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
【24h】

Phosphorus intensity determines short-term P uptake by pigeon pea (Cajanus cajan L.) grown in soils with differing P buffering capacity

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

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

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 µg 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 (R 2 = 0.83–0.90) than with the E-value (R 2=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清楚,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 µg P l-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缓冲能力不同的土壤。用KH2 PO4 对土壤进行不同的处理,然后将木豆(Cajanus cajan L.)种植25天。 P的强度为0.0008至50mg P 1-1 ,P的量为10至500mg P kg-1 。在所有土壤中,随P施用量的增加,苗干物质(DM)产量和P吸收量显着增加。相对于最大产量或P吸收量,地上部DM的产量和P吸收与孔隙水中的P浓度(R 2 = 0.83–0.90)之间的相关性比与E值(R 2 = 0.40-0.53)。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,豆类植物短期吸收磷主要受土壤中磷含量的控制,但在很大程度上还受土壤中PBC的影响。

著录项

  • 来源
    《Plant and Soil》 |2006年第2期|217-227|共11页
  • 作者单位

    Division of Soil and Water Management Department of Land Management and Economics K.U.Leuven;

    Division of Soil and Water Management Department of Land Management and Economics K.U.Leuven;

    Division of Soil and Water Management Department of Land Management and Economics K.U.Leuven;

    Division of Soil and Water Management Department of Land Management and Economics K.U.Leuven;

    Division of Soil and Water Management Department of Land Management and Economics K.U.Leuven;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    P buffering capacity; P intensity; P quantity; P uptake; Pigeon pea;

    机译:磷的吸收能力;磷的强度;磷的数量;磷的吸收;豌豆;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号