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Some Soil Factors Affecting Air Pollution by Ammonia Volatilization from Urea Fertilizer

机译:影响尿素氨气挥发造成大气污染的土壤因素

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AMMONIA volatilization from urea reduces nitrogen fertilizer efficiency of crops andvincreased air pollution. Some soil factors such as clay percent, calcium carbonate content, moisture regime and organic matter content were studied in two of laboratory incubation experiments under aerobic conditions at 20 ± 2 deg. Soil samples were collected from Qalubia Govemorate, Ismailia Govemorate and Alexandria Goyernorate which represented clay loam, sandy and calcareous soils, respectively. Ammonia volatilization losses from urea reached 14.4, 26.7 and 32.6% of the applied urea fertilizer to clay loam, sandy and calcareous soils, respectively. Whereas, ammonia volatilization increased as a result of increasing calcium carbonate content in the soil (calcareous soil) by about 2.3, and 1.2 times compared to clay loam and sandy soils, respectively. Moreover, the increases of ammonia volatilization from soil at 50% of water holding capacity were 38, 76 and 88 % relative to those found at 100 % water holding, capacity after three weeks of applied urea to the investigated soils, respectively. Also, application of cattle manure at rates of 2 and 5% decreased the amount of NH_3 volatilization from calcareous soil by about 43.1 and 53.6 % at full water holding capacity. The concentration of NH~+_4 in the soil solution increased due to application of urea fertilizer particularly when cattle manure and clay content were increased along with low water content in soil. Such increases recorded 57, 135 and 165% at theend of experiment (21 days) at low moisture in clay loam, sandy and calcareous soils, respectively. On the other hand, the values of nitrate concentration decreased with increasing water content in the different soils. So, the results showed that soil pH, water content and organic matter content are major factors influencing ammonia losses from soils compared with the other studied factors.
机译:尿素中的氨挥发会降低农作物的氮肥利用率,并加剧空气污染。在20±2度的有氧条件下的两个实验室培养实验中,研究了一些土壤因素,例如粘土百分比,碳酸钙含量,水分状况和有机质含量。从Qalubia Govemorate,Ismailia Govemorate和Alexandria Goyernorate收集土壤样品,分别代表粘土壤土,沙质和钙质土壤。尿素在氨肥,砂质和石灰质土壤上的氨挥发损失分别达到了施用尿素肥料的14.4%,26.7%和32.6%。然而,由于土壤(钙质土壤)中碳酸钙含量的增加,氨挥发增加了,分别比粘土壤土和沙质土壤增加了2.3倍和1.2倍。此外,相对于持水量为100%的尿素施用三周后的土壤,氨的挥发量在持水量为50%的情况下分别增加了38%,76%和88%。同样,以2%和5%的比例施用牛粪肥,在完全持水量下,钙质土壤中NH_3挥发量减少了约43.1%和53.6%。由于施用尿素肥料,土壤溶液中的NH〜+ _4浓度增加,特别是当牛粪和粘土含量增加且土壤含水量降低时。在试验结束时(21天),在低壤土,沙质和石灰质土壤中,这种增加分别记录为57%,135%和165%。另一方面,在不同土壤中,硝酸盐浓度的值随含水量的增加而降低。因此,结果表明,与其他研究因素相比,土壤pH,水分和有机质含量是影响土壤氨气损失的主要因素。

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