Geochemical analysis of suspension load of White Körös
Few studies are available concerning the Hungarian river load. Previously mainly qualitative measurements were performed and as well as is being performed more recently. In the literature chemical analysis of flapping river load is not common (BALLÓ M. L873: TAKÁTS T- L930: MEZŐSI J-DONÁTH É. 1951:...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
Szegedi Egyetem Ásványtani, Geokémiai és Kőzettani Tanszéke
Szeged
2000
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| Sorozat: | Acta mineralogica-petrographica
41 |
| Kulcsszavak: | Geokémia, Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24895 |
| Tartalmi kivonat: | Few studies are available concerning the Hungarian river load. Previously mainly qualitative measurements were performed and as well as is being performed more recently. In the literature chemical analysis of flapping river load is not common (BALLÓ M. L873: TAKÁTS T- L930: MEZŐSI J-DONÁTH É. 1951: BOGÁRDI J.). More papers are available regarding the characteristics of catchment areas of rivers Berettyó and Körös. Workers of Hydrology Institution are continuously measuring the hydrographic measurement. The complex mineralogical and geochemical analysis of suspension load of the rivers have been never done. During our study we are addressing the following questions: The quality and quantity of the suspension load of the river When and why does the river deliver the largest amount of load? What is the flapping particles roundness? Which part of the catchment area are these particles coming from? What difference can be found between the particles in the river and the mineral composite of the catchment area? To answer these questions we analyze the suspension load. |
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| Terjedelem/Fizikai jellemzők: | 119-128 |
| ISSN: | 0365-8066 |