ESTIMATION OF FACTORS OF THE MECHANISM OF FORMATION OF DRAINAGE WATERS OF VARIOUS TECHNOLOGICAL TYPES OF ORES OF COPPER SANDSTONE DEPOSITS BY THERMODYNAMIC MODELING OF THE «WATER-ROCK-GAS» SYSTEM

O. A. Limantseva, B. Ryzhenko
{"title":"ESTIMATION OF FACTORS OF THE MECHANISM OF FORMATION OF DRAINAGE WATERS OF VARIOUS TECHNOLOGICAL TYPES OF ORES OF COPPER SANDSTONE DEPOSITS BY THERMODYNAMIC MODELING OF THE «WATER-ROCK-GAS» SYSTEM","authors":"O. A. Limantseva, B. Ryzhenko","doi":"10.31554/978-5-7925-0584-1-2020-394-397","DOIUrl":null,"url":null,"abstract":"SUMMARY: In the paper the physical and chemical conditions are considered for the formation of the chemical com-position of waters draining rocks and ores of the copper sandstone deposit, with more attention to the main factors of their acidification. Thermodynamic simulation of water-rock-gas system shows that pyrite percentage is key factor for aggressive medium formation at pyrite content more than 1% and lgf O 2 >-20. Relative water filtration speed expressed by mass of rock (R) to mass of Water (W) decreases aqueous pH at R/W>0.1.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"73 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31554/978-5-7925-0584-1-2020-394-397","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

SUMMARY: In the paper the physical and chemical conditions are considered for the formation of the chemical com-position of waters draining rocks and ores of the copper sandstone deposit, with more attention to the main factors of their acidification. Thermodynamic simulation of water-rock-gas system shows that pyrite percentage is key factor for aggressive medium formation at pyrite content more than 1% and lgf O 2 >-20. Relative water filtration speed expressed by mass of rock (R) to mass of Water (W) decreases aqueous pH at R/W>0.1.
用“水-岩-气”系统的热力学模型估计铜砂岩矿床不同工艺类型矿石排水水形成机制的因素
摘要:本文考虑了铜砂岩排水岩和矿石化学成分形成的物理化学条件,重点研究了其酸化的主要因素。水-岩-气系统热力学模拟结果表明,黄铁矿含量大于1%,lgf o2 ~ 20时,黄铁矿含量是侵蚀介质形成的关键因素。以岩石质量(R)与水质量(W)表示的相对水过滤速度在R/W = 0.1时降低了水的pH值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信