增大晶片层间距离,从而有利于制备综合性能较好的复合材料。     

XRD和FTIR对沸石合成机制的光谱学解析

以粉煤灰为原料,采用优化的水热晶化一步法合成沸石。比较晶化反应过程沸石产物CEC值及化学成分的变化,推断固液体系中物质转换及元素迁移方式和途径。借助XRD,SEM,FTIR等表征反应过程沸石的晶型变化及成核特性,提出可能存在的沸石生成机制。合成产物主要为NaP1型沸石,反应24h后CEC值最大为135mmol/100g。12h后,产物中初步发现NaP1沸石相特征峰和亚晶结构,48h后出现羟基方钠石的特征弱峰。沸石生成过程涉及到固液体系间的物质流动:碱熔融作用将粉煤灰组分侵蚀进入液相体系,为沸石形成提供了原料组分,而固相体系为沸石生长提供骨架结构,液相体系和固相体系分别为晶化反应的"源"和"汇",这是液相转化机制和固相转化机制的客观反映。     

成都金沙遗址古人类与古动物牙齿的FTIR与XRD分析

利用FTIR与XRD判断成都金沙遗址古人类与古动物牙齿釉质和牙本质中羟基磷灰石受埋藏环境和成岩作用的污染程度。XRD图谱结果反映牙釉质和牙本质样品中最主要成分是羟基磷灰石,但衍射峰宽,且部分重叠,表明羟基磷灰石结晶度差。所有样品FTIR图谱中H₂O和OH-的振动带显著,PO3-₄和CO2-₃主要振动带的特征峰明显,近似现代生物羟基磷灰石。表征羟基磷灰石结晶程度的PCI指数值在2.4至4.0之间,同时利用BPI指数估算的羟基磷灰石中CO2-₃含量较高, 说明样品结晶程度不高。上述结果表明,所取的金沙遗址古人类与古动物牙釉质和牙本质中羟基磷灰石受埋藏和成岩作用的污染小。     

Pt/CNTs电催化剂制备的UV-Vis、FTIR和XRD光谱分析

采用在乙二醇溶液中添加十二烷基硫酸钠(SDS)作为稳定剂的调变乙二醇还原法,制备了高分散的碳纳米管(CNTs)负载Pt电催化剂Pt/CNTs。利用紫外-可见(UV-Vis)、傅里叶变换红外(FTIR)和X射线衍射(XRD)光谱研究了催化剂的制备过程和结构,考察了Pt/CNTs制备过程中SDS的添加对其结构和甲醇电催化氧化活性的影响。结果表明,在乙二醇溶液中PtCl2-₆与SDS形成了配合物,PtCl2-₆能够被乙二醇完全还原;超声处理后的CNTs表面接上了含氧基团,有利于Pt粒子的吸附,催化剂上不残留有SDS;Pt/CNTs电催化剂具有典型的面心立方结构,添加SDS制备的Pt/CNTs-2电催化剂Pt高度分散,粒径更小,达4.5 nm。循环伏安(CV)测试结果表明,添加SDS制备的Pt/CNTs-2电催化剂比传统乙二醇还原法制备的Pt/CNTs-1具有更高的甲醇电催化氧化活性。     

FTIR和XRD研究甲酰胺在高岭石插层复合体系中的形态及其复合物的微观结构

插层复合体系中,有机插层剂在插层的同时也可能吸附在复合物的表面或以自由态存在,对插层分子的表征将会产生较大的影响。以丙酮作淋洗剂,用FTIR及XRD技术对淋洗前后的插层复合体系监控,插层剂分子在复合体系中的可能存在形式,探讨水的作用及复合物微观结构的变化。结果显示：甲酰胺有插层、游离和吸附在复合物表面三种存在形态。3 355和3 462 cm-1处的红外振动峰归属于表面吸附的插层剂分子,3 626 cm-1的峰归属于插层的H₂O分子,在干燥后均消失。H₂O作为填充空间的分子参预了插层过程,且插入到层间,并在干燥后脱嵌。3 534 cm-1处的振动峰在淋洗前后一直存在,是由于插层的甲酰胺分子与高岭石层间形成氢键作用的结果。以丙酮作为淋洗剂,可以选择性的消除表面吸附的甲酰胺而不影响复合物的结构。插层的甲酰胺分子以C—N键垂直于层片呈单分子层排列,并通过氨基与高岭石铝氧八面体层的内表面羟基和硅氧四面体层的氧形成了两种氢键作用。     

