Mots-clés
Action anthropique ; Actuel ; Bassin-versant ; Chronostratigraphie ; Géochimie ; Morava ; Moyen Age ; Plaine d'inondation ; Taux de sédimentation ; Tchèque république ; Utilisation agricole du solAgricultural land use ; Chronostratigraphy ; Czech Republic ; Floodplain ; Geochemistry ; Human impact ; Middle Ages ; Moravia ; Present time ; Sedimentation rate ; WatershedAcción antrópica ; Actual ; Aprovechamiento agrícola del suelo ; Cronoestratigrafía ; Cuenca hidrográfica ; Edad Media ; Geoquímica ; Llanura de inundación ; Moravia ; República Checa ; Tasa de sedimentaciónSurprisingly small increase of the sedimentation rate in the floodplain of Morava River in the Strážnice area, Czech Republic, in the last 1300 years
Auteur(s) et Affiliation(s)
GRYGAR, T.M.
Inst. of Inorganic Chemistry ASCR, ŘEŽ, Tcheque, Republique
NOVÁKOVÁ, T.
Inst. of Inorganic Chemistry ASCR, ŘEŽ, Tcheque, Republique
Charles Univ., Fac of Science, Prague, Tcheque, Republique
Nuclear Physics Inst. ASCR, ŘEŽ, Tcheque, Republique
MIHALJEVIČ, M.
Charles Univ., Fac of Science, Prague, Tcheque, Republique
STRNAD, L.
Charles Univ., Fac of Science, Prague, Tcheque, Republique
SVĚTLÍK, I.
Nuclear Physics Inst. ASCR, ŘEŽ, Tcheque, Republique
KOPTÍKOVÁ, L.
Inst. of Geology ASCR, Prague, Tcheque, Republique
LISÁ, L.
Inst. of Geology ASCR, Prague, Tcheque, Republique
BRÁZDIL, R.
Masaryk Univ., Fac. Science, Dep. Geography, Brno, Tcheque, Republique
MÁČKA, Z.
Masaryk Univ., Fac. Science, Dep. Geography, Brno, Tcheque, Republique
STACHOŇ, Z.
Masaryk Univ., Fac. Science, Dep. Geography, Brno, Tcheque, Republique
Inst. of Botany ASCR, Průhonice, Tcheque, Republique
WRAY, D.S.
Univ. of Greenwich at Medway, Chatham Maritime, Royaume-Uni
Description :
Sediment profiles from the floodplain of Morava River in the Czech Republic have been collected from exposed river banks and cores and investigated using a set of geochemical proxies validated by granulometry and conventional geochemical analysis. The work was conducted to evaluate the increase in sedimentation rate during Medieval and modern time periods. Correlation of sediments along the current channel belt allows identification of 2 most important synchronous changes in the channel structure over the past 1300 years : in the 13th century and at the end of the 16th century. These changes could be related to central European climatic extremes rather than to land cover/land use practises. Surprisingly, the extrapolated aggradation rate is very small although Morava River watershed has been intensively used for agriculture and its land cover has changed in a manner similar to west and central European rivers.
Type de document :
Article de périodique
Source :
Catena (Giessen), issn : 0341-8162, 2011, vol. 86, n°. 3, p. 192-207, nombre de pages : 16, Références bibliographiques : 73 ref.
Date :
2011
Editeur :
Pays édition : Allemagne, Cremlingen-Destedt, Catena
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)