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Comparison of Bray-1 and Mehlich-3 tests in high phosphorus soils

机译:高磷土壤中Bray-1和Mehlich-3试验的比较

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Soil testing forms the basis for both agronomic recommendations and phosphorus (P) runoff risk assessment. Although several studies point to good linear correlations between Bray-1 and Mehlich-3 P in the agronomic soil test range, it is not known how these tests compare for soils that test very high in P and are of environmental concern. Our objectives were to determine the relationship between Mehlich-3 and Bray-1 P soil tests as affected by 1) P determination method: colorimetric or inductively coupled plasma atomic emission spectroscopy; 2) soil type and pH (pH < 6.8 and pH gtoreq 6.8); and 3) soil test P level. Soils were collected from 43 New York fields ranging from acidic to high pH soils with free CaCO3 (study 1) and 126 fields of a single farm with a long-term manure history (study 2). Bray-1 and Mehlich-3 P were linearly related independent of soil pH and detection method for soils with Mehlich-3icp less than 200 mg P kg-1 soil. For soils higher in P, concentrations in both the Bray-1 and Mehlich-3 extracts exceeded the linear portion of the standard curves of the, colorimetric method (1:9 dilution). Without further dilution of the extract, the colorimetric method failed to identify an increase in environmentally available dissolved inorganic P. States that currently use colorimetric analyses for P runoff risk assessment will need to evaluate its performance on high P sites and ensure that dilution protocols are in place to accurately analyze soils with greater than 200 mg P kg-1 soil.
机译:土壤测试是农艺建议和磷(P)径流风险评估的基础。尽管多项研究表明Bray-1和Mehlich-3 P在农艺土壤测试范围内具有良好的线性相关性,但尚不知道这些测试如何与P含量很高且环境相关的土壤进行比较。我们的目标是确定受以下因素影响的Mehlich-3和Bray-1 P土壤测试之间的关系:1)P测定方法:比色法或电感耦合等离子体原子发射光谱法; 2)土壤类型和pH(pH <6.8和pH gtoreq 6.8); 3)土壤测试P水平。从纽约的43个田地(从酸性到高pH值的土壤,含游离的CaCO3)收集土壤(研究1),在一个拥有长期肥料历史的单一农场的126个田地中收集研究(研究2)。 Bray-1和Mehlich-3 P与土壤pH呈线性相关,而Mehlich-3icp小于200 mg P kg-1的土壤的检测方法无关。对于含磷量较高的土壤,Bray-1和Mehlich-3提取物中的浓度均超过了比色法(1:9稀释)标准曲线的线性部分。如果不对提取物进行进一步稀释,则比色法无法确定环境中可溶的无机P的增加。当前使用比色分析进行P径流风险评估的国家将需要评估其在高P部位的性能,并确保采用稀释方案。精确分析200 mg P kg-1以上土壤的场所。

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