Saline Lake Deposits in Washington
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Brine Evolution in Qaidam Basin, Northern Tibetan Plateau, and the Formation of Playas As Mars Analogue Site
45th Lunar and Planetary Science Conference (2014) 1228.pdf BRINE EVOLUTION IN QAIDAM BASIN, NORTHERN TIBETAN PLATEAU, AND THE FORMATION OF PLAYAS AS MARS ANALOGUE SITE. W. G. Kong1 M. P. Zheng1 and F. J. Kong1, 1 MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, CAGS, Beijing 100037, China. ([email protected]) Introduction: Terrestrial analogue studies have part of the basin (Kunteyi depression). The Pliocene is served much critical information for understanding the first major salt forming period for Qaidam Basin, Mars [1]. Playa sediments in Qaidam Basin have a and the salt bearing sediments formed at the southwest complete set of salt minerals, i.e. carbonates, sulfates, part are dominated by sulfates, and those formed at the and chlorides,which have been identified on Mars northwest part of basin are partially sulfates dominate [e.g. 2-4]. The geographical conditions and high eleva- and partially chlorides dominate. After Pliocene, the tion of these playas induces Mars-like environmental deposition center started to move towards southeast conditions, such as low precipitation, low relative hu- until reaching the east part of the basin at Pleistocene, midity, low temperature, large seasonal and diurnal T reaching the second major salt forming stage, and the variation, high UV radiation, etc. [5,6]. Thus the salt bearing sediments formed at this stage are mainly playas in the Qaidam Basin servers a good terrestrial chlorides dominate. The distinct change in salt mineral reference for studying the depositional and secondary assemblages among deposition centers indicates the processes of martian salts. migration and geochemical differentiation of brines From 2008, a set of analogue studies have been inside the basin. -
Alluvial Fans in the Death Valley Region California and Nevada
Alluvial Fans in the Death Valley Region California and Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 Alluvial Fans in the Death Valley Region California and Nevada By CHARLES S. DENNY GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 A survey and interpretation of some aspects of desert geomorphology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publications as follows: Denny, Charles Storrow, 1911- Alluvial fans in the Death Valley region, California and Nevada. Washington, U.S. Govt. Print. Off., 1964. iv, 61 p. illus., maps (5 fold. col. in pocket) diagrs., profiles, tables. 30 cm. (U.S. Geological Survey. Professional Paper 466) Bibliography: p. 59. 1. Physical geography California Death Valley region. 2. Physi cal geography Nevada Death Valley region. 3. Sedimentation and deposition. 4. Alluvium. I. Title. II. Title: Death Valley region. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C., 20402 CONTENTS Page Page Abstract.. _ ________________ 1 Shadow Mountain fan Continued Introduction. ______________ 2 Origin of the Shadow Mountain fan. 21 Method of study________ 2 Fan east of Alkali Flat- ___-__---.__-_- 25 Definitions and symbols. 6 Fans surrounding hills near Devils Hole_ 25 Geography _________________ 6 Bat Mountain fan___-____-___--___-__ 25 Shadow Mountain fan..______ 7 Fans east of Greenwater Range___ ______ 30 Geology.______________ 9 Fans in Greenwater Valley..-----_____. 32 Death Valley fans.__________--___-__- 32 Geomorpholo gy ______ 9 Characteristics of fans.._______-___-__- 38 Modern washes____. -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
When “Evaporites” Are Not Formed by Evaporation: the Role Of
When “evaporites” are not formed by evaporation: The role of temperature and pCO2 on saline deposits of the Eocene Green River Formation, Colorado, USA Robert V. Demicco† and Tim K. Lowenstein Department of Geological Sciences and Environmental Studies, Binghamton University, Binghamton, New York 13902-6000, USA ABSTRACT INTRODUCTION rated with halite. During summer, the waters of the lake above the thermocline (at <25 m depth) Halite precipitates in the Dead Sea during Geologists studying salt deposits have noticed warm to ∼34 °C, become undersaturated with ha- winter but re-dissolves above the thermo- that very soluble minerals that occur in the cen- lite due to the temperature increase, and the bulk cline upon summer warming, “focusing” ha- ter of a basin do not extend out to the edges of of the winter-deposited halite above the thermo- lite deposition below the thermocline (Sirota the basin (Hsü et al., 1973; Dyni, 1981; Lowen- cline re-dissolves. Summer dissolution of halite et al., 2016, 2017, 2018). Here we develop an stein, 1988). This is true even where: (1) soluble occurs in the Dead Sea despite any increase in “evaporite focusing” model for evaporites salts are interpreted to have been deposited in evaporative concentration at the surface. The ha- (nahcolite + halite) preserved in a restricted a deep evaporitic lake or marine basin and (2) lite that settled into the deeper, cooler isothermal area of the Eocene Green River Formation deep-water deposits that encase salts in the cen- bottom waters, however, accumulates as an an- in the Piceance Creek Basin of Colorado, ter of the basin can be confidently traced to pe- nual layer at depths below the 25 m deep ther- USA. -
