Performance of the Agilent 7900 ICP-MS with UHMI for High Salt Matrix Analysis
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Dead Sea Overview: Students Will Visit the Dead Sea in Jordan. the Dead Sea Is Over 400M Below Sea Level – the Lowest Place on Earth
The Dead Sea Overview: Students will visit the Dead Sea in Jordan. The Dead Sea is over 400m below sea level – the lowest place on earth. It is part of the Great Rift Valley that runs from southern Turkey through Syria, Jordan, and the Red Sea, west into East Africa and south to Mozambique. The cataclysms that created the rift began some 30 million years ago and recurred until 15,000 years ago, forming mountains which on the east rise to around 1,500m above the Dead Sea. Until 100,000 years ago, the rift was an extension of the Red Sea; then the waters receded, forming the saline Lake Lisan, 200m higher than today’s Dead Sea. By 10,000 BC this had shrunk further, leaving the Dead Sea and Lake Tiberius, linked by the Jordan Valley. Tiberias became a freshwater lake, but the Dead Sea, with no outlet, became saline. As its name evokes, the Dead Sea is devoid of life due to the high salt concentration and minerals. However, this also means that the Dead Sea has curative powers, therapeutic qualities, and its buoyancy. Herod the Great recognized the Dead Sea more than 2000 years ago. You can float in the Dead Sea without trying. This is the only place you could read a newspaper while in the water without thinking about it! Scientifically speaking, its water contains more than 35 different types of minerals that are essential for the health and care of the body skin including Magnesium, Calcium, Potassium, Bromine, Sulfur, and Iodine. They are well known for relieving pains and sufferings caused by arthritis, rheumatism, psoriasis, eczema, headache and foot-ache, while nourishing and softening the skin. -
Following the Astrobiology Roadmap: Origins, Habitability and Future Exploration
caister.com/astro Astrobiology Roadmap O'Rourke et al Chapter 1 Following the Astrobiology Roadmap: Origins, Habitability and Future Exploration Aubrie O'Rourke1†*, Angela Zoumplis1,2†, Paul Wilburn3†, Michael D. Lee3, Zhi Lee4, Marissa Vecina4 and Kysha Mercader4 1J. Craig Venter Institute, La Jolla, CA, USA 2Scripps Institution of Oceanography, La Jolla, CA, USA 3NASA Ames Research Center, Moffett Blvd, Mountain View, CA 94035, USA 4UCSD, School of Engineering, Senior Design Group, La Jolla, CA, USA *[email protected] †equal contribution DOI: https://doi.org/10.21775/9781912530304.01 Abstract Astrobiology asks three fundamental questions as outlined by the NASA Astrobiology Roadmap: 1. How did Life begin and evolve?; Is there Life elsewhere in the Universe?; and, What is the future of Life on Earth? As we gain perspective on how Life on Earth arose and adapted to its many niches, we too gain insight into how a planet achieves habitability. Here on Earth, microbial Life has evolved to exist in a wide range of habitats from aquatic systems to deserts, the human body, and the International Space Station (ISS). Landers, rovers, and orbiter missions support the search for signatures of Life beyond Earth, by generating data on surface and subsurface conditions of other worlds. These have provided evidence for water activity, supporting the potential for extinct or extant Life. To investigate the putative ecologies of these systems, we study extreme environments on Earth. Several locations on our planet provide analog settings to those we have detected or expect to find on neighboring and distant worlds. Whereas, the field of space biology uses the ISS and low gravity analogs to gain insight on how transplanted Earth-evolved organisms will respond to extraterrestrial environments. -
View East Toward Ross Island and Mcmurdo Sound
