Global climate change and agricultural practices have increased atmospheric nitrogen (N) deposition, significantly affecting the nitrogen cycling process in grasslands. The impact of different N forms on key soil enzyme activities involved in N nitrification, particularly in the saline‐alkali grasslands of the Hexi Corridor, using natural grassland as a control (CK) and adding three N treatments: inorganic N (IN), organic N (ON) and a mixed N treatment (MN, with a 4:6 ratio of organic to inorganic N). Our study assessed the effects of these N forms on soil properties and enzyme activities crucial for N cycling. The findings indicate that different N forms significantly enhance soil mineral N content, with ON treatment leading to the highest increases in nitrate and ammonium content 92.44% and 35.6%, respectively, compared to CK. Both IN and ON treatments significantly boosted soil nitrate reductase and urease activities (p < 0.05), while MN treatment decreased nitrate reductase activity, with ON treatment showing the greatest sensitivity to enzyme activity changes. Soil pH slightly increased with N addition, but soil nitrite reductase activity remained relatively unchanged (0.372–0.385 mg g−1). Correlation analysis revealed that soil mineral N content and pH are key regulators of enzyme activities in saline‐alkaline grasslands. These results suggest that different N forms should be considered in nutrient cycling models, with organic N addition potentially enhancing soil N conversion and mitigating nutrient limitations in grassland ecosystems.
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机译:全球气候变化和农业实践增加了大气中氮 (N) 的沉积,显著影响了草原的氮循环过程。以天然草地为对照 (CK) 并添加三种氮处理:无机氮 (IN)、有机氮 (ON) 和混合氮处理 (MN,有机氮与无机氮的比例为 4:6),研究了不同氮形式对参与氮硝化的关键土壤酶活性的影响,特别是在河西走廊的盐碱草原中。我们的研究评估了这些 N 形式对土壤特性和对 N 循环至关重要的酶活性的影响。结果表明,不同形式的氮素显著提高了土壤矿物氮含量,与 CK 相比,ON 处理导致硝态氮和铵态氮含量分别增加了 92.44% 和 35.6%。IN 和 ON 处理均显著提高土壤硝酸盐还原酶和脲酶活性 (p < 0.05),而 MN 处理降低了硝酸盐还原酶活性,其中 ON 处理对酶活性变化表现出最敏感。土壤 pH 值随着 N 的添加而略有增加,但土壤亚硝酸盐还原酶活性相对保持不变 (0.372–0.385 mg g-1)。相关性分析表明,土壤矿物氮含量和 pH 值是盐碱草地酶活性的关键调节因子。这些结果表明,在养分循环模型中应考虑不同的 N 形式,有机 N 添加可能会增强土壤 N 转化并减轻草地生态系统的养分限制。
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