THE ROLE OF CHARACTERISTICS OF BED MATERIAL ON BANK EROSION IN KARUN RIVER

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.

TELVARI A.A.R.

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

Journal Paper

Paper Information

Journal: Year:2000 | Volume:13 | Issue:2 (47) Page(s): 52-57

Download Full-Text

Persian Verion

View:

1,326

Download:

Cites:

Information Journal Paper

Title

THE ROLE OF CHARACTERISTICS OF BED MATERIAL ON BANK EROSION IN KARUN RIVER

Author(s)

TELVARI A.A.R. | Issue Writer Certificate

Keywords

RIVER EROSIONQ4

BANK EROSIONQ4

MEANDERINGQ4

BED MATERIALQ4

PHYSICAL AND MECHANICAL CHARACTERISTICS OF SOILQ4

Abstract

Some characteristic of BED MATERIAL in banks of Karun River carried out between two hydrometric gauges. Plastisity index, percentage of saturated soil moisture, effective diameter of particles, homogeneity and non homogeneity of particles distribution and soil salinity were analysed for erodible and relatively non-erodible river banks. These analysis have been done for different river morphology. That means in the meander and straight alignment of river. The results show that the weaknees of shear strength for non choesive particles in lower layer as weel as salinity for chohesive particles are the main factors in fine alluvial BED MATERIAL which are affected by flow. These causes BANK EROSION and developed MEANDERING morphology.

Cites

TRACKING THE TRACES OF KARON RIVER IN QUATERNARY

References

Cite

APA: Copy

TELVARI, A.A.R.. (2000). THE ROLE OF CHARACTERISTICS OF BED MATERIAL ON BANK EROSION IN KARUN RIVER. PAJOUHESH-VA-SAZANDEGI, 13(2 (47)), 52-57. SID. https://sid.ir/paper/19466/en

Vancouver: Copy

TELVARI A.A.R.. THE ROLE OF CHARACTERISTICS OF BED MATERIAL ON BANK EROSION IN KARUN RIVER. PAJOUHESH-VA-SAZANDEGI[Internet]. 2000;13(2 (47)):52-57. Available from: https://sid.ir/paper/19466/en

IEEE: Copy

A.A.R. TELVARI, “THE ROLE OF CHARACTERISTICS OF BED MATERIAL ON BANK EROSION IN KARUN RIVER,” PAJOUHESH-VA-SAZANDEGI, vol. 13, no. 2 (47), pp. 52–57, 2000, [Online]. Available: https://sid.ir/paper/19466/en

Related Journal Papers