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付宇, 曹文庚, 张娟娟. 基于随机森林建模预测河套盆地高砷地下水风险分布[J]. 岩矿测试, 2021, 40(6): 860-870. DOI: 10.15898/j.cnki.11-2131/td.202108170099
引用本文: 付宇, 曹文庚, 张娟娟. 基于随机森林建模预测河套盆地高砷地下水风险分布[J]. 岩矿测试, 2021, 40(6): 860-870. DOI: 10.15898/j.cnki.11-2131/td.202108170099
FU Yu, CAO Wen-geng, ZHANG Juan-juan. High Arsenic Risk Distribution Prediction of Groundwater in the Hetao Basin by Random Forest Modeling[J]. Rock and Mineral Analysis, 2021, 40(6): 860-870. DOI: 10.15898/j.cnki.11-2131/td.202108170099
Citation: FU Yu, CAO Wen-geng, ZHANG Juan-juan. High Arsenic Risk Distribution Prediction of Groundwater in the Hetao Basin by Random Forest Modeling[J]. Rock and Mineral Analysis, 2021, 40(6): 860-870. DOI: 10.15898/j.cnki.11-2131/td.202108170099

基于随机森林建模预测河套盆地高砷地下水风险分布

High Arsenic Risk Distribution Prediction of Groundwater in the Hetao Basin by Random Forest Modeling

  • 摘要: 河套盆地浅层地下水砷污染严重,对当地居民健康造成严重影响。当前对河套盆地浅层地下水高砷分布的研究受限于采样时间和样本数量,难以从宏观角度对河套盆地高砷地下水的空间分布作出较为全面的评价。本文基于研究区506个浅层地下水样品,以9个地表环境参数为初始预测变量,经过最佳变量组合筛选,采用随机森林建模来产生风险概率,评价了预测变量的重要性以及对高砷地下水的影响。以气候因子为动态预测变量,根据模型识别不同季节地下水高砷的概率分布并制作了风险区专题图。结果表明:研究区的地下水样品砷含量为0.05~916.7μg/L,超标率(砷浓度>10μg/L)为50%;地下水高砷风险区主要分布在河套盆地的沉积中心地带,但冬季高砷风险区面积减少1907km2,占研究区总面积14.14%;降水、干旱指数、排灌渠影响、潜在蒸散、温度是影响高砷地下水最重要的指标。研究认为,河套盆地的气候变量(降水、干旱指数)与含水层砷含量显著相关,控制高砷地下水在河套盆地的沉积中心地带发生季节性变化。

     

    Abstract:
    BACKGROUNDArsenic pollution is a serious problem in shallow groundwater in the Hetao Basin, and has seriously affected the health of residents. The research on the distribution of high arsenic shallow groundwater in the Hetao Basin is limited by the sampling time and sample number.
    OBJECTIVESTo obtain a comprehensive understanding of the risk distribution characteristics and important influencing factors of high arsenic groundwater in different seasons in the region.
    METHODSBased on 506 shallow groundwater samples and 9 surface environmental parameters as prediction variables, a random forest model was established to evaluate the importance of prediction variables and the impact of important variables on high arsenic groundwater. Taking the climate factors as the dynamic prediction variables, the probability distribution of high arsenic groundwater in different seasons was identified and thematic maps of risk areas were made.
    RESULTSThe results showed that the arsenic content of 506 groundwater samples ranged from 0.05 to 916.7μg/L with an overshoot rate (>10μg/L) of 50%. Groundwater arsenic risk areas were mainly distributed in the depositional center of the Hetao Basin, but the area of groundwater arsenic risk areas decreased by 1907km2 in winter, accounting for 14.14% of the total area. Precipitation and drought index, influence of drainage and irrigation channels, potential evapotranspiration and temperature were the most important indexes affecting the high arsenic groundwater in this area.
    CONCLUSIONSIn the Hetao Basin, climate variables (precipitation and drought index) are significantly correlated with arsenic accumulation in the aquifer, which controls the seasonal variation of groundwater with high arsenic content in the depositional center of the Hetao Basin.

     

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