Article(id=1236327865105576014, tenantId=1146029695717560320, journalId=1235980550691926019, issueId=1236327863171993957, articleNumber=null, orderNo=null, doi=10.3969/j.issn.0253-6099.2023.02.005, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1663689600000, receivedDateStr=2022-09-21, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1772693132902, onlineDateStr=2026-03-05, pubDate=1680278400000, pubDateStr=2023-04-01, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1772693132902, onlineIssueDateStr=2026-03-05, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1772693132902, creator=13701087609, updateTime=1772693132902, updator=13701087609, issue=Issue{id=1236327863171993957, tenantId=1146029695717560320, journalId=1235980550691926019, year='2023', volume='43', issue='2', pageStart='1', pageEnd='170', issueExtLink='null', onlineDate='null', pubDate='null', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1772693132441, creator=13701087609, updateTime=1772693403732, updator=13701087609, preIssue=null, nextIssue=null, ext={EN=IssueExt(id=1236329001107640372, tenantId=1146029695717560320, journalId=1235980550691926019, issueId=1236327863171993957, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1236329001107640373, tenantId=1146029695717560320, journalId=1235980550691926019, issueId=1236327863171993957, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null}, startPage=21, endPage=25, ext={EN=ArticleExt(id=1236327865415954532, articleId=1236327865105576014, tenantId=1146029695717560320, journalId=1235980550691926019, language=EN, title=Evolution Characteristics of Pore Structure During Alkaline In-Situ Leaching of Sandstone Type Uranium Deposit, columnId=1236276106018484431, journalTitle=Mining and Metallurgical Engineering, columnName=MINING, runingTitle=null, highlight=null, articleAbstract=

A core of uranium deposit was taken in an experiment of column leaching with alkaline solution (NaHCO3+H2O2), and then the surface characteristics and pore distribution of sandstone-type uranium deposit were analyzed by using scanning electron microscope images. The variation in the microscopic pore structure of uranium-bearing sandstone in alkaline in situ leaching process was characterized by using T2 spectrum of nuclear magnetic resonance (NMR). The results show that the matrix in the core firstly becomes connected pores due to chemical dissolution of leaching solution, resulting in more pore throats among large and small pores. The Al(OH)3 mineral colloid and CaCO3 generated by the reaction are deposited intensively in the pores and microcracks, which reduces the effective reaction area between leaching solution and matrix, thus reducing the uranium leaching efficiency. During the period of 97-158 h, dissolution is predominant, leading to the amount of chemical dissolution much higher than the amount of precipitation and accumulation, thus forming a large number of connected pores. Further reaction and dissolution of uranium minerals in the leaching solution can increase the recovery of uranium mineral to the peak.

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采用NaHCO3+H2O2碱性溶浸液对铀矿柱状岩芯进行了柱浸实验,利用电镜扫描图像分析了砂岩型铀矿表面特征和孔隙分布状况,以核磁共振T2谱定量表征碱性地浸过程中含铀砂岩微观孔隙结构变化。结果表明,溶浸液化学溶蚀作用下岩芯内部基质首先形成连通型孔隙,大、小孔间孔喉增加;反应生成的Al(OH)3矿物胶体和CaCO3集中沉淀堆积于小孔和微裂隙中,减小了溶浸液与基质有效接触反应面积,降低了铀矿浸出效率;97~158 h为溶蚀优势期,该阶段化学溶蚀量远大于沉淀堆积量,形成大量连通型孔隙,使铀矿物与溶浸液进一步反应溶解,铀矿采收率达到峰值。

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张通(1990-),男,山东济宁人,副教授,博士,主要研究方向为煤及共伴生资源协调开发。
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杨鑫(1997—),男,安徽安庆人,硕士研究生,主要研究方向为煤岩渗流力学。

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杨鑫(1997—),男,安徽安庆人,硕士研究生,主要研究方向为煤岩渗流力学。

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砂岩型铀矿碱性地浸过程孔隙结构演化特征
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杨鑫 1, 2 , 张通 2, 3 , 杜志明 4 , 唐明 2, 3 , 李燕芳 2, 3 , 毛钧林 1, 2 , 王鸣超 2, 3
矿冶工程杂志 | 采矿 2023,43(2): 21-25
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矿冶工程杂志 | 采矿 2023, 43(2): 21-25
砂岩型铀矿碱性地浸过程孔隙结构演化特征
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杨鑫1, 2, 张通2, 3, 杜志明4, 唐明2, 3, 李燕芳2, 3, 毛钧林1, 2, 王鸣超2, 3
作者信息
  • 1.安徽理工大学 矿业工程学院,安徽 淮南 232000
  • 2.合肥综合性国家科学中心能源研究院(安徽省能源实验室),安徽 合肥 230031
  • 3.安徽理工大学 安全科学与工程学院,安徽 淮南 232000
  • 4.核工业北京化工冶金研究院,北京 101149
  • 杨鑫(1997—),男,安徽安庆人,硕士研究生,主要研究方向为煤岩渗流力学。

通讯作者:

