气候变暖对宁夏引黄灌区土壤盐分及其灌水量的影响

    Impact of climatic warming on soil salinity and irrigation amount of Yellow River irrigation areas in Ningxia Hui Autonomous Region

    • 摘要: 气候变暖加剧了土壤水分蒸发,带动土壤盐分向上移动,引起土壤盐分增加,导致土壤盐碱危害加剧。采用近35 a来的土壤盐分定位观测资料和气象资料,研究气候变暖对宁夏引黄灌区土壤盐分变化的影响。研究结果表明:近 35 a随着全球变暖,宁夏引黄灌区土壤全盐含量呈明显的增加趋势,轻盐化土壤、中盐化土壤和重盐化土壤全盐质量分数分别增加0.08、0.13和0.19 g/kg;当温度增加0.5~3.0℃时,宁夏引黄灌区轻盐化土壤、中盐化土壤和重盐化土壤淋洗土壤增加盐分所需的灌水量分别增加8.2%~9.1%、8.2%~8.7%和8.3%~8.8%,总灌水量增加1.29~1.40亿m3。

       

      Abstract: Climatic warming has intensified soil moisture evaporation and led the soil salinity moving upward, which results in salinity increase and aggravated the harm of saline and alkaline of the soil. This paper has, on the basis of location observational data of soil salinity and meteorological data in the recent 35 years, researched the influence of climatic warming on soil salinity change of Yellow River irrigation areas in Ningxia Hui Autonomous Region. The result shows that the total soil salt content has been an increasing trend because of global climatic warming in the recent 35 years, and total salt content of light, moderate and severe salty soil has increased by 0.08 g/kg, 0.13 g/kg and 0.19 g/kg, respectively, in Yellow River irrigation areas in Ningxia Hui Autonomous Region. When the temperature increased by 0.5-3.0℃, the irrigation amount of light, moderate and severe salty soil has increased by 8.2%-9.1%, 8.2%-8.7% and 8.3-8.8%, respectively, and the total irrigation amount has been increased by 129-140 million m3.

       

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