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Geochemical characteristics and source analysis of elements from dry and wet atmospheric deposition in the middle-high mountain and hilly region of Central Yunnan |
XU Lei1,2( ), LI Jun1,2( ), QU Qiang1,2, WEN Fang-Ping1,2, ZHAO Meng-Sheng1,2, CHENG Yan-Xun1,2, Xu Jie1,2, WANG Hao-Yu1,2 |
1. Kunming Natural Resources Comprehensive Survey Center of China Geological Survey, Kunming 650100, China 2. Technology Innovation Center for Natural Ecosystem Carbon Sink, Ministry of Natural Resources, Kunming 650100, China |
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Abstract Dry and wet atmospheric deposition is an essential input pathway for surface soil elements. To explore the geochemical characteristics and sources of elements from atmospheric deposition in the middle-high mountain and hilly region of Central Yunnan, this study investigated 35 dry and wet atmospheric deposition samples from three counties in Central Yunnan. The results show that nutrient elements exhibited high annual depositional fluxes, while heavy metal elements manifested low annual depositional fluxes, with their ranking as follows: TOC>Ca>K>I>F>Zn>B>Pb>Cr>Cu>As>Mo>Cd>Se>Ge>Hg. As revealed by the enrichment factors, principal components, and spatial distribution characteristics, Ca, Mo, B, As, and F originated primarily from soil dust; Cu, Cd, Pb, Cr, and Ge were mostly from anthropogenic sources, such as mining activities and coal dust; TOC, K, Se, and I came from both coal dust and soil dust, and Se was also affected by mining activities; and Hg stemmed from coal dust. Coal and copper-dominated polymetallic mineral resources spread extensively across the study area and are subjected to certain mining activities, which are intimately connected with the contents of heavy metals in the atmosphere. Therefore, targeted atmospheric monitoring should be conducted to ensure atmospheric quality and no pollution to soil.
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Received: 29 November 2022
Published: 23 January 2024
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Sampling sites and mineral resource distribution in the study area
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指标 | TOC | K | Ca | Cu | Cd | Pb | Zn | Mo | 年干 沉降 通量 | 最小值 | 4324 | 50 | 29 | 0.36 | 0.014 | 0.81 | 3.63 | 0.01 | 最大值 | 40625 | 782 | 13704 | 3.87 | 0.527 | 7.11 | 138.28 | 0.32 | 平均值 | 13119 | 268 | 990 | 1.42 | 0.080 | 2.52 | 15.45 | 0.07 | 中位值 | 12357 | 223 | 209 | 1.20 | 0.055 | 2.32 | 9.06 | 0.05 | 年湿 沉降 通量 | 最小值 | 337 | 26 | 82 | 0.01 | 0.000 | 0.00 | 0.01 | 0.00 | 最大值 | 39264 | 10585 | 24449 | 1.41 | 0.032 | 0.47 | 9.02 | 6.16 | 平均值 | 5620 | 624 | 2003 | 0.13 | 0.003 | 0.05 | 1.15 | 0.21 | 中位值 | 3163 | 176 | 856 | 0.05 | 0.002 | 0.03 | 0.59 | 0.01 | 年沉降 通量 | 最小值 | 8510 | 228 | 320 | 0.59 | 0.017 | 0.95 | 5.10 | 0.02 | 最大值 | 44555 | 10635 | 24851 | 3.90 | 0.529 | 7.14 | 138.89 | 6.18 | 平均值 | 18739 | 892 | 2993 | 1.55 | 0.083 | 2.57 | 16.60 | 0.28 | 中位值 | 17447 | 469 | 1829 | 1.23 | 0.057 | 2.33 | 9.23 | 0.09 | 指标 | Cr | B | Ge | As | Hg | Se | I | F | 年干 沉降 通量 | 最小值 | 0.40 | 0.23 | 0.007 | 0.04 | 0.001 | 0.01 | 26.10 | 3.79 | 最大值 | 9.33 | 4.57 | 0.063 | 2.70 | 0.154 | 0.06 | 389.44 | 71.26 | 平均值 | 2.02 | 1.29 | 0.025 | 0.25 | 0.007 | 0.03 | 110.29 | 17.35 | 中位值 | 1.60 | 1.00 | 0.019 | 0.14 | 0.002 | 0.03 | 0.10 | 14.68 | 年湿 沉降 通量 | 最小值 | 0.00 | 0.20 | 0.000 | 0.01 | 0.000 | 0.00 | 0.01 | 1.50 | 最大值 | 2.55 | 16.65 | 0.021 | 2.01 | 0.009 | 0.09 | 0.50 | 195.46 | 平均值 | 0.09 | 2.67 | 0.004 | 0.18 | 0.002 | 0.02 | 0.13 | 23.19 | 中位值 | 0.02 | 1.45 | 0.002 | 0.10 | 0.001 | 0.01 | 0.08 | 13.02 | 年沉降 通量 | 最小值 | 0.49 | 0.86 | 0.013 | 0.10 | 0.002 | 0.02 | 26.27 | 11.13 | 最大值 | 9.34 | 17.12 | 0.064 | 2.80 | 0.156 | 0.10 | 389.46 | 200.01 | 平均值 | 2.11 | 3.96 | 0.028 | 0.43 | 0.009 | 0.05 | 110.42 | 40.55 | 中位值 | 1.64 | 3.64 | 0.024 | 0.29 | 0.004 | 0.05 | 0.23 | 35.29 |
