有机物料施用对西北内陆盐碱土气态氮损失的影响及机制
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1.南京信息工程大学;2.北京师范大学;3.中国科学院南京土壤研究所

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S156.4;S154.3

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Effects and Mechanisms of Organic Material Application on Gaseous Nitrogen Losses in Salt-Alkali Soils of Northwest Inland Areas
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1.Nanjing University of Information Science &2.Technology;3.Beijing Normal University;4.Nanjing University of Information Science Technology;5.Institute of Soil Science, Chinese Academy of Science

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    摘要:

    为探究有机物料对西北内陆盐碱土气态氮损失的影响及其可能机制,以新疆典型盐碱土为研究对象,通过室内培养试验,比较不同施用量的小麦秸秆、生物炭、腐殖酸及生物炭与腐殖酸配施对氧化亚氮(N2O)排放和氨气(NH3)挥发的影响,结合土壤理化性质、氮循环功能基因丰度及偏最小二乘结构方程模型(PLS-SEM)分析其关联因素。结果表明,与单施尿素相比,各有机物料处理的N2O累积排放量降低27.3%~85.7%,单一物料处理的NH3累积挥发量降低27.6%~82.4%。其中,小麦秸秆的协同减排效果最为突出,N2O和NH3分别减少82.4%~85.7%和77.8%~82.4%。增加施用量对各单一物料处理的N2O累积排放量均无显著影响,却使生物炭和腐殖酸处理的NH3累积挥发量显著增加。生物炭与腐殖酸配施的N2O减排效果与对应低量单施处理无显著差异,NH3累积挥发量则较单施尿素增加32.4%。小麦秸秆处理的脲酶活性显著降低,且脲酶活性与两种气体累积排放量均呈显著正相关。PLS-SEM显示,土壤氮库通过氮有效性与氮转化与两种气体排放呈显著正向间接关联,pH及氮循环微生物的总效应均未达到显著水平。综上,在本试验条件下,施用小麦秸秆可同步降低西北内陆盐碱土的N2O排放和NH3挥发,其协同减排效应可能与尿素水解及后续氮素转化过程的变化有关。生物炭和腐殖酸的应用则需综合考虑施用量与配施方式,统筹评估其对N2O排放和NH3挥发的影响。上述结果可为西北内陆盐碱土有机物料的合理施用提供参考,其实际应用效果仍有待田间试验进一步验证。

    Abstract:

    This study investigated the effects of organic amendments on gaseous nitrogen losses from inland saline-alkali soil in northwestern China and their potential mechanisms. A laboratory incubation experiment was conducted using a typical saline-alkali soil from Xinjiang to compare the effects of wheat straw, biochar, and humic acid at different application rates, as well as combined biochar and humic acid application, on nitrous oxide (N2O) emissions and ammonia (NH3) volatilization. Soil physicochemical properties, nitrogen-cycling functional gene abundances, and partial least squares structural equation modeling (PLS-SEM) were used to examine the associated factors. Compared with urea application alone, all organic amendment treatments reduced cumulative N2O emissions by 27.3%–85.7%, while individual amendments reduced cumulative NH3 volatilization by 27.6%–82.4%. Wheat straw achieved the greatest simultaneous reductions, decreasing N2O emissions and NH? volatilization by 82.4%–85.7% and 77.8%–82.4%, respectively. Increasing application rates did not significantly affect cumulative N2O emissions for any individual amendment but significantly increased cumulative NH3 volatilization under biochar and humic acid treatments. Combined biochar and humic acid application did not significantly improve N2O mitigation compared with the corresponding individual amendments at low application rates and increased cumulative NH3 volatilization by 32.4% relative to urea alone. Wheat straw significantly decreased soil urease activity, which was significantly positively correlated with the cumulative losses of both gases. PLS-SEM indicated that soil nitrogen pools had significant positive indirect associations with both gas losses through nitrogen availability and transformation, whereas the total effects of pH and nitrogen-cycling microorganisms were not significant. In conclusion, under the experimental conditions, wheat straw application simultaneously reduced N2O emissions and NH3 volatilization from inland saline-alkali soil in northwestern China. This mitigation effect may be associated with changes in urea hydrolysis and subsequent nitrogen transformations. The use of biochar and humic acid requires consideration of application rates and amendment combinations, together with a joint assessment of their effects on N2O emissions and NH3 volatilization. These findings provide a reference for the appropriate use of organic amendments in inland saline-alkali soils in northwestern China, although their effectiveness under field conditions requires further verification.

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  • 收稿日期:2026-09-08
  • 最后修改日期:2026-10-17
  • 录用日期:2026-10-21
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