Determination of Elements in Natural-water, Biota, Sediment, and Soil Samples Using Collision/Reaction Cell Inductively Coupled Plasma-mass Spectrometry

Determination of Elements in Natural-water, Biota, Sediment, and Soil Samples Using Collision/Reaction Cell Inductively Coupled Plasma-mass Spectrometry
Author :
Publisher : CreateSpace
Total Pages : 100
Release :
ISBN-10 : 1500223050
ISBN-13 : 9781500223052
Rating : 4/5 (50 Downloads)

Book Synopsis Determination of Elements in Natural-water, Biota, Sediment, and Soil Samples Using Collision/Reaction Cell Inductively Coupled Plasma-mass Spectrometry by : John R. Garbarino

Download or read book Determination of Elements in Natural-water, Biota, Sediment, and Soil Samples Using Collision/Reaction Cell Inductively Coupled Plasma-mass Spectrometry written by John R. Garbarino and published by CreateSpace. This book was released on 2014-06-16 with total page 100 pages. Available in PDF, EPUB and Kindle. Book excerpt: A new analytical method for the determination of ele- ments in filtered aqueous matrices using inductively coupled plasma–mass spectrometry (ICP–MS) has been implemented at the U.S. Geological Survey National Water Quality Labo- ratory that uses collision/reaction cell technology to reduce molecular ion interferences. The updated method can be used to determine elements in filtered natural-water and other filtered aqueous matrices, including whole-water, biota, sediment, and soil digestates. Helium or hydrogen is used as the collision or reaction gas, respectively, to eliminate or substantially reduce interferences commonly resulting from sample-matrix composition. Helium is used for molecular ion interferences associated with the determination of As, Co, Cr, Cu, K, Mg, Na, Ni, V, W and Zn, whereas hydrogen is used for Ca, Fe, Se, and Si. Other elements that are not affected by molecular ion interference also can be determined simply by not introducing a collision/reaction gas into the cell. Analy- sis time is increased by about a factor of 2 over the previous method because of the additional data acquisition time in the hydrogen and helium modes.


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