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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

CN 11-5982/P

Postal Subscription Code 80-963

2018 Impact Factor: 1.205

Front. Earth Sci.    2023, Vol. 17 Issue (1) : 230-250    https://doi.org/10.1007/s11707-022-1018-x
RESEARCH ARTICLE
Geochemistry of rare earth elements and yttrium in Late Permian coals from the Zhongliangshan coalfield, southwestern China
Qingfeng LU1,2,3, Shenjun QIN2(), Hongyang BAI1,3, Wenfeng WANG1,3(), De’e QI2, Xin HE1,3, Bofei ZHANG1,3
1. School of Resources and Geosciences, China University of Mining & Technology, Xuzhou 221116, China
2. Key Laboratory for Resource Exploration Research of Hebei Province, Hebei University of Engineering, Handan 056038, China
3. Key Laboratory of Coalbed Methane Resources & Reservoir Formation Process, Ministry of Education, China University of Mining & Technology, Xuzhou 221008, China
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Abstract

Rare earth elements and yttrium (REY) in coal deposits are considered promising alternative sources for these resources owing to their increasing global demand. This paper reports the geochemical characteristics of REY in the Late Permian coals from an underground K1a seam section of the Zhongliangshan coalfield in Chongqing, southwestern China. The mineralogy, degree of enrichment, distribution patterns, modes of occurrence, and sediment origin of REY were investigated. Compared with the average of world coals, the concentration of REY in the K1a coals were normal, dominated by light REY (LREY), with less medium and heavy REY (MREY, HREY). The fractionation degree of the MREY and HREY are higher than that of LREY in most K1a coal samples, deduced from the mixed enrichment type of REY, mainly including M-H-type, and a few L-M type and H-type. In addition, the combination of anomalies of Ce, Eu, Gd, and Al2O3/TiO2 parameters, the terrigenous materials in the K1a coal were derived from the felsic-intermediate rocks at the top of the Emeishan basalt sequence, and the samples were affected by seawater intrusion during early peat accumulation. Although the minerals primarily consist of kaolinite, illite, pyrite, and small amounts of quartz, calcite and anatase, REY are correlated with ash yield, SiO2, and Al2O3, revealing that the REY mainly occur in aluminosilicate minerals, especially kaolinite and illite. Meanwhile, REY positively relate to P2O5 and Zr, which may exist in phosphate-containing minerals or zircon. Furthermore, most samples in the K1a coal or ash do not reach the cut-off grade for the beneficial recovery of REY. With the exception of central Guizhou, southwestern Chongqing, and the junction of western Guizhou and northeastern Yunnan, the REY content in coals from southwestern China are high, and its by-products are suitable as potential REY sources.

Keywords rare earth elements and yttrium      Zhongliangshan K1a coal      sediment source      modes of occurrence      geochemical characteristics     
Corresponding Author(s): Shenjun QIN,Wenfeng WANG   
About author:

* These authors contributed equally to this work.

