首页|期刊导航|植物营养与肥料学报|黄土高原旱地苹果园土壤硝态氮剖面特征及氮肥优化管理

黄土高原旱地苹果园土壤硝态氮剖面特征及氮肥优化管理OA

Vertical distribution of soil nitrate and optimized nitrogen management in rainfed apple orchards on the Loess Plateau

中文摘要英文摘要

[目的]研究过量施氮下苹果园土壤深剖面氮素特征,旨在为黄土高原旱地苹果园氮肥管理的靶向优化提供依据.[方法]以黄土高原苹果主产区土壤硝态氮为研究对象,通过文献数据整理、实地土壤样品采集与室内分析,明晰旱地苹果园 0-600 cm 剖面土壤硝态氮分布特征;基于回归分析,明确黄土高原不同产区苹果园氮肥适宜用量及减氮潜力;采用情景分析,预测不同管理模式下苹果园土壤剖面硝态氮累积量的发展趋势.[结果]黄土高原苹果主产区东部、南部、西部、北部和中部区域苹果园土壤剖面硝态氮累积量主要受施氮量调控;0-600 cm 剖面硝态氮浓度及累积量均表现为随树龄增大而增加的趋势;苹果园土壤硝态氮稳态深度(农田与果园硝态氮含量差异不显著的土层深度)随树龄增大而增加,最大深度为 540 cm,表明采用 600 cm 剖面揭示黄土高原旱地苹果园土壤硝态氮分布特征是可行的.以 25 年生苹果园为例,北部、东部、南部、西部和中部产区土壤硝态氮(NO3--N)累积量分别高达 4230、7210、6975、12740 和 8760 kg/hm2.旱地苹果园 100-400 cm 土层硝态氮累积量占整个 0-600 cm 剖面硝态氮累积量的比例均超过 50%,且硝态氮累积量随树龄增大而增加,与降雨量呈显著负相关,说明苹果种植时间越长和降雨量越大,硝态氮越容易淋洗至 100 cm 以下土层.0-40 cm土层硝态氮平均含量与0-600 cm土层硝态氮平均含量呈显著正相关,说明0-40 cm土层硝态氮含量对果园氮素供应能力有较好的指示性作用.幼树期(0~4 年)、初果期—盛果初期(5~10 年)、盛果初期—盛果期(11~17 年)、盛果期—衰老期(≥18 年)推荐施氮量分别是 135、270~390、390~420 和 420 kg/hm2;整合分析表明,黄土高原 17~30 年生苹果园具有 2~8 年不施氮而不减产的减氮潜力.果园重建和果树不砍伐模式下,农户传统施氮量进一步加剧剖面硝态氮累积,推荐施氮量下可基本维持原有氮素累积水平;土壤残留氮再利用+推荐施氮模式下,氮素累积量可降低并稳定在 17 年生果园水平.洛川县和礼泉县两个典型雨养苹果种植区地下水硝态氮含量均低于世界卫生组织(WHO)饮用水标准(11.9 mg/L),表明旱地苹果园土壤剖面虽然氮素盈余累积量较高,但当前对地下水污染风险相对较小.[结论]长期过量施氮导致黄土高原旱地苹果园土壤硝态氮大量盈余累积,可能诱发土壤酸化、地下水硝态氮潜在污染风险以及温室气体排放等问题.未来研究应重点关注黄土高原苹果园深土剖面残留硝态氮的再利用途径和调控机制.

