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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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233water c<strong>on</strong>tent in <str<strong>on</strong>g>the</str<strong>on</strong>g> surface arablelayer of an oxisol soil (red latosol) when<str<strong>on</strong>g>the</str<strong>on</strong>g> zero tillage system is adopted (7).This practice in <str<strong>on</strong>g>the</str<strong>on</strong>g> soybean-wheatrotati<strong>on</strong> leaves <str<strong>on</strong>g>the</str<strong>on</strong>g> soil surface coveredby <str<strong>on</strong>g>the</str<strong>on</strong>g> crop residues. This cover ormulch reduces water evaporati<strong>on</strong> andstabilizes <str<strong>on</strong>g>the</str<strong>on</strong>g> temperature in <str<strong>on</strong>g>the</str<strong>on</strong>g> arablelayer. By reducing soil disturbancethrough no-tillage. <str<strong>on</strong>g>the</str<strong>on</strong>g> soil structure isimproved. soil compacti<strong>on</strong> is minimizedand roots can penetrate more deeply.resulting in better growth. As ac<strong>on</strong>sequence of more uni<strong>for</strong>m andVigorous growth. <str<strong>on</strong>g>the</str<strong>on</strong>g> wheat crop canbetter tolerate inadequate rainfall. andgrain yields can be increased (Table 3).However. <str<strong>on</strong>g>the</str<strong>on</strong>g>re were negative effects offrost in <str<strong>on</strong>g>the</str<strong>on</strong>g> 1979 seas<strong>on</strong> under notillage;damage was more pr<strong>on</strong>ounceddue to <str<strong>on</strong>g>the</str<strong>on</strong>g> lower temperature caused by<str<strong>on</strong>g>the</str<strong>on</strong>g> mulching effect <strong>on</strong> <str<strong>on</strong>g>the</str<strong>on</strong>g> soil surface.Table 2. Rainfall during <str<strong>on</strong>g>the</str<strong>on</strong>g> various wheat growth stages as related to grain yields undernor<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Parana semitropical c<strong>on</strong>diti<strong>on</strong>s, Brazil, 1968 to 1978Rainfall (mm)AverageGrowth stage 1968 1972 1974 1968-78Sowing-shooting (M arch/ApriI) 93 157 197 60Shooting-heading (May/June) 68 156 313 108Heading-maturity (July/August) 88 415 80 167Total rainfall 249 728 590 875Wheat yields (kg/ha) (899) (245) (1547)Source: Godoy and Bernardes (3)Table 3. Comparis<strong>on</strong> of wheat yields under inadequate and normal rainfallc<strong>on</strong>diti<strong>on</strong>s related to tillage systems, nor<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Parana, Brazil, 1977 to 1980Rainfall/yearWheat yields (kg/ha)according to tillage systemC<strong>on</strong>venti<strong>on</strong>al No-tillageInadequate19771978Normal197919804-year average (1977-1980).,g/ Frost damageSource: Vieira (7)60950718541867120996720361281.,g/17991521

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