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Characteristics of selenium content in soil of eastern Baoqing County and its relationship with soil properties |
Yue-Ping WANG, Li ZHANG( ), Yu-Jun CUI, Shi-Jia LYU |
Heilongjiang Institute of Geological Survey, Haerbin 150036, China |
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Abstract In order to study the soil selenium content in the eastern part of Baoqing County and its relationship with soil properties, the authors collected 17 470 soil samples in the depth of 0~20 cm from the main agricultural areas in eastern Baoqing County according to the density of 4 points/km 2. Physical and chemical indicators such as selenium content, organic carbon and pH were analyzed. The results show that the selenium content in the topsoil is between 0.01×10 -6 and 1.17×10 -6, the average content is 0.326×10 -6, 73.53% of the soil is selenium-sufficient, 21.14% of the soil is selenium-abundant, and 4.56% of soil is of potential selenium-deficiency. Selenium-deficient soil only accounts for 0.77%, and there is no selenium poisoning area. The average content of selenium in different soil parent materials is arranged in decreasing order of alluvial deposits>alluvial deposits>granite>sedimentary rocks>basic-neutral volcanic rocks; the average content of selenium in different soil types in arranged in decreasing order of albic soil>meadow soil>black soil>marshy soil>dark brown soil>paddy soil; the average content of selenium in different land use is arranged in decreasing order of irrigated farmland>dry farmland>grassland>construction land>unused land>forest land. Correlation analysis shows that soil organic carbon (TOC) and pH are the main factors affecting the selenium content in the surface soil of the study area.
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Received: 08 January 2019
Published: 15 August 2019
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Corresponding Authors:
Li ZHANG
E-mail: 11741785@qq.com
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Geological sketch map of eastern Baoqing County
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土壤性质 | 平均值 | 变幅 | 标准差 | 变异系数/% | 总硒 | 0.326 | 0.01~1.17 | 0.116 | 35.58 | TOC | 2.684 | 0.03~32.96 | 1.655 | 61.65 | pH | 6.13 | 3.95~8.56 | 0.632 | 10.32 |
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Basic physicochemical properties of soil (n=17 470)
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硒含量分级 | 硒含量范围/10-6 | 硒效应 | 面积比例/% | 缺乏 | <0.125 | 缺硒 | 0.77 | 边缘 | 0.125~0.175 | 硒潜在不足 | 4.56 | 适中 | 0.175~0.4 | 足硒 | 73.53 | 高 | 0.4~3.0 | 富硒 | 21.14 | 过剩 | >3.0 | 硒中毒 | 0 |
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Limit value and statistical result of selenium content of soil in research area
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Distribution characteristics of selenium content in soil in eastern Baoqing County
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成土母质 | 样本数 | 平均值/10-6 | 变幅/10-6 | 标准差/10-6 | 变异系数/% | 冲积—洪积物 | 7463 | 0.304 | 0.01~1.17 | 0.107 | 35.20 | 残坡积物 | 6639 | 0.370 | 0.07~0.99 | 0.120 | 32.43 | 基性—中性火山岩 | 1195 | 0.270 | 0.08~1.15 | 0.094 | 34.81 | 沉积岩 | 1889 | 0.296 | 0.09~0.92 | 0.100 | 33.78 | 花岗岩 | 284 | 0.298 | 0.10~0.57 | 0.086 | 28.86 |
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Characteristics of selenium content in different soil-forming material
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土壤类型 | 样本数 | 平均值/10-6 | 变幅/10-6 | 标准差/10-6 | 变异系数/% | 草甸土 | 6396 | 0.353 | 0.01~1.17 | 0.116 | 33.14 | 沼泽土 | 4876 | 0.298 | 0.05~1.13 | 0.112 | 37.33 | 白浆土 | 2943 | 0.358 | 0.01~0.84 | 0.108 | 30.00 | 暗棕壤 | 1606 | 0.270 | 0.07~0.85 | 0.102 | 37.78 | 黑土 | 1593 | 0.300 | 0.10~0.83 | 0.104 | 34.67 | 水稻土 | 56 | 0.253 | 0.13~0.47 | 0.080 | 32.00 |
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Characteristics of selenium content in different soil types
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土地利用 | 样本数 | 平均值/10-6 | 变幅/10-6 | 标准差/10-6 | 变异系数/% | 旱地 | 10943 | 0.330 | 0.05~1.17 | 0.116 | 34.98 | 水田 | 3157 | 0.343 | 0.01~0.89 | 0.109 | 31.82 | 草地 | 976 | 0.307 | 0.05~1.13 | 0.140 | 45.43 | 林地 | 1712 | 0.284 | 0.08~0.80 | 0.102 | 36.08 | 建设用地 | 300 | 0.305 | 0.1~0.74 | 0.115 | 37.84 | 未利用地 | 382 | 0.303 | 0.01~0.72 | 0.117 | 38.51 |
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Characteristics of selenium content in different land use patterns
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Relations between pH and Se content in soil
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Relations between TOC and Se content in soil
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