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Revista Brasileira de Engenharia Agrícola e Ambiental

versão On-line ISSN 1807-1929

Rev. bras. eng. agríc. ambient. vol.18 no.5 Campina Grande maio 2014

http://dx.doi.org/10.1590/S1415-43662014000500005 

SOIL, WATER AND PLANT MANAGEMENT

 

Initial physic nut nutrition and potassium balance in the soil-plant system1

 

Nutrição inicial do pinhão-manso e balanço de potássio no sistema solo-planta

 

 

Mariângela B. FreibergerI,*; Iraê A. GuerriniII; Gustavo CastoldiIII; Fábio SteinerIV; Leonardo T. BüllV

IFCA/UNESP. Botucatu, SP. E-mail: maia_bf@yahoo.com.br
IIFCA/UNESP. Botucatu, SP. E-mail: iguerrini@fca.unesp.br
IIIFCA/UNESP. Botucatu, SP. E-mail: castoldi@fca.unesp.br
IVFIO. Ourinhos, SP. E-mail: fsteiner_agro@yahoo.com.br
VFCA/UNESP. Botucatu, SP. E-mail: bull@fca.unesp.br

 

 


ABSTRACT

The objectives of this study were to evaluate the mineral nutrition and the response of physic nut to potassium fertilization as well as to assess whether the species can absorb K from the non-exchangeable soil fraction. The study was conducted in a greenhouse, in randomized blocks, and with four repetitions. Physic nut plants were cultivated in plastic recipients filled with 50 dm3 of a Dark Red Latosol fertilized with rates of 0, 40, 80, 120 and 160 mg K dm-3 of soil. One hundred and fifty days after planting, the height, stem diameter and leaf area of the plants were measured, and the dry mass, concentration in leaf and total accumulation of macro and micronutrients were determined, as well as the soil contents of exchangeable and non-exchangeable K. The K balance in the soil-plant system was also calculated. The increase of potassium fertilization resulted in a greater uptake of K, Ca and Mn but did not alter the total dry mass production of physic nut. The species can release and absorb K from the non-exchangeable soil fraction.

Key words: Jatropha curcas, dynamic of nutrient uptake, non-exchangeable K


RESUMO

Objetivou-se, neste trabalho, avaliar a nutrição mineral e a resposta do pinhão-manso à adubação potássica, bem como se a espécie pode absorver K da fração não-trocável do solo. O estudo foi conduzido em estufa plástica, em blocos casualizados com quatro repetições. Plantas de pinhão-manso foram cultivadas em vasos plásticos preenchidos com 50 dm3 de um Latossolo Vermelho Escuro testando-se as doses de 0, 40, 80, 120 e 160 mg K dm-3 do solo; após 150 dias do plantio foram mensurados altura, diâmetro de colo e área foliar das plantas e se determinou massa seca, teores foliares e acúmulo total de macro e micronutrientes, além dos teores de K trocável e K não-trocável do solo. O balanço do K no sistema solo-planta também foi calculado. O aumento da adubação potássica resulta em maior absorção de K, Ca e Mn mas não altera a produção de massa seca total do pinhão-manso. A espécie é capaz de disponibilizar e absorver K da fração não-trocável do solo.

Palavras-chave: Jatropha curcas, dinâmica de absorção, K não-trocável


 

 

Introduction

Physic nut (Jatropha curcas L.) is a native oleaginous species of South America which has seeds with an oil content of approximately 37.5% and desirable characteristics for fuel purposes (Arruda et al., 2004). The species is perennial, monoecious and belongs to the family Euphorbiaceae (Nithiyanantham et al., 2013), as does the castor bean and cassava; however, physic nut is in plant breeding phase in Brazil, which has garnered interest from various research areas (Bhering et al., 2012).

Regarding the fertilization and mineral nutrition of physic nut several studies have defined the best cultivation conditions, which describe the quantity, time and application method of fertilizers as well as the leaf diagnosis and the appropriate nutrient concentrations.

The requirement for potassium (K) is known to be greater in the beginning of the reproductive phase of the plant (Laviola & Dias, 2008), possibly because this nutrient acts in the transport of photoassimilates and participates in fruit formation (Marschner, 1995). Fully opened leaves at positions 2 and 3 from the apex are the most appropriate samples for its diagnosis (Lima et al., 2011b).

In a study with a nutrient solution, the omission of K reduced the production of dry matter by 85% in 120-day-old physic nut plants (Silva et al., 2009), which underscores the importance of K for this species. When cultivated in the field, however, potassium fertilization did not affect growth and yield in the first and second years of physic nut growth (Oliveira et al., 2012).

The little or lack of response of this species to K fertilization, even in soils with low exchangeable K contents, is likely attributable to the contribution of the non-exchangeable K fraction in the soil that supplies the plant (Kamiski et al., 2007).

The K soil stock comprises the K in solution, exchangeable K (weakly retained in the CEC of the soil), non-exchangeable K (fraction of K "fixed" in the mineral structure) and structural K (resides in the interlayers of clay minerals and is slowly released by weathering). These forms maintain a specific equilibrium with the soil solution and define the K availability to the plants (Ernani et al., 2007). Under specific conditions, the exhaustion of K at the root surface produces a concentration gradient that causes the release of non-exchangeable K (Hinsinger et al., 1993), which can then be uptaken by the plants.