Online First Date: 28 October 2022    Issue Date: 03 July 2023
 Cite this article:   
Qingfeng LU,Shenjun QIN,Hongyang BAI, et al. Geochemistry of rare earth elements and yttrium in Late Permian coals from the Zhongliangshan coalfield, southwestern China[J]. Front. Earth Sci., 2023, 17(1): 230-250.
 URL:  
https://academic.hep.com.cn/fesci/EN/10.1007/s11707-022-1018-x
https://academic.hep.com.cn/fesci/EN/Y2023/V17/I1/230
Fig.1  Location of five coalfields (ZLS, Zhongliangshan; TF, Tianfu; YR, Yongrong; SZ, Songzao; NT, Nantong).
Fig.2  Stratigraphic column of the Late Permian Longtan Formation from the Zhongliangshan, Chongqing.
SamplesKaoliniteIllite+I/SQuartzCalcitePyriteAnatase
ZLS-R10.652.511.23.318.24.2
ZLS-134.318.31727.13.3
ZLS-362.211.69.913.72.6
ZLS-775.74.211.58.6
ZLS-935.954.41.41.96.4
ZLS-1357.239.82.70.3
ZLS-1739.535.729.813.0
ZLS-1833.444415.63.1
ZLS-P5135.106.37.6
ZLS-2155.726.78.46.52.8
Tab.1  The proportions of minerals in the Zhongliangshan coal LTAs (%)
Fig.3  Minerals in the Zhongliangshan K1a coal.
SamplesLREYMREYHREYSum
LaCePrNdSmEuGdTbDyYHoErTmYbLu
ZLS-R37.4670.038.5536.837.241.525.670.683.3116.000.651.760.251.580.28191.8
ZLS-118.0433.583.7416.953.090.632.760.361.9410.940.421.180.191.150.2095.17
ZLS-216.0028.332.5513.592.860.492.520.331.879.360.371.080.161.050.1780.73
ZLS-310.1718.912.119.381.870.341.850.271.509.740.310.840.130.750.1258.29
ZLS-47.7016.881.247.971.570.301.580.261.4510.000.300.900.130.760.1351.17
ZLS-56.4311.461.255.721.220.231.390.241.4710.270.320.900.140.850.1442.03
ZLS-66.5811.261.215.521.200.221.320.231.339.590.300.830.120.800.1340.64
ZLS-76.3611.231.245.401.110.201.280.221.298.840.290.790.130.770.1339.28
ZLS-810.8716.591.878.701.860.321.860.291.699.450.360.990.160.960.1556.12
ZLS-913.0628.312.7611.702.190.382.120.311.8010.960.411.130.181.160.1876.65
ZLS-1011.2421.532.039.250.990.361.920.301.5710.240.401.020.160.900.1562.06
ZLS-118.9517.101.948.721.750.341.790.271.5611.180.330.910.140.830.1455.95
ZLS-129.3621.572.379.372.120.401.900.291.5610.570.370.960.150.900.1562.04
ZLS-1314.9826.752.9612.912.390.422.220.291.5510.970.330.950.140.890.1577.9
ZLS-1413.2625.262.8611.292.400.472.240.301.6411.240.320.930.140.810.1473.3
ZLS-1511.6822.342.6311.962.440.502.310.331.7412.850.350.950.150.820.1471.19
ZLS-1620.3728.973.0319.563.060.573.030.422.3713.700.461.240.191.000.1698.13
ZLS-1724.5143.914.7921.203.870.893.710.492.5215.990.511.380.211.200.20125.4
ZLS-1820.3340.244.5721.004.031.004.020.603.0321.240.631.860.261.570.24124.6
ZLS-1916.7934.354.3020.454.251.124.430.633.6526.340.752.080.301.690.28121.4
ZLS-P18.2730.243.0219.243.961.004.240.623.0228.240.712.020.251.290.28116.4
ZLS-2015.6931.873.8518.263.890.984.220.613.5830.190.782.090.311.720.28118.3
ZLS-2115.2429.552.2411.023.020.273.060.522.3521.260.241.200.200.460.1290.75
Av.113.2224.762.6412.382.440.502.450.361.9713.570.411.150.171.000.1677.18
Av.227.8650.135.7928.035.601.264.950.653.1722.120.681.890.251.430.28154.1
World11233.51220.472.70.322.18.40.540.930.3110.268.47
Tab.2  Concentration of rare earth elements and yttrium in the ZLS K1a coal (μg/g)
Fig.4  Concentration distribution of LREY, MREY, and HREY in the ZLS K1a coal.
Fig.5  Vertical distribution of REY in the ZLS K1a coal (μg/g).
Fig.6  Concentration coefficients (CC) of REY in the ZLS K1a samples.
SamplesLREYMREYLREYHREYMREYHREYLaNLuNLaNSmNGdNLuNTypeLaNYbNCeNCeNEuNEuNGdNGdN