This dissertation has been microfilmed exactly as received 69-22,155 JONES, Lois Marilyn, 1934- THE APPLICATION OF STRONTIUM ISOTOPES AS NATURAL TRACERS: THE ORIGIN OF THE SALTS IN THE LAKES AND SOILS OF SOUTHERN VICTORIA LAND, ANTARCTICA. The Ohio State University, Ph.D., 1969 Geology University Microiilms, Inc., Ann Arbor, Michigan THE APPLICATION OP STRONTIUM ISOTOPES AS NATURAL TRACERS: THE ORIGIN OF THE SALTS IN THE LAKES AND SOILS OF SOUTHERN VICTORIA LAND, ANTARCTICA DISSERTATION Presented in Partial Fullfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Lois Marilyn Jones, B. Sc,, M. Sc The Ohio State University 1969 Approved by Adviser Department of Geology PLEASE NOTE: Several pages contain colored illustrations. Filmed in the best possible way. UNIVERSITY MICROFILMS ACKNOWLEDGMENTS I wish to express my gratitude to Professor Gunter Faure, whose advice, discussions, and encour agement have been indispensible in bringing this study to a satisfactory conclusion. This study also could not have been possible without the generosity of numerous people who willingly contributed valuable samples utilized in this investi gation. Dr. Derry D. Koob contributed the excellent series of samples from depth profiles of Lakes Vanda and Bonney and the sample from Don Juan Pond. Mr. R. E. Behling and Dr. K. R. Everett contributed the samples of soil from the vicinity of the Meserve Glacier and from Taylor Valley, as well as samples of salts and meltwater. Mr. H. J. E. Montigny collected the soils and water samples from the floor of Wright Valley and the extensive suites of rock samples from the basement complex of the valley. -
Control on ( U/ U) in Lake Water: a Study in the Dry Valleys of Antarctica
Chemical Geology 226 (2006) 298–308 www.elsevier.com/locate/chemgeo Control on (234U/238U) in lake water: A study in the Dry Valleys of Antarctica Gideon M. Henderson a,*, Brenda L. Hall b, Andrew Smith a, Laura F. Robinson a,1 a Department of Earth Sciences, Oxford University, Parks Road, Oxford, OX1 3PR, UK b Department of Geological Sciences and Institute for Quaternary Studies, University of Maine, Orono, ME 04469, USA Accepted 5 September 2005 Abstract The (234U/238U) ratio in surface waters is generally higher than secular equilibrium due to nuclide recoil during alpha-decay of 238U. The size of the deviation from secular equilibrium contains information about the environment in which the water is found. This potential tool for environmental reconstruction has previously been studied in rivers, groundwater, and sediment pore-water. Here we conduct a first assessment of the controls on (234U/238U) in lakewaters. Thirty-three waters from glacial melt, streams, and lakes of the McMurdo Dry Valleys (Antarctica) were analysed for U concentration and isotope ratio. Glacial melt has a low U concentration and a (234U/238U) identical to seawater, suggesting that U in Antarctic ice is largely sourced from sea-salt aerosols. Stream waters have higher U concentration (0.009 to 1.282 ppb) and (234U/238U) (1.280 to 1.832) due to chemical weathering of sediment in stream channels and 234U recoil from this sediment. Average (234U/238U) is 1.502, close to the average of observations from other surface waters worldwide. The absence of groundwaters in the Dry Valleys indicates that reasonably high (234U/238U) ratios do not require groundwater sources of U, so care should be taken before using high (234U/238U) as an indicator of groundwater inputs to stream waters. -
Glossary of Limnological Terms
GLOSSARY OF LIMNOLOGICAL TERMS Athalassohaline: Having a salt composition very different from that of seawater Chemocline: Water layer with steep gradients of concentrations of chemicals (nutrients, oxygen, salts, etc.) Epilimnion: The upper, mixed layer of a stratified lake Holomixis: Period of complete mixing of a lake with water circulation from top to bottom Hypolimnion: The lower water layer of a stratified lake Meromixis: Permanent stratification, in which the water layers of a lake do not mix at any time during the annual cycle Metalimnion: Intermediate layer between the epilimnion and the hypolimnion; often corresponding to the chemocline and/or pycnocline Mixolimnion: The upper mixed layer of a meromictic lake Monomixis: Regime in which a seasonally stratified lake turns over once each year Monimolimnion: The stagnant bottom layer of a meromictic lake Oxycline: Water layer with a steep oxygen concentration gradient Pycnocline: Water layer with a steep density (salinity) gradient Thalassohaline: Having a salt composition similar to that