Improving crop mineral nutrition
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Crops require adequate nutrition for the production of food, fibre and fuel, but soil conditions often limit the ability of crops to acquire mineral nutrients. To address this, mineral nutrients can be applied as inorganic or organic fertilisers to the soil or as liquid fertilisers to foliage. However, production and use of fertilisers can have negative environmental impacts. The articles in this Special Issue illustrate a number of ways to improve nutrient acquisition from the soil and their delivery through foliar application.
Articles highlighted here include those that discuss ways by which to assess a crop’s requirement for additional mineral elements, ways by which minerals can be supplied more effectively to crops both through roots and shoots, and ways by which the crop itself can be enhanced to acquire more mineral elements.
It is apparent from the information contained in this Special Issue that to improve the ability of crops to acquire mineral elements, a number of strategies are available. However, the success of any one intervention is dependent on how these strategies interact with the environment in which they are deployed and the suitability of the management system for the specific intervention.
KeywordsEssential elements Fertiliser Nutrient availability Phosphorus Plant-microbe interactions roots
Crop production requires adequate availability of the 14 essential mineral elements (mineral nutrients) necessary for plant growth (White and Brown 2010). Low input agriculture is generally limited by the phytoavailability of N, K, P or S, whilst the phytoavailability of Fe, Zn and Cu often limits crop production on alkaline and calcareous soils, that of K, P, Mg, Ca or Mo limits crop production on acid soils, and that of B can limit crop production on soils with various pH (Fageria et al. 2011; Mueller et al. 2012; White et al. 2013a). To address such limitations to crop production, mineral nutrients can be applied as inorganic or organic fertilisers to the soil (Fageria et al. 2011; White et al. 2012) or as liquid fertilisers to foliage (Fernández et al. 2013). However, the production and use of fertilisers can have a variety of negative environmental consequences, including the production of greenhouse gasses, deterioration of soil and water quality, and the exhaustion of non-renewable resources (White and Brown 2010; White et al. 2013b). Thus, it is necessary to optimise the efficiency with which mineral elements are acquired by crops and utilised physiologically for the production of food, fibre and fuel (White et al. 2013b). In this Special Issue, which complements a Special Issue edited by Schjørring and Cakmak (2014), we collect together a range of articles that demonstrate a number of approaches at our disposal to improve nutrient acquisition from the soil by plants and delivery of mineral nutrients through foliar applications to plants. Collectively, these articles demonstrate the importance of understanding how our interventions interact with the wider environment and the management systems in which they are deployed.
Improving nutrient acquisition from the soil
In the soil, all mineral elements move by a combination of mass flow and diffusion, and all strategies designed to improve mineral acquisition by crops affect one or both of these processes (Lynch 2007; Richardson et al. 2011; Simpson et al. 2011; White et al. 2013a). Diffusion of mineral elements is determined by the concentration gradients between the root surface and the soil solution (White and Greenwood 2013), which are often dictated by interactions with soil mineral surfaces. It operates over short distances, and is especially important for the macronutrients P and K that often limit crop production (Hinsinger et al. 2011). The mass flow of a mineral element to the root surface is determined by its concentration in the soil solution and the transpiration-driven movement of water to the root surface (White and Greenwood 2013). It is important for the acquisition of essential mineral elements with large concentrations in the soil solution, such as N, K, S, Ca, Mg and Cl in agricultural soils, and for mineral elements that are required in relatively small quantities by plants, such as Fe, Mn, Zn, Cu, Ni, B and Mo (White et al. 2013a).
If essential mineral elements are not present, or not phytoavailable, in the soil, then they must be supplied as fertilisers to enable crop production and ensure produce quality. Many agronomic strategies can be adopted to increase the efficiency with which inorganic and organic fertilisers are used to provide the essential mineral elements required by crops (Simpson et al. 2011). In principle, these optimise the chemistry, quantity, placement, and timing of fertiliser applications (Fageria et al. 2011; Simpson et al. 2011; Mueller et al. 2012; Noack et al. 2012; White et al. 2012; White and Greenwood 2013). The chemical form and quantity of a mineral element required for crop production in a particular location depends critically on soil characteristics. Many fertiliser recommendations are based on estimating the phytoavailability of mineral elements in the soil (e.g. Defra 2010). In this Special Issue, Włodarczyk et al. (2014) describe the development of a technique to determine the phytoavailability of B in agricultural soils, whilst Suriyagoda et al. (2014) provide a case study of how soil characteristics, fertiliser chemistry and quantity, and the environment interact. In the latter, the authors studied the benefits of incorporating straw on the growth of rice plants in either clay or sandy soils under a range of moisture conditions. They observed that incorporating straw increased plant growth in clay soils, but not those grown in sandy soils, and only when adequate P was supplied. This paper provides a good demonstration of the importance of understanding interactions between environment and management.
