TEMPORAL AND SPATIAL VARIABILITY OF GROUNDWATER SALINITY IN URMIA PLAIN

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.

SOKOUTI OSKOEE REZA

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

Journal Paper

Paper Information

Journal: JOURNAL OF WATER AND SOIL RESOURCES CONSERVATION Year:2012 | Volume:1 | Issue:4 Page(s): 19-25

Download Full-Text

Persian Verion

View:

1,756

Download:

Cites:

Information Journal Paper

Title

TEMPORAL AND SPATIAL VARIABILITY OF GROUNDWATER SALINITY IN URMIA PLAIN

Author(s)

SOKOUTI OSKOEE REZA | Issue Writer Certificate

Keywords

GEOSTATISTICSQ1

GROUNDWATER SALINITYQ2

KRIGINGQ2

URMIAQ2

Abstract

The intensify process of lowering URMIA lake level has led to reduce water quality, making it brackish and unusable in wells of Lake Marginal Lands. The present study investigated changes in GROUNDWATER SALINITY in URMIA plain using geostatistical models, and compares the results of the mapping in three time periods. To assess salinity of the groundwater, data from 57 wells in the period of 1380, 1384 and 1387 were analyzed, using KRIGING in GIS, GS+ and ARCVIEW8 soft wares. The results indicated that application of KRIGING, experimental semi-variogram with spherical model provided better predictions with correlation coefficient of 0.99. According to the obtained GROUNDWATER SALINITY maps, land area with more than 2 dS/m GROUNDWATER SALINITY in 1380 was equal to 1924 hectares that has increased to 8331 hectares in 1387. During these years, in the study area the GROUNDWATER SALINITY with less than 1 dS/m was decreased about 14675 hectares. The observed maximum salinity value in 1380 has increased from 1.91 to 5.8 dS/m in 1387.

Cites

THE USE OF A HYBRID FUZZY-AHP SYSTEM ON THE EVALUATION AND MAPPING OF SOIL FERTILITY

References

Cite

APA: Copy

SOKOUTI OSKOEE, REZA. (2012). TEMPORAL AND SPATIAL VARIABILITY OF GROUNDWATER SALINITY IN URMIA PLAIN. JOURNAL OF WATER AND SOIL RESOURCES CONSERVATION, 1(4), 19-25. SID. https://sid.ir/paper/232307/en

Vancouver: Copy

SOKOUTI OSKOEE REZA. TEMPORAL AND SPATIAL VARIABILITY OF GROUNDWATER SALINITY IN URMIA PLAIN. JOURNAL OF WATER AND SOIL RESOURCES CONSERVATION[Internet]. 2012;1(4):19-25. Available from: https://sid.ir/paper/232307/en

IEEE: Copy

REZA SOKOUTI OSKOEE, “TEMPORAL AND SPATIAL VARIABILITY OF GROUNDWATER SALINITY IN URMIA PLAIN,” JOURNAL OF WATER AND SOIL RESOURCES CONSERVATION, vol. 1, no. 4, pp. 19–25, 2012, [Online]. Available: https://sid.ir/paper/232307/en

Related Journal Papers