SOURCES OF SALINITY IN GROUNDWATER OF SHABESTAR PLAIN AQUIFERS

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.

ASGHARI MOGHADAM A.; MOHAMMADI A.

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

Journal Paper

Paper Information

Journal: JOURNAL OF AGRICULTURAL KNOWLEDGE Year:2003 | Volume:13 | Issue:3 Page(s): 69-78

Download Full-Text

Persian Verion

View:

2,437

Download:

Cites:

Information Journal Paper

Title

SOURCES OF SALINITY IN GROUNDWATER OF SHABESTAR PLAIN AQUIFERS

Author(s)

ASGHARI MOGHADAM A. | MOHAMMADI A. | Issue Writer Certificate

Keywords

GROUNDWATER POLLUTIONQ4

HYDROGEOCHEMISTRYQ4

SALINE WATER INTRUSIONQ4

SHABESTAR PLAIN.Q4

Abstract

The fertile plain of Shabestar is located 40km. west of Tabriz and northeast of Urumiyeh lake and its area is about 617 km^2. SHABESTAR PLAIN.is an active cultivated area with low annual precipitation and surface runoff thus. the groundwater resources have a vital role in supplying agricultural drinking domestic and industrial water demands. SALINE WATER INTRUSION into the fresh water aquifers is highly increased in recent years and some of abstraction wells are left unused. The purpose of this paper was to determine origin of the water salinity in the plain. Therefore from the previous hydro-geological data and several number of sampling from the plain wells two groups of saline water were distinguished. Group 1 contain the low ratios of S04/Cl and Na/Cl and high percent of Ca + Mg. Saline water of the central parts of the plain lies in this group. Group2 contain the high ratios of SO__4/Cl and Na/Cl and low percent of Ca+Mg. Saline water of the southeast and south margin of the plain lies in this group. In the central parts ratios of SO__4 and Cl to the sum of anions are similar to those of the Urumiyeh Lake. Consequently saline water source in these parts can be related to Urumiyeh Lake. However in the southeast and south margin of the plain ratios of SO4 and Cl to the sum of anions are different from those of the Urumiyeh Lake. Evaporation from the shallow groundwater seepage from saline rivers and dissolution of the evaporational deposits are causes of the salinity.

Cites

No record.

References

مطالعه فیزیکی و شیمیایی آب دریاچه ارومیه

Cite

APA: Copy

ASGHARI MOGHADAM, A., & MOHAMMADI, A.. (2003). SOURCES OF SALINITY IN GROUNDWATER OF SHABESTAR PLAIN AQUIFERS. JOURNAL OF AGRICULTURAL KNOWLEDGE, 13(3), 69-78. SID. https://sid.ir/paper/28985/en

Vancouver: Copy

ASGHARI MOGHADAM A., MOHAMMADI A.. SOURCES OF SALINITY IN GROUNDWATER OF SHABESTAR PLAIN AQUIFERS. JOURNAL OF AGRICULTURAL KNOWLEDGE[Internet]. 2003;13(3):69-78. Available from: https://sid.ir/paper/28985/en

IEEE: Copy

A. ASGHARI MOGHADAM, and A. MOHAMMADI, “SOURCES OF SALINITY IN GROUNDWATER OF SHABESTAR PLAIN AQUIFERS,” JOURNAL OF AGRICULTURAL KNOWLEDGE, vol. 13, no. 3, pp. 69–78, 2003, [Online]. Available: https://sid.ir/paper/28985/en

Related Journal Papers