冬季增温对土壤水分及盐碱化的影响

    Effect of winter warming on soil moisture and salinization

    • 摘要: 为了研究冬季增温对土壤水分及盐碱化的影响,采用红外线辐射器增温法,在宁夏引黄灌区西大滩试验站进行了大田试验。结果表明,冬季增温0.5~2.5℃与未增温比较,土壤层0~20、>20~40、>40~60?cm土壤含水率分别减少0.2%~3.9%、 0.4%~1.4%、0.3%~0.6%;碱化度分别增加1.2%~4.4%、0.1%~0.4%、0.2%~0.6%;总碱度分别增加0.01~0.04、0.01~0.03、0.01~0.02 cmol/kg;pH值分别增加0.1~1.0、0.1~0.5、0.1~0.6;全盐分别增加0.05~0.71、0.02~0.20、0.01~0.11 g/kg。冬季增温加剧了土壤水分蒸发, 增强了土壤盐碱化,导致土壤盐碱化危害加剧。

       

      Abstract: In order to study the effect of winter warming on soil moisture and salinization, the field experiments that increased temperature by an infrared radiator were designed at Xidatan experiment station of Yellow River irrigation areas in the Ningxia Hui Autonomous Region. The results showed that compared with no warming, winter warming by 0.5-2.5℃ reduced the moisture content of 0-20, >20-40 and >40-60 cm soil horizons by 0.2%-3.9%, 0.4%-1.4% and 0.3%-0.6%, respectively; correspondingly alkalization increased by 1.2%-4.4%, 0.1%-0.4% and 0.2%-0.6%; total alkalinity increased by 0.01~0.04, 0.01~0.03 and 0.01-0.02 cmol/kg; pH value increased by 0.1-1.0, 0.1-0.5 and 0.1-0.6; and total salt content increased by 0.05-0.71, 0.02-0.20 and 0.01-0.11 g/kg. Winter warming intensifies soil moisture evaporation and then increases the soil salinization.

       

    /

    返回文章
    返回