Publications
These publications showcase the significant science conducted in our Science Centers.
Filter Total Items: 16785
Hydrologic data collected in and around a surface coal mine, Clay and Vigo counties, Indiana, 1977-80
Few data are available for evaluating water-quality and other hydrologic properties in and around surface coal mines, particularly in areas where material having a high potential for acid-production is selectively buried. This report contains hydrologic data collected in an active coal mining area in Clay and Vigo Counties, Indiana, from September 1977 through February 1980. Methods of sampling an
Authors
Linda L. Bobo, Stephen E. Eikenberry
You asked for it! Using a catfish hatching trough for other eggs
No abstract available.
Authors
M. Martin
Tubifex worms identified as essential host for salmonid whirling disease
No abstract available at this time
Authors
K. Wolf
Fish smoking process inactivates whirling disease parasite
No abstract available at this time
Authors
K. Wolf
Use of ozone in a water reuse system for salmonids
A water reuse system is described in which ozone is used in addition to biological filters to remove toxic metabolic wastes from the water. The system functions at a higher rate of efficiency than has been reported for other reuse systems and supports excellent growth of rainbow trout (Salmo gairdneri).
Authors
R.C. Williams, S. G. Hughes, G. L. Rumsey
The immunosuppressive effect of antibiotics
No abstract available at this time.
Authors
W. B. van Muiswinkel, J.L. Grondel, D. P. Anderson
You asked for it! "Plank" method of trapping crawfish
No abstract available.
Authors
M. Martin, B. Rodgers
You asked for it! Crop spraying season in fish producing areas
No abstract available.
Authors
M. Martin
Erosional channels on the shoreface of Nauset Beach, Cape Cod, Massachusetts
Many channels (1 to 3 m relief)_are located offshore of Nauset Beach, Cape Cod, Massachusetts, in water 4 to 18 m deep. The channels are oblique to the shoreline, are spaced approximately 260 m apart, and deepen seaward. The southern flank of each channel is rippled whereas the northern flank and interchannel areas are smooth. The origin of the channels is unknown. They probably formed by erosion
Authors
S. W. Needell, William P. Dillon, H. J. Knebel