中国农业科学 ›› 2025, Vol. 58 ›› Issue (14): 2805-2820.doi: 10.3864/j.issn.0578-1752.2025.14.008

• 土壤肥料·节水灌溉·农业生态环境 • 上一篇    下一篇

长期不同施肥对潮土磷吸附解吸特性的影响

郭斗斗1,2(), 张珂珂1,2, 黄绍敏1,2,*(), 宋晓1,2, 张水清1,2, 岳克1,2, 丁世杰1,2, 郭腾飞1,2   

  1. 1 河南省农业科学院植物营养与资源环境研究所,郑州 450002
    2 北京昌平土壤质量国家野外科学观测研究站,北京 100086
  • 收稿日期:2024-09-13 接受日期:2025-02-09 出版日期:2025-07-17 发布日期:2025-07-17
  • 通信作者:
    黄绍敏,E-mail:
  • 联系方式: 郭斗斗,E-mail:guodoudou_822@163.com。
  • 基金资助:
    科技基础资源调查专项(2021FY100503); 2024年河南省农业科学院自主创新项目(2024ZC055); 2023年度河南省科技攻关项目(232102111021)

Effects of Long-Term Fertilization on Phosphorus Adsorption and Desorption Characteristics of Fluvo-Aquic Soils

GUO DouDou1,2(), ZHANG KeKe1,2, HUANG ShaoMin1,2,*(), SONG Xiao1,2, ZHANG ShuiQing1,2, YUE Ke1,2, DING ShiJie1,2, GUO TengFei1,2   

  1. 1 Institute of Plant Nutrient and Environmental Resources, Henan Academy of Agricultural Sciences, Zhengzhou 450002
    2 Beijing Changping Soil Quality National Observation and Research Station, Beijing 100086
  • Received:2024-09-13 Accepted:2025-02-09 Published:2025-07-17 Online:2025-07-17

摘要:

【目的】通过长期试验分析施肥对潮土磷素吸附-解吸特性的作用,揭示不同施肥措施如何影响磷素有效性,以期为磷素的高效利用提供理论依据。【方法】基于“国家潮土肥力与肥料效益长期定位试验基地”,对连续试验31年的7个典型施肥处理(只施氮肥(N2)、只施氮钾肥(N2K)、低量氮肥+磷钾肥(N1PK)、中量氮肥+磷钾肥(N2PK)、高量氮肥+磷钾肥(N4PK)、氮磷钾肥+有机肥(N2PK+M)、氮磷钾肥+玉米秸秆还田(N2PK+S))的土壤进行等温吸附-解吸试验,通过Langmuir方程分析施肥对磷素吸附-解吸特性参数的影响,并用冗余分析(RDA)中的层次分割(HP)模型量化土壤理化属性对关键参数的影响程度。【结果】随外源磷量增加,土壤磷吸附量上升而吸附率下降。只施化肥处理土壤磷吸附率(Ar)高于有机无机配施处理。吸附亲和力常数(Ka)以不施磷肥处理最高,长期化肥处理次之,有机无机配施处理最低。土壤最大吸附磷量(Qm)和最大缓冲容量(MBC)均以N2PK处理最高,与之相比,N2PK+M、N2PK+S、N2和N2K处理的Qm分别减少13.7%、16.0%、22.8%和21.5%,以无磷处理最低;MBC分别减少26.8%、28.4%、15.6%和11.7%,以有机无机配施处理最低。N2PK+M处理磷素吸附饱和度(DPS)达到21.3%,显著高于其他处理,其次为N4PK和N2PK+S处理。磷解吸量随溶液磷浓度的增加而上升,解吸率则下降。N2PK+M处理的磷解吸能力远高于其他处理,其最大解吸磷量(Dm)、解吸率(Dr)和易解吸磷量(RDP)均最高。N2K处理Dm值最低,而N1PK处理Dr和RDP值最低。基于层次分割模型的理化因子排序结果显示,TP、Olsen-P、ExCa、CaCO3和SOM是影响磷吸附参数的前5个因素,贡献率分别为18.0%、16.0%、12.6%、11.4%和8.8%;Olsen-P、TN、ExCa、SOM和AN是影响磷解吸参数的前5个因素,贡献率分别为17.9%、12.9%、12.6%、9.8%和9.0%。【结论】长期只施氮磷钾化肥提高了潮土磷吸附强度,降低了磷素解吸能力,且氮磷比低的土壤解磷能力更低;添加有机肥可降低磷吸附能力并提高解吸能力,但过量施用可能导致磷素流失;添加秸秆可降低土壤吸磷能力,是提高磷素活性的有效措施。土壤有效磷和交换性钙是影响潮土磷吸附解吸特征的主要因素。此外,全磷的增加有助于降低磷吸附能力,而全氮的增加有助于提升磷解吸能力。

