The Quality Resources

A significant element characterizing a lasting development in Braila Plain region, but also in any other similar area, would be anenvironment factor that is the water, with an increasing importance when considered against the high dryness background. Generally speaking, boththe consumed water and th...

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Main Author: Anca Gabriela TURTUREANU
Format: Article
Language:English
Published: Danubius University 2005-10-01
Series:Acta Universitatis Danubius: Oeconomica
Subjects:
Online Access:http://journals.univ-danubius.ro/index.php/oeconomica/article/viewFile/17/14
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spelling doaj-af67843ecd8140deb9fca44e8e09f2752020-11-24T23:03:27ZengDanubius UniversityActa Universitatis Danubius: Oeconomica2065-01752005-10-01116276The Quality ResourcesAnca Gabriela TURTUREANUA significant element characterizing a lasting development in Braila Plain region, but also in any other similar area, would be anenvironment factor that is the water, with an increasing importance when considered against the high dryness background. Generally speaking, boththe consumed water and the consumption structure reflect the quality and quantity of water resources and, implicitly, the economic potential of theregion at issue. As for Braila Plain, here there is a paradox to be considered: even if the region is bordered by highly significant rivers (The Danubeand Siret) with huge flows – not to mention here the salty water lakes or underground streams with a more or less drinking water – the need ofdrinking water becomes obvious, mostly in summer and autumn. The climate, morphometric and lithological conditions confer certain peculiaritiesupon the waters resources of the Northern-Eastern Romanian Plain. One can say about the Braila Plain hydrographical network that it is poor and thisis due to the discharge, situated under the value of 1 l/sqkm, but also to the very low relief energy. The allochthonous Rivers: the Danube, Siret,Buzau and Calmatui are affected by the relief climate conditions and also by the size and the geographic position of the hydrographical basins.http://journals.univ-danubius.ro/index.php/oeconomica/article/viewFile/17/14drynessevapo-perspirationmineralizationhydrographical basinclimate conditions
collection DOAJ
language English
format Article
sources DOAJ
author Anca Gabriela TURTUREANU
spellingShingle Anca Gabriela TURTUREANU
The Quality Resources
Acta Universitatis Danubius: Oeconomica
dryness
evapo-perspiration
mineralization
hydrographical basin
climate conditions
author_facet Anca Gabriela TURTUREANU
author_sort Anca Gabriela TURTUREANU
title The Quality Resources
title_short The Quality Resources
title_full The Quality Resources
title_fullStr The Quality Resources
title_full_unstemmed The Quality Resources
title_sort quality resources
publisher Danubius University
series Acta Universitatis Danubius: Oeconomica
issn 2065-0175
publishDate 2005-10-01
description A significant element characterizing a lasting development in Braila Plain region, but also in any other similar area, would be anenvironment factor that is the water, with an increasing importance when considered against the high dryness background. Generally speaking, boththe consumed water and the consumption structure reflect the quality and quantity of water resources and, implicitly, the economic potential of theregion at issue. As for Braila Plain, here there is a paradox to be considered: even if the region is bordered by highly significant rivers (The Danubeand Siret) with huge flows – not to mention here the salty water lakes or underground streams with a more or less drinking water – the need ofdrinking water becomes obvious, mostly in summer and autumn. The climate, morphometric and lithological conditions confer certain peculiaritiesupon the waters resources of the Northern-Eastern Romanian Plain. One can say about the Braila Plain hydrographical network that it is poor and thisis due to the discharge, situated under the value of 1 l/sqkm, but also to the very low relief energy. The allochthonous Rivers: the Danube, Siret,Buzau and Calmatui are affected by the relief climate conditions and also by the size and the geographic position of the hydrographical basins.
topic dryness
evapo-perspiration
mineralization
hydrographical basin
climate conditions
url http://journals.univ-danubius.ro/index.php/oeconomica/article/viewFile/17/14
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