共查询到20条相似文献,搜索用时 218 毫秒
1.
发展了一种新型的氢化物发生装置-可移动还原床氢化物发生器。应用该技术可将经毛细管区带电泳分离之后的各种砷的化合物转换为相应的氢化物,然后再被引入到电感耦合等离子体发射光谱进行检测。对不同形态砷的不同化合物的CZE分离条件进行了优化,包括缓冲溶液的PH值及及浓度,进样量等。CZE-MRBHG-ICP-AES应用于4种砷化合物的定量测定,峰面积的RSD(n=5)在1.9%-11.7%。4种砷的浓度检出 相似文献
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沉积型(贡溪式)重晶石矿床模式 总被引:5,自引:0,他引:5
车勤建 《大地构造与成矿学》1995,19(3):288-289
沉积型(贡溪式)重晶石矿床模式车勤建(湖南省地质研究所,长沙410007)AMETALLOGENICMODELFORSEDIMENTARYGONGXI-TYPEBARITEDEPOSITS¥CHEQinjian(HunanInstituteofGeo... 相似文献
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《Scientia Geologica Sinica》1998,(1)
PROVENANCEANALYSESOFLATEPALEOZOICCLASTICSINTHEKAMUSTEAREA,THEJUAGGURBASIN,XINJIANGZhangXiaohuiInstituteofGeology,ChineseAcade... 相似文献
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《Scientia Geologica Sinica》1997,(1)
GEOLOGICALEVIDENCEOFMUUSDESERTVO-LUTIONSINCE0.5MAB.P.TXGEOLOGICALEVIDENCEOFMUUSDESERTEVO┐LUTIONSINCE0.5MAB.P.SunJimin,DingZhon... 相似文献
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《Scientia Geologica Sinica》1997,(3)
DYNAMOMETAMORPHICMINERALIZATIONOFLALACOPERDEPPOSIT,HUILI,SICHUANPROVINCEZhouYongInstituteofGeology,AcademiaSinica,Beijing1000... 相似文献
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《Scientia Geologica Sinica》1997,(3)
SOMENEWOPINIONSABOUTTRIASSICGASTROPODASSEMBLAGESINCHINAPanYuntang(GraduateSchol,ChineseAcademyofSciences,Beijing100039)(Rece... 相似文献
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《Scientia Geologica Sinica》1998,(1)
MID-PROTEROZOICMETAMORPHICROCKS,METAMORPHISMANDCRUSTALEVOLUTIONINTHEWESTOFLIAONINGPROVINCEYuLiangjunInstituteofGeology,Chines... 相似文献
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《Scientia Geologica Sinica》1997,(4)
GENETICSEQUENCESOFGOLDDEPOSITSINEPICONTINENTALOROGENCMINERALIZATIONZONE———THETECTONICMETAMORPHICMINEROGENICBELTINTHEAILAOSH... 相似文献
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《Scientia Geologica Sinica》1997,(3)
METAMORPHOSEDMICROCLASTICROCKTYPEGOLDDEPOSITSINCHINALuDefuInstituteofGeology,ChineseAcademyofSciences,Beijing100029WangXiuzh... 相似文献
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《Scientia Geologica Sinica》1997,(2)
TIDALFLATSTORMDEPOSITSOFMIDDLECAMBRININSHIMENDISTRICT,HUNANPROVINCETXTIDALFLATSTORMDEPOSITSOFMIDDLECAMBRIANINSHIMENDISTRICT,HU... 相似文献
11.
