Professional Committee of Rock and Mineral Testing Technology of the Geological Society of China, National Geological Experiment and Testing CenterHost
2021 Vol. 40, No. 3
Article Contents

LI Hao-nan, REN Xiang-wen, SONG Zhao-jun, LI Huai-ming, WANG Wen-yu. Studies on Analysis Conditions of Specific Surface Area of Polymetallic Nodules[J]. Rock and Mineral Analysis, 2021, 40(3): 435-443. doi: 10.15898/j.cnki.11-2131/td.202008140114
Citation: LI Hao-nan, REN Xiang-wen, SONG Zhao-jun, LI Huai-ming, WANG Wen-yu. Studies on Analysis Conditions of Specific Surface Area of Polymetallic Nodules[J]. Rock and Mineral Analysis, 2021, 40(3): 435-443. doi: 10.15898/j.cnki.11-2131/td.202008140114

Studies on Analysis Conditions of Specific Surface Area of Polymetallic Nodules

More Information
  • BACKGROUND

    Polymetallic nodules are predominant in deep sea sedimentary mineral resources due to the enrichment of many critical metals. Polymetallic nodules are loose and porous, which is the critical material feature that contributes the adsorption of trace metals from seawater and pore water and then enrichment and mineralization. Therefore, specific surface area (SSA) is one of the key factors for studying the ore-forming process of polymetallic nodules. At present, the methods for SSA determination are well-developed. However, they are less applied in the analysis of the specific surface of polymetallic nodules, and the pretreatment conditions are not constant according to various research targets.

    OBJECTIVES

    In order to explore the pretreatment conditions for the BET SSA analysis of polymetallic nodules, and provide necessary parameters for the study of the enrichment of trace metals in polymetallic nodules.

    METHODS

    Polymetallic nodules from the Atlantic, Indian, and Pacific oceans were collected. The pretreatment conditions including temperature, duration, and particle size for SSA analysis of polymetallic nodules were studies by applying temperature programming, heating accumulation, and particle size comparing methods.

    RESULTS

    The results showed that the analysis values of SSA reached plateau when the heating temperature ranged from 210℃to 350℃. The analysis values of SSA remained constant after heating for 3 hours by a step of 1 hour at 210℃. The SSA values of samples with a size of several millimeters were 1.027-28.535m2/g higher compared with those of the same samples crushed into microns.

    CONCLUSIONS

    Reliable SSA values can be obtained when the polymetallic nodules with sizes of several millimeters are heated in a vacuum system for 3 hours at 210℃, which is the pretreatment condition for analyzing SSA of mineralization-related polymetallic nodules.

  • 加载中
  • [1] Hein J R, Koschinsky A, Kuhn T. Deep-ocean polymetallic nodules as a resource for critical materials[J]. Nature Reviews Earth & Environment, 2020, 1: 158-169.

    Google Scholar

    [2] Hein J R, Mizell K, Koschinsky A, et al. Deep-ocean mineral deposits as a source of critical metals for high-and green-technology applications: Comparison with land-based resources[J]. Ore Geology Reviews, 2013, 51: 1-14. doi: 10.1016/j.oregeorev.2012.12.001

    CrossRef Google Scholar

    [3] Hein J R, Spinardi F, Okamoto N, et al. Critical metals in manganese nodules from the Cook Islands EEZ, abundances and distributions[J]. Ore Geology Reviews, 2015, 68: 97-116. doi: 10.1016/j.oregeorev.2014.12.011

    CrossRef Google Scholar

    [4] Fu Y Z, Wen H J. Variabilities and enrichment mechanisms of the dispersed elements in marine Fe-Mn deposits from the Pacific Ocean[J]. Ore Geology Reviews, 2020, 121: 103470.

    Google Scholar

    [5] Morgan C L. Resource estimates of the Clarion-Clipperton manganese nodule deposits[M]//Cronan D S. Handbook of marine mineral deposits. Florida: CRC Press, 2000: 145-170.

    Google Scholar

    [6] 陈其慎, 张艳飞, 贾德龙, 等. 全球矿业发展报告2019[N]. 北京: 中国矿业报社, 2019.

    Google Scholar

    Chen Q S, Zhang Y F, Jia D L, et al. Global mining development report 2019[N]. Beijing: China Mining News Agency, 2019.

    Google Scholar

    [7] 杨卉芃, 王威. 全球钴矿资源现状及开发利用趋势[J]. 矿产保护与利用, 2019(5): 41-49.

    Google Scholar

    Yang H P, Wang W. Global cobalt resources status and exploitation trends[J]. Conservation and Utilization of Mineral Resources, 2019(5): 41-49.

    Google Scholar

    [8] 董志国, 王鸣, 李晓欣, 等. 航空发动机涡轮叶片材料的应用与发展[J]. 钢铁研究学报, 2011, 23(Supplement 2): 455-457.

    Google Scholar

    Dong Z G, Wang M, Li X X, et al. Application and progress of materials for turbine blade of aeroengine[J]. Journal of Iron and Steel Research, 2011, 23(Supplement 2): 455-457.

    Google Scholar

    [9] Kuhn T, Wegorzewski A, Rühlemann C, et al. Composition, formation, and occurrence of polymetallic nodules[M]//Sharma R. Deep-sea mining. Switzerland: Springer, 2017: 23-63.

    Google Scholar

    [10] Biller D V, Bruland K W. Analysis of Mn, Fe, Co, Ni, Cu, Zn, Cd, and Pb in seawater using the Nobias-chelate PA1 resin and magnetic sector inductively coupled plasma mass spectrometry (ICP-MS)[J]. Marine Chemistry, 2012, 130-131: 12-20. doi: 10.1016/j.marchem.2011.12.001

    CrossRef Google Scholar

    [11] Tamura H, Katayama N, Furuichi R. The Co2+ adsorption properties of Al2O3, Fe2O3, Fe3O4, TiO2 and MnO2 evaluated by modeling with the Frumkin isotherm[J]. Journal of Colloid and Interface Science, 1997, 195: 192-202.