Characterization of minerals in natural and manufactured sand in Cauvery River belt,Tamilnadu, India

The present study investigates the characterization of minerals in the River Sand (R – Sand) and the Manufactured sand (M-Sand) through FTIR spectroscopic studies. The R – Sand is collected from seven different locations in Cauvery River and M – Sand is collected from eight different manufactures around the Cauvery River belt in Salem, Erode, Tirupur and Namakkal districts of Tamilnadu, India. To extend the effectiveness of the analysis, the samples were subjected to grain size separation to classify the bulk samples into different grain sizes. All the samples were analyzed using FTIR spectrometer. The number of minerals identified with the help of FTIR spectra in overall (bulk) samples of R – Sand is 14 and of M – Sand is 13. The number has been increased while going for grain size separation, i.e., from 14 to 31 for R – Sand and from 13 to 20 for M – Sand. Among all minerals, quartz plays a major role. The relative distribution and the crystallinity nature of quartz have been discussed based on the extinction co-efficient and the crystallinity index values computed. There is no major variation found in M – Sand while going for grain size separation.     

硫氧镁化合物的水热合成、 FTIR光谱和Raman光谱表征

采用水热合成技术,于160℃时控制MgSO_4-NaOH-H_2O四元交互体系的组分,分别制得了3种不同组成的硫氧镁化合物晶体,即MgSO_4·5Mg(OH)_2·2H_2O,2MgSO_4·Mg(OH)_2和2MgSO_4·Mg(OH)_2·2H_2O。给出了这3种化合物的FTIR光谱和Raman光谱,探讨了结构与光谱峰值的关系,并用SEM对晶体的形貌进行了表征。     

FTIR, XRD, SEM and solid state NMR investigations of carbonate-containing hydroxyapatite nano-particles synthesized by hydroxide-gel technique

Nano-crystalline hydroxyapatite (HA), Ca₁₀(PO₄)₆(OH)₂ has been synthesized by a precipitate conversion technique using hydroxide gel at lower temperatures, e.g. 80 °C. HA crystallizes in hexagonal structure (space group: P6₃/m) having lattice parameters: and and around 17 nm in crystallite-size for the 80 °C-heated sample. SEM micrographs show hexagonal crystallites of average particle dimensions approximately 50×20 nm for 80 °C heated sample. The structure analysis by XRD, FTIR, ¹H and ³¹P MAS NMR show the existence of structural disorder at the particle surface that either does not form hydrogen bonding due to lack of adequate bonding parameters or forms a very weak dipolar bonding. The structural disorder has been explained as a result of chemical interactions between the phosphate groups either with the surface adsorbed water or the hydroxyl groups at the surface of the nano-particles.     

