三种FeSO4还原碱解体系在扩散法测定土壤有效氮中的应用
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作者单位:

1.农业农村部耕地质量监测与评价重点实验室(扬州大学),江苏 扬州 225127 ;2.江苏省有机固体废弃物资源化协同创新中心,江苏 南京 210095

作者简介:

汪晓丽(1977-),副教授,博士,主要从事植物营养生理和土壤农化分析的教学与研究。E-mail:xlwang@yzu.edu.cn。

通讯作者:

汪晓丽(1977-),副教授,博士,主要从事植物营养生理和土壤农化分析的教学与研究。E-mail:xlwang@yzu.edu.cn。

基金项目:

江苏省农业科技自主创新资金项目(CX203082);土壤与农业可持续发展国家重点实验室开放项目(Y20160017)


Applicability of FeSO4 reductant system in the determination of soil available nitrogen with the modified Conway’s diffusion method
Author:
Affiliation:

1.KeyLaboratory of Arable Land Quality Monitoring and Evaluation of the Ministry of Agriculture and Rural Affairs,YangzhouUniversity,Yangzhou Jiangsu 225127 ;2.Jiangsu Collaborative Innovation Center for Solid Organic Waste ResourcesUtilization,Nanjing Jiangsu 210095

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    摘要:

    还原碱解扩散法是测定旱地土壤有效氮的常规方法,建立和选择合适的还原碱解体系可提高测定结果的可靠性。通过土样实际测定和加标回收实验,比较了当前普遍应用的 3 种 FeSO4 还原碱解体系对土壤 NO3 - -N 的还原能力,并探讨了其在土壤有效氮测定中的适用性,旨在为土壤农化分析工作中有效氮测定方法的研究和应用提供参考。结果表明:供试土样的还原碱解氮测定值均以 0.2 g-Fe 体系(0.20 g FeSO4·7H2O + 1.14 mol/L NaOH)最低,1 g-Fe 体系(1.00 g FeSO4·7H2O + 1.68 mol/L NaOH)居中,1 g-ZnFe 体系(0.17 g Zn + 0.83 g FeSO4·7H2O + 1.55 mol/L NaOH)最高。与对照(CK,无还原剂 +1.00 mol/L NaOH)相比,0.2 g-Fe、1 g-Fe 和 1 g-ZnFe 分别使测定值增加了 6.9 ~ 14.0、8.9 ~ 77.6 和 10.2 ~ 169.5 mg/kg。3 种还原碱解体系的 NO3 - -N 还原率随加标量的增加而降低,且呈较好的幂函数关系。以回收率 90% 计,0.2 g-Fe、1 g-Fe 和 1 g-ZnFe 在空白加标实验中可分别还原 26.6、57.8 和 203.5 μg NO3 - -N,在样品加标实验中则分别为 29.0、50.3 和 153.2?μg。由于有土样时的 NO3 - -N 还原率低于无土样时,在进行土样实际测定时很可能会低于此估算值。相较于其他两种还原碱解体系,1 g-ZnFe 具有更强的 NO3 - -N 还原能力,更适用于当前的一般旱地农田土壤。在土壤 NO3 - -N 丰富时,不建议采用还原碱解法测定土壤有效氮。鉴于碱解氮和 NO3 - -N 具有不同的土壤肥料学意义,建议分别测定两者以从不同角度综合反映土壤供氮能力。

    Abstract:

    As a conventional method to determine available nitrogen in dryland soils,the modified Conway’s diffusion method should establish and optimize the conditions of alkali hydrolysis and reduction to ensure reliability of determination results. Nitrate reducing capacity and practical applicability of three common-used FeSO4 reduction systems were compared through soil sample tests and recovery tests,aimed to provide reference for available nitrogen determination methods in the of soil agrochemical analysis. The measured results of available nitrogen in 11 soil samples indicated that 0.2 g-Fe system (0.20 g FeSO4·7H2O and 1.14 mol/L NaOH)was the lowest,1 g-Fe system(1.00 g FeSO4·7H2O and 1.68 mol/L NaOH) was middle and 1 g-ZnFe system(0.17 g Zn,0.83 g FeSO4·7H2O and 1.55 mol/L NaOH)was the highest. Compared with CK(no reductant and with 1.00 mol/L NaOH),0.2 g-Fe,1 g-Fe and 1 g-ZnFe systems increased the measured results by 6.9-14.0,8.9-77.6 and 10.2-169.5 mg/kg,respectively. The reduction rate of nitrate nitrogen declined with the increase of spiked level and gave a good power function relationship. Based on a recovery rate of 90%,0.2 g-Fe,1 g-Fe and 1 g-ZnFe systems respectively reduced 26.6,57.8 and 203.5μg NO3 - -N in the blank spike test,while 29.0,50.3 and 153.2μg in the matrix spike test,respectively. For lower reduction rate in the actual soil sample measurement,these values were likely to be overestimating. With higher efficiency of NO3 - -N reduction and wider range of application than 0.2 g-Fe and 1 g-Fe,1 g-ZnFe was more suitable for current farmland soils. Nevertheless,when a large amount of nitrate accumulated in soils,all of the three FeSO4 reduction systems were not applicable. For alkaline-hydrolyzed nitrogen has a different significance from NO3 - -N in soil and fertilizer science,it was recommended to separately measure alkaline-hydrolyzed nitrogen and NO3 - -N in soil and further to integrate both as indicators of soil nitrogen supply capacity.

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汪晓丽,陈博文,李静怡,陆清泉,盛海君,王小兵.三种FeSO4还原碱解体系在扩散法测定土壤有效氮中的应用[J].中国土壤与肥料,2025,(5):239-247.

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  • 收稿日期:2024-08-29
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  • 录用日期:2024-10-19
  • 在线发布日期: 2025-07-16