دانلود مقاله ISI انگلیسی شماره 123455
ترجمه فارسی عنوان مقاله

تعیین حساسیت اسمیوم در آبهای طبیعی با استفاده از طیف سنجی جرم پلاسمایی با جریان الکتریکی پس از تولید بخارات فتوشیمیایی

عنوان انگلیسی
Sensitive determination of osmium in natural waters by inductively coupled plasma mass spectrometry after photochemical vapor generation
کد مقاله سال انتشار تعداد صفحات مقاله انگلیسی
123455 2017 6 صفحه PDF
منبع

Publisher : Elsevier - Science Direct (الزویر - ساینس دایرکت)

Journal : Microchemical Journal, Volume 130, January 2017, Pages 281-286

ترجمه کلمات کلیدی
اسسمیم، اثر حافظه، عکس تولید بخار شیمیایی، طیف سنجی جرمی پلاسما به صورت القایی،
کلمات کلیدی انگلیسی
Osmium; Memory effect; Photo chemical vapor generation; Inductively coupled plasma-mass spectrometry;
پیش نمایش مقاله
پیش نمایش مقاله  تعیین حساسیت اسمیوم در آبهای طبیعی با استفاده از طیف سنجی جرم پلاسمایی با جریان الکتریکی پس از تولید بخارات فتوشیمیایی

چکیده انگلیسی

Accurate analysis of osmium is important in geochemistry and geochronology. The current osmium analytical methods often suffer from low sensitivity, multi-step extraction, high procedural blank, and severe memory effect. In this work, a highly sensitive and simple method for the determination of osmium in natural waters was developed by coupling inductively coupled plasma-mass spectrometry with photochemical vapor generation. The procedural blank is low due to the needlessness of high concentration strong oxidant. What's more, the memory effect was successfully solved by using 5.0% ammonium hydroxide elution instead of using concentrated inorganic acid or oxidant reagent reported before. The influences of the concentration of nitric acid, the flow rate of carrier gas, the photo irradiation time on osmium detection were investigated. Under optimized conditions, the detection limit was 0.8 pg mL− 1. A precision of 3.2% (RSD, n = 5) was achieved at a concentration of 1 ng mL− 1. The accuracy is successfully validated in several natural water samples with spike recoveries from 97% to 106%. The proposed method is sensitive, simple, low blank, and memory effect-free, which has a great potential in relevant geochemistry and geochronology study.