基于XRD和SEM的含碳微细粒金矿氧化焙烧机理研究

含碳微细粒金矿是世界难处理金矿主要类型,且储量巨大,矿石中的有机碳、石墨碳能吸附溶液中的金氰络合物,因而含碳金矿在浸出之前需进行预处理。氧化焙烧是应用时间最长、可靠性和适应性最好的预处理工艺,已经成功的用于生产实践。针对传统氧化焙烧法存在生产成本高,收尘系统复杂等不足,近年来国内外学者在焙烧工艺和设备方面进行了大量的研究工作,取得了丰硕的研究成果,为氧化焙烧技术的发展注入了新的活力。但关于焙烧理论方面的研究较少,研究方法也比较单一,尤其是对于焙烧过程的相关理论研究比较薄弱,这在一定程度上影响了氧化焙烧技术的发展。焙烧时间是影响焙烧效果的关键因素,决定化学反应进度及物相变化程度。在不同时间条件下(焙烧温度650 ℃),对含碳微细粒金矿石进行焙烧-浸出试验,首次采用X射线衍射(XRD)、扫描电镜(SEM)、能谱分析(EDS)和孔结构分析等手段对含碳金矿及焙砂进行分析表征,进而揭示氧化焙烧过程中碳质物的氧化、矿石晶体结构变化、物相变化等对金浸出效果的影响机理。工艺矿物学研究表明： 矿石中主要矿物有石英、白云石、方解石、绢云母、高岭石、黄铁矿和石墨等;矿石中自然金粒度微细,以5～10 μm粒级为主,部分微粒自然金被石英、碳质组成的碎屑包裹;碳质(有机碳和石墨碳)含量高、粒度细,且与脉石矿物紧密共生。焙烧-浸出试验结果表明： 原矿直接浸出时,金浸出率仅为12.50%,碳质的“劫金”作用显著;随着焙烧时间的增加,金的浸出率先逐渐增大后变化平稳,焙烧时间为2 h时,金浸出率最高;当焙烧时间为1 h 时,绢云母发生了脱羟基变化,高岭石分解生成蒙脱石,黄铁矿氧化为赤铁矿,碳质(有机碳和石墨碳)氧化且产生CO₂,但未完全氧化,此时焙砂中石英的d₁₀₀和d₁₀₁值以及平均孔径较小,不利于浸出剂的扩散,导致金浸出率仅为58.09%;当焙烧时间为1.5 h 时,白云石开始分解,碳质已完全燃烧,产生的CO₂使微孔数量增多,有利于浸出剂的扩散,此时金浸出率增加到73.34%;当焙烧时间为2 h时,白云石分解较完全,焙砂中有MgO生成,此时焙砂中石英的d₁₀₁值达到最大值(4.255 03 nm),焙砂松散密度变大且孔容和平均孔径达到最大值,分别为0.009 954 cm3·g-1和6.640 80 nm,焙砂中产生的微孔最多,增加了浸出剂的扩散通道,有利于金的浸出,金浸出率也达到了最大值(91.28%);当焙烧时间为3 h时,焙砂表面生成Ca₂SiO₄和CaSO₄等在高温时易形成低熔点物质,发生微弱的烧结现象,导致颗粒内部的微孔被填充、闭合,微孔减少,孔容和平均孔径降低,内部结构变得致密,不利于浸出剂的扩散,同时造成金的浸出率下降。     

XRD,XPS, SEM/EDX and broadband impedance spectroscopy study of pyrophosphate (LiFeP2O7 and Li0.9Fe0.9Ti0.1P2O7) ceramics

LiFeP₂O₇ and Li_0.9Fe_0.9Ti_0.1P₂O₇ were synthesised by solid-state reaction and ceramics were sintered. The structure of compounds was studied in the temperature range 300–700 K by X-ray diffraction. Ceramics’ surfaces were investigated by scanning electron microscope. Binding energies of Fe 2p, P 2p and O 1s core levels at ceramics’ surfaces have been determined by X-ray photoelectron spectroscopy and different valence states of Fe and P were detected. Elemental compositions of the compounds were studied by energy dispersive X-ray spectrometer. Impedance spectroscopy was performed in the frequency range 10 Hz–3 GHz and in the temperature interval 400–700 K. The changes of the activation energy of ionic conductivity at 528 and 550 K for LiFeP₂O₇ and Li_0.9Fe_0.9Ti_0.1P₂O₇, respectively, were found. The phenomena can be related to disordering in the unit cells of the compounds.     

