首页> 外文期刊>Soil Science >IMPACT OF SOIL AMENDMENTS ON INTERMITTENT EVAPORATION, MOISTURE DISTRIBUTION AND SALT REDISTRIBUTION IN SALINE-SODIC CLAY SOIL COLUMNS
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IMPACT OF SOIL AMENDMENTS ON INTERMITTENT EVAPORATION, MOISTURE DISTRIBUTION AND SALT REDISTRIBUTION IN SALINE-SODIC CLAY SOIL COLUMNS

机译:盐碱土粘土柱中土壤改良剂对间歇蒸发,水分分布和盐分分布的影响

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摘要

Naturally occurring organic amendments and inorganic compounds are used as additives to improve soil physical conditions. This study was conducted to determine the effects of some organic and inorganic soil amendments on cumulative evaporation, moisture distribution, and salt leaching through saline-sodic clay soil columns. Organic amendments were mixed with the top 5 cm in 60-cm soil columns at the rate of 22 ton/ha for farmyard manure and water hyacinth and 44 ton/ha for chicken manure and dry sludge. The 1:2 sand-soil mixture was applied to the top 20 cm of the columns at a rate of 800 ton/ha, whereas gypsum was administered as a saturated solution with the irrigation water. In accordance with previous findings, the cumulative evaporation, E, was found to be a linear function of the square root of time (E C root t), where C, was determined largely by the type of amendment added. Sand increased soil water penetrability, lambda, and markedly reduced E by 32% over the control. Chicken manure,gypsum, water hyacinth, farmyard manure, and dry sludge reduced evaporation by 23, 17, 15, 10, and 6%, respectively. The soil moisture distribution was governed by the amount of water conserved. Sand and chicken manure additions increased the amount of water conserved by 72% and 52% respectively, compared with the control. The depth of the wetting front advanced deeper and the transmission zone of the moisture distribution lengthened as time progressed. Desalinization and dealkalization were governed largely by lambda. Sand addition was more effective in increasing the desalinized zone from 28.5 cm at the end of the first 30 days to 40.0 cm at the end of the experiment. Chicken manure was the most effective organic amendment, increasing the desalinized zone from 17.5 cm to 37.5 cm during the same two periods. Sand additions also increased the dealkanized zone from 18.7 cm to 33.5 cm, whereas, gypsum, which was more effective than the organic amendments on SAR redistribution, increased the dealkanized depth from 12.5 cm to 32.5 cm during the same two periods. Organic and inorganic amendments increased soil water penetrability into clay soils and enhanced salt leaching. This research which was conducted to acquire information relevant to the possible remediation of saline-sodic soils, used organic and inorganic amendments, which are both available and inexpensive.
机译:天然存在的有机改性剂和无机化合物用作改善土壤物理条件的添加剂。进行这项研究是为了确定一些有机和无机土壤改良剂对通过盐碱土粘土柱的累积蒸发,水分分布和盐分淋失的影响。将有机改良剂在60厘米土壤柱中与顶部5厘米混合,农家肥料和水葫芦的混合量为22吨/公顷,鸡粪和干污泥的混合量为44吨/公顷。将1:2的沙土混合物以800吨/公顷的速度施加到柱子的顶部20厘米处,而将石膏作为饱和溶液与灌溉用水一起施用。根据以前的发现,累积蒸发量E是时间平方根的线性函数(E C root t),其中C主要取决于添加的修正剂的类型。与对照相比,沙土增加了土壤水的渗透性,λ,并使E显着降低了32%。鸡粪,石膏,水葫芦,农家粪便和干污泥分别使蒸发减少了23%,17%,15%,10%和6%。土壤水分的分布受保存水量的控制。与对照相比,砂和鸡粪的添加分别使节水量增加了72%和52%。随着时间的流逝,湿润前沿的深度进一步加深,水分分布的传递区域延长。脱盐和脱碱主要由λ决定。在开始的30天结束时,添加砂子将脱盐区从28.5 cm增加到实验结束时的40.0 cm更有效。鸡粪是最有效的有机改良剂,在相同的两个时期内将脱盐区从17.5厘米增加到37.5厘米。砂的加入也将脱钙化区从18.7 cm增加到33.5 cm,而石膏比SAR再分配的有机改良剂更有效,在相同的两个时期内,脱钙深度从12.5 cm增加到32.5 cm。有机和无机改良剂增加了土壤水对粘土的渗透性,并增强了盐分浸出。进行这项研究的目的是获得与盐碱土壤可能的修复有关的信息,这些有机和无机改良剂既可利用,又价格便宜。

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