作物学报 ›› 2010, Vol. 36 ›› Issue (2): 303-312.doi: 10.3724/SP.J.1006.2010.00303
赵锋1,2,王丹英1,徐春梅1,张卫建2,李凤博1,毛海军3,章秀福1,*
摘要:
地表积水是导致水稻地下部分(根系)缺氧胁迫的主要原因。根际缺氧时,提高水稻根系通气(增加孔隙度)可能会减少营养物质的吸收面积,因此,根系必需在形态和代谢上进行一定的调节,而这种调节又会影响作物生长和根际状况。控制灌水(增加土壤和空气的接触时间)是目前常见的一种根际增氧途径,而化学物质增氧模式还处于试验阶段。为考察不同增氧模式对水稻根际缺氧调控的田间应用效果,本研究分别于2007年和2008年,采用过氧化尿素(T1)、过氧化钙(T2)以及干湿交替灌溉(T3)的根际增氧模式并以长期淹水田块为对照(CK),监测水稻根系及地上部分形态、生理、光合物质积累及产量形成特征。结果表明,与CK比较,处理T1、T2和T3对国稻1号和秀水09的增产幅度2007年分别为3.1%/11.5%、10.2%/14.9%和18.9%/16.4%;2008年分别为11.56%/6.57%、8.48%/9.20%和13.56%/9.39%。使根际增氧的响应大致表现为根系孔隙度下降、齐穗期根体积增大、根系活力提高;前期分蘖数增加较快,有效穗多;叶片叶绿素含量在齐穗后下降较慢,剑叶SOD和POD含量较高,MDA含量较低;齐穗后叶片光合作用对穗部干物质积累贡献大。不同增氧模式对水稻生长的影响虽然存在一定的差异,但对土壤淹水导致的根际缺氧胁迫,均起到一定的缓解作用。
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