Department of Environmental Engineering, Dokuz Eylül University, 35160, Buca-Izmir, Turkey.
Environ Monit Assess. 2011 Jan;172(1-4):445-62. doi: 10.1007/s10661-010-1346-2. Epub 2010 Feb 6.
The main objective of this study was to statistically evaluate the significance of seasonal groundwater quality change and to provide an assessment on the spatial distribution of specific groundwater quality parameters. The studied area was the Mount Nif karstic aquifer system located in the southeast of the city of Izmir. Groundwater samples were collected at 57 sampling points in the rainy winter and dry summer seasons. Groundwater quality indicators of interest were electrical conductivity (EC), nitrate, chloride, sulfate, sodium, some heavy metals, and arsenic. Maps showing the spatial distributions and temporal changes of these parameters were created to further interpret spatial patterns and seasonal changes in groundwater quality. Furthermore, statistical tests were conducted to confirm whether the seasonal changes for each quality parameter were statistically significant. It was evident from the statistical tests that the seasonal changes in most groundwater quality parameters were statistically not significant. However, the increase in EC values and aluminum concentrations from winter to summer was found to be significant. Furthermore, a negative correlation between sampling elevation and groundwater quality was found. It was shown that with simple statistical testing, important conclusions can be drawn from limited monitoring data. It was concluded that less groundwater recharge in the dry period of the year does not always imply higher concentrations for all groundwater quality parameters because water circulation times, lithology, quality and extent of recharge, and land use patterns also play an important role on the alteration of groundwater quality.
本研究的主要目的是从统计学上评估地下水水质季节性变化的重要性,并评估特定地下水水质参数的空间分布。研究区域是位于伊兹密尔市东南部的内夫谢希尔岩溶含水层系统。在雨季的冬季和旱季的夏季,在 57 个采样点采集地下水样本。研究的地下水水质指标包括电导率 (EC)、硝酸盐、氯化物、硫酸盐、钠、一些重金属和砷。创建了显示这些参数的空间分布和时间变化的地图,以进一步解释地下水质量的空间模式和季节性变化。此外,还进行了统计检验,以确认每个水质参数的季节性变化是否具有统计学意义。统计检验表明,大多数地下水水质参数的季节性变化没有统计学意义。然而,从冬季到夏季,EC 值和铝浓度的增加被发现具有统计学意义。此外,还发现采样高程与地下水质量之间存在负相关。研究表明,通过简单的统计测试,可以从有限的监测数据中得出重要结论。研究得出的结论是,一年中干旱期的地下水补给量较少并不总是意味着所有地下水水质参数的浓度都会升高,因为水循环时间、岩性、补给的质量和范围以及土地利用模式也会对地下水水质的变化产生重要影响。