FTIR，XPS和SEM研究聚羧酸盐分散剂在吡唑醚菌酯颗粒表面的吸附性能

采用傅里叶变换红外光谱、X射线光电子能谱和扫描电子显微镜相结合的方式，从微观角度研究梳状聚羧酸盐分散剂在吡唑醚菌酯颗粒表面的吸附性能，为聚羧酸盐分散剂在吡唑醚菌酯悬浮剂中的应用提供理论依据。研究结果表明：吡唑醚菌酯吸附聚羧酸盐分散剂后，红外谱图未出现新的吸收峰，聚羧酸盐分散剂与吡唑醚菌酯之间主要是物理吸附，范德华力是聚羧酸盐分散剂与吡唑醚菌酯颗粒表面结合的主要作用力。吡唑醚菌酯颗粒吸附聚羧酸盐分散剂后，吡唑醚菌酯颗粒界面的N和Cl电子峰强度减弱，C和O电子峰强度明显增强，还出现了Na的电子峰，这主要是聚羧酸盐分散剂中C，O和Na的贡献，说明聚羧酸盐分散剂在吡唑醚菌酯颗粒表面形成了良好的吸附。并以Cl元素为特征元素，计算出聚羧酸盐分散剂在吡唑醚菌酯颗粒表面的吸附层厚度约为1.22 nm。用扫描电子显微镜研究了样品的形貌，吸附聚羧酸盐分散剂后，原本光滑的吡唑醚菌酯颗粒表面吸附了很多细小的颗粒，且有序分布，这是由于分散剂疏水集团对吡唑醚菌酯颗粒形成了包覆，亲水基团充分外露，从而有效阻止吡唑醚菌酯颗粒间的团聚，提高了吡唑醚菌酯悬浮剂的物理稳定性。     

XRF,PXRD和FTIR的广藿香主要组分测定与表征

中药的质量控制和评价在现代化医学发展中起着至关重要的作用。为了客观和高精度的鉴别中药材特性,实现对中药材质量稳定性的控制,利用XRF,PXRD和FTIR对广藿香的主要组分及微结构进行测定,建立了基于XRF,PXRD和FTIR鉴别中药材主要组分及产地特征的新方法。实验结果表明,广藿香中含有K,Ca,Cl,Si和P等多种元素,独有的元素特征谱是广藿香形成药效好的道地药材的部分物质基础。广藿香含有大量的晶态物质及少量非晶态物质,且Ca在其中以CaC_2O_4·H_2O状态存在,被检样品中该晶体物质含量的多少与相关锐峰的强弱成正比。对FTIR谱峰进行了归属与分析,提供了醇类、黄酮及草酸钙等物质的化学组分信息。该法联用XRF,PXRD和FTIR技术从元素、原子和分子微观层面客观地表征了广藿香主要组分及微结构的相关信息,避免了单独使用某种方法的片面性,能避免因复杂的前处理导致样品固有组分的改变,具有快速、简洁、再现性好及易于接受等优点,为广藿香及其他中药材的质量控制和品质评价提供一种新方法。     

新阳炼焦煤结构的FTIR和XPS谱学表征

认知煤中主要元素的结构与赋存是获取煤结构参数的基础,对构建煤结构模型,研究煤的反应特性,合理利用煤炭资源具有重要意义。目前煤结构研究多是针对中低变质程度煤的,对炼焦煤结构研究较少,炼焦煤的结构模型尚未见报道。应用FTIR对新阳炼焦煤中羟基基团、脂肪结构、芳香结构、含氧官能团及杂原子结构进行谱学表征,通过XPS解析煤中氮和硫的赋存形式,掌握炼焦煤中主要元素的禀赋特征。结果表明： 新阳煤中与芳香环上的π电子形成的羟基π氢键是羟基的主要存在形式,多聚体是煤结构中缔合结构的具体表现;次甲基、甲基、亚甲基的含量依次增加,亚甲基和次甲基含量占煤中脂肪烃总量的82.05%,煤中烷基侧链较多;苯环二取代、苯环三取代是煤中芳香烃的主要结构,占芳香烃总量的86.74%;含氧官能团中,羟基和羰基是主要组成基团,羧基和醚基含量不足10%。新阳煤中硅的含量比较丰富,主要以Si-O-Si和Si-O-C的形态赋存。吡啶、吡咯和氮氧化物为氮的主要存在形式,绝大多数氮分布于煤分子结构单元的边缘;噻吩硫是煤中有机硫最主要的赋存形式,超过有机硫总量的60%,砜和亚砜的含量次之,硫醇和硫醚的赋存最少。     

