The Phase Diagram of Lithium Salt Systems and Its Application in Extraction of Lithium from Salt Lake Brine     

XIE Chao 《《地质学报》英文版》2014,88(Z1):386-386

正At present,the extraction of lithium from salt lake brine is the new trend of the salt lake industrialization.The saltine lake lithium resources are extremely rich in western china,especially in Qinghai-Tibetan plateau.Brine of salt  相似文献   

Influence of Painting and Dyeing?on?Temperature?Fluctuation of Northern Tibetan Salt Brines     

WU Zhiming  ZHENG Mianping  CUI Xiangmei  NIE Zhen 《《地质学报》英文版》2014,88(Z1):382-382

正Introduction The amount of the total dissolved salts(TDS)in most of the salt brines on northern Tibet is relatively lower.So the effective brine concentration technique is needed for lithium,boron and potassium extraction from these brine  相似文献   

An Eco-Friendly High-Effective Scale Inhibitor for High Salt Brine     

ZHANG Xin  SHAO Qianqian  CUI Zhaojie  TAN Xianfeng 《《地质学报》英文版》2014,88(Z1):408-409

正Now the mining of high salt underground brine has been an important aspect of salt lake mining,which is the necessary support to the development of national economy.With the change of underground geological  相似文献   

Simulated Dynamic Evaporation of Yiliping Salt Lake Brine     

CUI Xiangmei  WU Zhiming  WEN Xianming  ZHANG Xingru 《《地质学报》英文版》2014,88(Z1):305-306

正1 Introduction There are numerous salt lakes in western China(Zheng Mianping,et al.,2011).Yiliping playa on the western Qaidam Basin is a magnesium sulfate subtype dry salt lake with high concentrations of potassium,boron and lithium.  相似文献   

梅县嵩溪银（锑）矿流体包裹体轻烃组成及其矿床成因意义     

孙晓明  David I. Norman  孙凯  陈炳辉  陈敬德 《地质论评》1999,45(7):817-822

嵩溪是一个新发现的大型银（锑）矿,位于永梅拗陷南段寨岗上火山沉积盆地的边缘。前人多认为其形成与火山活动有关,主要有海底基性火山喷流和中低温火山热液充填等成因观点。但矿物流体包裹体超高真空四极气相质谱系统测定表明其中存在多种轻烃气体,它们主要由C1~4饱和烷烃组成,仅含微量C2~4不饱和烯烃和芳烃,说明成矿过程基本未受到岩浆作用的影响。这些轻烃气为微生物作用成因和沉积岩围岩中Ⅱ类干酪根热解成因的混合气体。从有机气体组成看,嵩溪矿床的成矿背景属裂谷环境。本文的研究从一个侧面支持了作者等提出的嵩溪银(锑)矿可能属沉积热卤水改造型矿床的看法。  相似文献   

Microthermometric Evidence for the Formation of Ca-rich Hypersaline Brine and CO₂–rich Fluid in the Mori Geothermal Reservoir, Japan     

Yoichi MURAMATSU  Ryo KOMATSU  † 《Resource Geology》1999,49(1):27-37

Abstract: Fluid inclusions in hydrothermal quartz and anhydrite samples from the Mori geothermal field, southwest Hokkaido, have been studied microthermometrically using heating/freezing stages. Based on homogenization temperatures of fluid inclusions, salinities after correction of effect of freezing-point depression of CO₂ on ice melting temperatures of fluid inclusions, and previous geochemical data by Yoshida (1991), we discuss the geneses of various types of inclusion fluids in the Mori geothermal reservoir.  相似文献   

Chemical Composition and Geologic History of Saline Waters in Aux Vases and Cypress Formations, Illinois Basin     

