Kendig S R, Rupe J C, Scott H D
Former Graduate Student.
Associate Professor, Department of Plant Pathology.
Plant Dis. 2000 Aug;84(8):895-900. doi: 10.1094/PDIS.2000.84.8.895.
The effects of irrigation and soil water stress on Macrophomina phaseolina microsclerotial (MS) densities in the soil and roots of soybean were studied in 1988, 1989, and 1990. Soybean cvs. Davis and Lloyd received irrigation until flowering (TAR2), after flowering (IAR2), full season (FSI), or not at all (NI). Soil water matric potentials at 15- and 30-cm depths were recorded throughout the growing season and used to schedule irrigation. Soil MS densities were determined at the beginning of each season. Root MS densities were determined periodically throughout the growing season. Microsclerotia were present in the roots of irrigated as well as nonirrigated soybean within 6 weeks after planting. By vegetative growth stage V, these densities reached relatively stable levels in the NI and FSI treatments (2.23 to 2.35 and 1.35 to 1.63 log [microsclerotia per gram of dry root], respectively) through reproductive growth stage R. After R, irrigation was discontinued and root densities of microsclerotia increased in all treatments. Initiation (IAR2) or termination (TAR2) of irrigation at R resulted in significant changes in root MS densities, with densities reaching levels intermediate between those of FSI and NI treatments. Year to year differences in root colonization reflected differences in soil moisture due to rainfall. The rate of root colonization in response to soil moisture stress decreased with plant age. Root colonization was significantly greater in Davis than Lloyd at R and R. This was reflected in a trend toward higher soil densities of M. phaseolina at planting in plots planted with Davis than in plots planted with Lloyd. Although no charcoal rot symptoms in the plant were observed in this study, these results indicated that water management can limit, but not prevent, colonization of soybean by M. phaseolina, that cultivars differ in colonization, and that these differences may affect soil densities of the fungus.
1988年、1989年和1990年研究了灌溉和土壤水分胁迫对大豆土壤及根系中菜豆壳球孢菌微菌核(MS)密度的影响。大豆品种Davis和Lloyd分别接受了直至开花期的灌溉(TAR2)、开花后灌溉(IAR2)、全生育期灌溉(FSI)或不灌溉(NI)。在整个生长季节记录15厘米和30厘米深度处的土壤水基质势,并用于安排灌溉。在每个季节开始时测定土壤MS密度。在整个生长季节定期测定根系MS密度。种植后6周内,灌溉和未灌溉大豆的根系中均存在微菌核。到营养生长阶段V时,在NI和FSI处理中(分别为每克干根2.23至2.35和1.35至1.63对数[微菌核数]),这些密度在生殖生长阶段R之前达到相对稳定的水平。R期之后,停止灌溉,所有处理中微菌核的根系密度均增加。在R期开始(IAR2)或终止(TAR2)灌溉导致根系MS密度发生显著变化,密度达到FSI和NI处理之间的中间水平。每年根系定殖的差异反映了降雨导致的土壤湿度差异。根系定殖速率对土壤水分胁迫的响应随植株年龄的增加而降低。在R期和R期,Davis的根系定殖显著高于Lloyd。这反映在种植Davis的地块比种植Lloyd的地块在种植时菜豆壳球孢菌的土壤密度有更高的趋势。尽管在本研究中未观察到植株出现炭腐病症状,但这些结果表明,水分管理可以限制但不能阻止菜豆壳球孢菌对大豆的定殖,不同品种在定殖方面存在差异,且这些差异可能影响该真菌的土壤密度。