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Exploring selenium enrichment criteria for soils in the Guanzhong area, Shaanxi Province: A case study of wheat |
REN Rui1,2( ), ZHANG Zhi-Min1,2, WANG Hui1,2, CHEN Ji-Ping1,2, QIAO Xin-Xing1,2, LIANG Dong-Li3 |
1. Shaanxi Hygrogeology Engineering Geology and Environment Geology Survey Center, Xi’an 710068, China 2. Shaanxi Health Geology Research Center, Xi’an 710054, China 3. College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China |
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Abstract Establishing the selenium threshold for soils in selenium-rich wheat producing areas in Shaanxi Province is closely related to the lean, fine-scale, and accurate production of natural selenium-rich wheat. Moreover, it can improve the utilization efficiency of selenium-rich land, thus promoting the development of selenium-rich industry in this province. This study determined the selenium threshold of soils in selenium-rich wheat producing areas in Shaanxi at 0.27×10-6 based on the 1∶250 000 land quality geochemical survey data, the selenium concentration data of 544 sets of soil samples and corresponding wheat seed samples collected in Shaanxi in recent years, the lower limit of geochemical anomalies of selenium in topsoil in the Guanzhong area, and the wheat-soil function. The empirical study showed that the validation set formed via random sampling yielded a selenium accumulation rate of 83.78%, while the third-party inspection yielded a selenium accumulation rate of 87.14%. The wheat produced from selenium-rich land delineated based on the selenium threshold 0.27×10-6 satisfies the recommended nutrient intake of selenium (60 μg/d) stipulated by the Chinese Nutrition Society. Furthermore, the area of the selenium-rich land is about 1 500 km2 (2 250 000 mu), increasing by 640 km2 (960 000 mu) compared with that of land delineated based on a selenium threshold of 0.3×10-6. Therefore, determining selenium-rich soil threshold by crop species can greatly improve the utilization efficiency of selenium-rich land, thus promoting the development of the selenium-rich industry. This study provides a scientific basis for setting selenium enrichment criteria for soils in Shaanxi Province.
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Received: 06 September 2022
Published: 27 October 2023
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Administrative division of Guanzhong region
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计算方法 | 地球化学定义 | 区间划分 | 表层Se含量区间/10-6 | 累积频率法 (n=10 114) | 低值区 | <5% | w(Se)<0.11 | 低背景区 | 5%~<25% | 0.11≤w(Se)<0.14 | 背景区 | 25%~<75% | 0.14≤w(Se)<0.20 | 高背景区 | 75%~<85% | 0.20≤w(Se)<0.22 | 弱异常区 | 85%~<95% | 0.22≤w(Se)<0.28 | 异常区 | 95%~<98.5% | 0.28≤w(Se)<0.37 | 强异常区 | ≥98.5% | w(Se)≥0.37 |
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Classification statistics of selenium content in surface soil
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土壤分组 | 1组 | 2组 | 3组 | 4组 | 5组 | 6组 | 根系土硒含量 | 0.1≤w(Se)<0.2 | 0.2≤w(Se)<0.3 | 0.3≤w(Se)<0.4 | 0.4≤w(Se)<0.5 | 0.5≤w(Se)<0.6 | w(Se)>0.6 | 样本量 | 32 | 174 | 139 | 78 | 46 | 66 | 根系土硒均值 | 0.156 | 0.249 | 0.346 | 0.441 | 0.537 | 0.808 | 小麦硒均值 | 0.079 | 0.086 | 0.133 | 0.207 | 0.255 | 0.488 | 小麦硒最小值 | 0.018 | 0.011 | 0.011 | 0.027 | 0.050 | 0.059 | 小麦硒最大值 | 0.339 | 0.590 | 0.525 | 0.472 | 0.856 | 1.395 |
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Group statistics of wheat samples data10-6
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根系土硒 含量组别 | 小麦硒含 量组别 | 显著性 | | 根系土硒 含量组别 | 小麦硒含 量组别 | 显著性 | 1 | 2 | 0.996 | | 4 | 1 | 0 | 3 | 0.009 | 2 | 0 | 4 | 0 | 3 | 0 | 5 | 0 | 5 | 0.461 | 6 | 0 | 6 | 0 | 2 | 1 | 0.996 | | 5 | 1 | 0 | 3 | 0 | 2 | 0 | 4 | 0 | 3 | 0 | 5 | 0 | 4 | 0.461 | 6 | 0 | 6 | 0 | 3 | 1 | 0.009 | | 6 | 1 | 0 | 2 | 0 | 2 | 0 | 4 | 0 | 3 | 0 | 5 | 0 | 4 | 0 | 6 | 0 | 5 | 0 |
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Multiple comparative tests of selenium content in wheat
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Broken line graph of wheat selenium content in different soils
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Correlation map of soil-wheat selenium content
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指标要求 | 土壤硒含量/ 10-6 | 土壤环境质量 | 富硒 | w(Se)≥0.27 | 镉、汞、砷、铅、铬、铜、镍和锌元素含量低于GB 15618—2018标准中农用地土壤污染风险筛选值 |
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Grading index of selenium-rich soil in wheat production area of Shaanxi
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Distribution map of verificaton samples
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统计量 | 小麦籽粒硒/ 10-6 | 根系土硒/ 10-6 | 土壤pH | 最小值 | 0.014 | 0.102 | 7.670 | 最大值 | 0.165 | 1.674 | 8.670 | 中位数 | 0.053 | 0.754 | 8.185 | 平均值 | 0.056 | 0.781 | 8.163 | 标准差 | 0.031 | 0.390 | 0.214 |
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Statistics of wheat sample data(n=76)
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