    Google Scholar

    [12] Hein J R, Koschinsky A. Deep-ocean ferromanganese crusts and nodules[M]. Holland H D, Turekian K K. Treatise on geochemistry (The second edition). Oxford: Elsevier, 2014: 273-291.

    Google Scholar

    [13] Huk C A, Ku T L. Radiochemical observations on manganese nodules from three sedimentary environments in the North Pacific[J]. Geochemica et Cosmochimica Acta, 1984, 48: 951-963.

    Google Scholar

    [14] Li D F, Fu Y, Sun X, et al. Critical metal enrichment mechanism of deep-sea hydrogenetic nodules: Insights from mineralogy and element mobility[J]. Ore Geology Reviews, 2020, 118: 1-13.

    Google Scholar

    [15] 刘珍, 曲希玉, 王伟庆, 等. 比表面积氮气吸附法在蒙脱石碱性溶蚀表征中的应用[J]. 岩矿测试, 2016, 35(6): 603-611.

    Google Scholar

    Liu Z, Qu X Y, Wang W Q, et al. Application of specific surface area nitrogen adsorption method to characterize the alkaline dissolution of montmorillonite[J]. Rock and Mineral Analysis, 2016, 35(6): 603-611.

    Google Scholar

    [16] 梁建伟, 房营光, 谷任国. 极细粒黏土的比表面积测试与分析[J]. 科学技术与工程, 2009, 9(9): 2371-2377.

    Google Scholar

    Liang J W, Fang Y G, Gu R G. Experiment and analysis of specific area of tiny-particle clay[J]. Science Technology and Engineering, 2009, 9(9): 2371-2377.

    Google Scholar

    [17] 唐洪明, 王俊杰, 张烈辉, 等. 页岩比表面积测试方法与控制因素研究[J]. 天然气地球科学, 2015, 26(11): 2009-2016.

    Google Scholar

    Tang H M, Wang J J, Zhang L H, et al. Testing method and controlling factors of specific surface area of shales[J]. Natural Gas Geoscience, 2015, 26(11): 2009-2016.

    Google Scholar

    [18] 陈生蓉, 帅琴, 高强, 等. 基于扫描电镜-氮气吸脱附和压汞法的页岩孔隙结构研究[J]. 岩矿测试, 2015, 34(6): 36-42.

    Google Scholar

    Chen S R, Shuai Q, Gao Q, et al. Analysis of the pore structure of shale in Ordos Basin by SEM with sitrogen gas adsorption-desorption[J]. Rock and Mineral Analysis, 2015, 34(6): 36-42.

    Google Scholar

    [19] Mastalerz M, Wei L, Drobniak A, et al. Responses of specific surface area and micro-and mesopore characteristics of shale and coal to heating at elevated hydrostatic and lithostatic pressures[J]. International Journal of Coal Geology, 2018, 197: 20-30.

    Google Scholar

    [20] Xiong F Y, Jiang Z X, Li P, et al. Pore structure of transitional shales in the Ordos Basin, NW China: Effects of composition on gas storage capacity[J]. Fuel, 2017, 206: 504-515.

    Google Scholar

    [21] Chen L, Jiang Z X, Liu K Y, et al. A combination of N2 adsorption to characterize nanopore structure of organic-rich Lower Silurian shale in the Upper Yangtze Platform, South China: Implications for shale sorption capacity[J]. Acta Geologica Sinica, 2017, 91(4): 1380-1394.

    Google Scholar

    [22] Bl the M, Wegorzewski A, Müller C, et al. Manganese-cycling microbial communities inside deep-sea manganese nodules[J]. Environmental Science and Technology, 2015, 49(13): 7692-7700.

    Google Scholar

    [23] Stashchuk M F, Chervonetsky D V, Kaplun E V, et al. Adsorption properties of ferromanganese crusts and nodules[M]. Northwest Pacific and Bering Sea sediment geochemistry and paleoceanographic studies, 1994.

    Google Scholar

    [24] Parida K M, Satapathy P K, Das N N, et al. Studies on Indian Ocean manganese nodules Part 2: Physico-chemical characteristics and catalytic activity of heat-treated marine manganese nodules[J]. Journal of Colloid and Interface Science, 1996, 179: 241-248.

    Google Scholar

    [25] 薛婷. 太平洋海山富钴结壳地球化学特征及成矿元素富集机制[D]. 广州: 中山大学, 2007.

    Google Scholar

    Xue T. Geochemical characters and ore-forming elements enrichment mechanism of ferromanganese crusts from Pacific Ocean[D]. Guangzhou: Sun Yat-Sen University, 2007.

    Google Scholar

    [26] Glasby G P. Manganese: Predominantrole of nodules and crusts[M]//Schulz H D, Zabel M. Marine geochemistry (2nd edition). Berlin: Springer, 2006: 371-427.

    Google Scholar

    [27] 钱江初, 初凤友, 冯旭文. 大洋多金属结核中几种常见锰矿相的特征及其相关性[J]. 矿物学报, 2006, 26(2): 152-158.

    Google Scholar

    Qian J C, Chu F Y, Feng X W. The main manganates in the polymetallic nodules and their correlations[J]. Acta Mineralogica Sinica, 2006, 26(2): 152-158.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(3)

Tables(3)

Article Metrics

Article views(2239) PDF downloads(89) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint