受渍小麦土壤氧含量的变化特征及渍害指标确定

Change characteristics of soil oxygen content of waterlogged wheat and waterlog damage index determination

  • 摘要: 【目的】分析小麦不同受渍时期的土壤氧含量变化特征,构建基于土壤氧含量的小麦受渍指标,为准确及时鉴别小麦受渍程度提供理论基础。【方法】选取小麦耐渍品种扬麦11与不耐渍品种郑麦7698,采用盆栽试验,分别在拔节—开花、开花—成熟2个时期进行渍水试验,设持续渍水0(CK)、5、12和20 d共4个处理,通过测定土壤氧含量和小麦产量,分析不同品种、不同处理冬小麦低氧胁迫受渍持续时长与产量的关系,筛选出以土壤氧含量为特征值的小麦受渍指标。【结果】土壤氧含量随着时间及生育期的推移逐渐降低,其高低起伏与自然降雨密切相关;拔节—开花时期受渍土壤氧含量减少量大于开花—成熟时期。CK的土壤氧含量随着生育期变化,在播种至拔节期以前主要保持在20 mg/L以上;从拔节期至灌浆期降至10 mg/L左右;灌浆期以后在10 mg/L以下。渍水处理阶段,2个生育时期小麦土壤氧含量低于5 mg/L;确定在4月下旬以前,可用土壤氧含量作为小麦受渍指标,受渍土壤氧含量的受渍阈值为5 mg/L。扬麦11和郑麦7698的产量与受渍处理天数均呈极显著负相关(P<0.01),不管品种是否耐渍,渍害持续时间越长,对小麦产量影响越大。生育前期土壤相对水含量对土壤氧含量影响较大,渍水下的土壤相对水含量使土壤氧含量维持在5 mg/L以下,而在生育后期,相对水含量对土壤氧含量影响不明显。分析小麦产量与土壤氧含量低于5 mg/L持续时长的关系,得出基于土壤氧含量的小麦受渍害指标标准,即在拔节—开花时期,扬麦11土壤氧气含量低于5 mg/L分别持续7、17和25 d以上时,郑麦7698分别持续8、18和24 d以上,认定小麦受轻度、中度、重度渍害影响;扬麦11与郑麦7698在开花—成熟时期持续11、18和27 d以上,认定小麦受轻度、中度、重度渍害影响。【结论】以小麦受渍时土壤氧含量的变化特征作为渍害判别标准符合江汉平原小麦种植实际生产现状,确定在4月下旬以前,可用土壤氧含量作为小麦渍害受渍指标,受渍土壤氧含量的阈值为5 mg/L。

     

    Abstract: 【Objective】To analyze the change characteristics of soil oxygen content in different waterlog periods of wheat,and set waterlog damage index wheat based on soil oxygen content,so as to provide a theoretical basis for accurate and timely determining waterlog degree of wheat.【Method】A waterlog experiment was carried out in 2 stages,jointing-flowering period and flowering-maturity period respectively with waterlog-resistant cultivar Yangmai 11 and the waterlog-unresistant cultivar Zhengmai 7698. Four treatments of continuous waterlog for 0(CK),5,12 and 20 d were set to determine soil oxygen content and wheat yield and to analyze the relationship between waterlog duration and yield of different winter wheat varieties under hypoxia stress and different treatments,in order to select waterlogged wheat indexes with soil oxygen content as eigenvalue.【Result】Soil oxygen content gradually decreased as time and growth period went on,and its fluctuation was closely related to natural rainfall;the decrease of oxygen content in waterlogged soil during jointing-flowering period was greater than that during flowering-maturity period;soil oxygen content in CK changed as growth period went on,which was above 20 mg/L before sowing to jointing period,decreased to around 10 mg/L from jointing period to grain filling period,and below 10 mg/L after grain filling period;in waterlog treatments,the soil oxygen content of wheat was lower than 5 mg/L in 2 growth periods,leading to a conclusion that before the end of April,soil oxygen content could be used as waterlog damage index of wheat,and the waterlogging threshold of soil oxygen content was 5 mg/L. The yield of Yangmai 11 and Zhengmai 7698 were extremely significantly negatively correlated with the days of waterlog treatment(P<0.01) and the longer the waterlogging treatment lasted,the greater the impact on the yield of wheat,regardless of whether the variety was waterlog-resistant or not. The soil relative water content greatly influenced oxygen in early growth period,and relative water content in waterlogged soil kept the soil oxygen content below 5 mg/L,yet in the late growth period,effects of relative water content on oxygen was not obvious. The relationship between wheat yield and the duration when soil oxygen was lower than 5 mg/L was analyzed,and the waterlog damage index standard of wheat based on soil oxygen content was set:during the jointing-flowering period,mild,moderate,and severe waterlog damage was determined when soil oxygen content in Yangmai 11 was lower than 5 mg/L for more than 7,17,and 25 d,Zhengmai 7698 for more than 8,18,and 24 d;mild,moderate and severe waterlog damage was determined when lowering-maturity period of Yangmai 11 and Zhengmai 7698 lasted for more than 11,18 and 27 d.【Conclusion】Taking the change characteristics of soil oxygen content when wheat is waterlogged as the waterlog damage identification standard is appropriate in wheat-planting Jianghan Plain. Before the end of April,soil oxygen content can be used as the waterlog damage index of wheat,and the threshold of the oxygen content in waterlogged soil is 5 mg/L.

     

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