Klímaváltozás - aridifikáció - változó tájak = Climate change - aridification - changing landscape

The effects of globalisation are becoming more and more obvious not only in the world economy but also in the natural processes. In the international scientific world the effects of global warming can be observed the most in aridification process but many scientists presume connection with the incre...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerző: Rakonczai János
Dokumentumtípus: Könyv része
Megjelent: 2006
Sorozat:Táj, környezet és társadalom : ünnepi tanulmányok Keveiné Bárány Ilona professzor asszony tiszteletére = Landscape, environment ans society : studies in honour of professor Ilona Bárány-Kevei on the occasion of her birthday
Kulcsszavak:Éghajlati változás, Éghajlatváltozás
Online Access:http://acta.bibl.u-szeged.hu/62431
LEADER 02226naa a2200193 i 4500
001 acta62431
005 20200715130742.0
008 191120s2006 hu o 0|| zxx d
020 |a 963 482 782 9 
040 |a SZTE Egyetemi Kiadványok Repozitórium  |b hun 
041 |a zxx 
100 1 |a Rakonczai János 
245 1 0 |a Klímaváltozás - aridifikáció - változó tájak = Climate change - aridification - changing landscape  |h [elektronikus dokumentum] /  |c  Rakonczai János 
260 |c 2006 
300 |a 593-601 
490 0 |a Táj, környezet és társadalom : ünnepi tanulmányok Keveiné Bárány Ilona professzor asszony tiszteletére = Landscape, environment ans society : studies in honour of professor Ilona Bárány-Kevei on the occasion of her birthday 
520 3 |a The effects of globalisation are becoming more and more obvious not only in the world economy but also in the natural processes. In the international scientific world the effects of global warming can be observed the most in aridification process but many scientists presume connection with the increasingly unpredictable flood events, too. Few think, however, that the changed climate of the several decades – through the change of water cycle – can be resulted in the transformation of the natural landscape. The most important long term effect is the decrease of ground water. The decrease of ground water, however, influences processes through many interactions. On the one hand deeper ground water level causes that vegetation can hardly reach and utilise it which results in a decrease in biomass and in case of more significant transformation vegetation change can occur. On the other hand the change of ground water modifies the vertical movement of water and salt in soils, which results in the genetic transformation of soils. In the consequences of aridification processes may start or in case of arid soils they may generate a process that decreases salt. In both cases the change in the quality of the soil accompanies with the transformation of the natural vegetation. 
695 |a Éghajlati változás, Éghajlatváltozás 
856 4 0 |u http://acta.bibl.u-szeged.hu/62431/1/keveine_baranyi_ilona_unnepi_kotet_593-601.pdf  |z Dokumentum-elérés