克山病患者与健康人心肌元素含量均值向量比较和对应分析

对18例克山病患者及43例健康人心肌 Ba、Ca、Cd、Co、Cr、Cu、Fe、K、Mg、Mn、Na、P、Ti、Zn 和 Se 含量的两个均值向量进行了比较,结果表明其差异非常显著(P<0.01)。对应分析取最大的两个特征根(其和超过全部特征根之和的85%)绘成二维图,可见:克山病组与健康组分界明确;Se、Zn、Cu、P、Mg 和 K 与健康组关系密切;Ca、Co 和 Na 与克山病组关系密切;Ba、Fe、Mn、Ti、Cd 和 Cr 似乎与两组关系都不密切。

稀土Al—Zn—Mg合金的研制及性能研究

本文介绍了我们研制的稀土作为微量添加元素的中等强度Al-Zn-Mg合金,对其制备工艺、性能和稀土的作用进行了研究和讨论。研究表明,该合金具有强度较高,高温塑性好,可焊性优良等特点,适用锻压,挤压等变形加工。可望在交通车辆等方面获得应用。

火焰原子吸收光谱法测定明胶中Mg、Ca、Cu、Fe等杂质

明胶是感光工业基本原料之一,其质量的好坏直接影响照像性能,因此对明胶中的杂质进行分析研究具有重要的实际意义。本文采用火焰原子吸收光谱法测定明胶中Mg、Ca、Cu、Fe四个元素。明胶样品经灰化除去有机成分后进行酸溶,然后定容到

电感耦合等离子体发射光谱测定稀土铝合金中稀土和非稀土元素

本工作用 ICP-AES 法测定稀土-6063变形铝合金中 La、Ce、Pr、Nd、Sm、Gd、Fe、Mg、Ti、Zn,Cu 和 Mn,本方法不用化学分离,可一次同时测定这些元素,并做了 ICP光源参数、基体量变化、酸度(HCl)变化、稀土总量变化、共存元素 Fe 和 Mg 量的变化对被测元素的影响。本方法速度快、准确度高(除 Cu 稍差)。回收率91.0～110.0%,相对标准偏差±1.4～8.0%。

电感耦合等离子体原子发射光谱测定混合稀土铜合金中稀土和非稀土元素

本文提出了用电感耦合等离子体原子发射光谱(ICP—AES)法直接测定混合稀土铜合金中13个非稀土和稀土元素。选用了合适的分析线对及ICP光源的工作参数。探讨了观察高度、功率、酸度、载气和基体量的变化对被测元素谱线强度的影响。不用化学分离,可一次同时测定La、Ce、pr、Nd、Sm、Sn、Zn、Fe、Al、Ni、Pb,Mg和Mn。测定范围(％):La_2O_3:0.096～6.4;CeO_2:0.24～16;Pr_6O_(11):0.0384～2.56;Nd_2O_3:0.096～6.4;Sn:0.096～3.2;Mg、Mn、Fe,Sm_2O_3:0.024～1.6;Zn:0.396～6.7;Pb:0.092～6.4;Ni:0.096～3.2;Al:0.0384～1.28。相对标准偏差±3.0～9.1％;回收率85～116％满足冶炼上的要求,得到了满意的结果。

HEH/EHP和伯胺N_(1923)萃取Zn(II)的协同与反协同效应

研究了HEH/EHP(HA)和伯胺N_(1923)盐酸盐(RNH_3C1)的正庚烷溶液从HC1介质中对Zn(Ⅱ)的萃取。发现当以RNH_3Cl为主体萃取剂时,添加HA有利于对Zn(Ⅱ)的萃取;当以HA为主体萃取剂时,添加RNH_3C1则抑制了对Zn(Ⅱ)的萃取。考察了温度对协萃平衡的影响,并计算了体系的热力学函数。

