This paper presents the results of laboratory experiments and numerical simulations carried out in order to understand the mechanism of sediment-wave formation by turbidity currents. Experimental turbidity currents were generated in a 10-m-long laboratory flume, so as to investigate the topographic
Possibility of simulating geophysical flow phenomena by laboratory experiments
β Scribed by H. Branover; A. Bershadskii; A. Eidelman; M. Nagorny
- Publisher
- Springer
- Year
- 1993
- Tongue
- English
- Weight
- 549 KB
- Volume
- 62
- Category
- Article
- ISSN
- 0006-8314
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
## Abstract Phosphate behaviour in natural estuarine systems can be studied by performing field measurements and by undertaking laboratory simulation experiments. Thus, in this paper we describe the use of a dynamic automated estuarine simulator to characterize the geochemical reactivity of phospha
Experimentally observed hydrodynamic flows generated by chemical waves propagating in thin solution layers of the Belousov-Zhabotinsky (BZ) reaction have been analyzed by computer simulation of a simplified time-independent model of the experimental conditions. The assumption of density differences