Microstructural and magnetic characterization of dusts from a stone crushing industry in Birbhum, India

Stone dust sample collected from a stone crushing industry situated at Muhammad Bazar in Birbhum, India, is studied for its physical characterization using various techniques. Morphology and compositional analysis of the stone dust by scanning electron microscopy (SEM) reveal that the dust is an agglomeration of many tiny particles (0.32-2.12 μm), mostly having sharp edges, as well show microstructure heterogeneity. Elements present in the sample are detected by energy dispersive X-ray spectrometry (EDX). The X-ray diffraction (XRD) pattern analysis shows that the sample mainly contains minerals like anorthite, augite, esseneite and albite. An overall antiferromagnetic interaction in this sample has been indicated by the nature of the thermal dependence of magnetization. The remnant magnetization study apparently indicates two magnetic transitions at low temperatures. ⁵⁷Fe Mössbauer spectroscopy has been employed to detect different possible iron sites as well as to estimate the respective site population. In general, Mössbauer spectroscopic results corroborate the observations made through XRD analysis in general.     

Micro‐Raman spectroscopy and VP‐SEM/EDS applied to the identification of mineral particles and fibres in histological sections

Histological sections of a patient affected by an important respiratory disease were analysed firstly by optical microscope(OM)—crossed polarisers—to identify the presence of incorporated inorganic particles, with particular attention to the fibrous ones. Then, the particles/fibres that were found were studied both with micro‐Raman spectroscopy and variable‐pressure scanning electron microscopy with energy‐dispersive spectroscopy (VP‐SEM/EDS). The two techniques allowed the in situ characterisation of the inorganic phases without disintegration of the organic matter. Micro‐Raman spectroscopy was able to identify the vibrating chemical groups of the mineral phase associated with the inorganic grain while the crystalline structure was preserved by the biological system. The VP‐SEM/EDS characterisation, defining the elemental chemical composition of the analysed particle/fibre, allowed confirmation of the mineral phase deducible from spectroscopic data or its identification with certainty when the spectroscopic data were not exhaustive. Copyright © 2009 John Wiley & Sons, Ltd.     

Effect of proton donors on the intramolecular coordination C=O→Si–F in (acyloxymethyl)trifluorosilanes. Ab initio,DFT and FTIR study,QTAIM analysis

The intramolecular С=O→Si coordination in H‐complexes of (acetoxymethyl)trifluorosilane and (benzoyloxymethyl)trifluorosilane with proton donors HCl, PhOH, MeOH, and CHCl₃ was investigated by density functional theory and second‐order Møller‐Plesset perturbation theory (MP2) methods. Interrelation and mutual influence of the intramolecular coordination bond С=O→Si and intermolecular hydrogen bonds C=O···H and Si–F···H in H‐complexes was established using the AIM and NBO analyses. The С=O→Si coordination is weakened by the C=O···H hydrogen bonding but enhanced by the Si–F_ax···H hydrogen bonding. The structure of H‐complexes of (acetoxymethyl)trifluorosilane with proton donors in solution was determined by comparing the ν(C=O) and ν(Si–F) frequencies calculated using the conductor‐like polarizable continuum model and their experimental Fourier transform infrared values. Copyright © 2014 John Wiley & Sons, Ltd.