关键词: 长期施肥, 潮土, 磷吸附解吸, 层次分割模型

Abstract:

【Objective】Through long-term experiments, this study analyzed the effects of fertilization on the phosphorus adsorption-desorption characteristics in fluvo-aquic soils, aiming to reveal how different fertilization practices influence phosphorus availability and provide a theoretical basis for the efficient use of phosphorus. 【Method】Based on the "National Long-term Monitoring Station of Fluvo-aquic Soil Fertility and Fertilizer Effects", the isothermal adsorption-desorption experiments were conducted on soils under seven typical fertilization treatments over a continuous 31-year period. These treatments included: only nitrogen fertilizer (N2), only nitrogen and potassium fertilizers (N2K), low nitrogen fertilizer+phosphorus and potassium fertilizers (N1PK), medium nitrogen fertilizer+phosphorus and potassium fertilizers (N2PK), high nitrogen fertilizer+phosphorus and potassium fertilizers (N4PK), nitrogen, phosphorus, and potassium fertilizers+organic fertilizer (N2PK+M), and nitrogen, phosphorus, and potassium fertilizers+maize straw return (N2PK+S). The Langmuir equation was used to analyze the impacts of fertilization on phosphorus adsorption-desorption characteristics, and the Hierarchical Partitioning (HP) Model in redundancy analysis (RDA) was employed to quantify the influence of soil physicochemical properties on key parameters. 【Result】As the external phosphorus amount increased, the amount of phosphorus adsorbed by the soil increased, but the adsorption rate decreased. Soils with only chemical fertilizers had higher phosphorus adsorption rates (Ar) compared with those with combined organic and inorganic fertilizers. Soils without phosphorus fertilization had the highest adsorption affinity constant (Ka), followed by soils with long-term chemical fertilization, and the lowest in soils with organic-inorganic combined fertilization. The maximum phosphorus adsorption capacity (Qm) and maximum buffering capacity (MBC) were the highest under N2PK treatment. In comparison, Qm decreased by 13.7%, 16.0%, 22.8%, and 21.5% under N2PK+M, N2PK+S, N2, and N2K treatments, respectively, with the lowest value observed in the no-phosphorus treatment; MBC decreased by 26.8%, 28.4%, 15.6%, and 11.7% in the same treatments, respectively, with the lowest value found in the organic-inorganic combined fertilization treatment. The degree of phosphorus saturation (DPS) under N2PK+M treatment reached 21.3%, significantly higher than other treatments, followed by the N4PK and N2PK+S treatments. During the phosphorus desorption process, the amount of desorbed phosphorus increased with the increase in solution phosphorus concentration, while the desorption rate decreased. The phosphorus desorption capacity under N2PK+M treatment was significantly higher than that under other treatments, with the highest maximum phosphorus desorption amount (Dm), desorption rate (Dr), and readily desorption phosphorus (RDP). The N2K treatment had the lowest Dm value, while the N1PK treatment had the lowest Dr and RDP values. The results of physicochemical factor ranking based on the HP model show that TP, Olsen-P, ExCa, CaCO3, and SOM were the top five factors influencing phosphorus adsorption parameters, with contribution rates of 18.0%, 16.0%, 12.6%, 11.4%, and 8.8%, respectively. Olsen-P, TN, ExCa, SOM, and AN are the top five factors influencing phosphorus desorption parameters, with contribution rates of 17.9%, 12.9%, 12.6%, 9.8%, and 9.0%, respectively. 【Conclusion】Long-term application of nitrogen, phosphorus, and potassium fertilizers increased soil phosphorus adsorption intensity and reduced phosphorus desorption capacity of fluvo-aquic soils, and soils with a lower nitrogen-to-phosphorus ratio showed even lower phosphorus desorption capacity. The addition of organic fertilizers could reduce phosphorus adsorption capacity and enhance desorption ability, although excessive application organic fertilizers might lead to phosphorus loss. The combination of chemical fertilizers and straw return could reduce soil phosphorus adsorption capacity, which was an effective measure to enhance phosphorus activity in fluvo-aquic soil. Olsen-P and ExCa were the primary factors determining the phosphorus adsorption-desorption characteristics of fluvo-aquic soil. Additionally, an increase in total phosphorus helped reduce phosphorus adsorption capacity, while an increase in total nitrogen contributed to enhancing phosphorus desorption capacity.

Key words: long-term fertilization, fluvo-aquic soils, phosphorus adsorption and desorption, Hierarchical Partitioning Model