[Objectives]A comprehensive understanding of soil nitrogen(N)characteristics at a deep-profile scale under long-term excessive N-fertilization is crucial for developing targeted N-fertilization regimes in apple production systems.[Methods]This study was conducted in rainfed apple-producing regions of the Loess Plateau.The objectives were:1)to clarify the vertical characteristics of soil nitrate nitrogen(NO3--N)in the 6-m profile by integrating literature data with field soil sampling and measurement;2)to identify appropriate N application rates and N reduction potential for different apple-planting regions of the Loess Plateau using regression analysis;and 3)to predict the accumulation trend of residual soil NO3--N in the 6-m profile(RSN6-m)under different scenarios.[Results]Across the eastern,southern,western,northern,and central regions of the Loess Plateau,RSN6-m was mainly regulated by fertilizer N application.Both NO3--N concentrations and RSN6-m showed an increasing trend with apple tree age.The stabilized depth of soil NO3--N—defined as the soil depth at which NO3--N contents no longer differ significantly between farmland and orchards—deepened with increasing tree age and reached a maximum of 540 cm,indicating that a 6-m profile is robust for evaluating vertical NO3--N patterns in rainfed apple orchards on the Loess Plateau.For 25-year-old apple orchards,RSN6-m in the northern,eastern,southern,western,and central apple-planting regions reached 4230,7210,6975,12740,and 8760 kg/hm2,respectively.Nitrate accumulation in the 1-4 m soil layer exceeded 50%of RSN6-m,with this proportion increasing with tree age but decreasing with increasing rainfall,indicating that longer apple-planting duration and higher rainfall accelerate NO3--N leaching into soils deeper than 1 m.A significant positive relationship was observed between average NO3--N contents in the 0-40 cm and 0-600 cm soil layers,indicating that soil NO3--N in the 0-40 cm layer can serve as a reliable indicator of orchard soil N supply.The recommended nitrogen application rates for the young-tree stage(0-4 years),initial-fruiting to early full-fruiting stage(5-10 years),early full-fruiting to full-fruiting stage(11-17 years),and full-fruiting to senescent stage(≥18 years)were 135,270-390,390-420,and 420 kg/hm2,respectively.Integrated analysis indicated that apple orchards aged 17-30 years possess a reduction potential of 2-8 years without N fertilizer application while maintaining yield.Under both orchard reconstruction and tree-retention scenarios,conventional farmer N application rates exacerbated RSN6-m accumulation,whereas recommended N-fertilization regimes potentially maintained RSN6-m at current levels.Combining residual soil NO3--N reuse with recommended N application rate can reduce RSN6-m and maintain it at the level observed in 17-year-old orchards.Groundwater NO3--N contents in two typical rainfed apple-planting regions of Luochuan and Liquan Counties were lower than the World Health Organization(WHO)limit of 11.9 mg/L,indicating a relatively low groundwater NO3--pollution risk despite a surplus of NO3--N being observed.[Conclusions]Long-term excessive N application caused a massive surplus of soil NO3--N,subsequently resulting in soil acidification,NO3--pollution risk of groundwater,and greenhouse gas emissions,ultimately leading to increasingly severe problems of soil degradation and environmental pollution in the rainfed production system on the Loess Plateau.Future research should prioritize strategies for the effective reuse of residual soil NO3--N in deep profiles of apple orchards on the Loess Plateau.

刘占军;翟丙年;王朝辉;徐新朋;雷秋良;樊庆鲁

新疆农垦科学院,新疆石河子 832000||作物抗逆与高效生产全国重点实验室/西北农林科技大学,陕西 杨凌 712100作物抗逆与高效生产全国重点实验室/西北农林科技大学,陕西 杨凌 712100作物抗逆与高效生产全国重点实验室/西北农林科技大学,陕西 杨凌 712100中国农业科学院农业资源与农业区划研究所,北京 100081中国农业科学院农业资源与农业区划研究所,北京 100081新疆农垦科学院,新疆石河子 832000

苹果园深土剖面硝态氮氮肥管理

apple orcharddeep soil profilenitrate nitrogennitrogen fertilizer management

《植物营养与肥料学报》 2026 (6)

1226-1238,13

财政部和农业农村部—国家现代农业产业技术体系项目(CARS-27)陕西省科技重大专项(2020zdzx03-02-01)中煤地华盛水文地质勘察有限公司科技项目(20250424).

10.11674/zwyf.2025459

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