张通(1990-),男,山东济宁人,副教授,博士,主要研究方向为煤及共伴生资源协调开发。
Evolution Characteristics of Pore Structure During Alkaline In-Situ Leaching of Sandstone Type Uranium Deposit
Xin YANG1, 2, Tong ZHANG2, 3, Zhiming DU4, Ming TANG2, 3, Yanfang LI2, 3, Junlin MAO1, 2, Mingchao WANG2, 3
Affiliations
  • 1.School of Mining Engineering, Anhui University of Science and Technology, Huainan 232000, Anhui, China
  • 2.Institute of Energy, Hefei Comprehensive National Science Center (Anhui Energy Laboratory), Hefei 230031, Anhui, China
  • 3.School of Safety Science and Engineering, Anhui University of Science and Technology, Huainan 232000, Anhui, China
  • 4.Beijing Research Institute of Chemical Engineering Metallurgy, Beijing 101149, China
出版时间: 2023-04-01 doi: 10.3969/j.issn.0253-6099.2023.02.005
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采用NaHCO3+H2O2碱性溶浸液对铀矿柱状岩芯进行了柱浸实验,利用电镜扫描图像分析了砂岩型铀矿表面特征和孔隙分布状况,以核磁共振T2谱定量表征碱性地浸过程中含铀砂岩微观孔隙结构变化。结果表明,溶浸液化学溶蚀作用下岩芯内部基质首先形成连通型孔隙,大、小孔间孔喉增加;反应生成的Al(OH)3矿物胶体和CaCO3集中沉淀堆积于小孔和微裂隙中,减小了溶浸液与基质有效接触反应面积,降低了铀矿浸出效率;97~158 h为溶蚀优势期,该阶段化学溶蚀量远大于沉淀堆积量,形成大量连通型孔隙,使铀矿物与溶浸液进一步反应溶解,铀矿采收率达到峰值。

砂岩型铀矿  /  碱性地浸  /  孔隙结构  /  核磁共振  /  铀  /  柱浸

A core of uranium deposit was taken in an experiment of column leaching with alkaline solution (NaHCO3+H2O2), and then the surface characteristics and pore distribution of sandstone-type uranium deposit were analyzed by using scanning electron microscope images. The variation in the microscopic pore structure of uranium-bearing sandstone in alkaline in situ leaching process was characterized by using T2 spectrum of nuclear magnetic resonance (NMR). The results show that the matrix in the core firstly becomes connected pores due to chemical dissolution of leaching solution, resulting in more pore throats among large and small pores. The Al(OH)3 mineral colloid and CaCO3 generated by the reaction are deposited intensively in the pores and microcracks, which reduces the effective reaction area between leaching solution and matrix, thus reducing the uranium leaching efficiency. During the period of 97-158 h, dissolution is predominant, leading to the amount of chemical dissolution much higher than the amount of precipitation and accumulation, thus forming a large number of connected pores. Further reaction and dissolution of uranium minerals in the leaching solution can increase the recovery of uranium mineral to the peak.

sandstone-type uranium deposit  /  alkaline in-situ leaching  /  pore structure  /  nuclear magnetic resonance (NMR)  /  uranium  /  column leaching
杨鑫, 张通, 杜志明, 唐明, 李燕芳, 毛钧林, 王鸣超. 砂岩型铀矿碱性地浸过程孔隙结构演化特征. 矿冶工程杂志, 2023 , 43 (2) : 21 -25 . DOI: 10.3969/j.issn.0253-6099.2023.02.005
Xin YANG, Tong ZHANG, Zhiming DU, Ming TANG, Yanfang LI, Junlin MAO, Mingchao WANG. Evolution Characteristics of Pore Structure During Alkaline In-Situ Leaching of Sandstone Type Uranium Deposit[J]. Mining and Metallurgical Engineering, 2023 , 43 (2) : 21 -25 . DOI: 10.3969/j.issn.0253-6099.2023.02.005
  • 合肥综合性国家科学中心能源研究院重大培育项目(21KZS216)
  • 国家自然科学基金(51904011)
  • 安徽省高校协同创新项目(GXXT-2021-019)
2023年第43卷第2期
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doi: 10.3969/j.issn.0253-6099.2023.02.005
  • 接收时间:2022-09-21
  • 首发时间:2026-03-05
  • 出版时间:2023-04-01
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  • 收稿日期:2022-09-21
基金
合肥综合性国家科学中心能源研究院重大培育项目(21KZS216)
国家自然科学基金(51904011)
安徽省高校协同创新项目(GXXT-2021-019)
作者信息
    1.安徽理工大学 矿业工程学院,安徽 淮南 232000
    2.合肥综合性国家科学中心能源研究院(安徽省能源实验室),安徽 合肥 230031
    3.安徽理工大学 安全科学与工程学院,安徽 淮南 232000
    4.核工业北京化工冶金研究院,北京 101149

通讯作者:

张通(1990-),男,山东济宁人,副教授,博士,主要研究方向为煤及共伴生资源协调开发。
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2种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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