赣州北部丘陵地区地下水溶质溯源及评价OA
Source Apportionment and Evaluation of Groundwater Solutes in the Hilly Area of Northern Ganzhou
[研究目的]赣州北部丘陵地区地下水开发利用程度高,受人类活动影响显著,为明确该区域地下水溶质的主要来源、人类活动对地下水的影响及地下水饮用与灌溉适宜性,并为区域地下水资源科学开发与保护提供科学依据.[研究方法]以赣州北部丘陵地区地下水为研究对象,在进行地下水空间采样的基础上,综合运用统计分析、离子对比、水岩反应分析及水质评价等方法,系统开展研究工作.[研究结果]① 研究区井、泉地下水阳离子均以 Ca2+和 Na+为主,阴离子以 HCO3-为主,且井中主要阴阳离子浓度高于泉,明显受到人类活动干扰;② 地下水化学成分主要受硅酸盐矿物风化作用控制,同时地下水具有较强的矿物溶蚀能力;③ 区内地下水污染源以化肥污染为主,部分井点还受到生活污染和粪便污染的叠加影响;④ Water Quality Index(WQI)法评价显示,区内地下水水质较好,满足饮用要求;通过钠百分比(Soluble Sodium Percentage,SSP)、钠吸附比(Sodium Adsorption Ratio,SAR)和渗透率(Permeability Index,PI)等指标评价表明,区内地下水灌溉钠危害较弱,但长期使用会降低土壤渗透性.[结论]研究区地下水溶质来源受自然地质过程与人类活动的共同影响,其中硅酸盐矿物风化是自然因素中控制地下水水化学组成的主导因素,化肥使用则是人为因素中地下水溶质的主要来源;地下水整体满足饮用和灌溉基本需求,但井中离子浓度偏高及长期灌溉对土壤渗透性的负面影响需重点关注,建议加强区域地下水污染精准管控与科学利用指导,保障地下水资源可持续利用.
[Objective]The hilly area of northern Ganzhou has a high degree of groundwater development and utilization and is significantly affected by human activities.To clarify the main sources of groundwater solutes,the impact of human activities on groundwater,and the suitability of groundwater for drinking and irrigation in this region,and to provide a scientific basis for the scientific development and protection of regional groundwater resources.[Methods]Taking the groundwater in the hilly area of northern Ganzhou as the research object,based on spatial groundwater sampling,comprehensive methods such as statistical analysis,ion comparison,water-rock interaction analysis,and water quality evaluation were applied to systematically conduct the research.[Results]① The main cations in groundwater from wells and springs in the study area are Ca2+and Na+,and the dominant anion is HCO3-.① The main cations in well and spring groundwater in the study area are Ca2+and Na+,and the main anion is HCO3-.The concentrations of major ions in wells are higher than in springs,indicating significant interference from human activities.② The chemical composition of groundwater is primarily controlled by the weathering of silicate minerals,and the groundwater has a strong mineral dissolution capacity.③ The main source of groundwater pollution in the area is fertilizer contamination,with some well points also experiencing superimposed effects from domestic pollution and fecal contamination.④ Evaluation using the Water Quality Index(WQI)method shows that the overall groundwater quality in the area is good and meets drinking water requirements.Evaluations based on indicators such as Soluble Sodium Percentage(SSP),Sodium Adsorption Ratio(SAR),and Permeability Index(PI)indicate that the sodium hazard for irrigation is relatively weak,but long-term use may reduce soil permeability.[Conclusion]The sources of groundwater solutes in the study area are influenced by both natural geological processes and human activities.Among natural factors,the weathering of silicate minerals is the dominant factor controlling the hydrochemical composition of groundwater.Among anthropogenic factors,fertilizer use is the main source of groundwater solutes.The groundwater generally meets basic requirements for drinking and irrigation.However,the relatively high ion concentrations in wells and the potential negative impact of long-term irrigation on soil permeability require focused attention.It is recommended to strengthen precise control and scientific utilization guidance for regional groundwater pollution to ensure the sustainable use of groundwater resources.
杨艳林;靖晶;邵长生;张楚涵;张宏鑫;余绍文;肖天宇
中国地质调查局武汉地质调查中心(中南地质科技创新中心),武汉 430205湖北师范大学城市与环境学院,黄石 435002中国地质调查局武汉地质调查中心(中南地质科技创新中心),武汉 430205兰州大学生态学院,甘肃 兰州 730000中国地质调查局武汉地质调查中心(中南地质科技创新中心),武汉 430205中国地质调查局武汉地质调查中心(中南地质科技创新中心),武汉 430205中国地质调查局武汉地质调查中心(中南地质科技创新中心),武汉 430205
天文与地球科学
赣州北部地下水溶质溯源适宜性评价
northern Ganzhougroundwatersolute traceabilitysuitability assessment
《华南地质》 2026 (2)
214-224,11
中国地质调查局地质调查项目(DD202605202304、DD20160248)
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