Characterization of the Groundwater Discharge to Moses Lake-QAPP
Characterization of the Groundwater DischargeDischarge to MosesMoses Lake,Lake, Washington Quality Assurance Project Plan By Charles F. Pitz April 2001 Washington State Department of Ecology Environmental Assessment Program Olympia, WA 98504-7710 Approvals: Approved by: April 23, 2001 Dave Knight, ERO Regional OfficeOffice Date Approved by: April, 2001 Carl Nuechterlein, Section ManaManager,ger, ERO Regional OfficeOffice Date Approved by: April 23, 2001 Bob Cusimano, TMDL Project Manager,Manager, Watershed Ecology Section Date Approved by: April 17,17, 2001 Jim Carroll, TMDL Principal InvestInvestigator,igator, Watershed Ecology Section Date Approved by: April 17,17, 2001 Dale Norton, Unit Supervisor, Contaminant Studies Unit Date Approved by: April 24, 2001 Will Kendra, Section Manager, Watershed Ecology Section Date Approved by: April 19,19, 2001 Stuart Magoon, Director, ManchesterManchester Environmental Laboratory Date Approved by: April 17,17, 2001 Cliff Kirchmer, Ecology Quality Assurance OfficerOfficer Date Approved by: April 17,17, 2001 Charles F. Pitz, Project Lead, Contaminant Studies Unit Date Page 11 Background/Problem Statement Due to concerns regarding excess levels of aannualnnual nutrient loading to Moses Lake, the Eastern Regional OfficeOffice (ERO) of the Washington DepartmentDepartment of Ecology (Ecology) has asked the Environmental Assessment Program (EAP) to conduct a comprehensive fieldfield study of water quality conditions for the lake durduringing the 2001 water year (Figure 1)l).. The ultimate goals of this effort are the development of a water quality model, and an allocation strategy for nutrient loading to the lake (C(Carroll,arroll, et al., 2000). This allocation strategy will be formalized through the development of a Total Maximum Daily Load (TMDL) for nutrients. -
Benchmark 3: Evaluation of Alternatives with Respect to Existing Conditions August 2015
Salton Sea Funding and Feasibility Action Plan Benchmark 3: Evaluation of Alternatives With Respect to Existing Conditions August 2015 Prepared by: Prepared for: This document is prepared as a living document for public review and comment. Comments may be provided to: Salton Sea Authority 82995 Hwy 111, Suite 200 Indio, CA 92201 Email: [email protected] Comments will be reviewed and incorporated as appropriate. If substantive comments are received, a revised document may be produced and distributed. Preferred citation: Salton Sea Authority (2015). Salton Sea Funding and Feasibility Action Plan Benchmark 3 Report: Evaluation of Alternatives With Respect to Existing Conditions, August Report. Revision Record Revisions to this document will be reviewed and approved through the same level of authority as the original document. All changes to the Benchmark 3 Report must be authorized by the Principal in Charge. Date Version Changes January Working Posted on Salton Sea Authority website. 2015 Draft Included changes from draft review by Salton Sea TCT. June 2015 First Updated hydrology section and inflow Complete projections including Figures 48-52, along with Document editorial revisions. August Revision 1 Added this Revision Record. Corrected title of 2015 California Department of Fish and Wildlife and other minor editorial revisions. Updated discussion of historical flows from 2003-present. Tetra Tech, Inc. i August 2015 Executive Summary This report presents a review of Salton Sea restoration alternatives and their components and determine how well they would perform under current and future inflows. Alternatives are considered with respect to existing hydrologic conditions at the Sea, as of 2014, and projected future hydrology. -
Consequences of Drying Lake Systems Around the World
