عنوان مقاله [English]
نویسندگان [English]چکیده [English]
Shahrekord aquifer is the primary resource of water for various uses across Shahrekord plain. The main objectives of this study were to investigate the fluctuations in spatial variability and zonal mapping of conductance (EC), total dissolved solids (TDS), total suspended solids (TSS) and turbidity of Shahrekord groundwater during a year. Ninety-seven wells were sampled during four occasions (June, July, September, and November) in 2010. The mean of EC (both approximately 530 µS/cm) in June and July reduced to 370 µS/cm.