核磁共振法研究DTPA-BIN稀土配合物的溶液结构

用核磁共振方法研究了抗磁稀土配合物 Ln( DTPA-BIN) ( Ln=La,Y,Lu,Sc)的水溶液结构 . 1 H和1 3 C NMR谱的谱形特征表明 ,每一种配合物在水溶液中存在着两种以上不对称的异构体 ,异构体之间的差别较小 .并由 Y3+ 与 Gd3+ 离子半径的相似性推测出 Gd( DTPA-BIN)的溶液结构 ,即 DTPA-BIN分子提供 8个配位点 :3个骨架氮、 3个乙羧基氧及 2个酰胺氧 ,1个水分子占据另一个配位点 ,从而与 Gd3+ 形成了九配位结构 .溶液结构随中心金属离子半径不同而呈规律性变化

三环己基锡-2-(1,2-亚乙二硫)亚甲基-3-羰基-5-芳基-4-戊烯酸酯的结构研究

合成了 3个三环己基锡 -2 -( 1 ,2 -亚乙二硫 )亚甲基 -3-羰基 -5 -芳基 -4 -戊烯酸酯化合物 .用 IR,1 H NMR,1 3 C NMR和 1 1 9Sn NMR光谱及 X射线衍射对所合成的化合物进行了表征 .结果表明标题化合物为四配位、具有畸变四面体结构的锡酯类化合物

2,2'-二(对胺苯甲酯)-1,1'联萘的核磁共振谱解析

利用~1HNMR,~(13)CNMR谱研究了2,2’-二(对胺苯甲酯)-1,1’联萘的结构,并通过~1H-~1HCOSY,~(13)C-~1H异核相关及~(13)C-~1H异核远程相关谱进一步地确定了~1H谱和~(13)C谱中各谱峰的归属,为同类化合物的表征提供了一个依据.

玉米秸秆堆腐过程中形成富里酸的结构分析

采用傅里叶变换红外光谱及~1H和~(13)C核磁共振波谱对玉米秸秆堆腐过程中形成的富里酸(CSR FA)的结构进行了表征.结果表明,玉米秸秆腐解过程中形成的富里酸包括羧基或羰基基团、芳香结构、烷基片断和碳水化合物结构.

六氟磷酸二(2,2’-联吡啶)(2,2’-联吡啶-4,4’-二羧酸)合钌(Ⅱ)的二维核磁共振谱分析

利用核磁共振氢谱和碳谱研究了电化学探针六氟磷酸二(2,2＇-联吡啶)(2,2＇-联吡啶-4,4’-二羧酸)合钌(Ⅱ)的立体结构,并通过二维~1H~1同核相关及~1H-~(13)C异核相关技术对其氢谱和碳谱进行了归属.

丙烯酰胺－丙烯酸钠共聚物的键结构和光散射研究

用溶液聚合方法制备了一组单体含量相同、分子量不同的丙烯酰胺－丙烯酸钠（ＡＭ－ＡＡ）共聚物样品，用１３ＣＮＭＲ和常规光散射方法进行了表征．该组样品的化学组成是均一的（ＡＡ摩尔含量１６．９±１．１％），ＡＡ单体在大分子链中的序列分布为孤立、无规的，聚电解质在盐水体系中的光散射理论适用于共聚物在０．１２ｍｏｌ／ＬＮａＣｌ水溶液体系．用恒化学位下的折光指数增量代替恒盐组成的折光指数增量，可从一次常规光散射实验分别求得共聚物样品的真实、第二维利系数Ａ２和均方旋转半径〈Ｒ２〉ｚ，其关系为：

三-(2-甲基氮丙啶)氧化膦异构体的核磁共振和量子化学研究

三-(2-甲基氮丙啶)氧化膦(MAPO)为黄色油状液体,其化学性质活泼,可用作塑料、橡胶及造纸业中高分子化合物的交联剂等。本文对MAPO进行了~1H、~(13)C、~(15)N、~(31)P和~(17)O的核磁共振研究及量子化学计算。结果表明,该化合物存在4种异构体,其中2种为对映体,并得到了这4种异构体的几何构型。

核磁共振波谱仪100MHz探头电路分析

对单线圈~1H、~2D和~(13)C核磁共振三调谐探头电路的等效电路进行了分析,得到了设计电路元件参数的一般公式.单线圈三调谐电路可同时完成三个通道不同频率信号的发射和接收.~1H通道和~(13)C通道的隔离度比交叉线圈隔离度高,~1H去耦效率明显增强.

