不同分子质量木质素磺酸钠对煤粉的分散作用研究

应用超滤分级方法，将木质素磺酸钠分成不同分子量范围的级分。傅立叶红外光谱（FTIR）分析结果表明，分子量为5 000～10 000的木质素磺酸钠分子中亲水基团如羟基、酚羟基、磺酸根质量分数最大，随着分子量的增加，亲水基团质量分数降低。实验结果发现分子量为10 000～50 000的木质素磺酸钠级分在煤粒表面的吸附等温线近似为L型，吸附量较大，并且使煤粒的表面动电电位（ζ电位）达到-52 mV，在各个级分中对盘江煤具有最好的分散降黏作用。进一步得出结论，分散剂的分散降黏作用与其在煤粒表面的吸附量和ζ电位的高低密切相关。     

脂肪胺聚氧乙基醚结构的核磁共振波谱表征

从工业和合成产品脂肪胺聚氧乙基醚中用TLC和快速色谱(FC)分离精制得到6个脂肪胺聚氧乙基醚模型化合物，用^1H、^13C、gCOSY，gHSQC和gHMBC等核磁共振波谱和质谱表征了其结构，完成了^1H和^13C NMR谱带的归属，为本系列化合物的结构和EO分布鉴定提供了依据，并给出了计算本系列化合物叔胺值的方法。考察了酸性条件对脂肪胺聚氧乙基醚化合物相关基团化学位移的影响。     

二正丁基锡(Ⅳ)双(二茂铁硫代甲酸酯)配合物的合成、结构表征及其体外抗癌活性研究

以二茂铁硫代甲酸和二正丁基氧化锡反应，合成了未见报道的二正丁基锡新型配合物(n—Bu)2Sn(FeCOS)2[Fe=(η^5-C5H5)Fe(η^5-C5H4)]．通过元素分析、红外光谱和核磁共振(^1H，^13C，^119Sn)谱等分析手段对配合物的组成和结构进行了表征．用X射线单晶衍射分析法测定了该配合物的晶体结构．晶体属四方晶系，空间群P421m，晶胞参数α=2．3351(7)nm，6=2．3351(7)nm，c=0．5870(2)nm，V=3．2005(18)nm^3，Z=4，De=1．501Mg／m^3,μ（Mo Kα)=1．823mm^-1,F(000)=1464．最终可靠因子R1=0．0733，wR2=0．1173．配合物中锡原子与2个S原子、2个O原子和2个C原子形成扭曲的八面体几何构型．体外抗癌活性测试结果表明，该配合物对人体的白血病HL-60、结肠癌HCT-8、胃癌BGC-823和鼻咽癌KB等癌细胞均有很好的抑制能力．     

用~1H 和~(13)C谱研究煤超临界流体抽提抽出油的组成结构

用~1H和~(13)C核磁共振谱研究了阜新烟煤,昭通褐煤和桦川泥煤超临界流体抽提抽出油的组成结构。~(13)C谱可以直接测定分子骨架碳原子的分布,由~1H 和~(13)C 谱脂肪区的信号直接算出烷基侧链H/C原子比。根据~1H 谱、元素分析、平均分子量和羟基测定,采用Bartle的方法计算了三种煤抽出油色谱馏分的平均分子结构参数。     

C(4)取代紫杉醇类似物的定量构效关系研究

用量子化学B3LYP／6-31G方法计算了23个C（4）取代紫杉醇类似物的结构,用遗传算法（GFA）对能量、电性、拓扑及热力学等类型的278个结构描述符进行筛选,并回归建立其抑制人体结肠癌细胞HCT-116活性的定量构效关系（QSAR）．QSAR方程含分子体积Vm、分子分支度指数CHI-O、分子中带正电荷原子的溶剂可积面积与其所带电荷之积的加和值Jurs-PPSA-3以及分子表面积S4个结构描述符．方程的拟合相关系数的平方R^0及交叉验证系数Q^2分别为0．956和0．913,所得QSAR具有可信的预报能力．由优化后的几何构型知,C（4）取代基、C（13）侧链和2-OBz三基团共同形成疏水腔,C（4）取代基的改变影响C（13）侧链的电子结构．C（13）连接的18号O原子的负电荷越大、3’位连接的NHBz基团的极性越小活性越高;C（4）取代基若为吸电子基对活性不利;适当增大分子体积、表面积和疏水性,保持一定的分支度对活性有利．     

