应用斐林试剂与碘液时的几点注意问题     

单林兰 《中学生物学》2006,22(11):40-40

实验原理：淀粉和蔗糖为非还原性糖，它们在酶的作用下，都能水解成还原性糖，还原性糖能与斐林试剂发生氧化还原反应，生成砖红色的氧化亚铜沉淀。  相似文献   

一类新季Sheng盐的合成     

李琴  刘继德 《荆州师专学报》1991,14(2):54-57

本文报道了两种新季Sheng盐的合成，并对其相应的肺叶立德的性质进行了初步的研究，两种季Sheng盐的结构均经红外光谱、核磁共振谱分析所证实。  相似文献   

《中文自修》袖珍试卷 上海民办张江集团学校语文组 初三语文试卷     

《中文自修》2011,(12)

  相似文献   

N-甲基苯氨基-4,6-二甲氧基-1,3,5三嗪的合成与表征     

李宪平  肖深初  熊知行  梅光泉 《宜春学院学报》2006,28(6):19-21

目的:为了进一步研究与发展均三嗪衍生物的制备方法.方法:在丙酮介质中,三聚氯氰先后与N-甲基苯胺、甲醇反应,合成了N-甲基苯氨基-4,6-二甲氧基-1,3,5三嗪.结果:标题化合物经红外光谱和质谱对它进行了表征,筛选出了最佳的工艺条件.结论:制备方法简单,反应条件温和,效果良好.  相似文献   

分光光度法测定海带中的碘   总被引：3，自引：0，他引：3  

谢少艾  陈虹锦  马荔  张卫 《实验室研究与探索》2005,24(7):16-17

讨论了用Fe^2＋-邻二氮菲体系分光光度法间接测定海带中微量碘含量的方法。本实验以NH4Fe（SO4）2作为氧化剂，使用邻二氮菲作为显色剂，通过测得吸光度与Fe^2＋溶液浓度成线性关系，可间接测定海带提取溶液中I^-的浓度。该法具有准确度高，重现性好，简便快速的特点，是测定海带中微量碘的一种较理想的方法。  相似文献   

偶氮苯聚合物(PGMAA-20)膜光栅结构的分子取向机制     

牛永平  张灵志  苏育志  梁兆熙  陆伟  佘卫龙 《浙江大学学报(A卷英文版)》2004,(3):183-189

设计合成及表征了一种含偶氮苯聚合物(PGMAA-20)材料.利用两束S偏振光作为泵浦光在PGMAA-20膜上刻写光栅并观察光栅的衍射信号;然后再用相衬显微镜直接观察偶氮苯薄膜上的光栅结构,并以分子取向机制为基础对光栅形成和消除过程提出了新解释,这种观点被实验观察结果进一步证实.  相似文献   

单扫描极谱法测定铜的研究     

徐茂田  汪怀仁 《商丘师范学院学报》1994,(Z3)

在０．０６５ｍｏｌ／Ｌ柠檬酸钠－０．０４６ｍｏｌ／ＬＨＣＩ（ｐＨ６．６）介质中，２，３，４－三羟基－４＇－磺基－偶氮苯和铜（Ⅱ）形成配合物，在单扫描示波极谱上于－０．２４ｖ（ｖｓ．ＳＣＥ）处产生灵敏的吸附波，测定铜的浓度范围为０．００５～０．３μｇ／ｍｌ，检出限为０．００２５μｇ／ｍｌ，利用该波应用于人发及硫酸镍中铜的测定，结果满意．  相似文献   

如何避免碘遇淀粉变蓝后又褪色     

刘忠慧 《生物学教学》2004,29(7):35-35

在用碘检验淀粉的实验中,常出现碘使淀粉变蓝后,过一段时间又褪色的情况。主要是碘与淀粉形成的络合物不稳定易分解,所以褪色。实验时,在碘液中加少量的盐酸或变蓝后加少量的盐酸,就会避免褪色。  相似文献   

检验Br^—和I^—的实验研究     

胥光勇 《化学教学》1994,(1):10-13

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Investigation of iodine concentration in salt,water and soil along the coast of Zhejiang,China     

陆颖理  王宁荐  朱岚  王国兴  吴晖  匡琳  朱文明 《Journal of Zhejiang University. Science. B》2005,6(12):1200-1205

Objective: We aim to describe the environment iodine concentration in salt, water and soil along Zhejiang Province coast in the China foreland. It will be helpful for us to judge whether this area is insufficient in iodine and universal iodized salt is necessary or not. Methods: We collected iodized salt samples, drinking water samples (tap water in the towns, and well water or spring water in the villages), water samples from different sources (ditches, lakes, rivers) and soil samples through random sampling in June, 2005. Salt, water and soil iodine was detected by arsenic-cerium redox method. Statistical analysis was expressed as mean±SEMby Windows SPSS 13.0. Results: (1) The iodine concentration in salt was 27.9±4.33 mg/kg (n=108). (2) Seventy-five water samples were collected. The water iodine value was 0.6～84.8 μg/L (mean of 11.66 μg/L). The watershed along the Qiantang River has significantly higher iodine content than the water in Lin'an in mountain area (P＜0.01). The iodine content and mean iodine content of tap water, well or spring water and natural water sources were 4.30±2.43 μg/L (n=34), 23.59±27.74 μg/L (n=19)and 12.72±10.72 μg/L (n=22) respectively. This indicated that among environmental water sources, the ditch iodine content was the highest with river water iodine being the lowest (P＜0.01). (3) Soil iodine value was 0.11～2.93 mg/kg (mean of 1.32 mg/kg).Though there was no statistical difference of soil iodine in different districts (P=0.131), soil iodine content correlated positively with water iodine content. Conclusion: Iodine concentration in salt accords with national policy of adding iodine in salt. Foreland has more iodine in water than mountain area. The data reflected that water and soil iodine in foreland area was not high, which suggests universal iodized salt should be necessary. Environment iodine has relatively close association with pollution.  相似文献