首页> 外文会议>Annual International Meeting of the American Society of Agricultural and Biological Engineers >Combined Effect of Leaching Fraction and Salinity on Barley (Hordeum vulgare L.) Growth and Salt Distribution Ahmed AI-Busaidi
【24h】

Combined Effect of Leaching Fraction and Salinity on Barley (Hordeum vulgare L.) Growth and Salt Distribution Ahmed AI-Busaidi

机译:浸出级分和盐度对大麦(Hordeum Vulgare L.)生长和盐分分配的综合作用Ahmed Ai-Busaidi

获取原文

摘要

Utilizing marginal quality water requires control of soil salinity by leaching and drainage of excess water and salt. This greenhouse study was carried out to determine the effect of saline irrigation (3 and 13 dS m~(-1)) and leaching process (0,1 and0.4 Leaching Fraction) on the growth of barley grown on sandy soil. Salt accumulation and distribution were also studied. Soil salinity increased linearly with distance from the emitter and salt concentrations were higher at the border of the wetting front. Salinity distribution with depth was mainly controlled by the quality and quantity of water applied in each treatment. Higher leaching fraction gave lower values of soil salinity even in highly saline treatments. Across treatments, salts were mostlyaccumulated in the soil surface and within the 20-40 cm depth. For all treatments, soil physical parameters such as infiltration rate and hydraulic conductivity were not significantly (P > 0.05) affected. Barley is a salt tolerant crop so its growth wasnot completely affected. There was a significant (P < 0.05) difference between low and high salinity. However leaching was mainly affected plant fresh weight and increased water content in plant as leaching fraction increased. That was clearly observedin fresh weight values between leaching fractions of low salinity (P < 0.05). A higher leaching fraction creates a good environment for plant by increasing water content and leaching salts to the lower horizons. Finally, barley can survive and give a good yield if grown under a good management of irrigation and leaching process.
机译:利用边缘水质水需要通过浸出和排水来控制土壤盐度的过量水和盐。进行了这种温室研究,以确定盐水冲洗(3和13ds m〜(-1))和浸出过程(0.1和0.4次浸出部分)对沙土生长的浸出过程(0.1和0.4次浸出部分)。还研究了盐积累和分布。土壤盐度随着距从发射器的距离而随着距离的距离而增加,在润湿前部的边界处较高。深度的盐度分布主要由每种治疗中施加的水的质量和量控制。即使在高度盐水处理中,较高的浸出率也使得较低的土壤盐度值较低。在治疗中,在土壤表面和20-40厘米的深度内盐大部分累积。对于所有治疗,诸如渗透速率和液压导电性的土壤物理参数没有显着(p> 0.05)。大麦是一种耐盐作物,所以其生长是完全影响的。低盐度之间存在显着(P <0.05)差异。然而,浸出主要是植物新鲜重量和植物中的水含量增加,因为浸出部分增加。在低盐度的浸出级分之间清楚地观察到鲜重的重量值(P <0.05)。通过将水含量增加和浸出盐在较低的地平线上,更高的浸出级分造成良好的植物环境。最后,如果在良好的灌溉和浸出过程中生长,大麦可以存活并给出良好的收益率。

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