[Zn~+{H_2N(CH_2)_4CH(NH_2)COONa}_2SO_4~-]·H_2O配合物的合成及其晶体结构

锌是人体必需的14种微量元素之一,现已知它与近200种酶的活性有关. L-赖氨酸是人体自身不能合成的8种氨基酸之一.它们与人体的新陈代谢密切相关,而在人类食物中又极易缺乏.二者供应不足,均会引起生理障碍进而导致疾病,尤其是儿童.因此,缺锌和赖氨酸已引起人们的关注,成为引人注目的重要课题.近年来,临床上常用的补锌剂多为硫酸

稀土对Al-Mg-Si合金性能影响和稀土作用机理研究

本文研究了稀土对铝镁硅合金性能的影响通过添加稀土改善合金的综合性能,提高合金的成品率,表面光泽性和致密度,讨论了稀土对铝镁硅合金的作用机理,为稀土在铝镁硅合金型材中的推广应用提供了有力的实验依据。

伯胺N_(1923)与中性磷萃取剂对Zn(Ⅱ)的协同萃取

本文研究了仲碳伯胺N_(1923)与中性磷萃取剂的正庚烷溶液,从盐酸介质中对Zn(Ⅱ)的协同萃取。用斜率法及等摩尔系列法确定协萃配合物的组成为:(RNH_3Cl)_3·ZnCl_2·TBP、(RNH_3Cl)_2·ZnCl_2·DBBP,求得协萃反应的平衡常数分别为logK_(12)(TBP)=3.09,logK_(12)(DBBP)=2.90,协萃配合物的生成常数分别为logβ_(12)(TBP)=1.34,logβ_(12)(DBBP)=1.90.计算了协萃反应的热力学函数值,并对协萃配合物的IR、NMR谱进行了讨论。

An efficient method for DNA isolation from red algae

A simple, inexpensive and efficient method was developed for rapid isolation of total genomic DNA from 15 red algal species. It resulted in 0.1 mug high quality DNA from 1 mg fresh algal material, with an A(260)/A(280) ratio of 1.68 - 1.90. Using this rapidly isolated DNA, the 18S ribosomal RNA genes ( rDNA) and the nuclear ribosomal DNA of the internal transcribed spacer (ITS) regions were amplified. The tested DNA was suitable for restriction endonuclease digestion, genetic marker analysis and polymerase chain reaction (PCR) amplification, and may be valid for other genetic manipulation.

Purification and characterization of agarases from a marine bacterium Vibrio sp. F-6

Marine bacterium Vibrio sp. F-6, utilizing agarose as a carbon source to produce agarases, was isolated from seawater samples taken from Qingdao, China. Two agarases (AG-a and AG-b) were purified to a homogeneity from the cultural supernatant of Vibrio sp. F-6 through ammonium sulfate precipitation, Q-Sepharose FF chromatography, and Sephacryl S-100 gel filtration. Molecular weights of agarases were estimated to be 54.0 kDa (AG-a) and 34.5 kDa (AG-b) by sodium dodecyl sulfate-polyacrylamide gel electrophoresis (SDS-PAGE). The optimum pH values for AG-a and AG-b were about 7.0 and 9.0, respectively. AG-a was stable in the pH range of 4.0-9.0 and AG-b was stable in the pH range of 4.0-10.0. The optimum temperatures of AG-a and AG-b were 40 and 55 degrees C, respectively. AG-a was stable at temperature below 50 degrees C. AG-b was stable at temperature below 60 degrees C. Zn2+, Mg2+ or Ca2+ increased AG-a activity, while Mn2+, Cu2+ or Ca2+ increased AG-b activity. However, Ag+, Hg2+, Fe3+, EDTA and SDS inhibited AG-a and AG-b activities. The main hydrolysates of agarose by AG-a were neoagarotetraose and neoagarohexaose. The main hydrolysates of agarose by AG-b were neoagarooctaose and neoagarohexaose. When the mixture of AG-a and AG-b were used, agarose was mainly degraded into neoagarobiose.

