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滇东富源地区岩溶地下水水化学特征及控制因素

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岩溶地下水是滇东富源地区工农业生产及居民生活饮用水的重要供水水源,为支撑区内岩溶地下水资源的合理开发利用及保护,系统采集了区内68组岩溶地下水样品,综合运用水化学分析、氢氧同位素分析以及多元统计分析等方法,对岩溶地下水水化学特征、氢氧同位素特征及影响因素进行了研究.结果表明:研究区岩溶地下水pH平均值为7.69,总体上呈弱碱性.水化学类型主要为HCO3-Ca和HCO3-Ca·Mg型,少部分为HCO3·SO4-Ca·Mg型.主要离子中除Ca2+和HCO3-以外,其余各离子均表现出很强的空间变异性.区内岩溶地下水微量组分Sr质量浓度为30.00~3 150.00 µg/L,平均值为522.38 µg/L,其中有40件岩溶地下水样品中Sr质量浓度达到了锶矿泉水的界限标准.此外,部分样品中Fe、Mn和Al含量较高,超过了Ⅲ类水质标准.区内岩溶地下水主要为当地大气降水补给,溶质组分主要受到碳酸盐岩溶解、人类活动以及阳离子交换作用的影响,但是阳离子交换作用总体上较弱.水化学组分中Ca2+、Mg2+、HCO3-以及Sr主要来源于碳酸盐岩矿物的溶解,Cl-、K+、Na+主要来源于生活污水,而Fe、Mn、Al以及SO42-主要来源于采煤活动产生的酸性废水,NO3-主要来源于农业施肥活动.因子分析表明,碳酸盐岩溶解、生活污水排放、采煤活动和农业施肥这4个因素对岩溶地下水水化学的贡献率分别为45.85%、22.24%、21.51%和10.40%,说明了人类活动对岩溶地下水水质有着不容忽视的影响,需要有针对性地采取防治措施.
Hydrogeochemical Characteristics and Controlling Factors of the Karst Ground water in the Area of Fuyuan,Estern Yunnan
The karst groundwater is an important source of water supply for industrial and agricultural production and domestic drinking water of residents in the area of Fuyuan,Eastern Yunnan.In order to support the rational development,utilization and protection of karst groundwater resources,68 groups of karst groundwater samples were systematically collected in Fuyuan.The chemical character-istics,hydrogen and oxygen isotopes and influencing factors of karst groundwater were studied by comprehensive use of water chemical analysis,hydrogen and oxygen isotope analysis,multivariate statistical analysis and other methods.The results indicate that the average pH value of karst groundwater in the study area is 7.69,which is generally weakly alkaline.The hydro-chemical types are mainly HCO3-Ca and HCO3-Ca·Mg,with a small portion being HCO3·SO4-Ca·Mg.Except for Ca2+and HCO3-,all other major ions exhibit strong spatial variability.The mass concentration of Sr in karst groundwater in the area is 30.00-3 150.00 µg/L,with an average val-ue of 522.38 µg/L.Among them,40 karst groundwater samples meet the boundary standard for strontium mineral water.In addition,some samples have high levels of Fe,Mn and Al,exceeding the Class Ⅲ water quality standard.The karst groundwater in the area is mainly supplied by local atmospheric rainfall,and the solute components are mainly affected by dissolution of carbonate rocks,human activities and the cation exchange reaction,but the cation exchange effect is generally weak.Ca2+,Mg2+,HCO3-and Sr mainly come from the dissolution of carbonate minerals.Cl-,K+and Na+mainly come from domestic sewage.Fe,Mn,Al and SO42-mainly come from acidic wastewater generated by coal mining activities.NO3-mainly come from agricultural fertilization activities.Factor analysis shows that the contribution rates of carbonate rock dissolution,domestic sewage discharge,coal mining activities,and agricultural ferti-lization to the hydrochemistry of karst groundwater are 45.85%,22.24%,21.51%and 10.40%,respectively.This indicates that hu-man activities have an undeniable impact on karst groundwater quality,and targeted prevention and control measures are needed.

karst groundwaterhydrogeochemical characteristicscontrolling factorsfactor analysisarea of Fuyuan,Eastern Yunnan

陶兰初、邹祖建、涂春霖、和成忠、马一奇、杨坤、刘振南、张七道

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中国地质调查局昆明自然资源综合调查中心,自然资源部自然生态系统碳汇工程技术创新中心,中国地质学会西南山地生态地质演化与保护修复创新基地,昆明 650100

中国地质大学(北京)水资源与环境学院,北京 100083

中国地质大学(武汉)资源学院,武汉 430074

岩溶地下水 水化学特征 控制因素 因子分析 滇东富源地区

中国地调局项目中国地调局项目中国地调局项目中国地调局项目

DD20208075DD20230483DD20230098ZD20220918

2024

地球与环境
中国科学院地球化学研究所

地球与环境

CSTPCD北大核心
影响因子:0.875
ISSN:1672-9250
年,卷(期):2024.52(2)
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