Soil Erosion In Upper Crasna Basin.

The assement of soil erosion in the Upper Crasna Basin was made by means of the ROMSEM model based on the universal relation used by the Soil Conservation Service in USA, taking into consideration the climatic conditions in Romania. It uses specific coefficients such as rain erosivity, soil erodabil...

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Main Author: OANA MOIGRĂDEAN
Format: Article
Language:English
Published: Casa Cartii de Stiinta Cluj-Napoca 2018-05-01
Series:Riscuri şi Catastrofe
Subjects:
Online Access: http://riscurisicatastrofe.reviste.ubbcluj.ro/Volume/XVII_Nr_22_1_2018/PDF/4_Moigradean_41_49.pdf
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author OANA MOIGRĂDEAN
author_facet OANA MOIGRĂDEAN
author_sort OANA MOIGRĂDEAN
collection DOAJ
description The assement of soil erosion in the Upper Crasna Basin was made by means of the ROMSEM model based on the universal relation used by the Soil Conservation Service in USA, taking into consideration the climatic conditions in Romania. It uses specific coefficients such as rain erosivity, soil erodability, the correction coefficient for the effect of cultures, the correction coefficient for the effect of anti-erosional works, the topographic factor. The values of the annual erosion were between 0 and 23,18 t/ha/year. There were defined six value classes, with different shares within the basin. Over half of the surface of the basin (63,31 %) is represented by terrains with very low erosion (between 0 – 0,05 t/ha/year). Only 0.24 % of the surface (1.9 km) represents surfaces with erosion of over 6 t/ha/year meaning that the problems are punctual and the solutions need to be found at a local level.
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spelling doaj.art-33d6d509140649c494bd39a73931e77d2022-12-22T02:11:12ZengCasa Cartii de Stiinta Cluj-NapocaRiscuri şi Catastrofe1584-52732069-76942018-05-01221/2018414910.24193/RCJ2018_4RCJ2018_4Soil Erosion In Upper Crasna Basin.OANA MOIGRĂDEAN0 Babes-Bolyai University The assement of soil erosion in the Upper Crasna Basin was made by means of the ROMSEM model based on the universal relation used by the Soil Conservation Service in USA, taking into consideration the climatic conditions in Romania. It uses specific coefficients such as rain erosivity, soil erodability, the correction coefficient for the effect of cultures, the correction coefficient for the effect of anti-erosional works, the topographic factor. The values of the annual erosion were between 0 and 23,18 t/ha/year. There were defined six value classes, with different shares within the basin. Over half of the surface of the basin (63,31 %) is represented by terrains with very low erosion (between 0 – 0,05 t/ha/year). Only 0.24 % of the surface (1.9 km) represents surfaces with erosion of over 6 t/ha/year meaning that the problems are punctual and the solutions need to be found at a local level. http://riscurisicatastrofe.reviste.ubbcluj.ro/Volume/XVII_Nr_22_1_2018/PDF/4_Moigradean_41_49.pdf soil erosionUSLErain erosivitysoil erodability
spellingShingle OANA MOIGRĂDEAN
Soil Erosion In Upper Crasna Basin.
Riscuri şi Catastrofe
soil erosion
USLE
rain erosivity
soil erodability
title Soil Erosion In Upper Crasna Basin.
title_full Soil Erosion In Upper Crasna Basin.
title_fullStr Soil Erosion In Upper Crasna Basin.
title_full_unstemmed Soil Erosion In Upper Crasna Basin.
title_short Soil Erosion In Upper Crasna Basin.
title_sort soil erosion in upper crasna basin
topic soil erosion
USLE
rain erosivity
soil erodability
url http://riscurisicatastrofe.reviste.ubbcluj.ro/Volume/XVII_Nr_22_1_2018/PDF/4_Moigradean_41_49.pdf
work_keys_str_mv AT oanamoigradean soilerosioninuppercrasnabasin