The cDNA cloning and mRNA expression of cytoplasmic Cu, Zn superoxide dismutase (SOD) gene in scallop Chlamys farreri

Cu, Zn superoxide dismutases (SODs) are rnetalloenzymes that represent one important line of defence against reactive oxygen species (ROS). A cytoplasmic Cu. Zn SOD cDNA sequence was cloned from scallop Chlamys farreri by the homology-based cloning technique. The full-length cDNA of scallop cytoplasmic Cu, Zn SOD (designated CfSOD) was 1022 bp with a 459 bp open reading frame encoding a polypeptide of 153 amino acids. The predicted amino acid sequence of CfSOD shared high identity with cytoplasmic Cu. Zn SOD in molluscs, insects, mammals and other animals, such as cytoplasmic Cu, Zn SOD in oyster Crassostrea sostrea gigas (CAD42722), mosquito Aedes aegypti (ABF18094), and cow Bos taurus (XP_584414). A quantitative reverse transcriptase real-time PCR (qRT-PCR) assay was developed to assess the mRNA expression of CfSOD in different tissues and the temporal expression of CfSOD in scallop challenged with Listonella anguillarum, Micrococcus luteus and Candida lipolytica respectively. Higher-level mRNA expression of CfSOD was detected in the tissues of haemocytes, gill filaments and kidney. The expression of CfSOD dropped in the first 8-16 h and then recovered after challenge with L. anguillarum and M. litteus, but no change was induced by the C. lipolytica challenge. The results indicated that CfSOD was a constitutive and inducible acute-phase protein, and could play an important role in the immune responses against L. anguillarum and M. luteus infection. (C) 2007 Elsevier Ltd. All rights reserved.

Formation of Fe-oxyhydroxides from the East Pacific Rise near latitude 13 degrees N: Evidence from mineralogical and geochemical data

The mineralogical and geochemical characteristics of Fe-oxyhydroxide samples from one dredge station (long. 103 degrees 54.48'W, lat. 12 degrees 42.30'N, water depth 2655 m) on the East Pacific Rise near lat 13 degrees N were analyzed by XRD, ICP-AES, and ICP-MS. Most Fe-oxyhydroxides are amorphous, with a few sphalerite microlites. In comparison with Fe-oxyhydroxides from other fields, the variable ranges in the chemical composition of Fe-oxyhydroxide samples are very narrow; their Fe, Si, and Mn contents were 39.90%, 8.92%, and 1.59%, respectively; they have high Cu (0.88%-1.85%) and Co (65x10(-6)-704x10(-6)) contents, and contain Co+Cu+Zn+Ni > 1.01%. The trace-element (As, Co, Ni, Cu, Zn, Ba, Sr) and major-element (Fe, Ca, Al, Mg) contents of these samples are in the range of hydrothermal sulfide from the East Pacific Rise near 13 degrees N, reflecting that this type of Fe-oxyhydroxide constitutes a secondary oxidation product of hydrothermal sulfide. The Fe-oxyhydroxide samples from one dredge station on the East Pacific Rise near 13 degrees N are lower in Sigma REE (5.44x10(-6)-17.01x10(-6)), with a distinct negative Ce anomaly (0.12-0.28). The Fe-oxyhydroxide samples have similar chondrite-normalized rare-earth-element (REE) patterns to that of seawater, and they are very different from the REE composition characteristics of hydrothermal plume particles and hydrothermal fluids, showing that the REEs of Fe-oxyhydroxide are a major constituent of seawater and that the Fe-oxyhydroxides can become a sink of REE from seawater. The quick settling of hydrothermal plume particles resulted in the lower REE content and higher Mn content of these Fe-oxyhydroxides, which are captured in part of the V and P from seawater by adsorption. The Fe-oxyhydroxides from one dredge station on the East Pacific Rise near 13 degrees N were formed by secondary oxidation in a low temperature, oxygenated environment. In comparison with the elemental (Zn, Cd, Pb, Fe, Co, Cu) average content of hydrothermal sulfide samples from the East Pacific Rise near 13 degrees N, the Zn, Cd, and Pb contents of the Fe-oxyhydroxides are lower, and their Fe, Co, and Cu contents are higher.