Please use this identifier to cite or link to this item: http://hdl.handle.net/11452/24523
Title: Alterations of the nitrogen mineralization rates in soils of forest community depending on the ski run construction (Mount Uludaǧ, Bursa, Turkey)
Authors: Uludağ Üniversitesi/Fen-Edebiyat Fakültesi/Biyoloji Anabilim Dalı.
Uludağ Üniversitesi/Gemlik Asım Kocabıyık Meslek Yüksek Okulu/Bitkisel ve Hayvansal Üretim.
0000-0002-2680-9815
0000-0001-5441-037X
Güleryüz, Gürcan
Kırmızı, Serap
Arslan, Hülya
Yakut, Ece Kondu
A-5538-2019
D-2584-2016
6603334913
6506756812
7006712783
36994816700
Keywords: Environmental sciences & ecology
Sub-alpine
Abies bornmuelleriana forest
Ski run
Disturbance
Nitrogen mineralization
Nitrification
Nutrient Status
Restoration
Quality
Nitrate
Losses
Issue Date: Feb-2011
Publisher: Science Press
Citation: Güleryüz, G. vd. (2011). "Alterations of the nitrogen mineralization rates in soils of forest community depending on the ski run construction (Mount Uludaǧ, Bursa, Turkey)". Journal of Mountain Science, 8(1), 53-61.
Abstract: Since 1940s, Mount Uludag (Bithynian Olympus) has been considered famous with winter sports center in Turkey. In addition, it is one of the rare places because of its plant diversity and is also one of the important plant areas of Turkey. The ski run constructions are rapidly increased in the past decades in the alpine and subalpine belts of the mountain. Rate of nitrogen mineralization and some properties of soil were investigated in the soils of the three ski runs and undisturbed neighborhood forest sites. These ski runs are at the upper part of the forest belt in the mountain. Abies bornmuelleriana forest community is the postclimax and very sensitive to destruction. The rates of the nitrogen mineralization in the soils were determined in controlled conditions (60% water-holding capacity, 20 degrees C). Nitrification and nitrogen mineralization were in the ski run inside where the natural recovery started, increased compared with the outside of the ski runs. Waterholding capacity, organic carbon, and total nitrogen were decreased in the massive damaged ski run, and due to these changes, the rates of mineralization and nitrification were also decreased.
URI: https://link.springer.com/article/10.1007/s11629-011-1127-6
https://doi.org/10.1007/s11629-011-1127-6
http://hdl.handle.net/11452/24523
ISSN: 1672-6316
1993-0321
Appears in Collections:Scopus
Web of Science

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