ASSESSMENT OF FRACTURES ROLE IN THE CHAMASIAB SPRING DISCHARGE IN THE NORTHEASTERN KHUZESTAN PROVINCE

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.

KALANTARI N.; KHOOBYARI A.; DORRANINEJAD M.S.

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

Journal Paper

Paper Information

Journal: JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY) Year:2012 | Volume:8 | Issue:1 Page(s): 65-72

Download Full-Text

Persian Verion

View:

890

Download:

Cites:

Information Journal Paper

Title

ASSESSMENT OF FRACTURES ROLE IN THE CHAMASIAB SPRING DISCHARGE IN THE NORTHEASTERN KHUZESTAN PROVINCE

Author(s)

KALANTARI N. | KHOOBYARI A. | DORRANINEJAD M.S. | Issue Writer Certificate

Keywords

SAND STONEQ2

AGHAJARIQ2

DISCHARGEQ2

JOINTS AND FRACTURES SYSTEMQ2

SAND STONE PERMEABILITYQ2

Abstract

Chamasiab watershed is located in the northeastern Khuzestan province. The sandstone unit of the AGHAJARI Formation has caused to be the formation of the sandstone aquifer in the area which DISCHARGEs to the surface via Chamasiab spring. This study discusses the importance of fractures in the DISCHARGE of Chamasiab spring and recognizing of the area groundwater system as well. For this purpose, in the different parts of the area, the JOINTS AND FRACTURES SYSTEM has been measured. Also, the fracture density map has been prepared by using GIS and remote sensing (RS) techniques. The results show that fractures in the thick layers of SAND STONE have a major role in the sandstones permeability, and it has also been considered as the most important factor of Chamasiab spring DISCHARGE in the studied area. Spring DISCHARGE changes from 20L/Sec to 60 L/Sec in wet and dry seasons respectively. This reflects the permeability of sandstone in the area, and also shows that the spring response with respect to rainfall is high in the studied area.

Cites

No record.

References

No record.

Cite

APA: Copy

KALANTARI, N., KHOOBYARI, A., & DORRANINEJAD, M.S.. (2012). ASSESSMENT OF FRACTURES ROLE IN THE CHAMASIAB SPRING DISCHARGE IN THE NORTHEASTERN KHUZESTAN PROVINCE. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), 8(1), 65-72. SID. https://sid.ir/paper/127096/en

Vancouver: Copy

KALANTARI N., KHOOBYARI A., DORRANINEJAD M.S.. ASSESSMENT OF FRACTURES ROLE IN THE CHAMASIAB SPRING DISCHARGE IN THE NORTHEASTERN KHUZESTAN PROVINCE. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)[Internet]. 2012;8(1):65-72. Available from: https://sid.ir/paper/127096/en

IEEE: Copy

N. KALANTARI, A. KHOOBYARI, and M.S. DORRANINEJAD, “ASSESSMENT OF FRACTURES ROLE IN THE CHAMASIAB SPRING DISCHARGE IN THE NORTHEASTERN KHUZESTAN PROVINCE,” JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), vol. 8, no. 1, pp. 65–72, 2012, [Online]. Available: https://sid.ir/paper/127096/en

Related Journal Papers