Consequences of Drying Lake Systems around the World Prepared for: State of Utah Great Salt Lake Advisory Council Prepared by: AECOM February 15, 2019 Consequences of Drying Lake Systems around the World Table of Contents EXECUTIVE SUMMARY ..................................................................... 5 I. INTRODUCTION ...................................................................... 13 II. CONTEXT ................................................................................. 13 III. APPROACH ............................................................................. 16 IV. CASE STUDIES OF DRYING LAKE SYSTEMS ...................... 17 1. LAKE URMIA ..................................................................................................... 17 a) Overview of Lake Characteristics .................................................................... 18 b) Economic Consequences ............................................................................... 19 c) Social Consequences ..................................................................................... 20 d) Environmental Consequences ........................................................................ 21 e) Relevance to Great Salt Lake ......................................................................... 21 2. ARAL SEA ........................................................................................................ 22 a) Overview of Lake Characteristics .................................................................... 22 b) Economic -
Saline and Hydromagnesite Depos 'Its O British Columbia
BRITISH COLUMBIA DEPARTMENT OF MINES Hon. W. J. ASSELSTINE, Minister JOHN F. WALKER, Deputy Minister BULLETIN No. 4 Saline and Hydromagnesite Depos ‘itso British Columbia by J.M. CUMMINGS CONTENTS . Page INTRODUCTION CHAPTER I . OCCURRENCES OF SODIUM AND MAGNESILIM SP.LTS IN BRITISH COLUMBIA SALINE DEPOSITSSALINE ............................................................................ ....... 1 Sodium CarbonateLakes ........................................................................................................ ................................. 1 Green Timber Plateau ............................................................................................................................................. 1 General i'jescription of Soda Lakes ............................. 3 Eighty-Three Mile Lake ................................................................................................................... 5 Goodenough and Safety Lake 6 Lake No . 6 ._ ............................................................................................................ 10 Liberty Lake 11 Snow White Lake .................................................................................................................................................... 12 Rob and Nan Lake ............................................................................................................................ 13 Last Chance Lake ............................................................................................................................................ -
Bromine Geochemistry of Salar De Uyuni and Deeper Salt Crusts
... .............. * .. ........, ., ;: ... ... ........ .. ........, ., '_.~' . ...: .. ,... ' :, .. , ._... , .-. ,; ..,. _I. ................. .. ; . ... ............ ~ .. .- ............'. ............ .... , . :.. , *.,:.:-' ' .., '. -. - .. 'c..;..,. CHEMICAL /./da 3-4 GEOLOGY lSCL1lDlNri L ISOTOPE GEOSCIEiYCE ELSEVIER Chemical Geology 167 (2000) 373-392 www.elsevier.com/locate/chemgeo Bromine geochemistry of salar de Uyuni and deeper salt crusts, Central Altiplano, Bolivia I FranGois/Risacher a, Bertrand Fritz i E IRD-Centre de Géochiiliie de Ia Siriface, Fralice CNRS 1 rite Blessig, 67084 Strasboiirg Cedex, France Received 15 August 1999; accepted 13 December 1999 Abstract The salar of Uyuni, in the central Bolivian Altiplano, is probably the largest salt pan in the world (10000 km'). A 121 m deep well drilled in the central salar disclosed a complex evaporitic sequence of 12 salt crusts separated by 11 mud layers. In the lower half of the profile, thick halite beds alternate with thin mud layers. The mud layers thicken upwards and show clear lacustrine features. The thickness of the salt beds decreases markedly from the base upward. The bromine content of the halite ranges from 1.3 to 10.4 mg/kg. The halite does not originate from the evaporation of the dilute inflow waters of the Altiplano, which would lead to Br content of tens of mg/kg. The presence of halite of very low Br content (2 mg/kg) in a gypsum diapir strongly suggests that most of the halite deposited at Uyuni originated from the leaching of ancient salt formations associated with the numerous gypsum diapirs of the Altiplano. The deep and thick halite beds were probably deposited in a playa lake, as suggested by their very low and fairly constant Br content (1.6-2.3 mg/kg) and by the abundance of detrital minerals. -
Gaylussite Na2ca(CO3)2 • 5H2O C 2001-2005 Mineral Data Publishing, Version 1
