ESTIMATION OF PALEOCLIMATE STATUS BY CHLORIDE GEOCHEMICAL TRACERS IN ARDABIL PLAIN VADOSE ZONE

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.

SAADATI HOSSEIN

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

Journal Paper

Paper Information

Journal: WATERSHED ENGINEERING AND MANAGEMENT Year:2016 | Volume:8 | Issue:3 Page(s): 310-321

Download Full-Text

Persian Verion

View:

488

Download:

Cites:

Information Journal Paper

Title

ESTIMATION OF PALEOCLIMATE STATUS BY CHLORIDE GEOCHEMICAL TRACERS IN ARDABIL PLAIN VADOSE ZONE

Author(s)

SAADATI HOSSEIN | Issue Writer Certificate

Keywords

CHLORIDE GEOCHEMICAL TRACERQ1

DRY AND WET PERIODSQ1

PALEOCLIMATEQ1

WATER AGE ARDABILQ1

IRANQ1

Abstract

In this study, rainfall, percolation and hydrogeological processes relationship were evaluated using geochemical tracers to determinate PALEOCLIMATE in the Ardabil Plain. The occurrence of DRY AND WET PERIODS was also determined with the help of tracer used in six profiles. The DRY AND WET PERIODS were then evaluated by the Edmund-Allison equations based on interpretation of soil water chloride concentrations and long– term precipitation measured in different periods. Applying the chloride mass balance technique to soil water chloride profiles improved the boundary conditions associated with wetter and drier climate in last times. The estimated ages through sediment cores chemistry varied from 737 years in Imijah core to 4511 years in Gharahlar core with two recorded DRY AND WET PERIODS. Precipitation of recently drier climate was estimated around 202 mm in 116 last years and second drier climate was estimated around 83 mm in 473 last years. Precipitation of recently wetter climate was also estimated around 451 mm in 210 last years and second wetter climate was estimated around 703 mm in 735 last years. The second wetter had the highest amount of precipitation in 3600 years period. The Ardabil plain had a moderate drier climate since 1100 to 2900 years ago. In addition, the results showed that the wetter climate happened during last 2900 to 3550 years. According to this results, the present climate moves towards drier climate. A comparative analysis of data from six profile sites indicated that there were short term oscillations of wetter and drier climate.

Cites

No record.

References

No record.

Cite

APA: Copy

SAADATI, HOSSEIN. (2016). ESTIMATION OF PALEOCLIMATE STATUS BY CHLORIDE GEOCHEMICAL TRACERS IN ARDABIL PLAIN VADOSE ZONE. WATERSHED ENGINEERING AND MANAGEMENT, 8(3 ), 310-321. SID. https://sid.ir/paper/234780/en

Vancouver: Copy

SAADATI HOSSEIN. ESTIMATION OF PALEOCLIMATE STATUS BY CHLORIDE GEOCHEMICAL TRACERS IN ARDABIL PLAIN VADOSE ZONE. WATERSHED ENGINEERING AND MANAGEMENT[Internet]. 2016;8(3 ):310-321. Available from: https://sid.ir/paper/234780/en

IEEE: Copy

HOSSEIN SAADATI, “ESTIMATION OF PALEOCLIMATE STATUS BY CHLORIDE GEOCHEMICAL TRACERS IN ARDABIL PLAIN VADOSE ZONE,” WATERSHED ENGINEERING AND MANAGEMENT, vol. 8, no. 3 , pp. 310–321, 2016, [Online]. Available: https://sid.ir/paper/234780/en

Related Journal Papers