Study and Application of a Wet Ball Milling Ultra-fine Method for Geological Samples
-
摘要:
当前实验室制备的地质样品存在大颗粒微粒,影响了样品代表性和分析结果的准确度,制备超细样品是有效的解决办法。本文建立了水为助磨剂,湿法球磨制备超细地质样品的方法。结果表明,氧化锆或碳化钨材质的球磨罐会污染样品中锆、钨及钴等微量元素,而玛瑙材质的球磨罐污染样品的风险较小;采用玛瑙材质的球磨罐,20g样品,液固比为1∶1,磨球配置为大8颗、中16颗、小48颗,球磨时间30min,运用该方法对四种代表性样品(岩石、土壤、沉积物及稀土矿石)进行球磨,粒度检测结果表明,球磨后的样品粒度均达到1000目;对60件未知基质类型的样品进行湿法球磨后,D50均小于5μm,D90均小于19μm,表明该方法具有一定的适用性;微观形貌研究表明,球磨制备的样品,大颗粒微粒显著减少,颗粒分布更加均匀;对球磨后的岩石标准物质(GBW07104)进行了取样量试验,所检测的46种元素结果进行统计,除Mo、Cd、Cr等元素外,取样量可减少至2mg;制备的超细样品与电感耦合等离子体质谱(ICP-MS)技术联用,可发挥ICP-MS高灵敏度的效能,同时提高检测效率、减少环境污染。
-
关键词:
- 地质样品 /
- 湿法球磨 /
- 超细化 /
- 微观形貌 /
- 电感耦合等离子体质谱法
Abstract:BACKGROUND At present, there are large particles in geological samples prepared in the laboratory, which affect the representativeness of the samples and the accuracy of the analysis results[1-3]. With the rapid development of modern analytical instruments, analytical methods based on inductively coupled plasma-mass spectrometry (ICP-MS) have been widely used in laboratories across the country for the simultaneous determination of multiple elements in geological samples due to their low detection limit, high analytical flux, and wide linear range[10-14]. Its characteristics of high sensitivity and analytical accuracy, small sample injection volume, and high requirements for sample representativeness are incompatible with the sample preparation technology that serves as the foundation of laboratory analysis work. Therefore, there is an urgent need to research and develop sample preparation methods that reduce sample size and improve representativeness, in order to meet the needs of ultra trace element detection. The main methods for preparing ultrafine geological samples include air flow pulverization and ball milling. Air flow pulverization is widely used in the preparation of geological standard material samples, but the sample size prepared in one step is large, which is prone to sample grading and requires secondary mixing[16-17]. Dry ball milling is a common geological sample preparation method in laboratories. Prolonging the ball milling time is beneficial for sample refinement, but it can easily cause contamination by the characteristic elements of the ball milling tank material. Wet ball milling can form a slurry between the sample and the grinding aid, which is conducive to the flow of the sample and the grinding ball during the ball milling process, increasing the friction between them, and achieving the goal of further refining the sample[21].
OBJECTIVES To establish a method of preparing ultra-fine geological samples by wet ball grinding with water as the grinding aid.
METHODS Weigh 20g samples into the ball mill tank made of agate material, and add 20mL water and grinding balls (8 pieces of Φ10mm balls, 16 pieces of Φ5mm balls, and 48 pieces of Φ2mm balls). Cover the lid, and grind at 300r/min for 30min. XRD were used to characterize the crystal state of the minerals during ball milling. The sampling quantity of different elements was explored by ICP-OES and ICP-MS.
RESULTS (1) A method for preparing ultrafine geological samples by wet ball grinding was established in laboratory. Agate tanks were used for ball milling, and there was a low risk of sample contamination. When water was used as a liquid grinding aid and the ratio of solid to liquid (m/V) was 1, the grinding effect was better. (2) Four representative samples (rock, soil, sediment, and rare earth ore) were ball milled using this method, and the test results showed that the particle size of the samples after ball milling reached 1000 mesh. After wet ball milling of 60 samples of unknown matrix types, the D50 was less than 5μm, and the D90 was less than 19μm. (3) The grinding aid can reduce the surface energy of the grinding material and improve the grinding efficiency. The micromorphology of the samples prepared by ball milling showed that the large particles were significantly reduced, wet ball milling makes the particle size of each sample finer and the particle distribution more uniform, and the maximum particle diameter was reduced by about 5 times. The sampling quantity test was carried out on the rock sample (GBW07104) after ball milling, and 46 elements results were statistically analyzed. The sampling quantity was reduced to 2mg except for Mo, Cd, Cr.