Agronomic strategies can be complemented by cultivating genotypes with appropriate below ground traits for nutrient acquisition (Lynch 2007, 2011, 2013; Richardson et al. 2011; White et al. 2012, 2013a, b). Below ground traits that influence the acquisition of mineral elements by plants include, (1) root characteristics, such as root elongation rate, lateral root production, specific root length (length/mass quotient), root length density (root length / soil volume), reduced metabolic load of roots (aerenchyma formation) and root hair length and abundance, all of which increase the volume of soil explored by the root system and the surface area for the uptake of mineral elements, (2) the proliferation of roots in discrete patches of soil containing greater concentrations of mineral elements, such as topsoil horizons rich in organic matter, (3) modification of rhizosphere pH and the exudation of low molecular weight organic solutes and/or enzymes, which influence the concentration of mineral elements in the soil solution, (4) high-capacity uptake systems for mineral nutrients, and (5) interactions with microbes either intimately, through mycorrhizal associations or nodulation by rhizobia, or loosely, through the culture of beneficial microbes or exclusion of detrimental microbes in the rhizosphere. None of these below ground traits work in isolation of one another and it is, therefore, important to consider (1) how they interact with one another (Brown et al. 2013), (2) how they interact with the environment (Oburger et al. 2011; Jin et al. 2012), and (3) how they interact with crop management practices (George et al. 2011; Nazeri et al. 2013).
Two papers in this Special Issue investigate how the acquisition of mineral elements is influenced by the rhizosphere environment. In one of these, Tanoi et al. (2014) demonstrate that Mg uptake by rice roots is mediated by both high-affinity and low-affinity transport systems, whose capacities increase with Mg starvation and return rapidly to a basal levels after Mg resupply. This work demonstrates that the Mg uptake system of rice roots is tightly regulated and reacts rapidly to changes in the rhizosphere environment. In the second example, Watts-Williams and Cavagnaro (2014) describe a meta-analysis of studies on nutrient uptake by a wild-type and an arbuscular mycorrhizal fungi (AMF)-defective tomato mutant (rmc) and go on to demonstrate that colonisation by AMF significantly affects the uptake of many mineral nutrients. They also observe that soil P and Zn phytoavailability influences the ability of mycorrhizal plants to acquire other mineral nutrients, with deficient plants having greater AMF colonisation, which assists mineral uptake.
Delivering mineral nutrients through foliar fertilisers
Foliar applications of mineral elements can be used both in combination with applications to soil or, for elements required in small amounts (i.e. micronutrients), as an alternative to soil applications (Fageria et al. 2009; Defra 2010; White and Greenwood 2013; Eichert and Fernández 2012; Fernández et al. 2013). The use of foliar fertilisers is not novel, and has been common practice in agriculture and horticulture for many decades (Fageria et al. 2009; Kannan 2010; Fernández et al. 2013). It is particularly effective in delivering (1) mineral nutrition when soil applications are impractical, such as when the topsoil is dry, (2) mineral elements with restricted phytoavailability in the soil, such as Zn, Fe, Cu and Mn in alkaline and calcareous soils, and (3) mineral elements required in large amounts during periods of great demand, such as N, P, K and S (Fageria et al. 2009; Eichert and Fernández 2012; White et al. 2012; Fernández et al. 2013; White and Greenwood 2013). In addition, it has the advantage over soil applications of mineral fertilisers in that it provides the opportunity to deliver appropriate amounts of specific mineral elements to particular tissues at particular developmental stages. Thus, it can be used (1) to improve the physical and nutritional quality of produce in a targeted fashion (White and Broadley 2011; Eichert and Fernández 2012; Fernández et al. 2013), (2) to correct mineral deficiencies as and when they occur (Fageria et al. 2009; Defra 2010; Eichert and Fernández 2012; Fernández et al. 2013), (3) to address mineral deficiencies of phloem-immobile elements in phloem-fed tissues, such as fruits (Ho and White 2005; Fageria et al. 2009; Eichert and Fernández 2012; Fernández et al. 2013) and (4) to minimise absolute fertiliser requirements, thereby reducing losses of mineral elements to the wider environment (Kannan 2010; Eichert and Fernández 2012; White et al. 2012; Fernández et al. 2013). Remedial applications of foliar fertilisers are often made when crops exhibit visible mineral deficiency symptoms. Traditionally, these are recorded by growers during crop walking, but crops could be monitored remotely and their nutritional status diagnosed using modern image analysis techniques, such as those described by Hong et al. (2014), in this Special Issue, to identify the N nutritional status of watermelon. Since foliar fertilisers can be applied with other foliar chemicals, financial costs can also be reduced.
