增施有机肥对长期微咸水补灌下土壤理化性质与作物产量的影响

Effects of applying manure on soil physical properties and crop yield under long-term saline water irrigation

  • 摘要: 环渤海低平原淡水资源短缺, 微咸水资源丰富, 长期微咸水补灌, 造成土壤盐分积累和土壤理化性状变差, 制约区域农业可持续发展。本研究依托环渤海低平原南皮试验站冬小麦-夏玉米一年两熟微咸水补灌定位试验(2015—2024), 设置小麦播期增施有机肥试验, 常规施肥作为对照。共4个灌水处理, 分别为: 在冬小麦底墒充足条件下, 在拔节期分别用3、4和5 g·L–1微咸水补灌, 矿化度1 g·L–1淡水灌溉作为对照。所有处理夏玉米播种用淡水灌溉出苗水。结果表明, 微咸水长期灌溉条件下施用有机肥后, 0~20 cm土壤有机质、有效钾、有效磷和全氮含量比不施有机肥处理分别提高46.8%、117.0%、75.7%和45.5%, 显著提高了土壤肥力; 施用有机肥降低了长期微咸水灌溉下耕层土壤容重, 提高了土壤水稳定性团聚体比例, 土壤理化性状得到改善。施用有机肥可显著提高耕层土壤微生物中细菌、真菌和放线菌3大菌群的数量, 比不施有机肥处理平均提高73.8%。由于有机肥本身的含盐量, 在冬小麦收获期, 施用有机肥处理0~40 cm、40~100 cm、100~200 cm土壤含盐量高于不施用有机肥处理, 至夏玉米收获期施用有机肥处理的土壤各层盐分含量仍高于不施有机肥处理, 但差异不显著。施用有机肥改善了土壤结构提高了雨季土壤的脱盐率, 在夏玉米收获期, 有机肥处理0~40 cm、40~100 cm和100~200 cm的脱盐率分别比不施用有机肥提高34.3%, 14.7%和20.4%, 尤其是0~40 cm土层脱盐率的提升为作物生长提供了低盐环境。长期微咸水灌溉下施用有机肥带来的小麦季土壤盐分增加使冬小麦产量平均减产0.12%, 但土壤肥力提高使夏玉米产量平均增加3.9%, 两季作物的产量变化均未达到显著水平。上述结果显示, 长期微咸水灌溉条件下增施有机肥可以有效提升土壤有机质含量, 维持土壤结构, 利于土壤脱盐, 生产上可选择含盐量低的有机肥或者减少有机肥的施用量, 在缓解长期微咸水灌溉对土壤物理性状不利影响下, 降低有机肥施用带来的盐分增加, 推动微咸水安全可持续利用。

     

    Abstract: To maintain soil quality under long-term saline water irrigation, the influence of manure on soil physical properties was examined. Long-term saline irrigation has been conducted from 2015 to 2024 at the Nanpi Experimental Station in the Low Plain of the North China Plain, comprising four irrigation treatments: irrigation once at the jointing stage for winter wheat with irrigation water containing salt at 1 g·L–1 (fresh water), 3, 4 and 5 g·L–1, and maize irrigation at sowing using fresh water. Manure application was conducted under all irrigation treatments, with treatments without manure application used as controls. The results showed that under long-term irrigation with saline water, the application of manure increased the soil organic matter content, exchangeable potassium, available phosphorus, and total nitrogen content in the 0–20 cm soil layer by 46.8%, 117.0%, 75.7%, and 45.5%, respectively, compared to treatments without manure application. The application of manure reduced soil bulk density. It also increased the proportion of water-stable aggregates and the abundance of bacteria, fungi, and actinomycetes in the tillage soil layer compared to the controls. Because of the salt contained in the manure, the application of manure had dual effects on soil salt content. During the winter wheat season, manure application increased soil salt content. The salt content was significantly reduced during the summer maize season, owing to the strong salt-leaching effects under manure application, resulting in a smaller difference in salt content between the manure and non-manure treatments. During the summer rainfall season, improvements in soil structure under manure application increased the soil desalination rate by 38.3%, 14.7%, and 21.3% compared to the no-manure treatments in the 0–40 cm, 40–100 cm, and 100–200 cm soil layers, respectively. The yield of winter wheat under manure application was slightly lower than that of the control, owing to the higher salt content during the winter wheat season. In contrast, the yield of summer maize improved by 3.9% under manure application, owing to the increased soil nutrient content and effective salt leaching. The annual yields of winter wheat and summer maize were similar for saline and freshwater irrigation treatments. The results of this study indicated that manure application helped maintain the soil physical structure, which is important for the long-term use of saline water. In practice, using manure with a low salt content is suggested to reduce the adverse effects of saline water irrigation on soil properties and achieve sustainable saline water use.

     

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