of seawater Thermocline: Water layer with a steep temperature gradient 559 ABOUT THE AUTHOR Aharon Oren was born in 1952 in Zwolle, the Netherlands. He obtained his M.Sc. degree in microbiology and biochemistry (1974) from the State University of Groningen, the Netherlands, and his Ph.D. degree in microbiology (1978) from the Hebrew University of Jerusalem, Israel. He is was appointed as senior lecturer (1985), associate professor (1991), and professor of microbial ecology (1996) at the Hebrew University, and serves as department chairman since 1998. He has been a post-doctoral research fellow (1982-1983) and visiting assistant professor (1983- 1984) at the University of Illinois at Urbana- Champaign, and was appointed affiliate professor of George Mason University, Fairfax, Virginia. -
Chemical Analysis of Gaet'ale, a Hypersaline Pond
Aquat Geochem (2017) 23:109–117 DOI 10.1007/s10498-017-9312-z ORIGINAL ARTICLE Chemical Analysis of Gaet’ale, a Hypersaline Pond in Danakil Depression (Ethiopia): New Record for the Most Saline Water Body on Earth 1 1 Eduardo Pe´rez • Yonas Chebude Received: 25 July 2016 / Accepted: 27 January 2017 / Published online: 23 March 2017 Ó Springer Science+Business Media Dordrecht 2017 Abstract The chemical analysis of the water of Gaet’ale Pond, a small water body located in Danakil Depression, Ethiopia, resulted to be the most saline water body on earth with total dissolved solids (TDS) of 433 g kg-1. The composition of the water indicates the predominance of two main salts: CaCl2 and MgCl2 at a proportion of Ca:Mg = 3.1 (w/w). ? ? - Traces of K ,Na and NO3 are also detected, as well as Fe(III) complexes that give the water a characteristic yellow color. Density measurements, elemental analysis, thermo- gravimetrical analysis (TGA) and powder X-ray diffraction data are consistent with the composition and salinity determined. The water of this pond has a similar composition to Don Juan Pond, Antarctica, but a higher salinity, which can be explained in terms of temperature and solubility of the main components. Keywords Ethiopia Á Hypersaline water bodies Á Danakil depression Á Dallol springs Á Chlorides solubility Á Salinity 1 Introduction A saline lake is a closed water body that contains a significant concentration of salts ([3gL-1). Saline lakes can be originated from marine environments by evaporation; hence, their composition of salts is similar to that of seawater and is then said to have a thalassohaline origin. -
Anions and Alkali Metals in Lake Vanda, Don Juan Pond, and the Onyx River: Further Indications of Brine Origin
Anions and alkali metals and Armitage 1963). Evidently, there has evidently been little change in lake composition over the last 24 years. in Lake Vanda, Don Juan Pond, Waters were taken from Lake Vanda using a 1.5-liter capacity and the Onyx River: sampler, lowered on a calibrated line through a 10-centimeter diameter hole in the ice cover. The sampler was constructed Further indications of ultra-high-molecular-weight polyethylene and all metal parts of brine origin of titanium or niobium (to minimize trace metal contamina- tion). Once at the required depth, a messenger weight dropped onto the top-mounted spring mechanism released the ten- sioned plugs, and sealed the sample chamber. Temperature J.G. WEBSTER and R.L. GOGUEL and pH were measured on site. (Eh and sulfide, also measured, are not reported here.) Salts were collected from the margin DSIR Chemistry Division, of Lake Vanda, from soils near the lake and from Don Juan Private Bag, Petone, Pond. New Zealand Halides and sulfate assays were made on a DIONEX Ion Chromatograph with a sodium bicarbonate/sodium carbonate eluent. An HPIC AS4 column and conductivity detector were During the 1987-1988 austral summer, we collected water used for low (<500 milligrams per kilogram) chloride, bromide, samples from Lake Vanda, Don Juan Pond, and the Onyx River flouride, and sulfate analysis, and a HPIC AG4 column with in the Wright Valley, McMurdo Oasis. Lake Vanda is approx- amperometric detector (silver/silver chloride electrode) for io- imately 8.5 kilometers long, 2.5 kilometers wide (maximum) dide analysis and to confirm the bromide data.