Drought is a phenomenon that threating water quality in addition to its shortage. In this paper we investigate the effect of drought on surface water quality of Kashkan watershed. For this purpose, during the collection of meteorological data and water quality data during 20 years (1987 to 2009) from Meteorology and Water Resources offices of Lorestan province, initially duration and severity of meteorological and hydrological droughts were determined by SPI, RDI and SDI Indices. Later in periods that intensity and duration of drought were more than other period, percent changes of water quality to the long-term average was calculated then agricultural and drinking water quality analysis in the form of two charts Schuler and Wilcox
was performed. Also, the linear trend of data was investigated for highlighting the effect of drought on water quality changes. Results indicate that drought has significant changes in parameters of surface water resources especially EC, TDS, NA, CL and SO24.Also the results showed that water quality in terms of Schuler & Wilcox graphs has changed in effect of drought. The quality of Afarineh and Chan Anjir rivers drinking water has changed from ok classes to acceptable grade and for agricultural purposes has changed from C2S1 grade to C3S1 grade. Finally, the overall analysis of linier trend graphs shows that the increasing trend of drought has a negative impact on surface waters quality of Kashkan watershed.
Mehrgerd region of Semirom County has been facing the water shortage for several years. The emergence of drought has led to a decline in water resources in recent years; and there are various reasons for climate change and increased consumption in order to reduce water resources. The present study aimed to investigate the process of temperature and precipitation variations and its possible effects on groundwater resources. Therefore, the Mann–Kendall test was applied to the climatic data of five selected stations during a 28-year statistical period as well as the groundwater level statistics of 33 observation wells. Effects of temporal temperature and precipitation variations on water resources were assessed using the correlation between climatic parameters, SPI drought index and water resources statistics. Results indicated that the average monthly temperature had an ascending trend in Mehrgerd region especially in winter and it could lead to changes in types of precipitation and early snow melting. The precipitation had no significant trend in most months (except for the observed precipitation reduction in January and March). Groundwater resources had a significant descending trend in almost all months of year. The study on the relationships of precipitation parameter and water resources of region indicated that the precipitation parameter affected groundwater resources with a delay of 6 months. The effects of wet and dry periods on the status of groundwater level are quite obvious; and the groundwater level of plain has had an annual decline since the onset of a drought period in 2008. Despite the fact that this level has fluctuated with the severity and weakness of drought in subsequent years, but the reduction of water level has been the overall trend of groundwater level in Mehrgerd plain.
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