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Growth and yield responses in wheat and barley to potassium supply under drought or moderately saline conditions in the south-west of Western Australia

机译:西澳大利亚州西南部干旱或中等盐度条件下小麦和大麦对钾供应的生长和产量响应

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摘要

This study assessed whether more potassium (K) was required for optimal growth and grain yield of cereal crops under drought and salinity than under non-stressed conditions. In 2011, three experiments on wheat (Triticum aestivum L.) with four K rates (0, 20, 40, 80kg K/ha), four application times (0, 5, 10, 15 weeks after sowing, WAS) and two sources (KCl, K2SO4) were conducted in the central and southern grainbelts of Western Australia. The lack of plant response to K supply at the sites of Bolgart (36mg K/kg at 0-30cm) and Borden (25mg K/kg at 0-30cm), compared with significant gain in K uptake, dry matter and grain yield at Dowerin (29mg K/kg at 0-30cm), was not explained by differences in soil K levels. However, rain fell regularly through the growing season at Bolgart and Borden, whereas a dry spell occurred from stem elongation to grain development at Dowerin. The effectiveness of K application time followed the trend of 0, 5>10>15 WAS. In 2012, barley (Hordeum vulgare L.) was grown on a moderately saline (saturation extract electrical conductivity ∼4dS/m) and low K (20mg K/kg) farm in the central grainbelt and treated with 0, 20, 40 and 120kg K/ha. Applying K increased K uptake but decreased Na uptake, especially at 120kg K/ha. Plant growth and grain yield increased with K supply, but the difference between the K rates was relatively small, indicating possible partial K substitution by Na. Higher than normal fertiliser K supply on low K soils would enhance the adaptation by cereals to water-limited environments, but K-fertiliser management on moderately saline soils may need to account for both K and Na uptake and use by the crops.
机译:这项研究评估了干旱和盐度条件下谷物作物最佳生长和谷物产量是否比非胁迫条件下需要更多的钾(K)。 2011年,对小麦(Triticum aestivum L.)进行了三个实验,四个钾肥施用量(0、20、40、80 kg K / ha),四个施用时间(播种后0、5、10、15周,WAS)和两个来源(KCl,K2SO4)在西澳大利亚州的中部和南部谷物带进行。在Bolgart(0-30cm处36mg K / kg)和Borden(0-30cm处25mg K / kg)的位点上,植物对钾的供应缺乏响应,而钾肥吸收,干物质和籽粒产量显着增加Dowerin(0-30厘米处为29mg K / kg)不能通过土壤钾水平的差异来解释。然而,Bolgart和Borden的整个生长季节都定期降雨,而Dowerin的干旱从茎伸长到谷物生长。钾肥施用时间的有效性遵循0,5> 10> 15 WAS的趋势。 2012年,大麦(Hordeum vulgare L.)在中央谷物带的中等盐度(饱和浸出电导率约为4dS / m)和低钾(20mg K / kg)农场上生长,并分别经0、20、40和120kg处理公顷施钾增加了钾的吸收,但减少了钠的吸收,特别是在120kg K / ha时。钾的供应增加了植物的生长和籽粒的产量,但钾的施用率之间的差异相对较小,表明钾可能被Na部分替代。在低钾土壤上钾肥的供应量比正常水平高,将增强谷物对水有限环境的适应性,但是在中度盐渍土壤上的钾肥管理可能需要考虑作物对钾和钠的吸收和利用。

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