聚苯胺在一些有机溶剂中溶解性

本文通过改变反应条件用化学方法制得了不同分子量的聚苯胺，考察了它们在有机溶剂中的溶解性．实验结果表明：分子量的大小是影响它们在有机溶剂中溶解度的主要因素，能在有机溶剂中溶解的只是聚苯胺中分子量较小的级分．我们还用聚苯胺（［η］＝０．４９ｄｌ／ｇ）与－ＣＯＣＩ封端的果对苯二甲酰对苯二胺（ＰＰＴＡ）进行嵌段共聚，经过产物的元素分析与计算结果比较，确定出特性黏数为０．４９ｄｌ／ｇ的聚苯胺平均分子量．     

固体核磁碳结构参数的修正及其在煤结构分析中的应用

为消除~(13)C CP/M AS/TOSS NM R测试中碳核NOE效应,获得相对准确的碳结构参数,考察了不同模型化合物的碳核NOE效应强度。结果表明,不同模型化合物碳谱分峰拟合的测试值与样品碳结构参数的理论值之间存在明显误差,其中,脂肪碳在25%-125%、芳香碳为4%-50%,NOE效应在固体核磁碳谱测试中影响显著。为此,将模型化合物脂肪碳和芳香碳的实测值和理论值进行回归分析,得到非线性回归方程。用该方程对9,10-二甲基蒽进行碳结构修正,发现修正后脂肪碳实测值与理论值之间误差由不修正时的119.60%减小至7.84%,芳香碳误差为由不修正时的-17.10%到1.11%,修正后误差均在10%以内;同时用该回归方程修正了不同煤的碳结构参数,发现不同煤未修正的H/C原子比与其元素分析H/C原子比误差在45%-53%,修正后误差只有4%-13%,与元素分析结果具有一致性,表明非线性回归方程能够方便、准确地消除固体核磁NOE效应,为煤中碳结构分析提供新的技术支撑。     

（HAINH）n（n=2—3）环状化合物的结构特征

用自洽场理论（HF）和密度泛函理论（DFT）的B3LYP方法，在6－3G的水平上对化合物（HAlNH)2和（HAlNH)3的几何结构进行优化，并分别与环丁二烯C4H4和苯分子C6H6的结构和成键方式进行比较。以B3LYP／STO－3G方法讨论其分子轨道波函数．。结果表明：C4H4和（HAlNH)2均为D2h对称，前者为长方形结构，形成两个孤立的π键，而后者为菱形结构，形成一个π4^4键。C6H6和（HAlNH)3分子点群分别为D6h和D3h，并均形成一个π6^6键，成键原子对分子轨道的贡献不同，其中C原子是完全等价的。而Al和N原子各不相同，N原子比Al的贡献要大得多。     

合成气制低碳烯烃用Fe／AC催化剂的制备及性能表征

 研究了以活性炭（AC）作为载体制备的铁基催化剂，通过对不同铁盐、活性炭和助剂的筛选，研制出对合成气转化为低碳烯烃具有高活性和高选择性的催化剂．对反应前及反应过程中催化剂体相结构的XRD测试结果表明，Fe－Cu－K／AC催化剂在反应前主要由α－Fe，Fe3O4和Cu0组成，经合成气反应后主要由α－Fe，Fe5C2，Fe7C3，Cu0和K2O组成．Fe－Mn－K／AC催化剂的晶体结构主要以Fe嵌入MnO中形成的（Fe，Mn）O结构存在．实验中得出的α－Fe，FexCy及（Fe，Mn）O与激光热解法制备的催化剂的的晶体结构相似．对催化剂的制备方法进行了筛选，考察了不同助剂Cu，Mn，Si和K等元素对催化剂性能的影响．结果表明，以草酸铁为铁源，椰壳炭为载体制备的Fe－Mn－K／AC催化剂的催化效果最佳，在空速600h－1，压力1．5MPa和温度320℃条件下，CO转化率可达97．4％，C＝2～C＝4选择性可达68．0％．     

