Salinity mapping of coastal groundwater aquifers using hydrogeochemical and geophysical methods: a case study from north Kelantan,Malaysia

Integrated hydrogeochemical and geophysical methods were used to study the salinity of groundwater aquifers along the coastal area of north Kelantan. For the hydrogeochemical investigation, analysis of major ion contents of the groundwater was conducted, and other chemical parameters such as pH and total dissolved solids were also determined. For the geophysical study, both geoelectrical resistivity soundings and reflection seismic surveys were conducted to determine the characteristics of the subsurface and groundwater contained within the aquifers. The pH values range from 6.2 to 6.8, indicating that the groundwater in the study area is slightly acidic. Low content of chloride suggests that the groundwater in the first aquifer is fresh, with an average concentration of about 15.8 mg/l and high geoelectrical resistivity (>45 ohm m). On the other hand, the groundwater in the second aquifer is brackish, with chloride concentration ranging from 500 mg/l to 3,600 mg/l and very low geoelectrical resistivity (<45 ohm m) as well as high concentration of total dissolved solids (>1,000 mg/l). The groundwater in the third aquifer is fresh, with chloride concentrations generally ranging from 2 mg/l to 210 mg/l and geoelectrical resistivity of greater than 45 ohm m. Fresh and saltwater interface in the first aquifer is generally located directly in the area of the coast, but, for the second aquifer, both hydrogeochemical and geoelectrical resistivity results indicate that the fresh water and saltwater interface is located as far as 6 km from the beach. The considerable chloride ion content initially suggests that the salinity of the groundwater in the second aquifer is probably caused by the intrusion of seawater. However, continuous monitoring of the chloride content of the second aquifer indicated no significant changes with time, from which it can be inferred that the salinity of the groundwater is not affected by seasonal seawater intrusion. Schoeller diagrams illustrate that sulphate concentrations of the groundwater of the second aquifer are relatively low compared to those of the recent seawater. Therefore, this result suggests that the brackish water in the second aquifer is probably from ancient seawater that was trapped within the sediments for a long period of time, rather than due to direct seawater intrusion.     

焦家金矿矿化元素因子分析

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廊坊市规划区土壤环境污染的地球化学评价

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面向直接入库的测量绘图系统的研制

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基于SXCORS网络的RTK技术在控制测量中的应用及精度分析

结合工程实例,对基于SXCORS网络的RTK技术在控制测量中与静态GPS、水准测量的数据进行了比较,对其精度进行了分析,得出了在有利条件下该技术的适用性。     

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大型贯通测量中常常使用加测陀螺边来提高贯通测量精度,但目前对于陀螺定向边的位置选取并无明确规范和要求。本文主要探讨了不同位置的陀螺定向边选取对贯通测量精度的影响。实验结果表明,井下选取的陀螺定向边与测定仪器常数的地面已知边之间距离过大对于贯通测量精度影响较大,在井下选取陀螺定向边位置时,应与测定仪器常数的地面已知边距离保持在3 000 m以内为优。     

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面向21世纪非测量专业测量教学的思考

分析了在测绘高新技术飞速发展条件下,非测量专业测量教学面临的诸多问题,并就一些关键性问题提出了自己的看法,仅供同行参考.