基于生物炭的氮肥施用对水稻生长土壤中氨挥发的影响:实验室规模密闭室研究

M. Jayarathna, R. S. Dharmakeerthi, A. D. Igalavithana
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引用次数: 0

摘要

水稻生长土壤中的氨挥发(AV)是降低氮肥利用效率的主要途径之一。直接播撒尿素可增加基质的可用性,从而促进氨挥发。尿素夹层生物炭(BC_U)可以作为一种新方法,在水稻种植中提高氮的利用效率并降低氮的转化效率。因此,我们进行了一项实验室实验,以量化 BC_U 颗粒对水稻生长 Entisol 中反式脂肪酸损失和氮动态的影响。我们测定了在淹水或饱和条件下向土壤施用 BC_U 后土壤脲酶活性(UA)和 pH 缓冲能力(pHBC)的变化。处理为零施氮(对照)、施尿素(U)和以 23 毫克氮千克土-1 的比例添加 BC_U 颗粒。在饱和条件下,添加尿素的土壤溶液中的 NH4+ 浓度明显更高,而尿素中的 NO3- 浓度最高;在淹水条件下,尿素中的 NH4+ 浓度明显更高,而 NO3- 浓度不受尿素施用的影响。一般来说,在调查的实验条件下,AV 的损失非常小,从添加尿素的 0% 到 2.72% 不等。在饱和条件下,氮处理对 AV 有显著影响(p0.05)。虽然施用氮肥后 AV 损失较小(<3%),但通过施用 BC_U 尿素和/或在施用氮肥后几天保持淹没水层,可以进一步减少 AV 损失。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of Biochar Based N Fertilizer Application on Ammonia Volatilization from a Rice Growing Soil: A Laboratory Scale Closed Chamber Study
Ammonia Volatilization (AV) in rice growing soils is one of the major pathways to lower the use efficiency of added nitrogen (N) fertilizers. Direct broadcasting of urea facilitates AV by increasing the substrate availability. Urea intercalated biochar (BC_U) can be a novel approach that could improve N use efficiency and reduce AV in paddy cultivation. Therefore, a laboratory experiment was conducted to quantify the effect of BC_U pellets on AV losses and N dynamics in a rice growing Entisol. We determined the changes in soil urease activity (UA) and pH buffer capacity (pHBC) after application of BC_U to soil under flooded or saturated conditions. Treatments were zero application of N (control), urea (U) and BC_U pellets added at a rate of 23 mg N kg soil-1. Under saturated conditions, significantly higher NH4+ concentration in soil solution was observed in urea added soils and the highest NO3- was observed in U. Under flooded conditions, a significantly higher NH4+ was in U and NO3- was not affected by urea application. In general, AV losses were very small under the investigated experimental conditions and it varied from 0 to 2.72 % of added urea. Under saturated conditions, AV was significantly (p<0.05) higher in U (2.72 %) and BC_U (1.21 %) than in the Control (0 %). Under flooded conditions, only U showed a significant AV (2.42 %; p<0.05). The pH buffer capacity (11-12 mmols kg-1 pH-1) and urease activity (6.3 - 8.5 μg NH4+-N g-1 hr-1) did not significantly changed (p>0.05) by N treatments. Although there was a small AV loss (<3 %) after N application, it could be further reduced by application of urea as BC_U and/or maintaining a flood water layer for few days after N application.
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