解释土壤养分浓度时,恒定容重假设导致的不确定性

IF 2.3 4区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Agricultural & Environmental Letters Pub Date : 2024-05-26 DOI:10.1002/ael2.20129
Arshdeep Singh, Meetpal S. Kukal
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引用次数: 0

摘要

土壤测试报告中的土壤养分浓度通常以百万分之一(ppm)表示。为了将其纳入养分管理决策,必须将基于 ppm 的浓度换算成每英亩磅数,通常普遍建议将换算系数(乘数)定为 2.0。不过,该转换系数是根据与淤泥质土壤相对应的容重假定值 (ρb)计算得出的,超出假定 ρb 的任何偏差都不会改变。在此,我们量化并评估了假设 ρb 值恒定对计算土壤氮抵消量的潜在影响。美国耕地土壤中,对 ρb 变化敏感的真实动态转换因子介于 1.28 和 2.68 之间。结果表明,如果不考虑这一动态转换系数,土壤氮素贷方会被低估达 40%。除了空间变化外,管理引起的 ρb 变化也很重要,需要纳入转换因子。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Uncertainty resulting from constant bulk density assumption when interpreting soil nutrient concentrations

Soil nutrient concentrations are often expressed as parts per million (ppm) in soil test reports. For incorporation into nutrient management decisions, ppm-based concentrations have to be converted into pounds per acre, and a conversion factor (multiplier) of 2.0 is typically recommended universally to do so. However, this conversion factor stems from an assumed value of bulk density (ρb) corresponding to silt loam soil and is invariant to any deviation beyond assumed ρb. Here, we quantify and evaluate the potential ramifications of assuming a constant ρb value on calculating soil nitrogen credits. A true dynamic conversion factor that is sensitive to variation in ρb ranges between 1.28 and 2.68 for soils across US cropland. Failure to account for this dynamic conversion factor was shown to result in an underestimation of soil N credits by up to 40%. In addition to spatial variation, management-induced changes in ρb are also important to incorporate into the conversion factor.

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来源期刊
CiteScore
3.70
自引率
3.80%
发文量
28
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