SOURCE IDENTIFICATION OF SOUTH BAFGH SAND DUNES

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.

AHMADI HASAN; FEYZNIA S.; EKHTESASI M.R.; GHANEI BAFGHI M.J.

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

Journal Paper

Paper Information

Journal: Desert Year:2001 | Volume:6 | Issue:2 Page(s): 33-49

Download Full-Text

Persian Verion

View:

2,298

Download:

Cites:

Information Journal Paper

Title

SOURCE IDENTIFICATION OF SOUTH BAFGH SAND DUNES

Author(s)

AHMADI HASAN | FEYZNIA S. | EKHTESASI M.R. | GHANEI BAFGHI M.J. | Issue Writer Certificate

Keywords

SOURCE OF EOLIAN SEDIMENTSQ4

DIRECTION AND LOCATION OF SOURCE AREASQ4

PEDIMENTQ4

EPANDAGE PLAINQ4

Abstract

South Bafgh lands are among the central Iran arid areas which have low rainfall and poor vegetation. Deflation of these bare lands has caused soil erosion and in addition to degradation of soil texture, damages to roads especially Tehran-Bandar Abbas and Tehran-Kerman railroads in South Bafgh and also agricultural lands and adjacent villages. Due to accumulation of transported sediments in southeast Bafgh, an Arg with 37Km2 area has been made. In order to control wind erosion in the region, first of all, the main source regions needed to be identified. Therefore, for determination of source area, the method of phase by phase source-identification was used in the region. The results showed that the erosive winds blow from south-west and transport sediments towards sand dunes. Geomorphologic and sedimentological studies showed that the source of sand dunes has been close and local and it is located on EPANDAGE PLAIN of south west part of Arg, beds of Zarand Shoor-River and the other eolion erosive facies of this plain. In general, the main source is adjacent regolite plain.

Cites

References

Cite

APA: Copy

AHMADI, HASAN, FEYZNIA, S., EKHTESASI, M.R., & GHANEI BAFGHI, M.J.. (2001). SOURCE IDENTIFICATION OF SOUTH BAFGH SAND DUNES. DESERT (BIABAN), 6(2), 33-49. SID. https://sid.ir/paper/5340/en

Vancouver: Copy

AHMADI HASAN, FEYZNIA S., EKHTESASI M.R., GHANEI BAFGHI M.J.. SOURCE IDENTIFICATION OF SOUTH BAFGH SAND DUNES. DESERT (BIABAN)[Internet]. 2001;6(2):33-49. Available from: https://sid.ir/paper/5340/en

IEEE: Copy

HASAN AHMADI, S. FEYZNIA, M.R. EKHTESASI, and M.J. GHANEI BAFGHI, “SOURCE IDENTIFICATION OF SOUTH BAFGH SAND DUNES,” DESERT (BIABAN), vol. 6, no. 2, pp. 33–49, 2001, [Online]. Available: https://sid.ir/paper/5340/en

Related Journal Papers