核磁共振波谱仪MLEV-16宽带去耦系统

在FX-100核磁共振波谱仪上建立了MLEV-16宽带去耦系统.对去耦电路的各级信号进行了分析,说明了MLEV-16去耦电略的控制关系.利用去耦电路实现了由计算机和可编程序器控制的宽带去耦,用波谱仪原有去耦功率作了~(13)C{F~(19)}氟宽带去耦的碳-13谱的观测,去耦范围达12.4kHz,可以满足大部分有机氟化物的~(13)C核磁共振研究。

一种新的亚结构线性编码方法及其应用

本文较详细地介绍了以“超碳原子”为中心的亚结构线性编码方法,提出了符号代码规则、编码优先级规则以及定位、亚结构分截等,并运用该编码方法,建立了初具规模的亚结构——~(13)C 化学位移相关性数据库及(?)结构检索系统,现已在结构自动解析系统中投入运行,其机型为 PDP 11/24。

Methane-derived authigenic carbonates from the Ulleung basin sediments, East Sea of Korea

Authigenic carbonates were sampled in methane-enriched piston core sediments collected from gas venting sites on the western continental slope of the Ulleung Basin, East Sea of Korea. Multidisciplinary investigations on these carbonates, including the scanning electronic microscope (SEM) observations and mineralogical-geochemical compositions, were carried out to identify the carbon and oxygen sources and the forming mechanism of these carbonates. The authigenic carbonates from the study area correspond to semi-consolidated, compact concretions or nodules ranging from 2 to 9 cm in size. X-ray diffraction and electron microprobe analyses showed that most of the sampled carbonate concretions were composed of almost purely authigenic high-Mg calcite (10.7-14.3 mol% MgCO3). Characteristically, microbial structures such as filaments and rods, which were probably associated with the authigenic minerals, were abundantly observed within the carbonate matrix. The carbonates were strongly depleted in delta C-13 (-33.85 parts per thousand to -39.53 parts per thousand Peedee Belemnite (PDB)) and were enriched in delta O-18 (5.16-5.60 parts per thousand PDB), indicating that the primary source of carbon is mainly derived from the anaerobic oxidation of methane. Such methane probably originated from the destabilization of the underlying gas hydrates as strongly supporting from the enriched O-18 levels. Furthermore, the strongly depleted delta C-13 values (-60.7 parts per thousand to -61.6 parts per thousand PDB) of the sediment void gases demonstrate that the majority of the gas venting at the Ulleung Basin is microbial methane by CO2 reduction. This study provides another example for the formation mechanism of methane-derived authigenic carbonates associated with gas-hydrate decomposition in gas-seeping pockmark environments. (c) 2009 Elsevier Ltd. All rights reserved.

Paleoceanographic records in the sedimentary cores from the middle Okinawa Trough

Two gravity piston cores (Cores 155 and 18) involved in this study were collected from the middle Okinawa Trough. Stratigraphy of the two cores was divided and classified based on the features of planktonic foraminifera oxygen isotope changes together with depositional sequence, millennium-scale climatic event comparison, carbonate cycles and AMS(14)C dating. Some paleoclimatic information contained in sediments of these cores was extracted to discuss the paleoclimatic change rules and the short-time scale events presented in interglacial period. Analysis on the variation of oxygen isotope values in stage two shows that the middle part of the Okinawa Trough may have been affected by fresh water from the Yellow River and the Yangtze River during the Last Glacial Maximum (LGM). The oxygen isotope value oscillating ranges of the cores have verified that the marginal sea has an amplifying effect on climate changes. The delta(13)C of benthic foraminifera Uvigerina was lighter in the glacial period than that in the interglacial period, which indicates that the Paleo-Kuroshio's main stream moved eastward and its influence area decreased. According to the temperature difference during the "YD" period existing in Core 180 and other data, we can reach the conclusion that the climatic changes in the middle Okinawa Trough area were controlled by global climatic changes, but some regional factors had also considerable influence on the climate changes. Some results in this paper support Fairbanks's point that the "YD" event was a brief stagnation of sea level rising during the global warming up procession. Moreover, the falling of sea level in the glacial period weakened the exchange between the bottom water of the Okinawa Trough and the deep water of the northwestern Pacific Ocean and resulted in low oxygen state of bottom water in this area. These procedures are the reasons for carbonate cycle in the Okinawa Trough area being consistent with the "Atlantic type" carbonate cycle.

