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Potassium acquisition by soybean affected by stratified soil potassium, growth stage, and soil water content.

机译:大豆对钾的吸收受分层土壤钾,生长期和土壤含水量的影响。

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摘要

A 2-year field study on a silt loam, no-till soil was designed to test the hypothesis that temporal variability and vertical stratification of soil water---having the greatest effect---and K through the profile of no-till soil will lower plant-available K and reduce soybean [Glycine max (L.) Merr.] growth and yield. The objectives of this study were to (1) quantify the impact of distribution and quantity of soil K and water through the growing season on soybean K uptake, shoot and root growth, and seed yield; (2) relate K accumulation patterns to grain K, protein, and oil concentration at harvest; and (3) compare the 5-minute sodium tetraphenylboron test (NaTPB), which access slowly available K, to the standard soil-test K (STK) under field conditions across years. A supplemental split-pot greenhouse study was designed to determine the effect of synchronous and asynchronous availability of localized K and soil water content on soybean root proliferation, K uptake and shoot development. Soil, root and shoot samples were collected by development stages and seed yields were determined at maturity. Highest yields were related to greater number of pods plant-1. Inadequate K fertility early in the season reduced overall crop growth, but soil K fertility above the optimum increased the amount of K cycling in the plant-soil system without improving yield or seed K, oil, and protein concentration. Prediction of tissue K concentrations in response to STK was improved 22% by sampling the 0 to 5 instead of the 0 to 20 cm depth increment. The STK was preferred over the NaTPB test because the STK was a more stable test across different growing season conditions and more closely assessed plant K uptake. Congruent soil K depletion, root growth, and higher K and water availability in the surface (0 to 5 cm depth increment) compared to the subsurface (5 to 20 cm depth increment) illustrated that in intermittent rainfed systems K stratification caused by no-till might not be detrimental to soybean production. Greenhouse results supported field findings and showed that root proliferation occurred in areas of localized soil water availability which, in turn, enhanced K uptake.
机译:对淤泥壤土,免耕土壤进行了为期两年的田间研究,目的是检验以下假设的假设:土壤水的时间变异性和垂直分层(效果最大)和免耕土壤剖面的钾素会降低植物的钾素含量,并降低大豆[Glycine max(L.)Merr。]的生长和产量。这项研究的目的是(1)量化整个生长期土壤钾和水的分布和数量对大豆吸收钾,枝条和根系生长以及种子产量的影响; (2)在收获时将钾的积累方式与籽粒的钾,蛋白质和油的浓度联系起来; (3)将多年来缓慢获取的钾的5分钟四苯硼钠测试(NaTPB)与标准土壤测试K(STK)进行比较。设计了一项补充式分盆温室研究,以确定同步和异步利用局部钾素和土壤水分对大豆根系增殖,钾素吸收和芽发育的影响。在发育阶段收集土壤,根和芽的样品,并确定成熟时的种子产量。最高产量与豆荚植物1的数量增加有关。季初钾肥不足会降低整体作物生长,但高于最佳水平的土壤钾肥会增加植物-土壤系统中钾素的循环量,而不会提高产量或种子钾,油和蛋白质的浓度。通过采样0到5而不是0到20 cm的深度增量,对STK响应的组织K浓度的预测提高了22%。 STK比NaTPB试验更可取,因为STK在不同生长季节条件下均能更稳定地进行试验,并且对植物K吸收的评估更为严格。与地下土壤(地下5至20厘米深度)相比,土壤K减少,根系生长一致,并且钾和水分的利用率更高(深度增加0至5厘米),这表明在间歇性雨养系统中,免耕导致钾分层可能对大豆生产无害。温室结果支持田间调查结果,并表明根系增殖发生在局部土壤水可利用的区域,从而增加了钾的吸收。

著录项

  • 作者

    Fernandez, Fabian Gerardo.;

  • 作者单位

    Purdue University.;

  • 授予单位 Purdue University.;
  • 学科 Agriculture Agronomy.; Agriculture Soil Science.
  • 学位 Ph.D.
  • 年度 2006
  • 页码 150 p.
  • 总页数 150
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 农学(农艺学);土壤学;
  • 关键词

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