PATTERNS OF FLOW EVOLUTION IN THE CENTRAL AREA OF THE ROMANIAN PLAIN, CASE STUDY: THE CALNISTEA CATCHMENT (ROMANIA)

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.

COCOS A.; COCOS O.; SARBU I.

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

Journal Paper

Paper Information

Journal: CASPIAN JOURNAL OF ENVIRONMENTAL SCIENCES (CJES) Year:2011 | Volume:9 | Issue:1 Page(s): 81-95

Download Full-Text

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

Persian Verion

View:

737

Download:

220

Cites:

Information Journal Paper

Title

PATTERNS OF FLOW EVOLUTION IN THE CENTRAL AREA OF THE ROMANIAN PLAIN, CASE STUDY: THE CALNISTEA CATCHMENT (ROMANIA)

Author(s)

COCOS A. | COCOS O. | SARBU I. | Issue Writer Certificate

Keywords

CALNISTEA CATCHMENTQ3

PRECIPITATIONQ3

STREAMSQ3

FLOWQ3

DISCHARGEQ3

Abstract

This paper seeks to emphasize the FLOW variability in the CALNISTEA CATCHMENT by analyzing the local physiographic factors. The research has shown that the amount of PRECIPITATION that falls to the ground is low, the rocks in the region are soft, but highly permeable, gradients are gentle in most of the territory and vegetal cover is sparse and therefore cannot hold important amounts of water. Under the circumstances, the FLOW is controlled especially by PRECIPITATION, gradient and rock permeability, which largely explains the rather low values of the drainage density, as well as the frequency with which the rivers dry up completely. The moisture deficit of the summer season is compensated to a certain extent by the existence of a chain of ponds along the main STREAMS. The situation could further be improved if local authorities will find the necessary financial means in order to excavate artificial channels to bring water from the neighboring catchments. Although the FLOW values are generally low, under exceptional synoptic conditions the heavy rainfalls can lead to the formation of flash floods that can damage settlements, transportation routes and crops. Consequently, it is necessary to build protection levees in the lowlands and to regulate the stream FLOW.

Cites

No record.

References

THE DYNAMIC FACTORS OF HYDROGEOMORPHIC VULNERABILITY IN THE CENTRAL SECTOR OF THE ROMANIAN PLAIN

Cite

APA: Copy

COCOS, A., COCOS, O., & SARBU, I.. (2011). PATTERNS OF FLOW EVOLUTION IN THE CENTRAL AREA OF THE ROMANIAN PLAIN, CASE STUDY: THE CALNISTEA CATCHMENT (ROMANIA). CASPIAN JOURNAL OF ENVIRONMENTAL SCIENCES (CJES), 9(1), 81-95. SID. https://sid.ir/paper/240736/en

Vancouver: Copy

COCOS A., COCOS O., SARBU I.. PATTERNS OF FLOW EVOLUTION IN THE CENTRAL AREA OF THE ROMANIAN PLAIN, CASE STUDY: THE CALNISTEA CATCHMENT (ROMANIA). CASPIAN JOURNAL OF ENVIRONMENTAL SCIENCES (CJES)[Internet]. 2011;9(1):81-95. Available from: https://sid.ir/paper/240736/en

IEEE: Copy

A. COCOS, O. COCOS, and I. SARBU, “PATTERNS OF FLOW EVOLUTION IN THE CENTRAL AREA OF THE ROMANIAN PLAIN, CASE STUDY: THE CALNISTEA CATCHMENT (ROMANIA),” CASPIAN JOURNAL OF ENVIRONMENTAL SCIENCES (CJES), vol. 9, no. 1, pp. 81–95, 2011, [Online]. Available: https://sid.ir/paper/240736/en

Related Journal Papers