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Statistics of annual element deposition flux of atmospheric dry and wet deposition in the study areamg·(m2·a)-1
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项目 | TOC | K | Ca | Cu | Cd | Pb | Zn | Mo | 区内大气干 沉降含量均值 | 34.05 | 0.65 | 1.63 | 36.28 | 2.02 | 69.63 | 393.54 | 1.67 | 区内表层土壤背景值 | 1.86 | 1.83 | 0.39 | 32.25 | 0.25 | 39.37 | 85.37 | 1.07 | 富集因子 | 12.84 | 0.24 | 1.00 | 0.77 | 5.10 | 1.30 | 2.58 | 0.90 | 项目 | Cr | B | Ge | As | Hg | Se | I | F | 区内大气干 沉降含量均值 | 46.36 | 33.11 | 0.63 | 6.59 | 0.18 | 0.78 | 3.03 | 414.91 | 区内表层土壤背景值 | 101.27 | 76.61 | 1.55 | 10.74 | 0.06 | 0.22 | 2.37 | 579.28 | 富集因子 | 0.30 | 0.29 | 0.28 | 0.32 | 1.12 | 2.51 | 0.87 | 0.45 |
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Elemental enrichment factor characteristics of atmospheric dry deposition
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成分 | 初始特征值 | 旋转载荷平方和 | 总计 | 方差百 分比/% | 累积贡 献率/% | 总计 | 方差百 分比/% | 累积贡 献率/% | F1 | 6.09 | 38.08 | 38.08 | 4.32 | 26.98 | 26.98 | F2 | 3.51 | 21.91 | 59.98 | 3.82 | 23.87 | 50.85 | F3 | 1.12 | 7.02 | 67.00 | 2.40 | 15.02 | 65.86 | F4 | 1.05 | 6.55 | 73.55 | 1.17 | 7.34 | 73.20 | F5 | 1.02 | 6.38 | 79.94 | 1.08 | 6.74 | 79.94 | F6 | 0.72 | 4.52 | 84.45 | | | | F7 | 0.71 | 4.44 | 88.89 | | | | F8 | 0.56 | 3.49 | 92.38 | | | | F9 | 0.36 | 2.24 | 94.62 | | | | F10 | 0.28 | 1.77 | 96.39 | | | | F11 | 0.19 | 1.17 | 97.56 | | | | F12 | 0.13 | 0.82 | 98.38 | | | | F13 | 0.11 | 0.70 | 99.08 | | | | F14 | 0.06 | 0.40 | 99.48 | | | | F15 | 0.05 | 0.29 | 99.77 | | | | F16 | 0.04 | 0.23 | 100.00 | | | |
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Characteristic value of principal components and their contribution rate in atmospheric dry and wet deposition
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元素 变量 | 成分 | F1 | F2 | F3 | F4 | F5 | TOC | 0.48 | 0.13 | 0.64 | 0.17 | 0.07 | K | 0.14 | -0.19 | 0.85 | 0.05 | -0.10 | Ca | 0.87 | 0.14 | 0.18 | 0.10 | 0.07 | Cu | 0.13 | 0.91 | 0.11 | 0.18 | 0.05 | Cd | -0.04 | 0.62 | 0.04 | -0.39 | -0.09 | Pb | -0.08 | 0.85 | -0.14 | -0.08 | -0.14 | Zn | 0.07 | 0.25 | 0.06 | 0.85 | -0.06 | Mo | 0.91 | -0.08 | 0.14 | 0.08 | 0.08 | Cr | 0.12 | 0.84 | 0.06 | 0.25 | 0.18 | B | 0.78 | -0.10 | 0.51 | 0.05 | -0.11 | Ge | 0.13 | 0.87 | 0.09 | 0.34 | -0.08 | As | 0.78 | 0.10 | 0.05 | -0.04 | -0.14 | Hg | -0.03 | -0.05 | 0.00 | -0.04 | 0.96 | Se | 0.49 | 0.44 | 0.57 | -0.17 | 0.09 | I | 0.44 | 0.25 | 0.65 | -0.05 | 0.13 | F | 0.87 | 0.09 | 0.39 | 0.05 | 0.02 |
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Factor load matrix of orthogonal variance rotation of atmospheric dry and wet deposition
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Three-dimensional schematic diagram of each component score of atmospheric dry and wet deposition
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Spatial distribution of annual element flux of atmospheric dry and wet deposition(unit: mg/(m2·a))
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