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首页> 外文期刊>Plant and Soil >Phosphorus intensity determines short-term P uptake by pigeon pea (Cajanus cajan L.) grown in soils with differing P buffering capacity.
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Phosphorus intensity determines short-term P uptake by pigeon pea (Cajanus cajan L.) grown in soils with differing P buffering capacity.

机译:磷的强度决定了在具有不同磷缓冲能力的土壤中生长的木豆(Cajanus cajan L.)的短期P吸收。

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Phosphorus (P) uptake by plant roots depends on P intensity (I) and P quantity (Q) in the soil. The relative importance of Q and I on P uptake is unknown for soils with large P sorption capacities because of difficulties in determining trace levels of P in the soil solution. We applied a new isotope based method to detect low P concentrations (&20 micro g P l-1). The Q factor was determined by assessment of the isotopically exchangeable P in the soil (E-value) and the I factor was determined by measurement of the P concentration in the pore water. A pot trial was set up using four soils with similar labile P quantities but contrasting P buffering capacities. Soils were amended with KH2PO4 at various rates and pigeon pea (Cajanus cajan L.) was grown for 25 days. The P intensity ranged between 0.0008 and 50 mg P l-1 and the P quantity ranged between 10 and 500 mg P kg-1. Shoot dry matter (DM) yield and P uptake significantly increased with increasing P application rates in all soils. Shoot DM yield and P uptake, relative to the maximal yield or P uptake, were better correlated with the P concentration in the pore water (R2=0.83-0.90) than with the E-value (R2=0.40-0.53). The observed P uptakes were strongly correlated to values simulated using a mechanistic rhizosphere model (NST 3.0). A sensitivity analysis reveals that the effect of P intensity on the short-term P uptake by pigeon pea exceeded the effect of P quantity both at low and high P levels. However, DM yield and P uptake at a given P intensity consistently increased with increasing P buffering capacity (PBC). The experimental data showed that the intensity yielding 80% of the maximal P uptake was 4 times larger in the soil with the smallest PBC compared to the soil with the largest PBC. This study confirms that short-term P uptake by legumes is principally controlled by the P intensity in the soil, but is to a large extent also affected by the PBC of the soil..
机译:植物根系对磷的吸收取决于土壤中磷的强度(I)和磷的数量(Q)。对于具有较大P吸附能力的土壤,Q和I对P吸收的相对重要性尚不明确,因为难以确定土壤溶液中的痕量P。我们应用了一种基于同位素的新方法来检测低P浓度(<20 micro g P-1)。通过评估土壤中同位素可交换的P(E值)来确定Q因子,通过测量孔隙水中的P浓度来确定I因子。盆栽试验使用了四种不稳定的P量但P缓冲能力相反的土壤。用KH2PO4对土壤进行不同程度的改良,并将木豆(Cajanus cajan L.)种植25天。 P强度在0.0008至50mg P l-1之间,并且P量在10至500mg P kg-1之间。在所有土壤中,随P施用量的增加,苗干物质(DM)的产量和P吸收显着增加。相对于最大产量或P吸收量,茎干DM产量和P吸收量与孔隙水中P浓度(R2 = 0.83-0.90)的相关性比与E值(R2 = 0.40-0.53)更好。观察到的P吸收与使用机械根际模型(NST 3.0)模拟的值高度相关。敏感性分析表明,低磷和高磷水平下,磷强度对木豆短期吸收磷的影响均超过了磷含量的影响。但是,在给定的P强度下,DM产量和P吸收量随P缓冲能力(PBC)的增加而持续增加。实验数据表明,与最大PBC的土壤相比,PBC最小的土壤产生的最大P吸收量的80%的强度大4倍。这项研究证实,豆类植物对短期P的吸收主要受土壤中P强度的控制,但在很大程度上还受土壤PBC的影响。

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