ZLS-R5.8935.426.011.430.781.71L-M1.740.891.211.20
ZLS-14.5324.015.300.960.881.16M-H1.150.931.111.20
ZLS-24.3522.385.151.010.841.25L-M1.120.990.931.19
ZLS-33.1019.746.370.900.821.30M-H0.990.930.931.16
ZLS-42.6015.936.120.630.741.02M-H0.741.220.931.07
ZLS-51.9211.105.790.490.790.84H0.550.920.861.07
ZLS-62.0311.825.820.540.820.86H0.600.900.841.06
ZLS-72.1412.015.610.520.860.83H0.610.910.821.08
ZLS-82.9315.235.190.770.881.04M-H0.830.830.851.11
ZLS-93.7318.965.090.770.890.99H0.831.070.891.15
ZLS-103.1317.135.470.801.701.08H0.921.021.351.31
ZLS-112.5416.376.440.680.771.08M-H0.790.930.971.15
ZLS-123.0417.705.820.670.661.07M-H0.761.040.981.09
ZLS-133.8824.396.281.070.941.25L-M1.230.910.941.22
ZLS-143.4723.536.791.010.831.35L-M1.200.931.041.20
ZLS-152.8821.187.360.890.721.39M-H1.040.921.071.16
ZLS-163.7324.596.591.361.001.59L-M1.490.820.961.20
ZLS-174.1628.086.741.310.951.56L-M1.500.921.221.23
ZLS-183.0219.776.550.900.761.41M-H0.950.951.251.15
ZLS-192.2215.717.090.640.591.33M-H0.730.921.331.20
ZLS-P2.0116.428.160.700.691.28M-H1.040.911.251.19
ZLS-201.8614.207.640.600.611.27M-H0.670.931.251.20
ZLS-212.2227.5112.371.350.762.15L-M2.431.120.431.05
Av.13.0219.116.460.850.851.23-1.010.961.001.15
Av.23.9525.927.091.060.731.49-1.390.901.231.19
Tab.3  Geochemical parameters of rare earth elements and yttrium in the ZLS K1a coal
Fig.7  Distribution patterns of REY in the ZLS K1a coal (UCC values are those of Taylor and McLennan, 1985).
Fig.8  Diagram of Ba vs. Eu (a), and Al2O3 vs. TiO2 (b) of the K1a coal.
Fig.9  Correlation between REY and Ad, SiO2, Al2O3, SiO2 + Al2O3, P2O5, St,d, Si,d, So,d, Fe2O3, CaO, and Zr.
Fig.10  Correlation between LREY, MREY, HREY with Ad, SiO2, Al2O3, SiO2 + Al2O3, Fe2O3, St,d, CaO, P2O5, and Zr.
Fig.11  Evaluation of REY in ZLS K1a coal ash (roof and parting are presented by black point).
Region coalfieldMineSeamAgeTAdLaCePrNdSmEuGdTbDyYHoErTmYbLuREYREOCoutlRef.
ChongqingZLSZLSK1aP2l2.115.113.2224.762.6412.382.440.52.450.361.9713.570.411.150.1710.1677.2607.41.13This paper
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ChongqingZLSZLSK1bP2l229.625547292.20.12.50.12.4210.92.30.22.20.2149.1595.60.95
ChongqingTFMXPK2P2l3.114.549.1272.459.9332.485.670.65.751.034.333.831.182.540.492.270.48222.11810.60.97Qin et al., 2018a
ChongqingTFMXPK2P2l0.412.152.195.110.740.96.960.879.011.348.2646.11.685.130.724.830.69284.42777.61.00Dai et al., 2017
ChongqingTFMXPK1P2l0.441.562.310716.571.114.93.4516.62.351495.32.747.91.046.680.97422.81210.71.64
ChongqingTFMXPK2P2l427.2911772085110.3120.19.5532.26.40.96.60.8475.82063.00.82Zhuang et al., 2005
ChongqingTFMXPK4P2l0.522.65011313485.40.14.70.14.8321.53.60.54.10.3281.11467.60.74
ChongqingTFMXPK5P2l0.625.229657312.30.13.40.13.7321.430.73.40.4182.5858.60.99
ChongqingTFMXPK7P2l0.640.0347794340.12.80.12.1170.92.10.22.50.3195.1574.20.80
ChongqingNTDL4P2l2.0313.517.834.83.9152.990.553.30.462.713.40.521.530.211.440.298.8867.00.91Chen et al., 2015
ChongqingNTDL6P2l0.7210.919.939.34.4316.83.320.423.780.563.5118.40.72.080.281.940.28115.71253.80.98
ChongqingSZ-12P2l0.4869.18174.818.3772.4812.971.9611.711.75410.8668.342.347.430.9886.630.99460.869.181548.20.88Dai et al., 2010b
ChongqingSZ-11P2l0.2433.271.513716.258.510.61.328.771.327.942.11.64.950.674.490.66367.61305.70.80
ChongqingSZ-10P2l0.3631.958.310813.651.210.31.748.941.37.5538.81.554.860.664.420.65311.91154.20.91
