scholarly journals MACROINVERTEBRATE STREAM DRIFT – AN AUSTRALIAN EXAMPLE

2007 ◽  
Vol 6 (1) ◽  
pp. 49-55
Author(s):  
D.P. THORNTON
Keyword(s):  
2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Ádám Pereszlényi ◽  
Dénes Száz ◽  
Imre M. Jánosi ◽  
Gábor Horváth

AbstractThere is a long-lasting debate about the possible functions of zebra stripes. According to one hypothesis, periodical convective air eddies form over sunlit zebra stripes which cool the body. However, the formation of such eddies has not been experimentally studied. Using schlieren imaging in the laboratory, we found: downwelling air streams do not form above the white stripes of light-heated smooth or hairy striped surfaces. The influence of stripes on the air stream formation (facilitating upwelling streams and hindering horizontal stream drift) is negligible higher than 1–2 cm above the surface. In calm weather, upwelling air streams might form above sunlit zebra stripes, however they are blown off by the weakest wind, or even by the slowest movement of the zebra. These results forcefully contradict the thermoregulation hypothesis involving air eddies.


Nature ◽  
1910 ◽  
Vol 84 (2124) ◽  
pp. 44-44
Author(s):  
H. BASSETT

1985 ◽  
Vol 42 (5) ◽  
pp. 909-918 ◽  
Author(s):  
P. A. Larkin ◽  
D. W. McKone

The model of McLay (J. Fish. Res. Board Can. 27: 359–370) for describing the drift of stream organisms was tested in a variety of field experiments in which organisms were disturbed from the substrate and/or the natural drift was blocked. In each situation, appropriate corrections may be made for the catch of drift organisms by the sampling nets. Disturbed animals drifted at a rate much less than stream velocity. The logarithm of the distance travelled was a linear function of the logarithm of mean stream velocity and conformed to the McLay model. Similarly, the model adequately described experiments in which two disturbances were done simultaneously, when drift was blocked for a 2-h period, and when there was both disturbance and blockage. A more comprehensive version of the model was only partially successful in describing the drift at various distances downstream of a blockage sustained for 4 d, probably because of upstream migration of organisms through the substrate, spatial differences in the densities of animals in the substrate, or a reduction in drift rate at lower density in the substrate.


1944 ◽  
Vol 14 (3) ◽  
pp. 333-357 ◽  
Author(s):  
Jack S. Dendy
Keyword(s):  

1971 ◽  
Vol 49 (2) ◽  
pp. 167-173 ◽  
Author(s):  
S. Frost ◽  
A. Huni ◽  
W. E. Kershaw

A square-framed, conical net (300-μ pores) was used in the kicking technique described herein for sampling the larger invertebrates of stony streams. Small samples have consistent percentage population components differing significantly from large ones. Even when bottom-dwellers are numerous, less than 20% of those present are collected (including less than 5.4% of the truly lithophilic species).Almost 60% of the fauna collected from any one site is taken at the first kick. Three kicks yield almost 90% of the organisms secured by 10. Some organisms bypass the net or swim from or through it, and if the net is maintained in position for any length of time, stream-drift animals will mask the sample.


1980 ◽  
Vol 58 (2) ◽  
pp. 232-246 ◽  
Author(s):  
D. R. Moorcroft

Radio-auroral Doppler measurements obtained with the 398-MHz Homer phased-array radar were compared with simultaneous and coincident measurements of electron density and electric field made by the Chatanika incoherent scatter radar. The results for this post-midnight period of observation are not consistent with a direct relationship between the radio-auroral Doppler velocity and the line of sight component of the electron drift velocity, in contrast to the previous observations at VHF. Instead, the observations are consistent with the hypothesis that the echoes arise from the two-stream/drift-gradient irregularities traveling at their threshold phase velocities, close to the local acoustic velocity, Cs. Some of the Doppler velocities observed are considerably less than Cs, and may indicate propagation away from perpendicular to the magnetic field, possibly resulting from magnetic field line distortion.


1977 ◽  
Vol 28 (6) ◽  
pp. 793 ◽  
Author(s):  
PJ Suter ◽  
WD Williams

Stream drift was recorded in the Acheron River, Victoria, on 23 October 1976. A total solar eclipse occurred at 1640-1643 h (Eastern Standard Time). No noticeable effect on the number or types of animals drifting was observed.


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