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Long-term changes in soil phosphorus status related to P budgets under maize monoculture and mineral P fertilization

机译:玉米单作和无机磷施肥下与磷预算相关的土壤磷素长期变化

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Monitoring soil phosphorus (P) changes under continuous cropping over decades is an important agronomic and environmental issue. The aim was to determine soil P dynamics in the plough layer as a function of cumulative P budgets (Bcum) across extended cropping periods (7, 12, and 17 yr) for four rates of mineral P fertilization. This field experiment was established in 1975 on a slightly alkaline, sandy loamy soil (luvic Arenosol). Soil P was assessed by three P tests: the concentration of P ions in solution (Cp), Olsen (POl), and Mehlich-3 P (PM). Annual P budget was calculated as P applied minus P exported by the grain. The Bcum values were the sum of annual P budgets. Bcum, Cp, POl, and PM values were significantly influenced by cropping periods and P rates. The nine combinations (3 periods x 3 soil P tests) of P dynamics versus Bcum were described by linear regressions. For each soil P test, all means fell on the same regression line for the three cropping periods indicating that the P transformation rates were similar for positive and negative P budgets. Relationships depended on soil test P but did not vary for cropping periods. For this specific soil, we calculated that a change in P budget of 100 kg/ha would change Cp, POl, and PM by 0.11 mg/L, 3.3 mg/kg, and 14 mg/kg, respectively. Although this result needs to be confirmed and extended to other soil types, we conclude that a single year of soil sampling after a decade of experimentation would be sufficient to establish the relationship between soil P status and P budgets.
机译:在连续数十年的作物中监测土壤磷的变化是一个重要的农业和环境问题。目的是确定耕作期(7、12和17年)对于四种矿物P的施肥速率,耕作层中土壤P的动态与累积P预算(Bcum)的函数关系。这项田间试验于1975年在弱碱性,沙质壤土(Luvic Arenosol)上建立。土壤磷通过三种磷测试进行评估:溶液中的P离子浓度(Cp),奥尔森(Pol)和Mehlich-3 P(PM)。每年的P预算是将P减去谷物输出的P得出的。 Bcum值是年度P预算的总和。 Bcum,Cp,POl和PM值受种植期和P率的影响很大。 P动力学与Bcum的9种组合(3个周期x 3个土壤P试验)通过线性回归描述。对于每个土壤P检验,在三个耕作期所有均值均落在同一回归线上,表明正P和负P预算的P转化率相似。关系取决于土壤测试P,但在种植期间没有变化。对于这种特定的土壤,我们计算出100公斤/公顷的磷预算变化将使Cp,POl和PM分别改变0.11 mg / L,3.3 mg / kg和14 mg / kg。尽管需要证实这一结果并将其推广到其他土壤类型,但我们得出的结论是,经过十年的试验,仅需进行一年的土壤采样就足以确定土壤磷状况与磷预算之间的关系。

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