CONCLUSIONS After ball milling, the large particles are significantly reduced and the particle distribution is more uniform, which better solves the problem of ultrafine preparation of relevant types of samples in the laboratory, but there are some problems such as a long sample preparation process. The ultra-fine preparation technology of geological samples, combined with XRF and LA-ICP-MS, establishes a green analysis method of solid sampling with small sample quantity, and assists in the development of the detection industry.
-
-
表 1 不同材质罐体制备超细样品粒径分布及W、Zr、Co元素含量(n=3)
Table 1. Particle size distribution and W, Zr, Co content of ultrafine samples prepared by tanks with different materials (n=3).
样品编号 球磨罐材质 粒径(μm) 元素含量(μg/g) D90 D50 D10 W Zr Co 1 未球磨处理 72.58 6.38 0.85 0.45 99 13.2 2 玛瑙罐 20.36 4.86 0.84 0.47 96 13.8 3 氧化锆罐 12.21 2.95 0.71 1.50 10401 14.5 4 碳化钨罐 7.78 1.64 0.15 4113 122 404 -
[1] 王毅民, 王晓红, 高玉淑, 等. 中国地质标准物质制备技术与方法研究进展[J]. 地质通报, 2010, 29(7): 1090−1104.
Wang Y M, Wang X H, Gao Y S, et al. Advances in preparing techniques for geochemical reference materials in China[J]. Geological Bulleti of China, 2010, 29(7): 1090−1104.
[2] 涂家润, 卢宜冠, 孙凯, 等. 应用微束分析技术研究铜钴矿床中钴的赋存状态[J]. 岩矿测试, 2022, 41(2): 226−238. doi: 10.15898/j.cnki.11-2131/td.202112060194
Tu J R, Lu Y G, Sun K, et al. Application of microbeam analytical technology to study the occurrence of cobalt from copper-cobalt deposits[J]. Rock and Mineral Analysis, 2022, 41(2): 226−238. doi: 10.15898/j.cnki.11-2131/td.202112060194
[3] 闫斌, 朱祥坤, 陈岳龙. 样品量的大小对铜锌同位素测定值的影响[J]. 岩矿测试, 2011, 30(4): 400−405. doi: 10.3969/j.issn.0254-5357.2011.04.004
Yan B, Zhu X K, Chen Y L. Effects of sample size on Cu and Zn isotope ratio measurements[J]. Rock and Mineral Analysis, 2011, 30(4): 400−405. doi: 10.3969/j.issn.0254-5357.2011.04.004
[4] 王祎亚, 王毅民. 超细标准物质与超细样品分析研究进展[J]. 光谱学与光谱分析, 2021, 41(3): 696−703.
Wang Y Y, Wang Y M. Research progress of ultra-fine reference materials and ultra-fine samples[J]. Spectroscopy and Spectral Analysis, 2021, 41(3): 696−703.
[5] 程志中, 刘妹, 黄宏库, 等. 镍矿石和镍精矿标准物质研制[J]. 岩矿测试, 2013, 32(4): 86-93. doi: 10.3969/j.issn.0254-5357.2013.04.009
Cheng Z Z, Liu M, Huang H K, et al. Preparation and certification of nickel ore and nickel concentrate reference materials[J]. Rock and Mineral Analysis, 2013, 32(4): 600−607. doi: 10.3969/j.issn.0254-5357.2013.04.009
[6] 王晓红, 何红蓼, 王毅民, 等. 超细样品的地质分析应用[J]. 分析测试学报, 2010, 29(6): 578−583.
