Abstract:Potassium (K) plays a major role in the basic functions of plant growth and development. In addition, K is also involved in numerous physiological functions related to plant health and resistance to biotic and abiotic stress. However, K deficiency occurs widely resulting in poor growth, lost yield, and reduced fiber quality. This review describes the physiological functions of K and its role in stress relief and also provides some agronomic aspects of K requirements, diagnosis of soil and plant K status, and a… Show more
“…Increasing the level of soil exchangeable K by fertiliser application would render more K available to plants for the needs of physiological functions (e.g. photosynthesis and turgor maintenance) and for better root growth under soil-water deficit (Grzebisz et al 2013;Oosterhuis et al 2013). Consistently in the present study, the positive response of wheat growth and grain yield to soil K supply was observed at the drought-affected site but not at the non-stressed sites.…”
Section: Soil K Supply and Droughtsupporting
confidence: 89%
“…Fertiliser K supply at Dowerin increased K concentration and content in shoots, total dry matter and grain yield. During soil drying period, the decrease in soil water potential would likely impair K movement to the root surface and reduce plant K uptake (Marschner 1995;Römheld and Kirkby 2010;Oosterhuis et al 2013). On the other hand, soil K deficiency reduces root growth to a greater extent than shoot growth in wheat and barley (Ma et al 2011(Ma et al , 2013, likely attributable to the critical role of K in supplying sucrose from leaves to roots to meet the energy requirements for root growth and ion uptake (Cakmak et al 1994;Marschner et al 1996).…”
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 aestivumL.) with four K rates (0, 20, 40, 80 kg 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 (36 mg K/kg at 0-30 cm) and Borden (25 mg K/kg at 0-30 cm), compared with significant gain in K uptake, dry matter and grain yield at Dowerin (29 mg K/kg at 0-30 cm), 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 ~4 dS/m) and low K (20 mg K/kg) farm in the central grainbelt and treated with 0, 20, 40 and 120 kg K/ha. Applying K increased K uptake but decreased Na uptake, especially at 120 kg 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.
“…Increasing the level of soil exchangeable K by fertiliser application would render more K available to plants for the needs of physiological functions (e.g. photosynthesis and turgor maintenance) and for better root growth under soil-water deficit (Grzebisz et al 2013;Oosterhuis et al 2013). Consistently in the present study, the positive response of wheat growth and grain yield to soil K supply was observed at the drought-affected site but not at the non-stressed sites.…”
Section: Soil K Supply and Droughtsupporting
confidence: 89%
“…Fertiliser K supply at Dowerin increased K concentration and content in shoots, total dry matter and grain yield. During soil drying period, the decrease in soil water potential would likely impair K movement to the root surface and reduce plant K uptake (Marschner 1995;Römheld and Kirkby 2010;Oosterhuis et al 2013). On the other hand, soil K deficiency reduces root growth to a greater extent than shoot growth in wheat and barley (Ma et al 2011(Ma et al , 2013, likely attributable to the critical role of K in supplying sucrose from leaves to roots to meet the energy requirements for root growth and ion uptake (Cakmak et al 1994;Marschner et al 1996).…”
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 aestivumL.) with four K rates (0, 20, 40, 80 kg 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 (36 mg K/kg at 0-30 cm) and Borden (25 mg K/kg at 0-30 cm), compared with significant gain in K uptake, dry matter and grain yield at Dowerin (29 mg K/kg at 0-30 cm), 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 ~4 dS/m) and low K (20 mg K/kg) farm in the central grainbelt and treated with 0, 20, 40 and 120 kg K/ha. Applying K increased K uptake but decreased Na uptake, especially at 120 kg 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.
“…A previous study showed that fertilization with K was causing a decreased allocation to roots, which enables increased growth in height and leaf number [38]. Moreover, the viewpoint that an optimal potassium nutrition status can reduce the effects of abiotic stresses, such as drought, heat, high light intensity, or salinity has been well established [14,39,40]. The characteristic of our study site is coastal sandy saline-alkali soil; thus, K fertilizer is essential in Yellow Sea Forest Park.…”
Ginkgo biloba L. is one of the most extensively planted and productive commercial species in temperate areas around the world, but slow-growth is the most limiting factor for its utilization. Fertilization is one of the key technologies for high quality and high forest yield. To better understand the impacts of fertilization on Ginkgo productivity, the effects of fertilization treatments (single fertilizer and combined fertilizer) on growth, nutrient content in Ginkgo leaves, and photosynthesis characteristics were studied in a 10-year-old Ginkgo plantation over two years. The single factor experiments suggested that DBH (diameter at breast height), H (height), NSL (length of new shoots), and V (trunk volume) showed significant differences between the different levels of single nitrogen (N) or phosphate (P) fertilizer application. Orthogonal test results showed that the nine treatments all promoted the growth of Ginkgo, and the formula (N: 400 g·tree −1 , P: 200 g·tree −1 , potassium (K): 90 g·tree −1 ) was the most effective. G s (stomatal conductance) and P n (net photosynthesis rate) showed significant differences between the different amounts of single N or P fertilizer application, while single K fertilizer only affected P n . Combined N, P, and K fertilizer had significant promoting effects on C i (intercellular CO 2 concentration), G s and P n . N and P contents in Ginkgo leaves showed significant differences between the different amounts of a single N fertilizer application. A single P fertilizer only improved foliar P contents in Ginkgo leaves. A single K fertilizer application improved N and K content in Ginkgo leaves. The effects of different N, P, and K fertilizer treatments on the nutrient content of Ginkgo leaves were different.
“…Potassium due to its impact on many physiological processes plays an important role in water use by crop plants (Grzebisz et al, 2013 andOosterhuis et al, 2013). A main function of K is unloading sugars from chloroplasts to phloem cells, and from phloem cells into storage cells such as grains, (Salisbury and Ross, 1978).…”
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