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Studies on Soil Water and Nitrate Distribution under Sprinkler Irrigation Conditions

机译:喷水灭火条件下土壤水和硝酸盐分布的研究

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摘要

Soil water and nutrition distribution is important for plant growth and environment protection. A field experiment was carried out to study the distribution characteristics of soil water and nitrate under sprinkler irrigation and surface irrigation in 2003. Results indicate that the main change of soil water content was within 0.6 m soil layers under sprinkler irrigation where main winter wheat roots distribute. Under surface irrigation, soil water could reach soil layer below the root zone. During the period of winter wheat growth, the concentration peak of soil nitrate appeared above 0.4 m soil layer and moved above 0.6 m under sprinkler irrigation. However, nitrate concentration peak appeared around 0.6 m and could move out root active zone under surface irrigation. The variation of average soil water content in 0~0.6 m layer and variation coefficient of soil water storage in 1.0 m layers under sprinkler irrigation were less than that under surface irrigation. Soil water percolates from root active zone under surface irrigation resulting in nitrate leaching. So, sprinkler irrigation can efficiently control water distribution depth and reduce irrigation water and nitrate percolation as well as control ground water pollution.
机译:土壤水和营养分布对于植物生长和环境保护至关重要。进行了田间实验,研究了2003年洒水灌溉和表面灌溉下土壤水分和硝酸盐的分布特性。结果表明,土壤含水量的主要变化在洒水灌溉下的洒水灌溉下的0.6米。主要冬小麦根源。在表面灌溉下,土壤水可以到达根区下方的土壤层。在冬小麦生长期间,土壤硝酸盐的浓度峰出现在0.4米的土层以上,并在喷洒灌溉下移动到0.6米以上。然而,硝酸盐浓度峰值出现约0.6μm,并且可以在表面灌溉下移出根源区。在洒水灌溉灌溉的1.0米层中,0〜0.6米层和土壤储水量的变化系数的平均土壤水分的变化小于表面灌溉。表面灌溉下的根源区土壤水渗透,导致硝酸盐浸出。因此,喷水灭火可以有效地控制水分布深度并减少灌溉水和硝酸盐的渗透以及控制地面水污染。

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