
TY  - JOUR
A1  - Morgan, J. M. 
T1  - Increases in grain yield of wheat by breeding for an osmoregulation gene: relationship to water supply and evaporative demand
JF  - Australian Journal of Agricultural Research
JO  - Aust. J.  Agric. Res.
Y1  - 2000
VL  - 51
IS  - 8
SP  - 971
EP  - 978
KW  - drought tolerance, osmotic adjustment, pollen selection.
UR  - https://doi.org/10.1071/AR00062 
N2  - The effect of water stress on yield increases produced by breeding for an osmoregulation gene (or) was examined using both backcross-bred lines (produced using allele identification in pollen grains) and inbred lines (produced using leaf tests). Yields were measured in 39 field experiments spanning 8 seasons. These included experiments where water was supplied through drip irrigators and rain excluded with a mobile shelter. Several approaches to the measurement of stress environment were examined. The commonly used site mean yield, although most accessible and so utilising the most data, was least effective in explaining variation in yield response. Comparatively high efficiency (84%) could be achieved using measurements of rainfall or evaporative demand for specific periods of crop ontogeny, but this suffered the limitation of being season or treatment specific. The results did, however, demonstrate the value of the pollen selection method in increasing yield under conditions of reduced water supply. In keeping with past climatic analyses, and with the theory underlying variations in leaf water potential to which osmoregulation responds, an index incorporating water supply and evaporative demand accounted well for the yield increase (85%) over the wide range of seasons and treatments examined. It requires inputs of available soil water at sowing, rainfall, and free-water evaporation during the growing period, together with sowing and anthesis dates. The index was used to assess potential yield responses in the various climates covered by the Australian wheatbelt. Greatest potential lay at the drier, inland, margins especially where soils are lighter and water-holding capacities lower. 
ER  -

