Abstract
Organic debris extracted from wheatfield soils was found to be significantly more infective following 2–3 yr continuous wheat than after the fifth successive crop. Plots with added nitrogen yielded more infective debris than those without. Short periods of contact with decline soil or its suspension, reduced infection of wheat roots by Gaeumannomyces when they were subsequently grown in non-decline soil. Hyphae emerging from previously infected root pieces or culture inocula showed a positive growth response to wheat roots or their exudates. This response was negatively correlated to the distance between root and inoculum. In the presence of decline soil, hyphal response was significantly reduced. This reduction can be related to the decreased infectivity of decline soil and may help to explain take-all decline.
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