Contrasting chemical and isotopic compositions of organic matter in Changjiang (Yangtze river) estuarine and East China Sea shelf sediments

To examine the source and preservation of organic matter in the shelf sediments of the East China Sea (ECS), we measured bulk C/N and isotopes, organic biomarkers (n-alkanes and fatty acids) and compound-specific (fatty acids) stable carbon isotope ratios in three sediment cores collected from two sites near the Changjiang Estuary and one in the ECS shelf. Contrasting chemical and isotopic compositions of organic matter were observed between the estuarine and shelf sediments. The concentrations of total n-alkanes and fatty acids in the shelf surface sediments (0-2 cm) were 5-10 times higher than those in estuarine surface sediments but they all decreased rapidly to comparable levels below the surface layer. The compositions of n-alkanes in the estuarine sediments were dominated by C-26-C-33 long-chain n-alkanes with a strong odd-to-even carbon number predominance. In contrast, the composition of n-alkanes in the shelf sediment was dominated by nC(15) to nC(22) compounds. Long-chain (> C-20) fatty acids (terrestrial biomarkers) accounted for a significantly higher fraction in the estuarine sediments compared to that in the shelf sediment, while short-chain (< C-20) saturated and unsaturated fatty acids were more abundant in the shelf surface sediments than in the estuarine sediments. Stable carbon isotopic ratios of individual fatty acids showed a general positive shift from estuarine to shelf sediments, consistent with the variations in bulk delta(CTOCTOC)-C-13. These contrasts between the estuarine and shelf sediments indicate that terrestrial organic matter was mainly deposited within the Changjiang Estuary and inner shelf of ECS. Post-depositional diagenetic processes in the surface sediments rapidly altered the chemical compositions and control the preservation of organic matter in the region.

The variation of upper ocean structure and paleoproductivity in the Kuroshio source region during the last 200 kyr

A core from the source region of the Kuroshio warm current (east of the Luzon Island) was analyzed using several proxies in order to study the variability of the Western Pacific Warm Pool (WPWP) during the last two glacial-interglacial cycles. Primary productivity (PP) variations were deduced from variations in the coccolith flora. Primary productivity was higher during glacial periods (the end of Marine Isotope Stage [MIS] 3, some periods in MIS 2 and 6), and decreased during interglacial periods (MIS 7, MIS Se and probably MIS 5c-5d), with the lowest PP in MIS 5e. variations in the delta C-13 difference in benthic and bulk carbonate, thus in the vertical gradient of delta C-13 in dissolved inorganic carbon (Delta delta C-13(c). (wuellerstorfi-N. dutertrei) and Delta delta C-13(c.) (wuellerstorfi-coccolith)) Coincided With the PP Changes, showing that export productivity was low during interglacial periods (MIS 7, MIS 5e and Holocene) and high during glacial periods (MIS 6, probably MIS 5c-5d, late MIS 4 and late MIS 3). Comparison of foraminiferal carbonate dissolution indicators and PP changes reveals that nannofossil assemblage in core Ph05-5 is not sensitive to carbonate dissolution intensity. The depth of the thermocline (DOT) was estimated from planktonic forminiferal assemblages, and was relatively greater during interglacial periods (MIS 7, MIS 5e, probably MIS 5c and Holocene) than during glacials (middle MIS 6, probably MIS 5b and 5d, some periods in MIS 4, MIS 3 and MIS 2). Good coherence between the paleoproductivity records and the DOT suggests that the DOT changes could be the primary control factor in changes of paleoproductivity, and the glacial high productivity in the Kuroshio source region could be associated with a global increase of nutrient concentration in the intermediate waters that upwelled into the photic zone. The low CO2 values derived for intervals of high productivity and a relatively shallow DOT suggest that the changes in biological productivity and DOT in the equatorial Pacific could have modified atmospheric CO2 concentrations. High Sea Surface Temperatures (SSTs) during the warm MIS 5e in combination with intensified monsoonal rain fall could have resulted in a more intense stratification of the upper waters, resulting in low nutrient supply to the surface waters and a resulting decrease in productivity. (C) 2010 Elsevier B.V. All rights reserved.

Carbon isotopic studies of individual lipids in organisms from the Nansha sea area, China

Carbon isotopes of individual lipids in typical organisms from the Nansha sea area were measured by the GC-IRMS analytical technique. delta(13)C values of saturated fatty acids in different organisms examined are from -25.6parts per thousand to -29.7parts per thousand with the average values ranging from -26.4parts per thousand to -28.2parts per thousand and the variance range of 11.8parts per thousand, between different organisms is also observed. Unsaturated fatty acids have heavy carbon isotopic compositions and the mean differences of 2.9%.9-6.8parts per thousand compared to the same carbon number saturated fatty acids. delta(13)C values of n-alkanes range from -27.5%o to -29.7parts per thousand and their mean values, ranging from -28.6parts per thousand, to -28.9parts per thousand, are very close in different organisms. The mean difference in delta(13)C between the saturated fatty acids and n-alkanes is only 1.5parts per thousand, indicating that they have similar biosynthetic pathways. The carbon isotopic variations between the different carbon-number lipids are mostly within +/-2.0parts per thousand, reflecting that they experienced a biosynthetic process of the carbon chain elongation. At the same time, the carbon isotopic genetic relationships between the biological and sedimentary lipids are established by comparative studies of carbon isotopic compositions of individual lipids in organisms and sediments from the Nansha sea area, which provides scientific basis for carbon isotopic applied research of individual lipids.