二氧化硅纳米粒子表面修饰及其表征

采用溶胶-凝胶法合成粒径在50—150nm范围内的二氧化硅（SiO2）纳米粒子。用甲基丙烯酸-3-（三甲氧基硅基）丙酯（MPS）对SiO2纳米粒子表面进行修饰，使其表面接枝能参与自由基聚合反应的碳碳双键基团。用元素分析、FTIR、^13C CP／MASNMR和^29Si CP／MASNMR等手段对修饰过的SiO2纳米粒子进行表征，以确证MPS接枝在SiO2纳米粒子上。分析修饰过的SiO2纳米粒子的^29Si CP／MASNMR和FTIR谱图，还可初步推断MPS接枝在SiO2纳米粒子表面的机理：MPS首先发生水解缩合反应形成低聚物，然后通过氢键作用吸附到SiO2纳米粒子表面，最后MPS低聚物中未缩合的硅羟基与SiO2纳米粒子表面的硅羟基发生缩合反应。     

NMR characterization of humic acid fractions from different Philippine soils and sediments

Humic acids from a peat soil, an agricultural soil and a lake sediment from the Philippines were fractioned by sorption chromatography on cross-linked dextran gels (Sephadex¹). The NMR spectra of these fractions have sharp, well resolved bands which can be attributed to lignin-like structures, carbohydrates and aliphatic groups. Similar bands have been observed in the NMR spectra of humic acid fractions from other environments; however, the chemical shifts of some of the lines vary from one humic acid to another. These lines appear to arise from well defined, partially decomposed plant components and probably are diagnostic of the types of plants that decomposed into these humic acids. The lines in the carbohydrate region are the best resolved and may prove to be the most useful in identifying the plant precursors of any particular humic acid fraction.     

土壤胡敏酸的^13C核磁共振研究

胡敏酸(HA)是土壤有机质的重要组分,其结构性质与土壤形成和肥力特性有密切关系,长期以来一直是土壤化学研究的难点和重点之一。NMR是研究HA结构的有效手段。自Bar-ton和Schnitzer(1963)首次用~1H NMR研究土壤有机质以来,国外已先后应用~1H、~(13)C NMR和CP-MAS-~(13)C NMR等对土壤及其它来源的HA进行了许多研究,并取得引人注目的进展。但在国内,这方面研究还刚刚开始。本文应用~(13)C NMR方法对东北几种主要耕作土壤以及泥炭和猪粪的HA进行了结构表征,为土壤腐殖酸化学的基础研究提供了资料。     

Humic acid fractionation upon sequential adsorption onto goethite

Mineral-humic complexes are commonly distributed in natural environments and are important in regulating the transport and retention of hydrophobic organic contaminants in soils and sediments. This study investigated the structural and conformational changes of humic acid (HA) and mineral-HA complexes after sequential HA adsorption by goethite, using UV-visible spectroscopy, high performance size exclusion chromatography (HPSEC), Fourier transform infrared (FT-IR) spectroscopy, and solid-state 13C nuclear magnetic resonance (NMR) spectroscopy. The HA remaining in the solution after adsorption showed low polarity index values ((N+O)/C), which indicates that polar functional moieties are likely to adsorb on the goethite surface. In addition, we observed decreased E4/E6 and E2/E3 ratios of unbound HA with increasing number of coatings, implying that aliphatic rich HA fractions with polar functional moieties readily adsorb to the goethite surface. According to IR spectra, carbohydrate carbon would be the important fractions associated with goethite. NMR spectra provided evidence for HA fractionation during adsorption onto the mineral surface; that is, aliphatic fractions were preferentially adsorbed by goethite while aromatic fractions were left in solution. Relatively small molecular weight (MW) HA fractions had a greater affinity for the goethite surface based on analyses of the HPSEC chromatograms, which differs from the results reported in the literature. Finally, our results suggest that the polar aliphatic fractions of HA were mainly adsorbed to goethite via electrostatic attraction and/or ligand exchange reactions.     

