Soil nitrogen dynamics on a saline-alkali sunflower land under arid region in Western Inner Mongolia

Liming Lai, Hanxiao Feng, Peng Zhang, Xueao Gao, Man Wang, Qiya Peng, Yang Yang, Haiwei Wang
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Abstract

Sunflower (Helianthus annuus L.), a dominant crop in Hetao Irrigation District, Western Inner Mongolia, is cultivated in arid and saline-alkaline fields due to their salt and alkali tolerance, ensuring that farmers’ income from these fields is not lower than those from fertile lands. However, little is known about the integrated analysis of nitrogen (N) dynamics, including soil total N (TN), nitrate (NO3), leachate TN and NO3, nitrous oxide (N2O) fluxes, and N cycling microbial gene abundance in sunflower fields. The specific objective was to explore N dynamics for 2021 through 2023 in sunflower seeded to saline-alkali croplands under arid condition based on treatments of irrigation rate (I rate: I1, 5110; I2, 4050; I3, 2985 m3 ha−1) for washing salinity by irrigation and nitrogen fertilization rate (N rate: N1, 750; N2, 600; N3, 450; N0, 0 kg ha−1). Our findings indicated that I rate did not affect soil N dynamics; N rate significantly increased soil TN, NO3 and N2O fluxes, especially showing an extremely significant increase for leachate TN and NO3 leachate. The interaction of I and N rates impacted soil TN, NO3, their leachate, and N cycling microbial gene abundances, especially denitrification genes. Soil leachate TN and NO3 increased exponentially over time. Soil N2O fluxes increased annually with the growth of sunflowers. In the saline-alkali sunflower fields, low N rate (450 kg ha −1) can be an optimal strategy, and the precise calibration of I and N rates can guarantee adequate N dynamics and yields, highlighting the intricate balance required for sustainable agricultural practices.

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内蒙古西部干旱区盐碱向日葵地土壤氮动态
向日葵(Helianthus annuus L.)是内蒙古西部河套灌区的优势作物,由于向日葵耐盐碱,因此在干旱盐碱地种植,确保了农民的收入不低于肥沃土地的收入。然而,对向日葵田土壤全氮(TN)、硝态氮(NO3−)、渗滤液TN和NO3−、氧化亚氮(N2O)通量和氮循环微生物基因丰度等氮素(N)动态的综合分析却知之甚少。具体目的是探讨干旱条件下向日葵种子盐碱地2021 - 2023年氮素动态变化,基于灌溉率(I率:I1, 5110;I2, 4050;I3, 2985 m3 ha−1)通过灌溉和施氮量(N: N1, 750;N2, 600;N3, 450;no, 0 kg ha−1)。结果表明,施氮量对土壤氮动态没有影响;施氮量显著增加了土壤TN、NO3−和N2O的通量,尤其显著增加了渗滤液TN和NO3−的通量。I和N的交互作用影响土壤TN、NO3−及其渗滤液和N循环微生物基因丰度,尤其是反硝化基因丰度。土壤渗滤液TN和NO3−随时间呈指数增长。随着向日葵的生长,土壤N2O通量逐年增加。在盐碱向日葵田,低施氮量(450 kg ha - 1)可能是一种最佳策略,精确校准I和N水平可以保证足够的N动态和产量,突出可持续农业实践所需的复杂平衡。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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