ABSTRACT:
The use of high-sand-content turfgrass putting greens in the last two decades has been associated with the increase in prevalence of microbiologically generated black plug layering. A transect horizontal section analysis of a die-back zone in a green at the Tor Hill Golf Course of the City of Regina, Saskatchewan, revealed a complex structural entity forming this layering. It was comprised of columnar processes, lateral plates, and globular masses. Much of the biomass occurred within a zone 4 to 16 mm (0.16–0.63 inch) below the surface, and a large surface area to volume ratio was evident from the convoluted nature of the surface of the black plug layer. Where grass roots penetrated through the layer, there was usually more than 3 mm (0.12 inch) of uninfested sand around the root.
Footnotes
D. R. Cullimore is director and professor of microbiology and S. Nilson is a Ph. D. candidate, Regina water Research Institute, University of Regina, Regina, Saskatchewan, S4S OA2. S. Taylor is a research technician with Droycon Bioconcepts Inc., Regina, Saskatchewan, S4V OP8. K. Nelson is a superintendent with the Parks Department, Regina, Saskatchewan, S4P 3C8, Financial support for this project was received from the City of Regina, the National Research Council of Canada IRAP program, and the Natural Sciences & Engineering Research Council of Canada (research grant-DRC). The authors thank Harold Berwald for technical assistance and Natalie Ostryzniuk for manuscript preparation.
- Copyright 1990 by the Soil and Water Conservation Society
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