刘秀位, 苗文芳, 王艳哲, 孙宏勇, 邵立威, 陈素英, 张喜英. 冬前不同管理措施对土壤温度和冬小麦早期生长的影响[J]. 中国生态农业学报(中英文), 2012, 20(9): 1135-1141. DOI: 10.3724/SP.J.1011.2012.01135
引用本文: 刘秀位, 苗文芳, 王艳哲, 孙宏勇, 邵立威, 陈素英, 张喜英. 冬前不同管理措施对土壤温度和冬小麦早期生长的影响[J]. 中国生态农业学报(中英文), 2012, 20(9): 1135-1141. DOI: 10.3724/SP.J.1011.2012.01135
LIU Xiu-Wei, MIAO Wen-Fang, WANG Yan-Zhe, SUN Hong-Yong, SHAO Li-Wei, CHEN Su-Ying, ZHANG Xi-Ying. Effects of different pre-winter management practices on soiltemperature and winter wheat seedling growth[J]. Chinese Journal of Eco-Agriculture, 2012, 20(9): 1135-1141. DOI: 10.3724/SP.J.1011.2012.01135
Citation: LIU Xiu-Wei, MIAO Wen-Fang, WANG Yan-Zhe, SUN Hong-Yong, SHAO Li-Wei, CHEN Su-Ying, ZHANG Xi-Ying. Effects of different pre-winter management practices on soiltemperature and winter wheat seedling growth[J]. Chinese Journal of Eco-Agriculture, 2012, 20(9): 1135-1141. DOI: 10.3724/SP.J.1011.2012.01135

冬前不同管理措施对土壤温度和冬小麦早期生长的影响

Effects of different pre-winter management practices on soiltemperature and winter wheat seedling growth

  • 摘要: 华北平原冬小麦/夏玉米一年两作下的少免耕和秸秆还田在减少耕作投入和降低农田无效蒸发方面作用显著, 但也存在一些不利影响。本研究通过详细测定镇压、冬灌、秸秆覆盖等措施对土壤温度和冬小麦早期生长的影响, 明确了少免耕和秸秆还田等措施的实施效果, 为农业生产提供指导。结果表明, 秸秆覆盖后土壤表层和5 cm深度最低地温越冬前、越冬期间和返青后比不覆盖分别高2.37 ℃、3.18 ℃、1.68 ℃和0.57 ℃、1.28 ℃、0.34 ℃, 最高温度分别低 2.68 ℃、4.40 ℃、4.82 ℃和0.54 ℃、0.75 ℃、1.85 ℃; 冬灌后至冬小麦返青期表层土壤和5 cm处土壤平均最低温度比不冬灌分别高0.88 ℃和 0.93 ℃, 返青至拔节期两个层次的最高温度相差5.35 ℃和5.57 ℃; 镇压与不镇压温度差异不明显。与对照相比, 越冬前后秸秆覆盖和冬灌后冬小麦的茎蘖数和生物量都较低, 尤其是在返青期, 秸秆覆盖和冬灌下的茎蘖数和生物量比对照分别低29.8%、27.7%和5.2%、21.2%。秸秆覆盖和冬灌在冬季可降低最低温度的降幅, 但春季不利于地温回升, 有延缓冬小麦生长发育的可能。

     

    Abstract: For winter wheat/summer maize double cropping system in the North China Plain (NCP), the practices of straw incorporation into the top soil and minimum tillage have some negative effects on winter wheat growth. This study examined the effects of straw mulching, winter irrigation and soil compaction on soil temperature and winter wheat seedling growth. Results showed that straw mulching reduced both maximum and minimum soil temperature. Compared with CK, straw mulching increased the average daily minimum soil temperature (Tmin) by 2.37 ℃, 3.18 ℃ and 1.68 ℃ at the soil surface and by 0.57 ℃, 1.28 ℃ and 0.34 ℃ at the 5 cm soil layer at pre-wintering, during over-wintering and after winter dormancy, respectively. Straw mulching reduced daily maximum temperature on the average by 2.68 ℃, 4.40 ℃ and 4.82 ℃ at the soil surface and by 0.54 ℃, 0.75 ℃ and 1.85 ℃ at the 5 cm soil depth for the three periods, respectively. Straw mulching reduced soil temperature, which slowed down winter wheat development. Wheat tiller and biomass reduced by 29.8% and 5.2% during recovery. Although straw mulching positively influenced soil water conservation, winter wheat growth was negatively affected. Winter irrigation increased soil moisture, which in turn reduced both the maximum and minimum soil temperature during over-winter and recovery stage of winter wheat. Average daily minimum temperatures were respectively 0.88 ℃ and 0.93 ℃ higher for treatments with winter irrigation than that for treatments without winter irrigation at the soil surface and 5 cm soil layer during over-wintering. For the same treatments, the differences were 5.35 ℃ and 5.57 ℃ during recovery. Wheat tiller number and biomass also reduced by 27.7% and 21.2% during recovery. Good soil moisture after winter irrigation at the recovery stage reduced soil temperature, which negatively affected winter wheat. Soil compaction after winter wheat sowing did not significantly affect soil temperature and winter wheat seedling growth.

     

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