1- Corresponding author. assistant Professor, Department of Geography Education, Farhangian University,Tehran, Iran, Farhangian Birjand University , m.motamedirad@cfu.ac.ir
2- assistant Professor, Department of Geology, Payame Noor University, Tehran, Iran, Payam Noor University of Bojnord
3- assistant Professor, Department of Geography Education, Farhangian University,Tehran, Iran, Farhangian University of Bojnoord
4- BA student of Architectural engineering, Bojnourd Branch,Islamic Azad University, Bojnourd, Iran., Islamic Azad University, Bojnord branch
2- assistant Professor, Department of Geology, Payame Noor University, Tehran, Iran, Payam Noor University of Bojnord
3- assistant Professor, Department of Geography Education, Farhangian University,Tehran, Iran, Farhangian University of Bojnoord
4- BA student of Architectural engineering, Bojnourd Branch,Islamic Azad University, Bojnourd, Iran., Islamic Azad University, Bojnord branch
Abstract: (785 Views)
| The continuation of drought and the simultaneous increase in dependence on underground water sources in the past decades have expanded the range of areas subject to subsidence to many different parts of the country, which results in a lot of damage.In order to reduce the damages caused by land subsidence, it is necessary to have a complete and accurate understanding of this phenomenon. In recent decades, the virtual aperture radar (SAR) interferometric technique has become a common method for measuring subsidence. In this research, field data such as piezometric wells and groundwater drop in the minimum and maximum periods and exploitation wells were used to calculate the amount of discharge in the aquifer using IDW interpolation, aiming at analyzing the time series of the subsidence of the Esfarayen plain. besides, radar data including Sentinel 1 images were used to calculate the subsidence rate in the first 8 months of 2023. The results of the research show that the amount of subsidence in the study basin was from 1 to 12 mm in a period of 8 months and 75.2% of the area of the basin was in the medium critical and very critical zone, which can be recognized based on this. He showed that the Esfrain plain is in a critical state.The most water extraction and subsidence has been related to to south of Sankhasat, south of Kharasha, south of Arg, south of Gazan, Jafarabad Kharaba and Mehdiabad of Kal Beko wells, which are located in the very critical area and require efficient management of groundwater resources in order to control land subsidence. |
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This work is licensed under a Creative Commons — Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)