Land-Use References

Year Title (Author, Description) File Download
1995

Relationships Between Stand Age, Stand Structure, and Biodiversity in Aspen Mixedwood Forests in Alberta

J.B. Stelfox (editor)

Resource managers and the environmental community are concerned that intensive clearcut logging of Alberta's aspen-dominated boreal mixedwood forests at 60–70 year rotations may alter the age class structure of the forest landscape and result in a change in forest structure and biota. In response to these concerns, we described forest structure and composition of plant and animal communities in young (20–30 years), mature (50–65 years) and old (120+ years) aspen mixedwood stands of fire origin in Alberta. The information collected in this study will serve as a reference against which structure and biota in harvested forests can be compared.

Contact ALCES for J.B. Stelfox (editor), 1995
1993

Application of a GIS for simulating hydrological responses in developing regions

Stefan W. Kienzle

Present capturing, processing and manipulation of spatial data and information as well as coupling processes between the ARC/INFO GIS and the ACRU HMS (Agricultural Catchment Research Unit) is demonstrated for the Mgeni basin in Natal, South Africa.

Contact ALCES for Stefan W. Kienzle, 1993
1992

Catchment Disturbance and Stream Response: An Overview of Stream Research at Coweeta Hydrologic Laboratory

Webster, Golladay, Benfield, Meyer, Swank, Wallace

People interested in stream pollution frequently make a distinction between point-source and non-point-source pollution. Point-source pollution comes out of a pipe; non-point pollution generally enters streams in run-off from surrounding land. It is our contention that non-point-source pollution is a major contributor to degradation of water quality and ecosystem integrity in rivers; the direct effects are primarily to small streams and are then transmitted downstream to larger rivers. In this chapter we illustrate how a terrestrial disturbance affects small streams and how these streams respond to and recover from the disturbance.

Contact ALCES for Webster, Golladay, Benfield, Meyer, Swank, Wallace , 1992
1990

Sediment Production from Forest Roads with Wheel Ruts

Randy b. Foltz and Edward R. Burroughs, Jr.

Artificial rainfall was applied to two sets of paired plots 30.5 m long by 1.52 m wide, each set on a different soil type. One plot in each set contained a wheel rut while the other did not. Measurements of water and sediment yield on rutted plots showed sediment production declined with cumulative runoff while unrutted plots did not show a significant sediment depletion. This difference was a result of concentrated flow versus sheet flow.

Contact ALCES for Randy b. Foltz and Edward R. Burroughs, Jr., 1990
1984

A Policy for Resource Management of the Eastern Slopes

Alberta Energy and Natural Resources

Management in the Eastern Slopes, past and present, and a framework of provincial natural resource goals.

Contact ALCES for Alberta Energy and Natural Resources, 1984
1982

The Sediment Delivery Problem

D.E. Walling

The linking of on-site rates of erosion and soil loss within a drainage basin to the sediment yield at the basin outlet, and improved knowledge and representation of the associated processes of sediment delivery, represent a major research need within the field of erosion and sedimentation and also an important scale problem in drainage basin studies. This paper reviews the limitations of the sediment delivery ratio concept by considering the problems of temporal and spatial lumping and its blackbox nature. Some recent advances in our understanding of the sediment delivery system and its modelling are described and the lack of empirical investigations is highlighted. The significance of recent concern for the role of sediments in the transport of nutrients and contaminants to sediment delivery studies is introduced, and the need for further work in this field is emphasized.

Contact ALCES for D.E. Walling, 1982
1980

Cumulative Effects of Logging Road Sediment on Salmonid Populations in the Clearwater River Jefferson County Washington

C.J. Cederholm, L.M. Reid, E.O. Salo

The nature of sediment production from logging roads and the effect of the resulting sediment on salmonid spawning success in the Clearwater River drainage have been studied for eight years. The study includes intensive and extensive analyses of field situations, supplemented by several controlled experiments. It was found that significant amounts (15-25 percent) of fine sediments (less than 0.85 mm diameter material) are accumulating in spawning gravels of some heavily roaded tributary basins. This accumulation is highest in basins where the road area exceeds 2.5 percent of the basin area. Tributaries of relatively steep gradient are less likely to accumulate high levels of fines. The survival of salmonid eggs to emergence is inversely correlated with percent fines when the percentage of fines exceeds the natural levels of 10 percent. There is a rapid decrease in survival to emergence for each 1 percent increase in fines over natural levels. The presence of 2.5 km/km2 of gravel-surfaced roads undergoing an average distribution of road uses is found to be responsible for producing sediment at 2.6-4.3 times the natural rate in a drainage basin. Sixty percent of the road-related sediment production is caused by landslides while erosion on road surfaces accounts for an additional 18-26 percent. If fine sediment alone is considered, production from road surfaces and landslides is nearly equal. The tributaries of the Clearwater River may be underseeded for coho salmon due to heavy harvest rates in the commercial and sport fisheries. This underseeded condition becomes significant when the efficiency of the spawning environment in producing recruits is lowered by logging-caused sedimentation.

Contact ALCES for C.J. Cederholm, L.M. Reid, E.O. Salo, 1980
1964

Catalogue of Coal Mines of the Alberta Plains

J. D. Campbell

A comprehensive catalogue is presented of all coal mines that have been registered or opened in the plains regions of Alberta. Included are data on surrounding terrain, geology and composition of the coal, and a location map on a scale of one inch to 12 miles.

Contact ALCES for J. D. Campbell, 1964
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