土壤有机质和pH对Olsen法测定有效磷的影响
作者:
作者单位:

1.北京林业大学森林培育与保护教育部重点实验室,北京 100083 ;2.北京山水云图科技有限公司,北京 100089 ;3.农业农村部耕地质量监测与保护中心,北京 100081

作者简介:

王登芝(1973-),博士,高级实验师,从事土壤与植物营养研究。E-mail:wangdengzhi_2002@sina.com。

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基金项目:

北京林业大学“卓越实验师”培育专项基金(BJFUSY20230005);鄂尔多斯市科技合作重大专项(2021EEDSCXQDFZ012)


Determination of available phosphorus by Olsen method as influenced by soil organic matter and pH
Author:
Affiliation:

1.The Key Laboratory for Silvicultureand Conservation of Ministry of Education,College of Forestry,Beijing Forestry University,Beijing 100083 ;2.BeijingShanshui Yuntu Technology Co.,Ltd.,Beijing 100089 ;3.Cultivated Land Quality Monitoring and Protection Center,Ministry of Agriculture and Rural Affairs,Beijing 100081

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    摘要:

    Olsen 法是测定中性、石灰性土壤有效磷最常用的分析方法。该方法需用无磷活性炭脱去有机质颜色和用 2,4- 硝基酚或对硝基酚酸碱指示剂调节溶液酸度,这使得操作步骤繁琐而耗时,危险试剂使用易污染环境。以 Olsen 法为基础,采用钼蓝-抗坏血酸分光光度法测定两种国家认证标准土壤样品和采自中国北方和西北地区 15 种不同土壤类型的农业表层土壤样品的有效磷(Olsen-P)含量,其中钼锑抗显色剂中含有 5.5 mol/L(H+ )H2SO4、 10 g/L 钼酸铵、0.5 g/L 酒石酸锑钾和 15 g/L 抗坏血酸。采用标准曲线中添加有机质(腐植酸)和指示剂调节溶液酸度对磷(P)标准曲线的影响研究,在此基础上研究活性碳和指示剂对土壤样品 Olsen-P 测定结果的影响。结果表明,在土壤有机质含量低于 45.6 g/kg 和 pH 在 6.69 ~ 9.07 范围内,不使用无磷活性炭脱去有机质颜色和不用指示剂调节溶液酸度对 Olsen-P 的测量结果没有显著影响,相对误差在 -10.9% ~ 8.3%,并且与常规方法测定结果具有良好的线性相关关系(y=1.0006x,R2 =0.9994)。因此,土壤有机质含量和 pH 在一定范围对 Olsen-P 的测量结果没有显著影响,并且作为干扰因素被消除,同时优化了 Olsen 法使其测定有效磷更加准确、高效和环保,从而更好地满足农业和其他行业对土壤有效磷测定的要求。

    Abstract:

    The most widely used method for determination of available phosphorous(P)in neutral,calcareous and alkaline soils was Olsen method. It was cumbersome operation by using activated carbon to remove organic matter color and indicator (2,4-Nitrophenol or p-nitrophenolic acid)to adjust acidity. In this study,available P of two national certified standard soils and agricultural topsoil samples of fifteen different soil types chose from northern and northwestern China were determined by Olsen method,base on molybdenum blue-ascorbic acid,in which contained 5.5 mol/L(H+ )H2SO4, 10 g/L ammonium molybdate,0.5 g/L potassium antimony tartrate and 15 g/L ascorbic acid. Adding organic matter(humic acid)and adjusting acidity had little effect on the result of P standard curve,and on the basis of this,the experiments were conducted to investigate the influences of whether adding AC0 and adjusting acidity on the results of measuring Olsen-P in soil samples. The results demonstrated that whether using AC0 to remove organic matter color and indicator to adjust the acidity of solution had no influence on the measurement results of Olsen-P with soil organic matter content below 45.6 g/kg and pH range of 6.69-9.07. The relative error was between -10.9%-8.3%,and had a good relationship(y=1.0006x,R2 =0.9994)with the conventional method. So organic matter and pH of soils had no significant effect on the measurement results of Olsen-P,and which as interference factors were eliminated. It simultaneously showed Olsen-P method was optimized with convenient and environmentally friendly,and could better meet the requirements of agriculture and other industries for determination of soil available phosphorus.

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王登芝,任忠秀,李寒,薛思远,栾亚宁.土壤有机质和pH对Olsen法测定有效磷的影响[J].中国土壤与肥料,2025,(5):248-254.

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  • 收稿日期:2024-09-03
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  • 录用日期:2024-11-24
  • 在线发布日期: 2025-07-16