The most effective use of foliar fertilisers can be achieved using responsive genotypes, which can take up mineral elements efficiently into shoot tissues and re-translocate them appropriately. Mineral elements supplied as foliar fertilisers enter the leaf across the cuticle or through open stomata (Fageria et al. 2009; Kannan 2010; Eichert and Fernández 2012; Fernández et al. 2013). The relative contributions of each pathway to the uptake of mineral elements are debated, but will depend upon both the form in which the element is supplied and leaf surface properties (Eichert and Fernández 2012). Two articles in this Special Issue address the effects of leaf characteristics on the absorption and delivery of P to reproductive tissues of wheat (Triticum aestivum L.). Peirce et al. (2014) observe that greater P accumulation in the ear of wheat following foliar application to adaxial, compared to abaxial, leaf surfaces, is directly related to stomatal density, although they concede that trichome density and cuticular composition might also influence P uptake, whilst Fernández et al. (2014) observe that P absorption is affected by leaf P status, with more P being absorbed by leaves of P-replete plants than by those of P-deficient plants. They attribute the latter phenomenon to impaired stomatal functioning and a reduction in stomatal density in leaves of P-deficient plants. It is commonly observed that the uptake of mineral elements applied to leaves is related to stomatal abundance (Fernández et al. 2013), but the effects of nutritional status on stomatal density and functioning are rarely studied (Cramer et al. 2009; Waraich et al. 2011; Wimmer and Eichert 2013; Rothwell and Dodd 2014). Since there is considerable genetic variation in stomatal density, trichome density and cuticular chemical composition within plant species (e.g. Araus et al. 1991; Sadras et al. 2012; Chitwood et al. 2013; Khazaei et al. 2013; Parsons et al. 2013; Zhang et al. 2013; Bloomer et al. 2014; Doroshkov et al. 2014; Ray et al. 2014), there exists the possibility to select or breed for genotypes with improved response to foliar fertilisers.
The ability to re-translocate mineral elements applied as foliar fertilisers to deficient or developing tissues is essential for preventing contemporaneous and future mineral deficiencies within the plant. However, mineral deficiencies often limit the re-translocation of mineral elements (Hermans et al. 2006; Fernández et al. 2013), especially those with limited phloem mobility, which necessitates direct and repeated application of foliar fertilisers to deficient tissues (Fernández et al. 2013). In addition, it has also been hypothesised that the translocation of mineral elements within the plant might alleviate the effects of toxic mineral elements by promoting dilution through redistribution, increased growth, biochemical competition, or co-precipitation in non-vital compartments. In this Special Issue, Iqbal (2014) has tested, and disproven, the hypothesis that the translocation of P from roots grown in aluminium (Al)-free soil can alleviate Al-toxicity in roots of the same plant exposed to toxic soil Al concentrations using a split-root system.
It is apparent from the information contained in this Special Issue that in order to improve the ability of crops to acquire mineral elements, a number of strategies are available. These include better monitoring of nutrient status, improved formulations of fertilisers, access to alternative sources of nutrients, better agronomy and improved genotypes for nutrient use and better understanding of the physiology of uptake of nutrients through both roots and shoots. However, the success of any one intervention is dependent on how these strategies interact with the environment in which they are deployed and the suitability of the management system for the specific intervention.
This work was supported by the Rural and Environment Science and Analytical Services Division (RESAS) of the Scottish Government.
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