新型的氢化物发生技术-可移动还原床氢化物发生器可以实现微升级样品的测定而不需要对样品进行酸化和使用气-液分离器。应用MRBHG-电感耦合等离子体发射光谱取得了同等质量的而不同形态的As,Se的相同信号强度,证明了在MRBHG体系中氢化物元素之间的干扰得到消除,方法用于合金钢,富硒茶叶等实际样品的测定,标准加入的回收率在93%-114%。 相似文献
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不同氢化反应条件下原子发射光谱同时测定锗锡砷锑铋 总被引:7,自引:0,他引:7
研究了不同氢化反应条件下电感耦合等离子体原子发射光谱同时测定锗,,锡,砷,锑和铋的方法。主要对锗,锡的氢化反应酸度,缓冲溶液的选择,动态线性范围,氧化剂的选择,共存元素的干扰及其消除进行实验。方法经国家一级标准物质分析验证,结果与标准值基本相符。 相似文献
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Ludwik HALICZ 《Geostandards and Geoanalytical Research》1990,14(3):459-460
Germanium in thirty-four SRM's was determined by hydride generation and ICP-AES after separation of germanium from the concomitant matrix into carbon tetrachloride, and finally back-extraction into water. This procedure permits the determination of 0.1 ppm of germanium in as small as 50 mg sample. The precision and accuracy of the method was established using Basalt BCR-1 as the most precisely determined standard available. 相似文献
16.
Shigeru TERASHIMA 《Geostandards and Geoanalytical Research》1986,10(2):127-130
The arsenic and antimony contents of 85 geochemical reference samples have been determined by atomic absorption spectrometry with hydride generation and heated quartz cell atomizer. The sample is decomposed with a mixture of perchloric, nitric and hydrofluoric acids and potassium permanganate solution; interferences are eliminated by addition of potassium iodide, aluminium chloride and ascorbic acid. The agreement between the present results and published data is fairly good. 相似文献
17.
在线双管氢化AAS法是一种新的原子吸收氢化光谱法 ,具有简便、快速、灵敏度高和硼氢化钾用量少的优点。采用正交试验设计法对在线双管氢化AAS法测定低含量As、Sb和Bi的测定条件进行了系统的研究 ,确定了乙炔流量、燃烧器高度、硼氢化钾浓度和溶液酸度的最佳测定条件。在最佳条件下对实际样品土壤GSS -5、水系沉积物GSD -11、钨矿石GSO -W -1和GSO -W -2中As ,Sb ,Bi的含量进行了测定 ,测定的结果较准确 ,RSD <3 .2 6%。 相似文献
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水浴浸提-氢化物发生-原子荧光光谱法同时测定地质样品中痕量砷和汞 总被引:2,自引:2,他引:0
采用盐酸-硝酸混合酸(盐酸-硝酸-水体积比3∶1∶4)水浴浸取地质样品,在样品消解后的母液中直接加入硫脲-抗坏血酸混合溶液,以氢化物发生-原子荧光光谱法同时测定地质样品中的痕量砷和汞。方法检出限为砷0.033 6 ng/mL,汞0.003 7 ng/mL;相对标准偏差(RSD,n=1)为砷1.1%,汞3.0%。对国家一级标准物质GBW 07109~GBW 07114、GBW 07301~GBW 07312、GBW 07401~GBW 07408中的砷和汞进行测定,测定值与标准值相吻合。 相似文献
20.
A method is described to estimate the chemical forms of arsenic (As) and antimony (Sb) in a variety of geochemical reference materials, combining a sequential extraction scheme with hydride generation and atomic absorption spectrometry (HG-AAS). The fractions dissolved by sequential extraction are empirically defined as the exchangeable, EDTA soluble, oxide, sulfide and residual fractions. The amount of As and Sb in the EDTA soluble fraction have been derived mainly from oxide phases, and partly from carbonate minerals. Most sulfide minerals in common geological samples were considered to be dissolved with the digestion of 0.7 mol l−1 NaOCl, but only small fraction of arsenopyrite and loellingite in ores could be dissolved in this way. Satisfactory agreement was observed between the sum of the As or Sb values from exchangeable to residual fractions and the reported total As or Sb values, with a few exceptions. Analytical results of As and Sb for thirty five geochemical reference materials are tabulated, and geochemical and mineralogical features are discussed. 相似文献