{"title":"地球物理和地球化学数据在尼日尔三角洲西部萨佩莱大都市地下水资源评价中的应用","authors":"O. Ohwoghere-Asuma, K. Aweto","doi":"10.5987/UJ-NJSE.16.040.1","DOIUrl":null,"url":null,"abstract":"An integration of geoelectrical and geochemical data was used in Sapele metropolis to delineate the aquifer unit(s) and evaluated the geochemical parameters of the groundwater in the area. Ten (10) water samples were collected from hand-dug wells for geochemical analysis. The geochemi- cal parameters showed average values of 6.20 pH; 156.0μs/cm EC; 7.60mg/l TH; 4.50mg/l, Ca2+; 4.20mg/l Mg2+; 0.95mg/I K+; 1.00mg/l Na+; 0.87mg/l ∑Fe; 0.03mg/I Cu2+; 0.04mg/I Cr2+ ; 28.68mg/l Cl- ; 5.40mg/I HCO3-; 2.41mg/l NO3-; 0.80mg/l SO42- and average sodium absorption ratio (SAR) of 1.36. The relative abundance of cations using these concentrations is in the order of Ca2+> Mg2+ > Na+> K+ > ∑Fe > Cr2+ > Cu2+ while those of anions are in the order Cl- > HCO3- > NO3- >SO42+. Fifteen (15) vertical electrical soundings were carried out in the study area using Schumberger electrode configuration. The result of the interpretation of the VES curves showed that the area is made up of four and five geoelectric layer. The third and fourth layer made up of medium, coarse and gravelly sand constitutes the aquifer unit(s), the average depth to the aquifer is 35.2m. The concentration of the various parameters determined in the groundwater were relatively in accordance with WHO recommended standard for domestic and agricultural purposes except pH and ∑Fe in Okirighwre , Ajogodo and Ogorode. Cr2+ concentrations generally were below stipu- lated standard in most of Sapele metropolis, except at Ugbeyiyi and Ugberikoko where concentra- tions exceeded WHO maximum allowance limit of 0.05mg/l.","PeriodicalId":119603,"journal":{"name":"Nigerian Journal of Science and Environment","volume":"41 2","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2013-05-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"AN INTEGRATION OF GEOPHYSICAL AND GEOCHEMICAL DATA IN EVALUAT- ING GROUNDWATER RESOURCES IN SAPELE METROPOLIS, WESTERN NIGER DELTA\",\"authors\":\"O. Ohwoghere-Asuma, K. Aweto\",\"doi\":\"10.5987/UJ-NJSE.16.040.1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"An integration of geoelectrical and geochemical data was used in Sapele metropolis to delineate the aquifer unit(s) and evaluated the geochemical parameters of the groundwater in the area. Ten (10) water samples were collected from hand-dug wells for geochemical analysis. The geochemi- cal parameters showed average values of 6.20 pH; 156.0μs/cm EC; 7.60mg/l TH; 4.50mg/l, Ca2+; 4.20mg/l Mg2+; 0.95mg/I K+; 1.00mg/l Na+; 0.87mg/l ∑Fe; 0.03mg/I Cu2+; 0.04mg/I Cr2+ ; 28.68mg/l Cl- ; 5.40mg/I HCO3-; 2.41mg/l NO3-; 0.80mg/l SO42- and average sodium absorption ratio (SAR) of 1.36. The relative abundance of cations using these concentrations is in the order of Ca2+> Mg2+ > Na+> K+ > ∑Fe > Cr2+ > Cu2+ while those of anions are in the order Cl- > HCO3- > NO3- >SO42+. Fifteen (15) vertical electrical soundings were carried out in the study area using Schumberger electrode configuration. The result of the interpretation of the VES curves showed that the area is made up of four and five geoelectric layer. The third and fourth layer made up of medium, coarse and gravelly sand constitutes the aquifer unit(s), the average depth to the aquifer is 35.2m. The concentration of the various parameters determined in the groundwater were relatively in accordance with WHO recommended standard for domestic and agricultural purposes except pH and ∑Fe in Okirighwre , Ajogodo and Ogorode. Cr2+ concentrations generally were below stipu- lated standard in most of Sapele metropolis, except at Ugbeyiyi and Ugberikoko where concentra- tions exceeded WHO maximum allowance limit of 0.05mg/l.