Spatial and Temporal Variation of Groundwater Flow in Southeastern bank of Urmia Lake

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

SHEMSHAKI AMIR; KARAMI GHOLAM HOSSEIN

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: HYDROGEOLOGY Year:2019 | Volume:4 | Issue:1 Page(s): 26-41

Download Full-Text

Persian Verion

View:

573

Download:

Cites:

Information Journal Paper

Title

Spatial and Temporal Variation of Groundwater Flow in Southeastern bank of Urmia Lake

Author(s)

SHEMSHAKI AMIR | KARAMI GHOLAM HOSSEIN | Issue Writer Certificate

Keywords

Urmia lake

temporal and spatial deviation

hydraulic gradient

groundwater portion

Abstract

In recent years, Urmia lake has dried up and its salinity has increased significantly. There are various reasons for this phenomenon. There is even a difference in the manner and rate of direct or indirect role of groundwater compared to surface water. Therefore, in this study, in order to identify the interaction of groundwater and surface water in the southeastern coast of the lake as the most important input to the surface waters of the lake, the temporal and spatial variations of groundwater flow were investigated. This study was carried out using the groundwater level map in May 2008, 2013 and 2016, as well as the groundwater transmissivity map and the rate of groundwater inflow and outflow using groundwater gradient changes. In addition, five cross sections including groundwater leveling and slope information at the desired time, as well as type of sediment deposits were used. In this study, it was found that groundwater inflow and outflow do not play an important role in aquifer volume in the region. Therefore, severe and local groundwater withdrawal due to over pumping, as well as changes in the volume and distribution of surface water resources, play a very important role in changing the direction and gradient of groundwater flows. There is a risk of saline water intrusion to the aquifers where there is a severe withdrawal in groundwater. In some areas, especially in the southern regions, the presence of underground dams of clay deposits with very high plasticity prevents the saline water intrusion into inland areas.

Cites

No record.

References

No record.

Cite

APA: Copy

SHEMSHAKI, AMIR, & KARAMI, GHOLAM HOSSEIN. (2019). Spatial and Temporal Variation of Groundwater Flow in Southeastern bank of Urmia Lake. HYDROGEOLOGY, 4(1 ), 26-41. SID. https://sid.ir/paper/268179/en

Vancouver: Copy

SHEMSHAKI AMIR, KARAMI GHOLAM HOSSEIN. Spatial and Temporal Variation of Groundwater Flow in Southeastern bank of Urmia Lake. HYDROGEOLOGY[Internet]. 2019;4(1 ):26-41. Available from: https://sid.ir/paper/268179/en

IEEE: Copy

AMIR SHEMSHAKI, and GHOLAM HOSSEIN KARAMI, “Spatial and Temporal Variation of Groundwater Flow in Southeastern bank of Urmia Lake,” HYDROGEOLOGY, vol. 4, no. 1 , pp. 26–41, 2019, [Online]. Available: https://sid.ir/paper/268179/en

Related Journal Papers