Transformation and Transport of Nitrogen Forms in a Sandy Entisol Following a Heavy Loading of Ammonium Nitrate Solution: Field Measurements and Model Simulations

S. Paramasivam, Ashok K. Alva, Ali Fares
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引用次数: 23

Abstract

Understanding the factors influencing water and nutrient transport through soil profile is important for the efficient management of nutrient and irrigation to minimize nutrient leaching below the rootzone. Transport of NO3-N and NH4-N was studied in a Candler fine sand following a heavy loading of a liquid fertilizer containing ammonium nitrate. Both NO3-N and NH4-N transported quite rapidly (within 3 d) and accumulated above the clay layer at about depth of 2.7 m. The concentrations of NH4-N and NO3-N approached background levels throughout the soil profile by 184 d. More than 50% of ammonium and nitrate contained in the spilled solution leached from the entire depth of soil profile sampled during the first 95 d. The cumulative amount of rainfall during this period was 329 mm, which accounted for 65% of the total rainfall for the entire study period. The concentrations of NH4-N and NO3-N at various depths within the entire soil profile reasonably predicted by the Leaching Estimation and Chemistry Model (LEACHM) and compared favorably with the measured concentrations, however, there are few places with high concentrations. The cumulative amount of leachate at the bottom of the soil profile predicted by LEACHM represented 90% of total rainfall that occurred during the study period. This demonstrated a substantial potential for leaching of soluble nutrients through the sandy soil profile.
在大量硝酸铵溶液后,沙质土壤中氮形态的转化和运输:现场测量和模型模拟
了解土壤剖面中水分和养分运移的影响因素对于有效管理养分和灌溉以减少根区以下养分淋失具有重要意义。研究了重载硝酸铵液肥后烛状细砂中NO3-N和NH4-N的迁移。NO3-N和NH4-N运移速度较快(3 d内),并在约2.7 m深度的黏土层上方积累。在184 d时,NH4-N和NO3-N的浓度接近本底水平。溢出溶液中超过50%的铵态氮和硝态氮在前95 d从采样的土壤剖面的整个深度中浸出。这段时间的累计降雨量为329 mm,占整个研究期总降雨量的65%。淋溶与化学模型(LEACHM)对全剖面不同深度的NH4-N和NO3-N浓度预测较为合理,且与实测值较为吻合,但浓度较高的地方较少。LEACHM预测的土壤剖面底部渗滤液累积量占研究期间总降雨量的90%。这表明了可溶性养分通过沙质土壤剖面淋滤的巨大潜力。
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