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Characteristics and influencing factors of selenium content in soils and crops in typical high-selenium-content regions of western Hubei Province, China |
QIN Hao-Lin1( ), LI Ming-Long2,3( ), ZHENG De-Shun1, SUN Feng-Bo1, ZHANG Kai3 |
1. School of Resources and Environment, Henan Polytechnic University, Jiaozuo 454000, China 2. Hubei Key Laboratory of Resource and Eco-Environment Geology (Hubei Geological Bureau), Wuhan 430034, China 3. Second Geological Brigade of Hubei Geological Bureau, Enshi 445000, China |
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Abstract Understanding the distribution patterns of selenium in soils and crops is critical to developing selenium-rich industries. Enshi City in Hubei Province is known for its extensive selenium-rich soils, establishing this city as a promising area for selenium-rich agriculture. This study investigated Xintang Township in Enshi. Based on the organization and analysis of the geochemical data of 2 469 soil samples and 237 crop samples of maize, potatoes, rice, radish, cabbage, and tea, this study offered a systematic summary of the selenium distribution in soils and factors influencing selenium content in crops in the study area. The results indicate that the topsoils exhibit selenium content ranging from 0.14×10-6 to 25.74×10-6, with a background value of 0.81×10-6, which is 3.7 times the national background of selenium content in soils. Selenium-rich soils cover 86.23% of the total area of the study area, and two NEE-directed selenium-rich belts are found. The spatial distribution of selenium in soils is closely related to soil-forming parent materials. Soils with Permian black rock series as parent materials exhibit notably higher selenium content, with an enrichment coefficient of 3.74. In high-selenium-content areas, rice, radish, and cabbage exhibit selenium enrichment rates exceeding 65%. Except for potatoes, crops display positive correlations between their selenium content and the selenium content in their root soils, with tea showing the highest correlation (P<0.01, R=0.84). This suggests a close relationship between the selenium content in crops and their root soils. The crops in cultivated areas with Permian black rock series and Triassic carbonate rock series as soil-forming parent materials exhibit high bioconcentration factors of selenium, with soils and crops with Permian black rock series as soil-forming parent materials presenting the highest average selenium content. This highlights the significant impacts of soil-forming parent materials on crop selenium content.
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Received: 04 November 2023
Published: 22 April 2025
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Soil parent material distribution (a) and sampling points distribution (b) of Xintang Township[18]
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地区 | 背景值/10-6 | 变幅/10-6 | 数据来源 | 新塘乡 | 0.81 | 0.14~25.74 | 本文 | 恩施市 | 9.36 | 2.70~87.30 | [22] | 黑龙江省 | 0.15 | 0.01~0.66 | [23] | 香港 | 0.76 | 0.07~2.26 | [24] | 全国 | 0.22 | 0.05~0.99 | [25] | 巴西 | 0.19 | 0.09~1.61 | [26] | 全球 | 0.40 | — | [27] |
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Comparison of background values of soil Se between Xintang and other areas
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The distribution map (a) and grade map (b) of selenium content in surface soil of Xintang Township
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指标 | 缺乏 | 边缘 | 适量 | 丰富 | 极丰富 | 富硒标准 | 标准值/ 10-6 | ≤0.125 | 0. 125~ 0.175 | 0.175~ 0.40 | 0.40~ 3.00 | ≥3.00 | ≥0.45 | 样品数量 | 0 | 5 | 225 | 1964 | 275 | 2129 | 占比/% | 0 | 0.20 | 9.11 | 79.55 | 11.14 | 86.23 |
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Soil selenium classification
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成土母质 | 硒含量/10-6 | 总样 品数 | EF值 | 范围 | 平均值 | S1lr碎屑沉积岩类风化区 | 0.18~1.04 | 0.47 | 65 | 0.55 | S1-2s碎屑沉积岩类风化区 | 0.24~1.10 | 0.51 | 178 | 0.61 | D2y-D3C1x 碎屑沉积岩类 风化区 | 0.19~2.80 | 0.71 | 431 | 0.84 | C2d+h碳酸盐岩类风化区 | 0.26~3.54 | 0.74 | 133 | 0.94 | P1l+q黑色岩系风化区 | 0.16~9.41 | 0.85 | 224 | 1.19 | P1m+g黑色岩系风化区 | 0.33~25.74 | 2.19 | 448 | 3.12 | P2l-d黑色岩系风化区 | 0.20~20.70 | 2.82 | 419 | 3.74 | T1d碳酸盐岩类风化区 | 0.14~23.23 | 1.44 | 571 | 1.71 |
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Selenium content in surface soil of different geological background areas
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Composite analysis diagram of soil parent material and selenium content grade
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作物 | 总样品数 | 样品数 | 硒含量/10-6 | CV/% | 富硒率/% | 一级 | 二级 | 三级 | 极差 | 平均值 | 标准差 | 玉米 | 70 | 13 | 17 | 40 | 0.02~3.54 | 0.16 | 0.38 | 235 | 42.86 | 土豆 | 48 | 3 | 3 | 42 | 0.01~1.59 | 0.05 | 0.05 | 105 | 12.50 | 水稻 | 25 | 17 | 2 | 6 | 0.05~3.99 | 0.50 | 0.57 | 114 | 76.00 | 萝卜 | 38 | 25 | 10 | 3 | 0.06~3.85 | 0.41 | 0.79 | 193 | 65.79 | 白菜 | 31 | 21 | 6 | 4 | 0.05~3.74 | 1.42 | 1.78 | 125 | 67.74 | 茶叶 | 38 | 14 | 13 | 11 | 0.03~3.48 | 0.40 | 0.68 | 170 | 36.84 |
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Statistics of crop selenium content in Xintang Township
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Scatter diagram of selenium content of crops and root soil in Xintang Township
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农作物 | S | D | C | P | T | 玉米 | 5.69 | 3.74 | 5.96 | 7.14 | 15.06 | 土豆 | 4.19 | 2.89 | 4.36 | 5.21 | 5.38 | 水稻 | 13.46 | 14.94 | 10.83 | 23.60 | 15.17 | 萝卜 | 18.95 | 14.10 | 21.74 | 36.60 | 60.04 | 白菜 | 23.68 | 17.86 | 19.23 | 55.88 | 83.34 | 茶叶 | 11.60 | 10.51 | 8.16 | 26.42 | 23.92 |
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Crop bioconcentration coefficients in soil-forming matrices of different geologic ages%
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The relationship between soil parent material and crop bioconcentration factor in different geological years
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