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宿州农业区矿井水水化学特征及灌溉适宜性评价

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针对宿州矿井水的水化学特征和灌溉适宜性进行研究对宿州农业具有现实的意义.收集区域地质资料,采集矿井水样品并对其pH值、TDS以及常规离子进行测试,将实验数据进行统计处理并绘制相关图件对矿井水水化学特征、主要离子来源及成因以及灌溉适宜性进行分析.结果表明,宿南矿区矿井水呈弱碱性,TDS值偏高,水化学类型包含HCO3-Na、Cl-Na、SO4-Na·Mg型三种,Na+和HCO3-含量明显偏高,SO42-含量略高,Ca2+与Mg2+含量相当,反映了该区水化学控制因素主要是水岩相互作用引起的硅酸盐矿物溶解.结合样品的SAR值和SC值,研究区矿井水大部分不能直接用于农业灌溉.
Chemical Characteristics of Mine Water and Evaluation of Irrigation Suitability in Suzhou Agricultural Area
Studying the hydrochemical characteristics and irrigation suitability of mine water has practical signifi-cance for agriculture in Suzhou.By collecting regional geological data,collecting mine water samples and testing their pH value,TDS,and conventional ions,the experimental data is statistically processed and relevant graphs are drawn to analyze the chemical characteristics,main ion sources and causes,and irrigation suitability of the mine wa-ter in the area under investigation.The results show that the mine water in the southern mining area of Suzhou is weakly alkaline,with a higher TDS value than standard drinking water.The hydrochemical types include HCO3-Na,Cl-Na,and SO4-Na·Mg types,with significantly higher Na+and HCO-3 content,slightly higher SO42-con-tent,and comparable Ca2+and Mg2+content.This reflects that the main controlling factor for hydrochemical control in the area is the dissolution of silicate minerals caused by water rock interaction.Based on the SAR and SC values of the samples,most of the mine water in the study area cannot be directly used for agricultural irrigation.

Mine waterHydrochemical characteristicsIrrigation suitabilitySuzhou

张海涛、冯永军、马杰、胡显响、巩伟、许继影、赵景宇

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宿州学院资源与土木工程学院,安徽宿州,234000

宿州市河道管理处埇桥新汴河管理中心,安徽宿州,234000

淮北矿业股份有限公司朱仙庄煤矿,安徽宿州,234000

矿井水 水化学特征 灌溉适宜性 宿州

宿州学院重点科研项目宿州学院重点科研项目

2022yzd012023yzd08

2024

宿州学院学报
宿州学院

宿州学院学报

影响因子:0.322
ISSN:1673-2006
年,卷(期):2024.39(6)
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