摘要
A hydrochemical and tracer study(uranine injection) was conducted in Jurassic limestone of the Posht-e-Naz area in the Alborz belt to evaluate hydraulic relations between a large diameter(about 100 m) sinkhole and springs and aquifer parameters.A main goal of the project was to find out the source of turbidity of the Emarate drinking water supply spring(SP4) in rainy season.Springs discharge were measured and hydrochemical investigation were carried out.The uranine tracer was injected and eight springs,three wells and the Neka River were selected and totally 989 samples in 107 days were collected.Hydrochemical data demonstrated a relative connection between sinkhole(Sh1) and spring(SP4).The results of the tracing by sampling water indicated only a hydraulic connection between Sange-Nou spring(SP8) and injection point,while the charcoal packets analysis revealed tracer exits from spring numbers SP1,SP3,SP4,SP5,SP8,in wells W1 and W2,and in the Neka River.The concentration-time curves of charcoal packets for qualitative analysis and exit tracer for quantitative analysis is also assessed.
A hydrochemical and tracer study （uranine injection） was conducted in Jurassic limestone of the Posht-e-Naz area in the Alborz belt to evaluate hydraulic relations between a large diameter （about 100m） sinkhole and springs and aquifer parameters. A main goal of the project was to find out the source of turbidity of the Emarate drinking water supply spring （SP4） in rainy season. Springs discharge were measured and hydrochemical investigation were carried out. The uranine tracer was injected and eight springs, three wells and the Neka River were selected and totally 989 samples in 107 days were collected. Hydrochemical data demonstrated a relative connection between sinkhole （Shl） and spring （SP4）. The results of the tracing by sampling water indicated only a hydraulic connection between Sange- Nou spring （SP8） and injection point, while the charcoal packets analysis revealed tracer exits from spring numbers SP1, SP3, SP4, SP5, SP8, in wells W1 and W2, and in the Neka River. The concentration - time curves of charcoal packets for qualitative analysis and exit tracer for quantitative analysis is also assessed.
