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冷浸田地下水位与农田小气候生境特征研究*

Study on Ground Water Level and Microclimatic Characteristics of Cold-waterlogged Paddy Field

  • 摘要: 以福建闽侯典型冷浸田为例,通过连续两年定位监测比较的方法,研究了同一小流域冷浸田与非冷浸田(灰泥田)地下水位与农田小气候生境特征及其差异。结果表明,灰泥田地下水位常年波动较大,且主要发生在地表之下0-50cm,而相应的冷浸田地下水位波动较小,主要分布在地表之上10-40cm,较灰泥田常年平均高出49.3cm。冷浸田地下水还原性物质总量是灰泥田的2.8倍,Fe2+则是灰泥田的1.8倍。冷浸田光合有效辐射年均值较灰泥田降低26.9%,达显著差异水平。冷浸田单季稻生育期(6-10月)平均地表温度、5cm地温、10cm地温、15cm地温分别比灰泥田低0.4℃、0.4℃、0.5℃、0.6℃,尤其是9-10月的抽穗灌浆期地温与灰泥田差异进一步加大;其单季稻生育期平均气温均也较灰泥田低0.6℃。山垄冷浸田地下水位高并伴随强还原性、较低的光合有效辐射与水稻生育后期地温下降较快是区别于非冷浸田的重要生境特征,这可能是冷浸田生产力低下的综合原因。基于冷浸田生境特征,从工程与农艺措施等方面提出治理利用对策。

     

    Abstract: In this paper, taking typical cold-waterlogged paddy field in Minhou County, Fujian Province as an example, 2-year continuous monitoring and contrast were carried out to study the ground water level and microclimatic characteristics between cold-waterlogged paddy field and not cold-waterlogged paddy field (grey clayey field) at same drainage basin as well as their differences. The results show that ground water levels which take place in 0-50cm range below the ground vary from wide range for grey clayey field, but for cold-waterlogged paddy field, ground water levels which take place in 10-40cm range up the ground and yearly higher by 49.3cm than that of grey clayey field vary gently. The total reducing substances of cold-waterlogged paddy field is 2.8 times as many as that of grey clayey field, and the content of ferrous ion is 1.8 times as well. Compared with the grey clayey field, the yearly photosynthetically active radiation(PAR) of cold-waterlogged field is reduced by 26.9%, with showed significantly difference. In comparison to grey clayey field, the surface temperature, 5cm, 10cm and 15cm geotherm of cold-waterlogged paddy field are lower by 0.4℃, 0.4℃, 0.5℃ and 0.6℃ during single cropping rice growth period (from June to October), respectively, and the differences between the two type of soil become more obvious in September and October at heading and filling stage, especially. In addition, the average air temperature of cold-waterlogged paddy field is also lower by 0.6℃ than that of grey clayey field. The possible integrated reasons why the cold-waterlogged field become low productivity are including higher ground water level with strong reducing substances, lower PAR and geotherm decreased quickly at late growth of rice stage compared with Not cold-waterlogged paddy field. Above are important microclimatic characteristics for cold-waterlogged paddy field. Based on microclimatic characteristics, some countermeasure were offered including engineer and agricultural aspect for cold-waterlogged paddy field.

     

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