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the Symposium on Wheats for More Tropical Environments - cimmyt

the Symposium on Wheats for More Tropical Environments - cimmyt

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216sites. but field work at CIANO (15) andelsewhere suggests <str<strong>on</strong>g>the</str<strong>on</strong>g> followingrelati<strong>on</strong>ship, as shown <strong>for</strong>representative cultivars (Figure 3):Grain weight (mg) = 64-1.6 x T(Equati<strong>on</strong> 2)Here T is <str<strong>on</strong>g>the</str<strong>on</strong>g> mean temperature duringgrain filling (30 to 40 days followingan<str<strong>on</strong>g>the</str<strong>on</strong>g>sis).Equati<strong>on</strong>s 1 and 2 can be multiplied togive <str<strong>on</strong>g>the</str<strong>on</strong>g> a<strong>for</strong>ementi<strong>on</strong>ed simple index ofgrain yield:Yield (g/m2) = corrected Q x(700-17 x T) (Equati<strong>on</strong> 3)This equati<strong>on</strong> c<strong>on</strong>tains <str<strong>on</strong>g>the</str<strong>on</strong>g> two majornegative influences of increasedtemperature <strong>on</strong> grain yield. namely thatof temperature <strong>on</strong> durati<strong>on</strong> of <str<strong>on</strong>g>the</str<strong>on</strong>g> spikegrowth period and <strong>on</strong> grain weight.Increased radiati<strong>on</strong>, through Q. has apositive effect <strong>on</strong> yield.It is possible to use Equati<strong>on</strong> 3 toestimate grain yield as a functi<strong>on</strong> ofan<str<strong>on</strong>g>the</str<strong>on</strong>g>sis date <strong>for</strong> <str<strong>on</strong>g>the</str<strong>on</strong>g> locati<strong>on</strong>s inFigure 1 (Table 3). Q was calculated <strong>for</strong><str<strong>on</strong>g>the</str<strong>on</strong>g> m<strong>on</strong>th prior to an<str<strong>on</strong>g>the</str<strong>on</strong>g>sis. assumingfull light intercepti<strong>on</strong>, and T <strong>for</strong> <str<strong>on</strong>g>the</str<strong>on</strong>g>m<strong>on</strong>th after. Q tends to peak inFebruary (August in <str<strong>on</strong>g>the</str<strong>on</strong>g> sou<str<strong>on</strong>g>the</str<strong>on</strong>g>rnhemisphere). but <str<strong>on</strong>g>the</str<strong>on</strong>g> steepness withwhich T rises be<strong>for</strong>e and. especially.after January also influences an<str<strong>on</strong>g>the</str<strong>on</strong>g>sisdate <strong>for</strong> maximum yield (Figure 5). Thisis seen to be January at all tropicallocati<strong>on</strong>s except Los Banos. Philippines.where temperature changes less40......t::'c./)....Il)~l::~ ....d3020DOPoza Rica...TlaltizapanDEI Batan"'Toluca0o... ...... ...... ....... ...... ... .............ooo16 18 20 22Mean filling temperature (0C)24 26Figure 3. The relati<strong>on</strong>ship of individual grain dr.y weight to mean grainfiningtemperature <strong>for</strong> <str<strong>on</strong>g>the</str<strong>on</strong>g> sowings of Figure 2, and <str<strong>on</strong>g>the</str<strong>on</strong>g> linear relati<strong>on</strong>shipderived from disease-free sowings at CIANO, Ciudad Obreg<strong>on</strong>, Mexico.Source: R.A. Fischer, unpublished

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