首页> 外文期刊>Agriculture and Biology Journal of North America >Estimation of root-zone salinity using SaltMod in the irrigated area of Kalaat El Andalous (Tunisia)
【24h】

Estimation of root-zone salinity using SaltMod in the irrigated area of Kalaat El Andalous (Tunisia)

机译:在卡拉德安达卢斯(突尼斯)灌溉区,使用SaltMod估算根区盐度

获取原文
           

摘要

The objective of this study was to predict the root zone salinity in the irrigated area of Kalaat El Andalous using the SaltMod simulation model over 10 years. En general, the model predicts more or less similar values of electrical conductivity in the root zone. Highest electrical conductivity values equal to 7.7 dS m-1 would be reached during the irrigation season. Following the rains fall particularly during the winter season there would be a decrease of the soil salinity when the average minimum value of electrical conductivity would reach 3.1 dS m-1. This seasonal variation of root zone salinity was confirmed from the measured values. Investigations were made also to study the impact of varying drain spacing and drain depth on root zone salinity and water table depth and drain discharge. The simulation show that the decrease in the depth of the drain does not change significantly the root zone salinity which reaches 6.21 dS m-1 during the irrigation season and 3.67 dS m-1 during the non irrigated season. The depth of the drain can be reduced to 1.6 m without any damage to crops. A water table depth (Dw= 1.8 m) appears to be excessive and would increase the cost of system installation. We can see a slight reduction in drainage flow when the depth of the drain goes from 1.8 m to 1.2 m. A decrease of the drain depth decreases the water table level. Although there was no variation in root zone salinities due to change in drain spacing. The predicted drainage flows have registered an evolution related to the occurrence of irrigation and rainfall. This evolution was confirmed by observed values. In this study, calibration of SaltMod for water-salt balance parameters shows the reliable validity of the model for the local conditions.
机译:这项研究的目的是使用SaltMod模拟模型来预测Kalaat El Andalous灌溉区的根区盐度,历时10年。总体而言,该模型预测根部区域的电导率或多或少相似。在灌溉季节将达到7.7 dS m-1的最高电导率值。随着降雨的减少,特别是在冬季,当平均电导率的最小值达到3.1 dS m-1时,土壤盐分会降低。从测量值证实了根区盐度的这种季节性变化。还进行了研究,以研究不同排水间距和排水深度对根区盐度,地下水位深度和排水的影响。模拟表明,排水深度的减少并没有显着改变根区盐度,在灌溉季节根区盐度达到6.21 dS m-1,而在非灌溉季节达到3.67 dS m-1。排水管的深度可以减小到1.6 m,而不会损坏农作物。地下水位深度(Dw = 1.8 m)似乎过大,会增加系统安装成本。当排水深度从1.8 m减小到1.2 m时,我们可以看到排水量略有减少。排水深度的减小会降低地下水位。尽管由于排水间距的变化,根区盐度没有变化。预测的排水流量已经记录了与灌溉和降雨发生有关的演变。观察值证实了这种演变。在这项研究中,针对水盐平衡参数对SaltMod进行的校准显示了该模型在当地条件下的可靠有效性。

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