覆膜及秸秆还田对黄土高原旱地麦田根区土壤不稳定氮库、酶及氨挥发的影响

Effects of film mulching and straw return on soil labile nitrogen pool, enzymes and ammonia volatilization in the root zone of winter wheat in the drylands on the Loess Plateau

  • 摘要: 地膜覆盖和秸秆还田是目前旱区普遍使用的保护性耕作措施。本文通过田间试验研究地膜覆盖及秸秆还田条件下冬小麦根区土壤不稳定氮库和土壤酶活性对氨挥发的影响。本试验于2017年在西北农林科技大学曹新庄试验农场开展, 采用裂区试验设计, 主区为常规耕作、秸秆还田和地膜覆盖, 副区为不施氮、常规施氮和减氮20%。在第5季冬小麦播种后42、166、194和217天, 采集0~20 cm土层小麦根区土, 测定土壤硝铵态氮含量、微生物生物量氮含量、硝酸还原酶活性、羟胺还原酶活性和脲酶活性, 分析氨挥发对耕作方式、土壤不稳定氮库和土壤酶的响应。结果表明: 施氮可以显著提高土壤不稳定氮库含量、土壤酶活性和土壤氨挥发。地膜覆盖施氮处理小麦全季氨挥发累积量(6.41~7.38 kg·hm−2)显著低于相同施氮水平的秸秆还田(8.37~9.45 kg·hm−2)和常规耕作处理(8.81~11.06 kg·hm−2) (P<0.05)。在冬前分蘖期和返青拔节期, 秸秆还田施氮处理下土壤微生物生物量氮含量显著高于常规耕作和地膜覆盖处理(P<0.05)。秸秆还田处理下, 土壤氨挥发累积量与土壤铵态氮含量、微生物生物量氮含量和脲酶活性呈显著或极显著正相关(P<0.05或P<0.01或P<0.001)。地膜覆盖处理下, 土壤氨挥发累积量与土壤铵态氮含量、微生物生物量氮含量、羟胺还原酶活性和脲酶活性均呈极显著正相关(P<0.01或P<0.001)。在减氮20%处理下, 与常规耕作相比, 地膜覆盖能够在显著减少全生育期氨挥发累积量的同时, 显著提高冬前分蘖期土壤微生物生物量氮含量, 在本研究区旱地冬小麦种植中具有一定优势。本研究结果可为后续黄土高原旱地冬小麦氮肥利用率提高和氨挥发损失减少提供理论支撑。

     

    Abstract: Film mulching and straw return are common conservation tillage measures in arid regions. A field experiment was conducted to investigate the changes in soil labile nitrogen pools and soil enzyme activities, as well as ammonia volatilization, in the root zone soil of winter wheat under film mulching and straw return. The experiment was conducted at the Caoxinzhuang Experimental Farm of Northwest A&F University starting from 2017. A split-zone experimental design was used. The main zones were conventional cultivation, straw return, and film mulching, while the secondary zones were no nitrogen application, conventional nitrogen application, and 20% reduction in nitrogen application rate. Wheat root zone soil (0–20 cm) was collected 42, 166, 194, and 217 days after winter wheat sowing in the fifth season, to determine contents of soil nitrate nitrogen, ammonium nitrogen, and microbial biomass nitrogen, and activities of soil nitrate reductase, hydroxylamine reductase, and urease. Ammonia volatilization from agricultural soils was also measured during the wheat season to analyze the response of ammonia volatilization to cultivation patterns, soil labile N pools, and soil enzymes. The results showed that nitrogen application could increase the liable soil nitrogen pool, soil enzyme activities, and ammonia volatilization. For the nitrogen application treatments, ammonia volatilization accumulation in wheat season was significantly lower (P<0.05) under the film mulching treatment (6.41−7.38 kg·hm−2) than under the straw return (8.37−9.45 kg·hm−2) and conventional cultivation treatments (8.81−11.06 kg·hm−2) with identical fertilization levels. During the pre-winter tillering, and the reviving and jointing periods, the microbial biomass nitrogen content was significantly higher (P<0.05) under the straw return treatment than under the conventional cultivation and film mulching treatments. Soil accumulative ammonia emissions was found to have a significant positive correlation with soil ammonium nitrogen content, microbial biomass nitrogen content, and urease activity under the straw return treatment (P<0.05 or P<0.01 or P<0.001). It also had a significant positive correlation with soil ammonium nitrogen content, microbial biomass nitrogen content, hydroxylamine reductase activity, and urease activity under the film mulching treatment (P<0.01 or P<0.001). Under the 20% nitrogen reduction treatment, compared to conventaional cultivation, film mulching significantly reduced accumulative ammonia emissions througout the wohle growth period, and significantly increased soil microbial biomass nitrogen content at pre-winter tillering period, which is feasible for local winter wheat cultivation. This study provides theoretical support for reducing ammonia volatilization losses and improving the utilization rate of nitrogen fertilizers in the drylands on the Loess Plateau.

     

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