Investigation of hydraulic properties on groundwater resources discharge of Bam plain
Subject Areas :
1 - کارشناس ارشد آبهای زیرزمینی، شرکت مهندسی آب و فاضلاب کرمان،
Keywords: Groundwater, discharge, resources, Aquifer, hydraulic properties, Bam plain,
Abstract :
Bam plain in Kerman province, about 207 kilometers Southeast of the center is located at edge of Lut Desert is an arid country. In this study, all the hydraulic parameters of the aquifer including hydraulic conductivity(K), transmissivity (T) and the thickness of the aquifer (b) has been studied. With the implementation of aquifer pumping test wells observational transfer coefficient is measured and the thickness of the aquifer was estimated using geophysical plain in different directions. The hydraulic conductivity calculated by the formula Darcy and all data processing software for Excel, Surfer and GIS data. Hydraulic parameters, transmissivity coefficient and the thickness of aquifer as zoning plans and results have been interpreted. The results show t Bam plain in Kerman province, about 207 kilometers Southeast of the center is located at edge of Lut Desert is an arid country. In this study, all the hydraulic parameters of the aquifer including hydraulic conductivity(K), transmissivity (T) and the thickness of the aquifer (b) has been studied. With the implementation of aquifer pumping test wells observational transfer coefficient is measured and the thickness of the aquifer was estimated using geophysical plain in different directions. The hydraulic conductivity calculated by the formula Darcy and all data processing software for Excel, Surfer and GIS data. Hydraulic parameters, transmissivity coefficient and the thickness of aquifer as zoning plans and results have been interpreted. The results show that hydraulic conductivity in parts of eastern and south-eastern lowland plains has been higher that other parts. As well as the ability to transfer coefficient of the aquifer from the northwest to southeast is rising. In general, the thickness of aquifer from the southeast to the northwest and central plains are on the rise. So if a well or aqueduct to exploit groundwater resources in eastern and southeastern plains discharge dig a well than other areas will be plain. Because due to the high permeability sediments above the aquifer transfer coefficient is higher. hat hydraulic conductivity in parts of eastern and south-eastern lowland plains has been higher that other parts. As well as the ability to transfer coefficient of the aquifer from the northwest to southeast is rising. In general, the thickness of aquifer from the southeast to the northwest and central plains are on the rise. So if a well or aqueduct to exploit groundwater resources in eastern and southeastern plains discharge dig a well than other areas will be plain. Because due to the high permeability sediments above the aquifer transfer coefficient is higher.