\",\"PeriodicalId\":119603,\"journal\":{\"name\":\"Nigerian Journal of Science and Environment\",\"volume\":\"41 2\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2013-05-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Nigerian Journal of Science and Environment\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5987/UJ-NJSE.16.040.1\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Nigerian Journal of Science and Environment","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5987/UJ-NJSE.16.040.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
摘要
利用地电学和地球化学综合数据,对Sapele大都市的含水层单元进行了圈定,并评价了该地区地下水的地球化学参数。采集10口手挖井水样进行地球化学分析。地球化学参数平均值为6.20 pH;156.0μs EC /厘米;7.60 mg / l TH;4.50 mg / l, Ca2 +;4.20 mg / l Mg2 +;0.95毫克/我K +;1.00 mg / l Na +;0.87 mg / l∑铁;0.03毫克/我Cu2 +;0.04mg/I Cr2+;28.68mg/l Cl-;5.40毫克/我HCO3 -;2.41 mg / l NO3;0.80mg/l SO42-,平均钠吸收比(SAR)为1.36。各浓度下阳离子的相对丰度顺序为Ca2+> Mg2+ > Na+> K+ >∑Fe > Cr2+ > Cu2+,阴离子的相对丰度顺序为Cl- > HCO3- > NO3- >SO42+。使用Schumberger电极配置在研究区域进行了15次垂直电测深。探测曲线解释结果表明,该地区由四层和五层地电层组成。第三层和第四层由中砂、粗砂和砾石砂组成,构成含水层单元,平均至含水层深度为35.2m。除Okirighwre、Ajogodo和Ogorode的pH和∑Fe外,地下水中各项参数的浓度基本符合世界卫生组织推荐的生活和农业标准。除Ugbeyiyi和Ugberikoko的Cr2+浓度超过世界卫生组织的最高允许值0.05mg/l外,萨佩勒大部分城市的Cr2+浓度普遍低于规定标准。
AN INTEGRATION OF GEOPHYSICAL AND GEOCHEMICAL DATA IN EVALUAT- ING GROUNDWATER RESOURCES IN SAPELE METROPOLIS, WESTERN NIGER DELTA
An integration of geoelectrical and geochemical data was used in Sapele metropolis to delineate the aquifer unit(s) and evaluated the geochemical parameters of the groundwater in the area. Ten (10) water samples were collected from hand-dug wells for geochemical analysis. The geochemi- cal parameters showed average values of 6.20 pH; 156.0μs/cm EC; 7.60mg/l TH; 4.50mg/l, Ca2+; 4.20mg/l Mg2+; 0.95mg/I K+; 1.00mg/l Na+; 0.87mg/l ∑Fe; 0.03mg/I Cu2+; 0.04mg/I Cr2+ ; 28.68mg/l Cl- ; 5.40mg/I HCO3-; 2.41mg/l NO3-; 0.80mg/l SO42- and average sodium absorption ratio (SAR) of 1.36. The relative abundance of cations using these concentrations is in the order of Ca2+> Mg2+ > Na+> K+ > ∑Fe > Cr2+ > Cu2+ while those of anions are in the order Cl- > HCO3- > NO3- >SO42+. Fifteen (15) vertical electrical soundings were carried out in the study area using Schumberger electrode configuration. The result of the interpretation of the VES curves showed that the area is made up of four and five geoelectric layer. The third and fourth layer made up of medium, coarse and gravelly sand constitutes the aquifer unit(s), the average depth to the aquifer is 35.2m. The concentration of the various parameters determined in the groundwater were relatively in accordance with WHO recommended standard for domestic and agricultural purposes except pH and ∑Fe in Okirighwre , Ajogodo and Ogorode. Cr2+ concentrations generally were below stipu- lated standard in most of Sapele metropolis, except at Ugbeyiyi and Ugberikoko where concentra- tions exceeded WHO maximum allowance limit of 0.05mg/l.