萨拉乌苏河流域干沟子剖面全新世湖相沉积的地球化学元素特征及其反映的物源变化
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周维鑫, 温小浩, 李保生, 王晨, 田梦圆, 邱明昆
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Geochemical characteristics of holocene lacustrine sediments in Gangouzi section and its sedimentary sources in the Salawusu River Valley
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Weixin Zhou, Xiaohao Wen, Baosheng Li, Chen Wang, Mengyuan Tian, Mingqun Qiu
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表3 干沟子剖面微量元素含量分布 (ppm)
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Table 3 Content distribution of trace element in Gangouzi section (ppm)
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沉积层段 | 数值类型 | Sr | P | Zr | Cl | Rb | V | Zn | Co | Cu | Pb | Nb | Br |
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0—110 cm | 最大值 | 1 371 | 625 | 195 | 1129 | 76 | 62 | 13.2 | 17.7 | 21.4 | 15 | 9.9 | 9.9 | | 最小值 | 140 | 117 | 78 | 0 | 32 | 23 | 51.6 | 3.5 | 6.9 | 5 | 5.6 | 0.9 | | 平均值 | 908.52 | 318.05 | 112.27 | 190.25 | 48.95 | 44.89 | 26.08 | 6.18 | 12.89 | 8.68 | 7.16 | 3.18 | 110—250 cm | 最大值 | 152 | 521 | 226 | 205 | 84 | 60 | 38.8 | 29 | 18.9 | 18 | 11.7 | 1.4 | | 最小值 | 136 | 172 | 112 | 0 | 58 | 30 | 8.6 | 13.1 | 4.2 | 7 | 8.0 | 1.2 | | 平均值 | 141.29 | 275.63 | 172.78 | 89.07 | 69.98 | 42.31 | 21.27 | 18.93 | 9.69 | 11.85 | 9.50 | 1.24 | 全剖面 | 最大值 | 1 371 | 625 | 226 | 1129 | 84 | 62 | 51.6 | 29.0 | 21.4 | 18 | 11.7 | 9.9 | | 最小值 | 136 | 117 | 78 | 0 | 32 | 23 | 7.0 | 3.5 | 4.2 | 5 | 5.6 | 0.9 | | 平均值 | 528.36 | 297.30 | 142.25 | 139.41 | 59.37 | 43.61 | 23.70 | 12.50 | 11.30 | 10.25 | 8.32 | 2.22 | | 标准偏差 | 447.93 | 117.54 | 39.02 | 193.51 | 13.31 | 8.19 | 9.11 | 7.05 | 4.01 | 2.86 | 1.51 | 1.84 | | 变异系数 | 0.85 | 0.40 | 0.27 | 1.39 | 0.22 | 0.19 | 0.38 | 0.56 | 0.35 | 0.28 | 0.18 | 0.82 |
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