土壤腐殖质各组分红外光谱研究

土壤腐殖质是土壤中所特有的一类特殊的高分子化合物,具有重要的肥力和环境调节功能。其中胡敏素的提取和纯化很困难,从而限制了对其性质和结构的研究。为揭示胡敏素的结构性质,本研究按Pallo分组,将胡敏酸(HA)分为焦磷酸钠提取的胡敏酸(HAP)、氢氧化钠提取的胡敏酸(HAS);富里酸(FA)分为焦磷酸钠提取的富里酸(FAP)和氢氧化钠提取的富里酸(FAS);胡敏素(HM)分为铁结合胡敏素(HMi)、粘粒结合胡敏素(HMc)和不溶性胡敏素(HMr)三个组分,采用红外光谱法对黑土、草甸土以及黑土底土加入大量玉米秸秆培养后腐殖质各组分的结构特征进行研究。腐殖质各组分按Pallo法分组。结果表明:铁结合胡敏素(HMi)、粘粒结合胡敏素(HMc)与胡敏酸(HA)、富里酸(FA)具有相似的光谱特征,但存在明显差异。黑土、草甸土中HMi和HMc的脂族性强于HA和FA;HMi与HMc相比,HMi具有较高的脂族性。黑土中氢氧化钠提取的胡敏酸(HAS)的脂族性强于焦磷酸钠提取的胡敏酸(HAP);NaOH提取的富里酸(FAS)的脂族性强于Na4P2O7提取的富里酸(FAP)。草甸土中HAP的脂族结构较多,而HAS脂族结构相对较少。在培养土中,新形成的FA脂族性强于HA、HMi和HMc组分。新形成的HMc脂族性强于HMi和HMc的脂族性强于HAP,而弱于HAS。     

Spectroscopic and chemical characterizations of molecular size fractionated humic acid

A sample of humic acid was divided by ultrafiltration into five fractions of different molecular size (F1; 300 000: F2; 100 000-300 000: F3; 50 000-100 000: F4; 10 000-50 000: F5; 1000-10 000 daltons). Characterization by IR, and CPMAS C-13 NMR spectroscopy indicated that the molecules of the fraction of >/=100 000 daltons were primarily aliphatic, while the smaller molecules of the >/=10 000 dalton fraction were predominantly aromatic. Titration (pH) data were consistent with an increase in the number of carboxylate groups per unit mass as molecular size became smaller. A comparative study with unpurified and purified (by treatment with ion exchange elution, acid precipitation and alkaline dissolution) humic acid samples showed chemical alteration with some loss of carboxyl groups in the humic acid.     

裂解技术研究Pahokee泥炭腐殖酸的组成和来源特征

通过原位裂解．色谱．质谱(Py-GC-Ms)技术,应用直接裂解和原位裂解甲基化两种手段,从分子水平研究了Pahokee泥炭腐殖酸的来源和组成特征,结果表明：两种裂解方式都得到大量芳香结构的裂解产物,少量游离脂肪酸和脂肪链状结构裂解产物,以及一些含氮或呋喃结构的裂解产物,表明Pahokee泥炭腐殖酸的形成主要与陆生木质素有关,而微生物和其他物质对腐殖酸形成也有重要贡献。     

Comparability of composition of carbon functional groups in humic acids between inverse-gated decoupling and cross polarization/magic angle spinning 13C nuclear magnetic resonance techniques

