Evaluation of nitrate redistribution in surface and subsurface drip irrigation systems

IF 1 4区 环境科学与生态学 Q4 WATER RESOURCES
Sogand Arab, Javad Mozaffari, Mohammad Javad Nahvivia
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Abstract

Nitrogen compounds added to the soil may convert to nitrate and cause contamination. The distribution and uniformity of soil nitrate in surface vs. subsurface drip irrigation systems were compared in a physical model consisting of a transparent glass box (1.20 x 0.5 x 1 m) and sandy loam soil, and considering emitter installation depths of 0 and 30 cm, discharge rates of Q1 = 2, Q2 = 4, Q3 = 8 L/h, and fertilizer levels of S1 = 125, S2 = 250, S3 = 375 mg/L. Irrigation continued for 6 h and nitrate and moisture sampling was performed for 68 h after the initiation of water front advance. The result showed that doubling the discharge caused the wetted area to triple in size in the subsurface drip irrigation system whereas it only doubled in size in the surface drip irrigation system. Thus in the subsurface system, when increasing the fertilizer level, the nitrate spread out extensively and therefore its concentration was greatly reduced. Also, by increasing discharge, the difference in soil nitrate concentration between the two systems increases because of increasing non-uniformity of nitrate distribution in the surface system, such that by increasing the fertilizer concentration form 125 to 375 mg/L, the difference in nitrate concentration increases from 22% to 500% (for Q1 = 2 L/h), 43% to 352% (for Q2 = 4 L/h), and 14% to 166% (for Q3 = 8 L/h). Thus the subsurface drip irrigation system has a more uniform trend of nitrate distribution than the surface drip irrigation system. Also, treatment with maximum flow and fertilizer level will create the most optimal nitrate concentration in the soil.
地表和地下滴灌系统中硝酸盐再分配的评价
添加到土壤中的氮化合物可能转化为硝酸盐,造成污染。以透明玻璃箱(1.20 x 0.5 x 1 m)和砂壤土为物理模型,考虑灌水器安装深度为0和30 cm,排水量为Q1 = 2、Q2 = 4、Q3 = 8 L/h,施肥量S1 = 125、S2 = 250、S3 = 375 mg/L,比较了地表和地下滴灌系统土壤硝酸盐的分布和均匀性。灌溉持续6 h,在水锋推进开始后68 h进行硝酸盐和水分采样。结果表明,在地下滴灌系统中,流量增加一倍使湿区面积增加两倍,而在地表滴灌系统中,湿区面积仅增加一倍。因此,在地下系统中,随着施肥水平的增加,硝酸盐广泛扩散,其浓度大大降低。此外,随着流量的增加,由于地表系统中硝酸盐分布的不均匀性增加,两种系统之间的土壤硝酸盐浓度差异也会增加,例如,当肥料浓度从125 mg/L增加到375 mg/L时,硝酸盐浓度差异从22%增加到500% (Q1 = 2 L/h), 43%增加到352% (Q2 = 4 L/h), 14%增加到166% (Q3 = 8 L/h)。因此,地下滴灌系统比地表滴灌系统具有更均匀的硝态氮分布趋势。此外,最大流量和肥料水平的处理将在土壤中产生最优的硝酸盐浓度。
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来源期刊
Water SA
Water SA 环境科学-水资源
CiteScore
2.80
自引率
6.70%
发文量
46
审稿时长
18-36 weeks
期刊介绍: WaterSA publishes refereed, original work in all branches of water science, technology and engineering. This includes water resources development; the hydrological cycle; surface hydrology; geohydrology and hydrometeorology; limnology; salinisation; treatment and management of municipal and industrial water and wastewater; treatment and disposal of sewage sludge; environmental pollution control; water quality and treatment; aquaculture in terms of its impact on the water resource; agricultural water science; etc. Water SA is the WRC’s accredited scientific journal which contains original research articles and review articles on all aspects of water science, technology, engineering and policy. Water SA has been in publication since 1975 and includes articles from both local and international authors. The journal is issued quarterly (4 editions per year).
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