FORESTIST
Araştırma Makalesi (Research Article)

E FFE C T IV E N E SS O F C L A SSIC A L D A M S IN T O R R E N T C O N TR O L W O R K S IN W E ST E R N A N A T O L IA : K A Y R A N T O R R EN T

1.

İstanbul University, Faculty of Forestry, Department of Forest Construction and Transportation

2.

Retired Forest Engineer

FORESTIST 2006; 56: -
DOI: 10.17099/jffiu.24183
Read: 864 Downloads: 589 Published: 30 December 2019

L and use in the B üyük M enderes R iver basin of vvestern T urkey has been changed from ancient civilizations until today and erosion in different intensities has been experienced. E specially right bank (as to flow ) stream s of low er B üyük M enderes R iver basin had caused m ajör torrents until 1970s. In K ayran creek vvatershed, w hich w as chosen as a representative of the right bank, torrent control vvorks started in 1948 and vvas com pleted in 2003. A dm inistrative, technical and biological torrent control vvorks vvere im plem ented in the area. In the context of technical vvorks, classical consolidation dam s vvere used for bed stabilization. R esults shovved that no torrent has been experienced since 1984 and 92.6% o f check dam s vvere constructed until that tim e. W hile forest land increm ent vvas occurred only 1.06% in V Ilh and V II11' land capability classes via slope stabilization vvorks, classical check dam s have prevented bed degradation and stabilized the slopes by supporting toes vvith storing sedim ent.

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