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The environmental terrestrial gamma-radiation dose rate estimation and the living environment safety evaluation in Fujian Province |
YU Gen-Xin( ) |
Fujian Institute of Geological Survey,Fuzhou 350013,China |
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Abstract Fujian Province is located in the southeast coastal area of China, where granite is extensively exposed, which causes the fact that radionuclide is generally high in the soil, so that the environmental terrestrial gamma-radiation dose rate is higher too. In recent years, the living environment safety has aroused more and more attention, and the problem whether higher gamma radiation dose rate there is a risk has become much concern from the people. This study chose Luofang of Yong'an and Zhongdi of Wuping which are two key areas to carry out the 1∶50 000 environment terrestrial gamma radiation dose rate measurement, supported by soil samples at the same collection points. Through the study of relationship between specific activity of soil radioactive elements238U, 232Th, 40K and gamma radiation dose rate, a multivariate regression equation was established. The U, Th, K test results of 31 303 surface soil samples obtained from 1∶250 000 multi-purpose regional geochemical survey in Fujian Province were converted into 2 km×2 km grid environmental terrestrial gamma-radiation dose rate in Fujian Province,so that human settlement environment suitability evaluation could be conducted.The authors have reached the conclusion that gamma radiation safety area (with no risk) in Fujian Province possesses about 121 000 km2, accounting for 99.64%, the risk area (probably with some risk) possesses 433 km2,accounting for 0.36%,and controlarea (with risk) only possesses 4 km2, suggesting an excellent natural radioactive environment.
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Received: 07 May 2020
Published: 01 March 2021
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Regional geologic map of key areas
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The profile soil radioactive elements and gamma-radiation dose rate of Luofang
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岩性 | 测量数 | 统计数 | γ辐射剂量率/(10-8 Gy·h-1) | 变异系数/% | 范围 | 均值±标准差 | 二长花岗岩(ηγJ3) | 130 | 127 | 4.5~23.0 | 13.2±2.36 | 17.9 | 正长花岗岩(ξγJ3) | 33 | 33 | 7.5~18.3 | 14.3±2.41 | 16.8 | 林田组(∈1-3l) | 29 | 29 | 8.4~18.7 | 14.8±2.45 | 16.5 | 全区 | 192 | 189 | 4.5~23.0 | 13.6±2.46 | 18.0 |
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Statistics of gamma radiation dose rate and eigenvalue in different lithology of Luofang
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The profile soil radioactive elements and gamma-radiation dose rate of Zhongdi
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岩性 | 测量数 | 统计数 | γ辐射剂量率/(10-8 Gy·h-1) | 变异系数/% | 范围 | 均值±标准差 | 二长花岗岩(ηγJ3) | 118 | 118 | 6.7~19.6 | 13.5±2.60 | 19.3 | 正长花岗岩(ξγJ3) | 90 | 90 | 9.4~18.6 | 13.2±2.37 | 18.0 | 全区 | 208 | 208 | 6.7~19.6 | 13.4±2.50 | 18.7 |
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Statistics of gamma radiation dose rate and eigenvalue in different lithology of Zhongdi
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指标 | 含量 | 核素 | 含量/(Bq·kg-1) | U | 1 | 238U | 12.36 | Th | 1 | 232Th | 4.11 | K | 1 | 40K | 0.0312 | K2O | 1 | 40K | 257.30 |
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Content of unit conversion coefficient of U, Th and K
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来源 | 平方和 | 自由度 | 方差 | 方差比(检验值) | 回归 | U=896.47793 | m=3 | U/m=298.826 | F=66.2585 | 剩余 | Q=1785.95957 | n-m-1=396 | Q/(n-m-1)=4.510 | | 总计 | Syy=2682.4375 | n-1=399 | | |
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Results of variance analysis
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岩性 | 网格点数 | γ辐射剂量率/(10-8 Gy·h-1) | 范围 | 均值 | 标准差 | 沉积岩 | 4853 | 8.2~19.8 | 10.4 | 0.92 | 变质岩 | 4686 | 8.5~17.4 | 11.0 | 0.82 | 火成岩 | 18762 | 8.2~22.7 | 12.1 | 1.62 | 第四纪沉积物 | 2573 | 7.8~15.0 | 10.9 | 1.12 | 滩涂 | 370 | 7.7~13.8 | 11.0 | 0.90 |
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Statistics of gamma radiation dose rate in different lithology of Fujian Province
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The living environment suitable for evaluation of high radioactive area of Fujian Province
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人居环境适宜性分区 | 面积/km2 | 比率/% | 放射性安全区(D<16.8×10-8 Gy/h) | 120963 | 99.64 | 放射性风险区 (16.8×10-8Gy/h ≤D<22.0×10-8 Gy/h) | 433 | 0.36 | 放射性管制区(D≥22.0×10-8 Gy/h) | 4 | |
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The living environment safety partition of Natural gamma radiation dose rate
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