To find a certain relation between the composition of carbon functional groups of humic acids derived from liquid state ¹³C nuclear magnetic resonance (NMR) spectra acquired with inverse-gated decoupling (IGD), known as a quantitative pulse sequence, and that by solid-state ¹³C NMR with cross polarization/magic angle spinning (CPMAS) techniques, fifteen soil humic acid samples with a wide range of aromaticity were analyzed. Relationships between the proportions of humic acid carbon as alkyl, O-alkyl, and aromatic carbon assessed by the two methods could be regressed to y = ax (r = 0.932-0.956; P < 0.005), respectively. The contents of alkyl, O-alkyl, and aromatic carbon assessed by CPMAS method were larger than those found by IGD method. However, the differences between the two methods were small and exclusive regression to y = x was also significant (r = 0.775-0.941; P < 0.005). Aromaticity calculated from ¹³C CPMAS NMR data also did not differ significantly from those computed from ¹³C NMR spectra with IGD. These observations indicated the comparability of the relative content of carbon functional groups in humic acids except for carboxyl and carbonyl carbon.     

Evaluation of copper(II)-binding ability of humic acids in peat using sulphopropyl-Sephadex C-25 cation exchanger

A method for the determination of copper(II) complexes with humic acids was developed by batch operation with the cation exchanger sulphopropyl-Sephadex C-25 (C-25). The copper-binding ability (conditional stability constants and copper-complexing capacities) of humic acids which were extracted from peat in Hokkaido was evaluated. A solution containing copper(II) ions and humic acids was shaken with the C-25 exchanger. The copper-humic acid complexes remained in the supernatant and the uncomplexed free copper ion was retained on the C-25. The copper-humic acid complexes were determined by flame atomic absorption spectrometry. The copper-binding ability of nitrilotriacetic acid (NTA) as a model ligand was similarly determined with a Scatchard plot. The conditional stability constant obtained at pH 4.5 was in good agreement with the reported value. The copper-binding abilities of the humic acids from peat were estimated using a Scatchard plot adopting a two-site model. The functional groups in the humic acids which contribute to the complexation with copper were investigated by conductimetric and pH titration, and the relationship between the copper-binding sites and functional groups in the humic acids was investigated.     

High-performance liquid chromatography (HPLC)-size exclusion chromatography (SEC) for qualitative detection of humic substances and dissolved organic matter in mineral soils and peats in Lithuania

High-performance liquid chromatography (HPLC) with size exclusion (SEC) separation function was used to isolate and examine the molecular mass (MM) distributions and polydispersity of humic substances (HSs) and dissolved organic matter (DOM) from mineral soils and peats. The aim was to improve their detailed characterisation and to inform of their soil carbon (C) sequestration and environmental quality. This is the first study conducted in Lithuania in which HSs and DOM, separated from two soil types, have been used to characterise soil at the molecular level. The HPLC-SEC, as a separation method, was coupled with diode-array detection (DAD), thus enabling the separation of molecular fractions. Results showed that HPLC-SEC can be used to determine the MM of HSs in soil, provided that the relation between retention time and MM is known and a suitable method for fitting the HS peak is available. The UV-spectra analysis showed that DOM has a larger MM (M_w = 2439–3436 Da), which contains more aliphatic C. The HS fraction has a smaller MM (M_w = 2776 Da), with aromatic structures that reflect a higher aromaticity. Separated fractions had characteristic MMs of humic acid (HA) and fulvic acid (FA) and DOM. The HSs separated from peat samples were characterised by higher aromaticity, humification and stability. The HSs extracted from mineral soil samples showed a higher degradability level. The results also show the MM distribution and polydispersity of HS and DOM fractions (M_w/M_n = 1.009–1.252) are relatively homogenous in both soil types. Findings confirm that chromatographic and spectrometric parameters can be used for characterisation of both HSs and DOM, and for detecting changes in organic matter quality. Moreover, they can also be used for a further understanding the C-cycle and could be applied for enhancing soil C-sequestration and informing environmental quality management.