【24h】

The Role of Mole Drainage in Degradation Soils Under Saline Groundwater Table, Egypt

机译:盐渍地下水位下埃及排水在退化土壤中的作用

获取原文
获取原文并翻译 | 示例

摘要

Agricultural salt affected heavy textured lands of poor productivity are commonly found throughout the northern periphery of the Nile Delta. Clay-salt affected soils are known to be difficult to manage. The present work is conducted in El-Serw Farm, north Delta. The salinity is due to a shallow saline groundwater table (EC ≈ = 39dS/m at 40 cm depth). The aim is to develop suitable local techniques for land improvement in rootzone and sustainable agriculture. An experimental field was designed with different treatments of mole drain spacing 0, 3.0, 2.0 and 1.5 m combined without or with gypsum addition. Rice was cultivated in the summer of 1999 and 2000. AH agricultural practices are similar to that in neighbour fields. Irrigation water salinity ranges from 1.5 to 2.0 dS /m. In the first year, results revealed that only negligible reduction in salinity occurred in the plots under 3 m mole spacing with or without gypsum. Better desalinization is obtained in plots under 2 m and 1.5 m without gypsum up to 60 cm soil depth. Salinity reduction is clear enough under the same spacing with gypsum, since the EC dropped to values around 6 and 5 dS/m, respectively. For exchangeable sodium percentage, ESP, the soil at all depths is initially highly sodic ESP>40. The sodicity almost persists in the different treatments, even in plots under 2 and 1.5 m mole spacing either without or with gypsum, the sodicity is still high (ESP ~ 26). The rice yield in the control being 1 Ton/fd reached 2.6 and 1.75 Ton/fd under 1.5 m treatment with and without gypsum, respectively. Almost the same yield is obtained with 2 m spacing. In the second year, there is a progressive improvement in soil conditions. In general, salinity decreased with decreasing mole drain spacing; EC dropped to less than 4 dS/m in 1.5 m mole drain spacing with gypsum treatments comparing to the other treatments. Regarding exchangeable sodium percentage, there is a relative reduction in ESP at the soil surface than in the deeper depth especially with gypsum and narrow drain spacing. The ESP is still high. Concerning plant growth and production, there is a good cover plant for mole drain spacing especially with gypsum treatments compared to that without gypsum addition. The best treatment is 1.5 m mole drain spacing with gypsum. Data of rice yield follows the same trend to that in the first year with a relative increase in all treatments.
机译:受农业盐影响的生产力低下的重质土地通常在尼罗河三角洲的北部边缘发现。已知受粘土盐影响的土壤难以处理。目前的工作是在北部三角洲的El-Serw农场进行的。盐度是由于地下水位浅而引起的(在40 cm深度处EC≈39dS / m)。目的是开发适合当地的技术来改善根区和可持续农业的土地。设计了一个实验场,在不添加石膏或不添加石膏的情况下,对摩尔排水间距0、3.0、2.0和1.5 m进行了不同处理。水稻是在1999年和2000年夏季种植的。AH的耕作方式与邻地相似。灌溉水盐度范围为1.5至2.0 dS / m。在第一年,结果表明,在有或没有石膏的情况下,在3 m摩尔间距以下的地块中,盐度的降低仅可忽略不计。在2 m和1.5 m以下,土壤深度不超过60 cm的情况下,在没有石膏的情况下可获得更好的脱盐效果。在与石膏相同的间距下,盐度降低已足够明显,因为EC分别降至6和5 dS / m左右。对于可交换的钠百分比(ESP),所有深度的土壤最初都是高度钠的ESP> 40。在不同处理条件下,碱度几乎保持不变,即使在不使用石膏或使用石膏的2和1.5 m摩尔间距的样地中,碱度仍然很高(ESP〜26)。在有和没有石膏的情况下,在1.5 m处理下,对照的水稻产量分别为1吨/ fd达到2.6吨和1.75吨/ fd。以2 m的间距获得几乎相同的产量。第二年,土壤条件逐渐改善。通常,盐度随着摩尔排泄间距的减小而降低;与其他处理相比,采用石膏处理的EC在1.5 m摩尔排水空间中下降至小于4 dS / m。关于可交换的钠含量,特别是在石膏和排水沟较窄的情况下,土壤表层的ESP相对较深处有减少。 ESP仍然很高。关于植物的生长和生产,与没有添加石膏的植物相比,有一个良好的覆盖植物,可以减少mole鼠的排水距离,尤其是使用石膏处理时。最好的处理方法是与石膏的排水孔间距为1.5 m。稻米产量数据遵循与第一年相同的趋势,所有处理均相对增加。

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