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Amelioration of an arid-land sodic soil with aluminum polynuclear species and humic acid.

机译:用铝多核物种和腐殖酸改善干旱地区的钠盐土壤。

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摘要

The conventional methods used for sodic soil reclamation are often difficult and time consuming. This research was conducted to examine the effects of aluminum polynuclear species, humic acid, gypsum and aluminum polynuclear species plus humic acid treatments on the hydraulic conductivity (sc K), exchangeable sodium percentage, and cation exchange capacity (CEC) of a sodic soil. Aluminum was added at OH/Al molar ratios of 2.0 and 2.5 to Pachappa soil (fine-loamy, mixed, thermic Mollic Haploxeralf) and at 2.5 to Arlington soil (mixed, thermic, Haplic Durixeralf). Irrigation water with 0.01 M Cl{dollar}sp-{dollar} and SAR 20 and tap water with SAR = 1.33 were used to leach the Pachappa and Arlington soils, respectively.; The adsorption of aluminum was linear and irreversible at pH 5.0 and 7.0. The sc K and infiltration rate increased significantly (p {dollar}<{dollar} 0.05) with the amount of aluminum added. There was no significant difference between the two OH/Al molar ratios tested. The aluminum treatment did not significantly (p {dollar}<{dollar} 0.05) change the CEC and pH of the soils. Nonexchangeable aluminum was found to have a dominant role in stabilizing soil aggregates. The treatment effects on sc K of Arlington soil were in the following order: aluminum OH/Al = 2.5 {dollar}approx{dollar} humic acid pH 3.5 {dollar}>{dollar} humic acid pH 3.5 plus aluminum OH/Al = 2.5 {dollar}>{dollar} gypsum {dollar}>{dollar} humic acid pH 3.5 raised to pH 7.0 {dollar}approx{dollar} humic acid plus aluminum OH/Al = 2.5 {dollar}>{dollar} control {dollar}>{dollar} humic acid. The reduction in the ESP is ranked in the following order: humic acid pH 3.5 plus aluminum OH/Al = 2.5 {dollar}>{dollar} gypsum {dollar}>{dollar} humic acid pH 3.5 {dollar}>{dollar} aluminum OH/Al = 2.5. The other treatments did not appreciably lower the ESP. Humic acid pH 3.5 treatment was not considered further, as pH 3.5 is too low for agricultural production. Also the adsorption of humic acid was reversible in the pH range of arid-land soils. Based on the quantity of water and the time required to achieve an ESP of {dollar}<{dollar}20, the effectiveness of treatments may be ranked as humic acid pH 3.5 plus aluminum OH/Al = 2.5 {dollar}<{dollar} aluminum OH/Al = 2.5 {dollar}<{dollar} gypsum.
机译:用于苏打土壤开垦的常规方法通常是困难且耗时的。进行了这项研究,以研究铝多核物种,腐殖酸,石膏和铝多核物种以及腐殖酸处理对苏打水的水力传导率(sc K),可交换钠百分比和阳离子交换容量(CEC)的影响。以2.0 / 2.5的OH / Al摩尔比将铝添加到Pachappa土壤(细质壤土,混合的,热的Mollic Haploxeralf)和以2.5:添加的阿林顿土壤(混合的,热的,Haplic Durixeralf)。分别用0.01 M Cl {dollar} sp- {dollar}和SAR 20的灌溉水和SAR = 1.33的自来水对Pachappa和Arlington土壤进行浸出。铝的吸附是线性的,并且在pH 5.0和7.0下不可逆。随着铝的加入,sc K和渗透率显着增加(p {dollar} <{dollar} 0.05)。在所测试的两个OH / Al摩尔比之间没有显着差异。铝处理未显着改变土壤的CEC和pH(p {dollar} <{dollar} 0.05)。发现不可改变的铝在稳定土壤聚集体中起主要作用。对阿灵顿土壤sc K的处理效果如下:铝OH / Al = 2.5 {美元}约{美元}腐殖酸pH 3.5 {美元}> {美元}腐殖酸pH 3.5加铝OH / Al = 2.5 {美元}> {美元}石膏{美元}> {美元}腐殖酸pH 3.5提高到pH 7.0 {美元}腐殖酸加铝OH / Al = 2.5 {美元}> {美元}对照{美元} > {美元}腐殖酸。 ESP的减少按以下顺序排列:腐殖酸pH 3.5加铝OH / Al = 2.5 {美元}> {美元}石膏{美元}> {美元}腐殖酸pH值3.5 {美元}> {美元}铝OH / Al = 2.5。其他治疗并未明显降低ESP。由于pH 3.5对于农业生产而言太低,因此不再考虑使用腐殖酸pH 3.5进行处理。腐殖酸的吸附在干旱土壤的pH范围内也是可逆的。根据水的量和达到{ESP} <{USD} 20所需的时间,可以将处理的效果定为腐殖酸pH 3.5加铝OH / Al = 2.5 {USD} <{USD}铝OH / Al = 2.5 {美元} <{美元}石膏。

著录项

  • 作者

    Elamin, Elamin Abdelmagid.;

  • 作者单位

    University of California, Riverside.;

  • 授予单位 University of California, Riverside.;
  • 学科 Agriculture Agronomy.
  • 学位 Ph.D.
  • 年度 1991
  • 页码 111 p.
  • 总页数 111
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 农学(农艺学);
  • 关键词

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