Can river flow prevent land subsidence in urban areas?
(2024) In Science of the Total Environment 917(170557).- Abstract
- Land subsidence, a silent death, occurs due to various factors like significant reduction in groundwater (GW) levels. It is a widespread phenomenon with irreparable consequences on buildings, infrastructures, and, in severe cases, groundwater aquifers. This study aims to assess the impact of river flow on the acceleration and control of land subsidence in an arid and semi-arid region. To achieve this goal, we analyze the interconnection between GW and SW and investigate the role of the Zayandeh-Rud River's drying up on land subsidence in the Isfahan-Borkhar aquifer in Iran's central plateau. To facilitate this assessment, we utilize the Interferometric Synthetic Aperture Radar (InSAR) technique to estimate the vertical deformation velocity... (More)
- Land subsidence, a silent death, occurs due to various factors like significant reduction in groundwater (GW) levels. It is a widespread phenomenon with irreparable consequences on buildings, infrastructures, and, in severe cases, groundwater aquifers. This study aims to assess the impact of river flow on the acceleration and control of land subsidence in an arid and semi-arid region. To achieve this goal, we analyze the interconnection between GW and SW and investigate the role of the Zayandeh-Rud River's drying up on land subsidence in the Isfahan-Borkhar aquifer in Iran's central plateau. To facilitate this assessment, we utilize the Interferometric Synthetic Aperture Radar (InSAR) technique to estimate the vertical deformation velocity of the aquifer (average land subsidence rate). The results show that the Isfahan-Borkhar aquifer has experienced a significant annual decline of more than 25 m, with an alarming rate exceeding 0.8 m/year. Our analysis of 31 piezometric wells (P-Wells) from 2000 to 2022 reveals a downward monotonic (in 16 P-Wells) and nonmonotonic (in 12 P-Wells) trend in groundwater table changes. Moreover, the GW table in the P-Wells near the river depends entirely on river flow. Furthermore, our findings indicate that river regulation exerts a dominant role in the control of land subsidence. Consequently, when water flows in the Zayandeh-Rud River, the rate of land subsidence declines significantly, particularly in urban regions. Therefore, maintaining a constant flow of water in the river can prevent or reduce ongoing land subsidence in Isfahan. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/cb4296e8-ce25-4e67-b9ab-8e13dd5ab884
- author
- Sharifi, Alireza ; Khodaei, Behshid LU ; Ahrari, Amirhossein ; Hashemi, Hossein LU and Torabi Haghighi, Ali
- organization
- publishing date
- 2024-01-27
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- River regulation, Groundwater depletion, InSAR
- in
- Science of the Total Environment
- volume
- 917
- issue
- 170557
- publisher
- Elsevier
- external identifiers
-
- scopus:85185175378
- ISSN
- 1879-1026
- DOI
- 10.1016/j.scitotenv.2024.170557
- language
- English
- LU publication?
- yes
- id
- cb4296e8-ce25-4e67-b9ab-8e13dd5ab884
- date added to LUP
- 2024-02-05 11:38:48
- date last changed
- 2024-04-04 04:01:42
@article{cb4296e8-ce25-4e67-b9ab-8e13dd5ab884, abstract = {{Land subsidence, a silent death, occurs due to various factors like significant reduction in groundwater (GW) levels. It is a widespread phenomenon with irreparable consequences on buildings, infrastructures, and, in severe cases, groundwater aquifers. This study aims to assess the impact of river flow on the acceleration and control of land subsidence in an arid and semi-arid region. To achieve this goal, we analyze the interconnection between GW and SW and investigate the role of the Zayandeh-Rud River's drying up on land subsidence in the Isfahan-Borkhar aquifer in Iran's central plateau. To facilitate this assessment, we utilize the Interferometric Synthetic Aperture Radar (InSAR) technique to estimate the vertical deformation velocity of the aquifer (average land subsidence rate). The results show that the Isfahan-Borkhar aquifer has experienced a significant annual decline of more than 25 m, with an alarming rate exceeding 0.8 m/year. Our analysis of 31 piezometric wells (P-Wells) from 2000 to 2022 reveals a downward monotonic (in 16 P-Wells) and nonmonotonic (in 12 P-Wells) trend in groundwater table changes. Moreover, the GW table in the P-Wells near the river depends entirely on river flow. Furthermore, our findings indicate that river regulation exerts a dominant role in the control of land subsidence. Consequently, when water flows in the Zayandeh-Rud River, the rate of land subsidence declines significantly, particularly in urban regions. Therefore, maintaining a constant flow of water in the river can prevent or reduce ongoing land subsidence in Isfahan.}}, author = {{Sharifi, Alireza and Khodaei, Behshid and Ahrari, Amirhossein and Hashemi, Hossein and Torabi Haghighi, Ali}}, issn = {{1879-1026}}, keywords = {{River regulation; Groundwater depletion; InSAR}}, language = {{eng}}, month = {{01}}, number = {{170557}}, publisher = {{Elsevier}}, series = {{Science of the Total Environment}}, title = {{Can river flow prevent land subsidence in urban areas?}}, url = {{http://dx.doi.org/10.1016/j.scitotenv.2024.170557}}, doi = {{10.1016/j.scitotenv.2024.170557}}, volume = {{917}}, year = {{2024}}, }