首页> 外文期刊>Water Science and Technology >Soil moisture dynamics modeling considering multi-layer root zone
【24h】

Soil moisture dynamics modeling considering multi-layer root zone

机译:考虑多层根区的土壤水分动力学模拟

获取原文
获取原文并翻译 | 示例
           

摘要

The moisture uptake by plant from soil is a key process for plant growth and movement of water in the soil-plant system. A non-linear root water uptake (RWU) model was developed for a multi-layer crop root zone. The model comprised two parts: (1) model formulation and (2) moisture flow prediction. The developed model was tested for its efficiency in predicting moisture depletion in a non-uniform root zone. A field experiment on wheat (Triticum aestivum) was conducted in the sub-temperate sub-humid agro-climate of Solan, Himachal Pradesh, India. Model-predicted soil moisture parameters, i.e., moisture status at various depths, moisture depletion and soil moisture profile in the root zone, are in good agreement with experiment results. The results of simulation emphasize the utility of the RWU model across different agro-climatic regions. The model can be used for sound irrigation management especially in water-scarce humid, temperate, arid and semi-arid regions and can also be integrated with a water transport equation to predict the solute uptake by plant biomass.
机译:植物从土壤中吸收水分是植物生长和土壤-植物系统中水运动的关键过程。针对多层作物根系区域开发了非线性根系吸水(RWU)模型。该模型包括两个部分:(1)模型制定和(2)水分流量预测。测试了开发的模型在预测不均匀根区水分消耗方面的效率。在印度喜马al尔邦Solan的亚温带半湿润农业气候下,进行了小麦(Triticum aestivum)的田间试验。模型预测的土壤水分参数,即不同深度的水分状态,根部区域的水分耗竭和土壤水分剖面,与实验结果非常吻合。模拟结果强调了RWU模型在不同农业气候地区的实用性。该模型可用于合理的灌溉管理,尤其是在缺水稀少的温带,温带,干旱和半干旱地区,还可以与水运移方程集成以预测植物生物量对溶质的吸收。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号