Ata Joodavi

Dr. Ata Joodavi

orcid

Research Focus & Metrics

Academic Career Length

14Years (2013-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
11 December 2014 in Hydrogeology Journal
Verified
Journal Article
Closed access
PDF file
AIAzizallah Izady
Azizallah Izady
KDK. Davary
K. Davary
AAA. Alizadeh
A. Alizadeh
AZA. N. Ziaei
A. N. Ziaei
SAS. Akhavan
S. Akhavan
MBM. L. Brusseau
M. L. Brusseau

16 May 2013 in Arabian Journal of Geosciences
Verified
Journal Article
Closed access
PDF file
AIAzizallah Izady
Azizallah Izady
KDK. Davary
K. Davary
AAA. Alizadeh
A. Alizadeh
AZA. N. Ziaei
A. N. Ziaei
AAA. Alipoor
A. Alipoor
MBM. L. Brusseau
M. L. Brusseau

26 February 2015 in Stochastic Environmental Research and Risk Assessment
Verified
Journal Article
Closed access
PDF file
AJAta Joodavi
Ata Joodavi
MZMohammad - Zare
Mohammad - Zare
MMMASOUD MAHOOTCHI
MASOUD MAHOOTCHI

9 August 2017 in Hydrological Processes
Verified
Journal Article
Closed access
PDF file
AIAzizallah Izady
Azizallah Izady
OAOsman Abdalla
Osman Abdalla
AJAta Joodavi
Ata Joodavi
AKAkbar Karimi
Akbar Karimi
MCMingjie Chen
Mingjie Chen
ATAndrew Tompson
Andrew Tompson

1 October 2021 in Journal of Hydrology: Regional Studies
Verified
Journal Article
Open access
AJAta Joodavi
Ata Joodavi
RAReza Aghlmand
Reza Aghlmand
JPJoel Podgorski
Joel Podgorski
RDReza Dehbandi
Reza Dehbandi
AAAli Abbasi
Ali Abbasi

24 February 2017 in Water
Verified
Journal Article
Open access
PDF file
AIAzizallah Izady
Azizallah Izady
OAOsman Abdalla
Osman Abdalla
AJAta Joodavi
Ata Joodavi
Mingjie ChenMingjie Chen
Mingjie Chen
This study aims at modeling groundwater flow using MODFLOW in a transboundary hardrock–alluvium aquifer, located in northwestern Oman. A three-dimensional stratigraphic model of the study area representing the vertical and spatial extent of four principal hydro-geologic units (specifically, the Hawasina, ophiolite, Tertiary and alluvium) was generated using data collected from hundreds drilled borehole logs. Layer elevations and materials for four layers grid cells were taken from the generated stratigraphic model in which the materials and elevations were inherited from the stratigraphic model that encompasses the cell. This process led to accurate grid so that the developed groundwater conceptual model was mapped to simulate the groundwater flow and to estimate groundwater balance components and sustainable groundwater extraction for the October 1996 to September 2013 period. Results show that the long-term lateral groundwater flux ranging from 4.23 to 11.69 Mm3/year, with an average of 5.67 Mm3/year, drains from the fractured eastern ophiolite mountains into the alluvial zone. Moreover, the long-term regional groundwater sustainable groundwater extraction is 18.09 Mm3/year for 17 years, while it is, respectively, estimated as 14.51, 16.31, and 36.00 Mm3/year for dry, normal, and wet climate periods based on standardized precipitation index (SPI) climate condition. Considering a total difference in groundwater levels between eastern and western points of the study area on the order of 228 m and a 12-year monthly calibration period (October 1996 to September 2008), a root mean squared error (RMSE) in predicted groundwater elevation of 2.71 m is considered reasonable for the study area characterized by remarkable geological and hydrogeological diversity. A quantitative assessment of the groundwater balance components and particularly sustainable groundwater extraction for the different hydrological period would help decision makers to better understand the water resources in the Al-Buraimi region. In addition, it would assist decision makers to improve existing strategies to enhance the decision making for future developments.