Premium
Influence of Water Exchange and Dissolved Oxygen in Redds on Survival of Steelhead Trout Embryos
Author(s) -
Coble Daniel W.
Publication year - 1961
Publication title -
transactions of the american fisheries society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.696
H-Index - 86
eISSN - 1548-8659
pISSN - 0002-8487
DOI - 10.1577/1548-8659(1961)90[469:iowead]2.0.co;2
Subject(s) - hatching , trout , hydrology (agriculture) , environmental science , fishery , salmo , streams , zoology , geology , biology , fish <actinopterygii> , geotechnical engineering , computer network , computer science
A field study of spawning gravel conditions affecting the survival of steelhead trout (Salmo gairdneri Richardson) embryos was conducted in two small streams in the Alsea River Basin in Lincoln County, Oregon, from February to June 1959. Holes 10 inches deep, approximating natural redds, were dug in arbitrarily selected spawning locations. Plastic mesh sacks containing gravel and 100 fertilized trout eggs were placed in the upstream end of each hole. A stand‐pipe was placed in the lower end of each excavation about 10 inches away from the eggs, and the hole was filled with gravel to the streambed level. Periodically, determinations were made of gravel permeability and of the apparent velocity and dissolved‐oxygen content of the intra‐gravel water. A month after calculated hatching times, the bags were removed from the stream‐bed, and the fry contained in them were counted and preserved. The permeability of the spawning gravel fluctuated while embryos were in the gravel. During this period mean gravel permeabilities ranged from 80 to 400 meters per hour; apparent velocities from 5 to almost 110 centimeters per hour; and dissolved‐oxygen concentrations from 2.6 to 9.25 milligrams per liter. Embryonic survival percentages ranged from 16 to 62. There was positive correlation between the apparent velocity of ground water and embryonic survivals, and between the dissolved‐oxygen levels of the gravel water and survivals. Apparent velocities and dissolved‐oxygen concentrations were closely related in the intra‐gravel water, and effects of these factors could not be separated.