Wang X H, He H L, Wang Y M, et al. Geoanalytical techniques using ultra-fine samples[J]. Journal of Instrumental Analysis, 2010, 29(6): 578−583.
[7] 刘青山, 靳宏, 臧世阳, 等. 粒度不均匀铬矿石取样代表性的研究[J]. 岩矿测试, 2012, 31(6): 997−999. doi: 10.15898/j.cnki.11-2131/td.2012.06.015
Liu Q S, Jin H, Zang S Y, et al. A study on the representativeness of sampling for non-uniform particle size chrome ore[J]. Rock and Mineral Analysis, 2012, 31(6): 997−999. doi: 10.15898/j.cnki.11-2131/td.2012.06.015
[8] Flores É M M, Barin J S, Mesko M F, et al. Sample preparation techniques based on combustion reactions in closed vessels—A brief overview and recent applications[J]. Spectrochimica Acta Part B:Atomic Spectroscopy, 2007, 62: 1051−1064. doi: 10.1016/j.sab.2007.04.018
[9] 熊英, 陈文科, 田萍, 等. 含粗粒金矿样品采集加工与分析研究进展[J]. 岩矿测试, 2015, 34(1): 12−18. doi: 10.15898/j.cnki.11-2131/td.2015.01.004
Xiong Y , Chen W K , Tian P, et al. Review on collection, processing and analysis of coarse gold-containing ore samples[J]. Rock and Mineral Analysis, 2015, 34(1): 12-18. doi: 10.15898/j.cnki.11-2131/td.2015.01.004
[10] Agatemor C, Beauchemin D. Matrix effects in inductively coupled plasma mass spectrometry: A review[J]. Analytica Chimica Acta, 2011, 706(1): 66−83. doi: 10.1016/j.aca.2011.08.027
[11] Linge K L. Trace element determination by ICP-AES and ICP-MS developments and applications reported during 2006 and 2007[J]. Geostandards and Geoanalytical Research, 2008, 32: 16.
[12] Guerrero M M L, Alonso E V, García de Torres A, et al. Simultaneous determination of traces of Pt, Pd, Os, Ir, Rh, Ag and Au metals by magnetic SPE-ICP-OES and in situ chemical vapour generation[J]. Journal of Analytical Atomic Spectrometry, 2017, 32: 2281−2291. doi: 10.1039/C7JA00271H
[13] Sébastien A, Michel V, Mireille P, et al. A routine method for oxide and hydroxide interference corrections in ICP-MS chemical analysis of environmental and geological samples[J]. Geostandards and Geoanalytical Research, 2007, 24: 19−31.
[14] Eggins S M, Woodhead J D, Kinsley L P J, et al. A simple method for the precise determination of ≥40 trace elements in geological samples by ICP-MS using enriched isotope internal standardisation[J]. Chemical Geology, 1997, 134: 311−326. doi: 10.1016/S0009-2541(96)00100-3
[15] 王娜, 徐铁民, 魏双, 等. 微波消解-电感耦合等离子体质谱法测定超细粒度岩石和土壤样品中的稀土元素[J]. 岩矿测试, 2020, 39(1): 68−76.
Wang N, Xu T M, Wei S, et al. Determination of rare earth elements in ultra-fine rock and soil samples by ICP-MS using microwave digestion[J]. Rock and Mineral Analysis, 2020, 39(1): 68−76.
[16] 郑存江, 刘清辉, 胡勇平, 等. 富钴结壳超细标准物质的加工制备[J]. 岩矿测试, 2010, 29(3): 301−304.
Zheng C J, Liu Q H, Hu Y P, et al. Processing and preparation of ultra-fine Co-rich crust reference materials[J]. Rock and Mineral Analysis, 2010, 29(3): 301−304.