Gaylussite Na2Ca(CO3)2 • 5H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. As flattened wedge-shaped crystals with dominant {110}, {011}, {001}, smaller {010}, {100}, {101}, {112}; also as prismatic to dipyramidal crystals elongated along [100], to 6 cm. Physical Properties: Cleavage: On {110}, perfect; on {001}, imperfect. Fracture: Conchoidal. Tenacity: Very brittle. Hardness = 2.5–3 D(meas.) = 1.991 D(calc.) = 1.991 Dehydrates with efflorescence in dry air; slowly decomposes in H2O leaving CaCO3 as calcite or aragonite. Optical Properties: Transparent to translucent. Color: Colorless to pale yellow or pale gray, white; colorless in transmitted light. Streak: White to pale gray. Luster: Vitreous. Optical Class: Biaxial (–). Orientation: X = b; Z ∧ c = –15◦. Dispersion: r< v,strong, crossed. α = 1.444 β = 1.516 γ = 1.523 2V(meas.) = 34◦ Cell Data: Space Group: C2/c. a = 11.589 b = 7.780 c = 11.207 β = 102.5◦ Z=4 X-ray Powder Pattern: John Hay, Jr. Well No. 1, Wyoming, USA. 6.403 (100), 3.18 (80), 2.70 (80), 2.61 (80), 1.91 (80), 2.49 (70), 1.98 (70) Chemistry: (1) (2) CO2 30.02 29.72 SiO2 0.08 Fe2O3 0.03 MnO 0.01 MgO 0.01 CaO 19.02 18.94 Na2O 20.40 20.93 H2O 30.47 30.41 insol. 0.16 Total 100.20 100.00 • (1) Taboos-nor salt lake, Mongolia. (2) Na2Ca(CO3)2 5H2O. Occurrence: Typically in evaporites or shales from alkali lakes; rarely in veinlets cutting alkalic igneous rocks. -
Lled Basins of the Red
Deep-Sea Research I 46 (1999) 1779}1792 Hydrographic changes during 20 years in the brine-"lled basins of the Red Sea Pierre Anschutz! *,GeH rard Blanc!, Fabienne Chatin", Magali Geiller", Marie-Claire Pierret" !De& partement de Ge& ologie et Oce&anographie (D.G.O.), Universite& Bordeaux 1, CNRS UMR 5805, 33405 Talence Cedex, France "Centre de Ge& ochimie de la Surface, Institut de Ge&ologie, Universite& Louis Pasteur, CNRS UMR 7517, 67084, Strasbourg, France Received 16 June 1998; accepted 8 February 1999 Abstract Many of the deep basins "lled by hot brines in the Red Sea have not been investigated since their discovery in the early 1970s. Twenty years later, in September 1992, six of these deeps were revisited. The temperature and salinity of the Suakin, Port Sudan, Chain B, and Nereus deeps ranged from 23.25 to 44.603C and from 144 to 270&. These values were approximately the same in 1972, indicating that the budget of heat and salt was quite balanced. We measured strong gradients of properties in the transition zone between brines and overlying seawater. The contribution of salinity to the density gradient was more than one order of magnitude higher than the opposite contribution of temperature across the seawater}brine interface. Therefore the interface was extemely stable, and the transfer of properties across it was considered to be controlled mostly by molecular di!usion. We calculate that the di!usional transport of salt from the brines to seawater cannot a!ect signi"cantly the salinity of the brines over a 20 year period, which agrees with the observations. -
New Mineral Names*
American Mineralogist, Volume 75, pages 240-246, 1990 NEW MINERAL NAMES* JOHN L. JAMBOR CANMET, 555 Booth Street, Ottawa, Ontario KIA OGI, Canada EDWARD S. GREW Department of Geological Sciences, University of Maine, Orono, Maine 04469, U.S.A. Baiyuneboite-(Ce) the formula for cordylite-(Ce) requires revision such that Pigqiu Fu, Xlanze Su (1987) Baiyuneboite-A new min- cordylite-(Ce) and baiyuneboite-(Ce) may be identical. The eral. Acta Mineralogica Sinica, 7, 289-297 (in Chinese, Chairman therefore withdrew the approval and asked that English abstract). the authors withhold publication of their description of Pingqiu Fu, Youhua Kong, Guohong Gong, Meicheng baiyuneboite-(Ce) until the matter could be resolved. The Shao, Jinzi Qian (1987) The crystal structure of bai- request, unfortunately, was ignored. J.L.J. yuneboite-(Ce). Acta Mineralogica Sinica, 7, 298-304 (in Chinese, English abstract). Diaoyudaoite* Electron-microprobe analyses of ten grains, whose va- lidity was checked by single-crystal X-ray methods prior Shunxi Shen, Lirong Chen, Anchun Li, Tailu Dong, Qiu- to analysis, gave an average ofNa20 4.73, CaO 1.04, BaO huo Huang, Wenqiang Xu (1986) Diaoyudaoite-A new 20.38, Ce20, 24.21, La20, 10.92, Pr20, 0.62, Nd20, 10.04, mineral. Acta Mineralogica Sinica, 6, 224-227 (in Gd20, 0.13, F 2.50, C02 (by gas chromatography) 24.64, Chinese, English abstract). o == F 1.05, sum 98.16 wt%, corresponding to Nal.OS- The average of 13 electron-microprobe analyses gave (BaO.94CaO.I,)n07( Ce I.OSLao.4sN do.42Pr 0.0'Gdo.OI)"1.99F 0.9'C,.97- Na20 4.54, AI20, 93.00, Cr20, 1.95, MgO 0.10, CaO 0.10, 012.07'ideally NaBaCe2F(CO')4' The mineral occurs as yel- SiOz 0.23, K20 0.12, sum 100.04 wt%, corresponding to low, irregular grains 0.3 to 3 mm in size, frequently as (N ao.87Ko.ozMgo.02CaO.01)ro.92(AllO.84CrO.lsSio.02)"'1.01 0,7, ide- thin hexagonal tablets.