ChongqingSZ-9P2l0.4134.214.3283.3812.92.720.52.810.53.1318.80.672.120.32.020.3192.5321.21.21
ChongqingSZ-8P2l1.8315.526.249.35.821.34.180.753.710.593.618.80.732.210.31.980.29139.71067.70.90
ChongqingSZ-7P2l0.5126.028.151.36.123.54.721.114.170.63.619.20.722.250.292.010.3148.0672.30.92
ChongqingSZ-6P2l1.1625.712.9253.0912.22.570.612.530.42.5914.40.531.690.231.590.2480.6371.21.16
ChongqingSECQDGK1P2wjp0.8524.52648.67.2731.16.961.558.561.38.1261.41.685.040.664.250.63213.11038.81.94Zou et al., 2020
GuizhouQDBYD4P2wjp124.2116.3241.224.3288.9518.491.41716.512.39515.7986.753.269.171.3249.5351.358636.73105.00.80Li et al., 2020b
GuizhouQDBJQ4P2wjp1.1825.212224224.5988.1518.871.54117.832.69819.32113.53.84110.91.53810.371.418678.63186.20.91
GuizhouLPSTC3P2l1.6214.711.123.32.6210.62.160.382.260.311.8610.40.381.120.151.040.1667.8546.60.99Liu et al., 2020
GuizhouLPSTC6P2l1.4520.414.230.93.6215.33.360.673.670.543.3918.60.692.020.281.9110.2899.4578.71.19
GuizhouLPSDHBD101P2l0.8918.073.315818.87213.22.05131.68.96421.654.90.684.610.66415.42715.90.79Liu et al., 2019
GuizhouLPSWJZw407P2l1.214.428.670.88.0833.36.51.47131.63.616.40.651.810.241.650.24187.91537.10.79
GuizhouLPSYLT19P2l1.722.816.1135.093.88915.223.0980.6673.3780.5043.14814.340.6061.8250.251.6950.237100.1517.50.94Wang et al., 2016
GuizhouTZCLB4P2wjp2.2515.222.1240.934.27816.143.1040.1292.680.1521.91812.360.1371.19601.1840106.3824.00.75Li et al., 2019
GuizhouZNFHS23P2l3.2912.213.5828.273.1410.762.310.772.28-1.929.99-0.96---74.8836.80.86Li et al., 2017
GuizhouZNFHS27P2l1.2623.813.9728.703.3010.892.170.672.18-2.2012.81-1.41-1.32-79.6766.00.93
GuizhouZNWJB6P2wjz1.8817.711.3123.482.699.112.030.651.96-1.9010.01-1.12---65.2624.60.97
GuizhouZNWJB7P2wjz1.0529.713.5728.713.2711.082.220.702.19-2.2010.57-1.18-1.10-76.9382.00.86
GuizhouZNKLS6P2l1.3514.916.5034.904.2317.203.280.673.330.442.5412.200.481.330.181.210.1798.7782.40.93Liu et al., 2021
GuizhouZNSJC7P2l1.7516.614.4029.803.2712.702.520.442.720.402.5012.700.501.450.201.340.1985.1608.20.94
GuizhouGDGC3P2wjp1.0117.76.4813.61.596.731.40.31.650.251.815.40.391.30.181.290.2252.6355.31.64Dai et al., 2015b
GuizhouGDHST3P2wjp1.0329.713.829.63.2413.32.430.552.590.352.19140.431.350.181.280.2185.5340.91.00
YunnanZXRSHC5bP2l1.7529.918.0137.855.06620.714.1830.8514.2770.5973.1613.910.6261.8170.2771.8540.289113.5447.11.00Duan, 2017
YunnanXWBLC1P2xw1.4628.730.767.97.54295.851.086.180.883.9320.80.772.050.291.940.3179.2736.30.81Li et al., 2021
YunnanXWLBC1P2xw2.3534.521.9549.365.54821.814.4230.8644.7480.7373.65520.130.7462.0550.2871.8970.291138.5474.90.94
SichuanGXSP19P2l0.5017.45.4811.71.294.721.080.2541.340.2221.3910.60.3130.9690.1490.9940.15940.7278.41.36Luo et al., 2016
SichuanGXSP25P2l1.3027.377.86143.518.669.113.281.34714.162.1612.7487.252.6727.7711.1117.1491.048459.71995.11.16
SichuanGXSP25P2l1.1021.051.4790.1310.7641.337.8090.8118.6361.2297.28846.151.4374.3290.5853.8640.548276.41562.61.05Dai et al., 2016b
SichuanHYSLSDK1P2l2.0320.951.510512.446.88.611.068.941.337.4641.81.544.480.674.410.67296.71680.00.92Dai et al., 2014b
Tab.4  REY concentration (μg/g) and some parameters of coals from southwestern China
Fig.12  The content contour image of total REY in coals from southwestern China.
Fig.13  Diagram of the REO vs. Coutl from some coalfields of southwestern China.
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