高级检索+

农林复合模式蒸散耗水的研究

Study on Evapo-transpiration on Agroforestry

  • 摘要: 应用土壤分层水量平衡模型,对林带与冬小麦的根系吸水量、林带和农田的蒸散耗水量、林带影响农田土壤水分范围与程度进行了研究,结果表明:(1)冬小麦拔节至乳熟期间,林带根系吸水以消耗农田土壤水分为主,主要表现在0.0~1.5H(H为树高)范围内。(2)林带可降低12.3%的农田蒸散量。(3)由于林带的影响,在农田中,0.0~0.5H为土壤水分降低区,0.5~5.0H为土壤水分提高区。总体平均,0~200cm农田土壤贮水量可提高11.2%.

     

    Abstract: This dissertation,applying the model of soil layered water balance of agro-forestry,calculates the water uptake by the roots of wheat and shelterbelt,the evapo-transpiration, and the extent that the effects of shelterbelt exerted on the field soil water,then to study the evapo-transpiration of agroforestry.The results show that:(1) Water uptake byroots of the shelterbelt mostly come from the field at the jointing-filling stage of winter wheat,which is obviously indicated in 0.0H~1.5H.(2)If the field is protected by the shel-terbelt,the average evapo-transpiration is 12.3% lower than that of the open wide field.(3)The field soil water content reduces in 0.0H~0.5H and raises in 0.5H~5.0H because of the shelterbelt effect.In general,the soil water capacity at the field soil depth of 0~200 cmcan be raised by 11.2%.

     

/

返回文章
返回