bistriȚa river channel changes in the subcarpathian sector, in the last two centuries
Clicks: 110
ID: 176809
2013
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Steady Performance
30.0
/100
110 views
10 readers
AI Quality Assessment
Not analyzed
Readership in this journal
SteadyRanked #35 of 39 articles by views in progress in nuclear energy
Most read
Least read
Bar heights use a square-root scale.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
Over time, the hydrographic network corresponding to Bistrița basin has undergone numerous changes, mostly human induced, materialized through the hydrotechnical works made in order to create accumulation lakes (especially after 1960, to encrease electricity production), regularization, damming and embankment, land reclamation or achievement of adduction related to public water supply, and also for built-up area or transport routes network expansion. These actions have led to significant changes regarding the hydrographic network morphometry, by reducing the length of the river, degreasing slopes or sinuosity index. The succesion of changes was analyzed by using the following cartographic documents: Austrian maps published by von Otzellowitz (1788-1790), topographic maps (1:50.000 scale) published in 1894, military maps (1:20.000 scale) edited in 1917-1920, topographic plans (1:5.000 scale), 1975-1976 edition, cadastral plans printed in 1986 (1:10.000 scale) and 2005-2006 ortophotomaps at 1:5.000 scale. Overlapping these maps using GIS techniques highlighted the significant reduction of unplaite and sinuosity index. Also, following the deviation of the natural course of Bistrița river through the creation of a 30 kilometers drainage channel were brought important changes to the river channel morphometry, to the position and river confluences angles, and to the whole hydrographic network of the subcarpathian sector of this river.
| Reference Key |
chelaru2013aerulbistria
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | ;D-.A. CHELARU;I. MINEA |
| Journal | progress in nuclear energy |
| Year | 2013 |
| DOI |
DOI not found
|
| URL | |
| Keywords |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.