Ilham Demir  Beverly Seyler 《Aquatic Geochemistry》1999,5(3):281-311

Seventy-six samples of formation waters were collected from oil wells producing from the Aux Vases or Cypress Formations in the Illinois Basin. Forty core samples of the reservoir rocks were also collected from the two formations. Analyses of the samples indicated that the total dissolved solids content (TDS) of the waters ranged from 43,300 to 151,400 mg/L, far exceeding the 35,400 mg/L of TDS found in typical seawater. Cl-Br relations suggested that high salinities in the Aux Vases and Cypress formation waters resulted from the evaporation of original seawater and subsequent mixing of the evaporated seawater with concentrated halite solutions. Mixing with the halite solutions increased Na and Cl concentrations and diluted the concentration of other ions in the formation waters. The elemental concentrations were influenced further by diagenetic reactions with silicate and carbonate minerals. Diagenetic signatures revealed by fluid chemistry and rock mineralogy delineated the water-rock interactions that took place in the Aux Vases and Cypress sandstones. Dissolution of K-feldspar released K into the solution, leading to the formation of authigenic illite and mixed-layered illite/smectite. Some Mg was removed from the solution by the formation of authigenic chlorite and dolomite. Dolomitization, calcite recrystallization, and contribution from clay minerals raised Sr levels significantly in the formation waters. The trend of increasing TDS of the saline formation waters with depth can be explained with density stratification. But, it is difficult to explain the combination of the increasing TDS and increasing Ca/Na ratio with depth without invoking the controversial 'ion filtration' mechanism.  相似文献   

青海一里平盐湖卤水Li-Na-K-Mg-Cl-SO_4-H_2O体系25℃时渗透系数、活度系数和饱和度的预测   总被引：2，自引：0，他引：2  

姚燕  宋彭生  张契 《海洋与湖沼》1999,(1)

将Ritrer离子作用模型的应用扩展到中国富含锂的一里平盐湖卤水Li－Na-K-Mg－Cl-SO4－H2O体系,综合1990－1997年作者对该体系的含锂三元次级体系25℃时的活度系数和渗透系数的研究结果和文献数据,给出了该体系的Pitzer离子作用模型参数;计算了溶解平衡常数;预测了青海一里平盐湖晶间卤水中离子和盐的活度系数、卤水的渗透系数、水活度、蒸汽压以及盐类的饱和度;揭示了卤水在蒸发和稀释过程中上述热力学性质随离子强度变化的规律,用离子强度与盐类饱和度的关联图（I-ln（K’／K）图）分析了该卤水的折盐顺序。计算结果表明,一旦平盐湖晶间因水在25℃时只有石盐饱和,与野外观测结果相一致;用参数化的Pitzer离子作用模型预测该卤水多组分体系的热力学性质和溶解平衡是可行的。  相似文献   

青藏高原盐湖资源的开发利用     

郑喜玉 《湖泊科学》1994,6(3):267-275

本文首先介绍了青藏高原盐湖的基本概况,分布特征;重点叙述了该区盐湖自然资源的类型、盐类沉积矿物组合,卤水的水化学成分,盐湖资源的规模和开发利用现状;提出了今后开发利用盐湖资源的方向和途径。  相似文献   

江西吉泰盆地卤水型锂钾矿物源区岩石地球化学特征及成因分析   总被引：1，自引：0，他引：1  

王春连  刘丽红  李强  孟令阳  刘成林  张媛媛  王九一  余小灿  颜开 《岩石矿物学杂志》2020,39(1):65-84

中国探明锂钾资源主要分布于青藏、罗布泊盐湖和川西等地,资源开发成本高、难度大,难以满足产业发展需求。目前,在江西吉泰盆地勘探发现卤水中氯化锂浓度超过600 mg/L,氯化钾含量接近1%,锂钾含量均超过或接近工业品位,综合利用价值高。本文在前人研究的基础上,通过对吉泰盆地中生代火成岩开展矿物学、岩石学、地球化学、流体包裹体研究以及高压釜水-岩反应模拟实验,重点研究了时间、温度、流体成分等对火成岩水-岩反应的影响,探究其对富钾锂卤水物质来源和成因机制的指示意义。研究结果表明,吉泰盆地卤水具有高锂低镁的特征,表明吉泰盆地卤水在成因上受到火山活动的影响;研究区岩浆发生不同程度的分异,火成岩蚀变作用强烈,表明地下热液对研究区火成岩的交代作用强烈,火成岩通过水-岩反应为富锂钾卤水矿提供了物质来源;温度是流体对元素的淋滤能力的主要控制因素,高盐度流体是各成矿元素主要的迁移载体;地表成因的卤水中Mg/Li值主要受原岩成分控制;水-岩反应是卤水形成的重要过程,而地表蒸发浓缩是卤水成矿最主要机理。  相似文献