Queen's University - Utility Bar

QSpace at Queen's University >
Theses, Dissertations & Graduate Projects >
Queen's Theses & Dissertations >

Please use this identifier to cite or link to this item: http://hdl.handle.net/1974/6046

Title: Hydrated Sodium-Magnesium Sulfate Minerals Associated with Inland Saline Systems
Authors: Leduc, Evelyne Marie Sylvie

Files in This Item:

File Description SizeFormat
Leduc_Evelyne_MS_201009_MSc.pdf11.32 MBAdobe PDFView/Open
Keywords: Geology
Mineralogy
Sulfates
Crystal structure
Issue Date: 2010
Series/Report no.: Canadian theses
Abstract: Hydrated sodium-magnesium sulfate minerals are common in many continental evaporite settings around the world. The crystallization sequence of these minerals depends on such parameters as the composition of the parent brine, the temperature, the evaporation rate of the brine, and the differences in the atomic structure and water content of the minerals. The atomic structures of konyaite [Na2Mg(SO4)2·5H2O] and sodium-magnesium decahydrate [Na2Mg(SO4)2·10H2O], a newly described sulfate salt, have been determined from single-crystal X-ray diffraction experiments. The refined structures are discussed and compared to that of blödite [Na2Mg(SO4)2·4H2O]. The arrangement and importance of hydrogen bonds within all three structures are also discussed, and have been further investigated by infrared spectroscopy. Löweite [Na12Mg7(SO4)13·15H2O] was included in this experiment to provide a low-hydration end-member. Differences in water content and the importance of hydrogen bonds in the respective structures were clearly reflected in the generated infrared spectra. The growth conditions of the decahydrate, konyaite, blödite, löweite, and other phases of the Na2O-MgO-H2O system, as well as their stability relationships, were studied in a temperature-controlled crystal-growth experiment. Konyaite and the decahydrate phase were found as first precipitates over a range of temperatures and brine compositions where they are not considered to be the thermodynamically stable phase. The importance of evaporation rate in the formation of these, and other metastable phases, is discussed in relation to inland saline systems. Possible localities where the decahydrate could exist in nature are discussed, and challenges for future research are presented.
Description: Thesis (Master, Geological Sciences & Geological Engineering) -- Queen's University, 2010-09-16 09:02:33.843
URI: http://hdl.handle.net/1974/6046
Appears in Collections:Queen's Theses & Dissertations
Geological Sciences & Geological Engineering Graduate Theses

Items in QSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

 

  DSpace Software Copyright © 2002-2008  The DSpace Foundation - TOP