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Effects of calcium based surface amendments on hydraulic conductivity and selected physical properties of subsurface drained sodic soils.

机译:钙基表面改性剂对地下排水的钠土的水力传导率和选定的物理性质的影响。

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摘要

Managing excess soil water in agricultural fields in the Northern Great Plains through subsurface drainage increases the risk of sodification in high-risk soils. Leaching sodic soils with low electrical conductivity (EC) water, rainfall, may result in the swelling of soil, dispersion of clay particles and consequently the breakdown of soil structure leading to changes in physical and mechanical properties of soils (e.g., reduced infiltration, hard-setting and reduced trafficability). In this dissertation, the effectiveness of calcium amendments of gypsum and spent lime, a byproduct of the processing sugar beets, with water-management treatments of free drainage (FD) and no drainage (ND) on improving physical properties of the soil were examined.;The first objective was to evaluate the effects of drainage and surface treatments on the penetration resistance (PR). The second objective was to use infiltration tests with a mini-disk tension infiltrometer and a Cornell sprinkle infiltrometer to investigate changes in hydraulic properties. Lastly, a drawbar dynamometer was used to measure draft on a chisel plow as it was pulled across the plots by a tractor equipped with an auto-guidance system and instrumentation interfaced with the controller area network of the tractor.;The results show that the PR values of plots with gypsum application at high rate of 22.4 Mg ha-1 (GH) were significantly higher than other surface amendments. GH increased the hydraulic conductivity of the soil matrix compared to spent lime application at rate of 22.4 Mg ha-1 (SL); however, the overall flow of water through the soil profile, including the soil matrix and the macropores, was not affected. Both GH and gypsum application at high rate of 11.2 Mg ha-1 (GL) lowered the drawbar power requirements compared to spent lime application. For many farmers, drainage enables early planting and the adding of ameliorants will safeguard against further sodification of their fields.
机译:通过地下排水管理北大平原北部农田中的过量土壤水,会增加高风险土壤中被水化的风险。浸出低电导率(EC)水的苏打土壤,降雨可能会导致土壤溶胀,粘土颗粒分散并因此破坏土壤结构,从而导致土壤物理和机械性质发生变化(例如,渗透减少,坚硬设置并减少了可访问性)。本文研究了加工甜菜的副产品石膏和废石灰的钙改良剂,采用水管理措施(自由排水(FD)和不排水(ND))改善土壤的物理性能。 ;第一个目标是评估排水和表面处理对渗透阻力(PR)的影响。第二个目标是使用微型磁盘张力渗透仪和康奈尔洒水渗透仪进行渗透测试,以研究水力特性的变化。最后,用拉力计来测量凿犁上的吃水深度,因为它是由配备有自动引导系统和与拖拉机控制器区域网络连接的仪表的拖拉机拉过地块的。结果表明,PR以22.4 Mg ha-1(GH)的高比例施用石膏的地块的土壤肥力值显着高于其他表面改良剂。与施用生石灰相比,GH以22.4 Mg ha-1(SL)的速率增加了土壤基质的水力传导性;但是,通过土壤剖面的整个水流,包括土壤基质和大孔,都没有受到影响。与废石灰施用相比,GH和石膏以11.2 Mg ha-1(GL)的高施用量均降低了牵引杆的功率要求。对于许多农民而言,排水使他们能够早日种植,而添加改良剂将防止他们的田地进一步变质。

著录项

  • 作者

    Wamono, Anthony Walekhwa.;

  • 作者单位

    North Dakota State University.;

  • 授予单位 North Dakota State University.;
  • 学科 Agricultural engineering.;Natural resource management.;Engineering.
  • 学位 Ph.D.
  • 年度 2016
  • 页码 95 p.
  • 总页数 95
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:44:35

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