...
首页> 外文期刊>The Indian Journal of Agricultural Sciences >Soil water distribution and simulation under subsurface drip irrigation in cotton (Gossypium hirsutum)
【24h】

Soil water distribution and simulation under subsurface drip irrigation in cotton (Gossypium hirsutum)

机译:棉花地下滴灌条件下的土壤水分分布与模拟

获取原文
获取原文并翻译 | 示例
           

摘要

To see the effect of salinity of irrigation water under subsurface drip irrigation on cotton (Gossypium hirsutum) yield, a field experiment was conducted on loamy soils at Precision Farming Development Center, Water Technology Center, IARI, New Delhi,during 2009 and 2010 kharif. Irrigation water having four levels of salinity (EC_1= 2 dS/m (ground water), EC_2= 5 dS/m, EC_3= 8 dS/m and EC_4=11 dS/m) taken as main plot treatment was used as drip with laterals placed at three depths (at the surface, 15 cm and 30 cm below the soil surface) as sub-plot treatments in a split plot design with three replications. The results indicated that cotton yields were not influenced by irrigation water salinity up to 8 dS/m and different lateral depths during two years but decreased by 37.3, 44.3 and 36.0% in 2009 year and 26.6, 35.1 and 42.2 % in 2010 years at 11 dS/m as compared with EC_1, EC_2 and EC_3 treatments, respectively. Distribution of soil moisture data showed a horizontal decrease in soil water content at a distance of 20 and 40 cm away from drip line and vertical soil depths. Distribution of soil moisture was simulated by Hydrus 2D model. The model evaluated by AE and RMSE showed a good correspondence on soil water distribution between observed datafrom field experiment and simulated by model. The AE ranged from -0.015 to -0.002 and RMSE from 0.003 to 0.015.
机译:为了了解地下滴灌条件下灌溉水的盐度对棉花产量的影响,在2009年和2010年的卡里夫新德里国际农业研究中心水技术中心精密农业发展中心,对壤土进行了田间试验。以四种盐度(EC_1 = 2 dS / m(地下水),EC_2 = 5 dS / m,EC_3 = 8 dS / m和EC_4 = 11 dS / m)作为主要地块处理的灌溉水用作滴灌剂。在具有三个重复的分割地块设计中,将子侧面放置在三个深度处(在土壤表面以下15 cm和30 cm处)作为子地块处理。结果表明,在两年内,高达8 dS / m的灌溉水盐度和不同的侧向深度对棉花单产没有影响,但在2009年和11年,棉花产量分别下降了37.3%,44.3%和36.0%,以及2010年的26​​.6%,35.1%和42.2% dS / m分别与EC_1,EC_2和EC_3处理相比。土壤水分数据的分布显示,在距滴灌线和垂直土壤深度20和40 cm处,土壤含水量水平下降。用Hydrus 2D模型模拟土壤水分的分布。 AE和RMSE评估的模型在田间试验的观测数据和模型模拟之间显示出良好的土壤水分分布对应性。 AE范围为-0.015至-0.002,RMSE范围为0.003至0.015。

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