[17] 赵晓亮, 李志伟, 王烨, 等. 铌钽精矿标准物质研制[J]. 岩矿测试, 2018, 37(6): 687−694. doi: 10.15898/j.cnki.11-2131/td.201711230185
Zhao X L, Li Z W, Wang Y, et al. Preparation and certification of niobium-tantalum concentrate reference materials[J]. Rock and Mineral Analysis, 2018, 37(6): 687−694. doi: 10.15898/j.cnki.11-2131/td.201711230185
[18] Balcerzak M. Sample digestion methods for the determination of traces of precious metals by spectrometric techniques[J]. Analytical Sciences, 2002, 18: 737−750. doi: 10.2116/analsci.18.737
[19] 孙德忠, 何红蓼. 封闭酸溶-等离子体质谱法分析超细粒度地质样品中42个元素[J]. 岩矿测试, 2007, 26(1): 21−25. doi: 10.3969/j.issn.0254-5357.2007.01.006
Sun D Z, He H L. Determination of 42 elements in ultra-fine geological samples by inductively coupled plasma-mass spectrometry with pressurized acid digestion[J]. Rock and Mineral Analysis, 2007, 26(1): 21−25. doi: 10.3969/j.issn.0254-5357.2007.01.006
[20] 王毅民, 陈幼平. 近30年来我国地质分析重要成果评介[J]. 地质论评, 2008, 54(5): 653−669. doi: 10.3321/j.issn:0371-5736.2008.05.010
Wang Y M, Chen Y P. Review on important achievements of geoanalysis in last 30 years of Cnina[J]. Geological Review, 2008, 54(5): 653−669. doi: 10.3321/j.issn:0371-5736.2008.05.010
[21] 杜高翔, 王海荣, 柴红勇, 等. 粉体制备中助磨剂的应用研究现状[J]. 化工矿物与加工, 2004(10): 6−9. doi: 10.3969/j.issn.1008-7524.2004.10.002
Du G X, Wang H R, Chai H Y, et al. Study status of application of grinding aids in the preparation of powders[J]. Industrial Minerals & Processing, 2004(10): 6−9. doi: 10.3969/j.issn.1008-7524.2004.10.002
[22] 高伟, 王泽红, 毛勇. 助磨剂在石英粉磨中的应用研究现状及发展趋势[J]. 金属矿山, 2019, 48(9): 22−27. doi: 10.19614/j.cnki.jsks.201909004
Gao W, Wang Z H, Mao Y. Research status and development trend of grinding aid in quartz grinding[J]. Metal Mine, 2019, 48(9): 22−27. doi: 10.19614/j.cnki.jsks.201909004
[23] He M, Forssberg E. Rheological behaviors in wet ultrafine grinding of limestone[J]. Minerals and Metallurgical Processing, 2007, 24: 19−29.
[24] Hasegawa M, Kimata M, Shimane M, et al. The effect of liquid additives on dry ultrafine grinding of quartz[J]. Powder Technology, 2001, 114: 145−151. doi: 10.1016/S0032-5910(00)00290-4
[25] Wang X, Li G, Zhang Q, et al. Determination of major/ minor and trace elements in seamount phosphorite by XRF spectrometry[J]. Geostandards and Geoanalytical Research, 2004, 28: 81−88. doi: 10.1111/j.1751-908X.2004.tb01044.x
[26] Wang Y, Gao Y, Wang X, et al. Investigations into the preparation of ultra-fine particle size geochemical reference materials[J]. Geostandards and Geoanalytical Research, 2007, 28: 113−121.
[27] 王焰, 钟宏, 曹勇华, 等. 我国铂族元素, 钴和铬主要矿床类型的分布特征及成矿机制[J]. 科学通报, 2020, 65(33): 3825−3838. doi: 10.1360/TB-2020-0202
Wang Y, Zhong H, Cao Y H, et al. Genetic classification, distribution and ore genesis of major PGE, Co and Cr deposits in China: A critical review[J]. Chinese Science Bulletin, 2020, 65(33): 3825−3838. doi: 10.1360/TB-2020-0202
[28] 周成胶, 张刚阳, 张丁川. 铼金属矿床类型, 元素赋存形式和富集机制[J]. 地质科技情报, 2021, 40(4): 115−130.
Zhou C J, Zhang G Y, Zhang D C. Types, element occurrence forms and enrichment mechanisms of rhemium metal deposits[J]. Bulletin of Geological Science and Technology, 2021, 40(4): 115−130.
-