Some plants exhibit specific abilities, such as exuding organic acids (Wang et al., 2011) and accumulating cations in the root rhizosphere (Scherer, 1993), which can allow them to release K in varying magnitudes and absorb it from the non-exchangeable soil fraction (Rengel & Damon, 2008). These observations can affect the crop management and must be considered in the fertilization program. Given the above, the objective of this study was to evaluate the mineral nutrition and the response of physic nut to K fertilization as well as to assess whether the species can release and absorb K from the non-exchangeable soil fraction.

 

Material and Methods

The experiment was conducted under a greenhouse in the Department of Natural Resources/Soil Sciences of the College of Agronomic Sciences of the São Paulo State University Júlio de Mesquita Filho (FCA/UNESP), in Botucatu, SP, Brazil. During the experimental period, which lasted from October 2010 to February 2011, the maximum and minimum experimental temperatures were 41 and 21 ºC, respectively. Five doses of K were evaluated: 0, 40, 80, 120 and 160 mg dm-3. The statistical delineation was performed in randomized blocks with four replicates. Each experimental unit was composed of a plastic recipient filled with 50 dm3 of Dark Red Latosol of sandy texture (Carvalho et al., 1983) and contained a physic nut seedling. The chemical and physical analysis of the soil was performed (Table 1). The contents of exchangeable K (Raij et al., 2001) and non-exchangeable K (Knudsen et al., 1986) were also determined, which were 7.8 and 42.2 mg dm-3, respectively.

The base saturation was corrected to 60% by incorporating 2.3 g of soil of dolomitic limestone dm-3. The potassium, as potassium chloride, was incorporated in the soil 40 days after incubating the soil with limestone (29% CaO, 18% MgO and 96% PRNT), and the treatments also received fertilization with triple superphosphate (150 mg P dm-3 soil), urea (80 mg N dm-3 soil) and micronutrients (0.012 g of manganese sulfate, 0.019 g of zinc sulfate and 0.005 g of boric acid dm-3 of soil).

Physic nut seedlings were produced in the Seedling Nursery of the FCA from seeds of the best genotypes of the EMBRAPA Semi-Arid (Brazilian Agency for Agricultural Research). The seedlings were developed in 116 cm3 tubes filled with the Carolina® commercial substrate and suspended by fixed supports on the working benches of the germination in greenhouse for 45 days.

For planting, the seedlings were selected as a function of the development pattern; they exhibited an average height of 15 cm, an average stem diameter of 0.8 cm, one opened leaf and one newly developing leaf. The soil water content was monitored daily by weighing the vases and restoring the amount of water required to maintain the soil moisture close to 70% of the field capacity, as described by Ramos Júnior et al. (2013).

One hundred and fifty days after planting, the following parameters were measured: the stem diameter at 1 cm from the surface of the soil (using a digital caliper) and the height corresponding to the surface of the soil to the apical bud (using a graduated ruler).

The leaves were detached from the plants to determine the leaf area using Model LICOR LI-3000. Each plant was divided into the leaves, stem, petiole and root, which were packed in paper bags and kept in an oven at 60 ºC with air circulation until a constant mass.

The dry plant matter was weighed, crushed in a Willey type mill and sampled to quantify the total concentrations of N, P, K, Ca, Mg, S, B, Cu, Fe, Mn and Zn (Malavolta et al., 1997). The total nutrient accumulation in the plant was determined by multiplying the total dry mass (g) by the total concentration of each nutrient and dividing by 1,000 to obtain the result in g and mg, for macro and micronutrients, respectively.

The total quantity of each nutrient absorbed by the plant was obtained by summing the accumulated quantities in each part of the plant. With an open-probe type auger, three soil samples were also collected from each recipient. The soil was dried and after sieving in a 2 mm mesh to analyse the contents of exchangeable K (Raij et al., 2001) and non-exchangeable K (Knudsen et al., 1986).

The K balance in the soil-plant system was calculated based on the quantity of K provided via fertilization (in g), the quantity of K absorbed by the plant (g), and the Δ K in the soil -which represents the difference between the total quantity of exchangeable K in the soil before and after the cultivation of the plants, which was 0.39 g -calculated as suggested by Castilhos et al. (2002):

ΔK in soil(g) = K available at the end of the experiment —
  — K initiaky available

For the calculation of ΔK, the contents of exchangeable K in the soil (in mg dm-3) and the volume of soil used in each recipient (50 dm-3) were considered. As the water supply was controlled, losses by leaching were disregarded. The K balance in the soil-plant system was calculated by subtracting the value of ΔK in the soil from the difference between the K provided by fertilization and the total K uptaken by the plant, according to the following equation:

K balance in the soil-plant system (g) = K fertilization —
  — K uptake by plants ΔK in soil

Negative values of the K balance in the soil-plant system represent the quantity of K released from the non-exchangeable fraction, and positive values represent the quantity of K added to the non-exchangeable and/or structural fractions.

To compare the effect of potassium fertilization on the K balance in the soil-plant system, the statistical test used was the comparison of means, using the confidence interval for the mean of 95% (p = 0.05) (Payton et al., 2000). The other results were subjected to a variance analysis and F test. When a significant effect was verified, the data were analyzed by regression and adjusted to polynomial (linear or quadratic) or exponential equations of the type "Rise to Max", as a function of the regression parameters significance, the value of F and the adjusted coefficient of determination (R2). When using the exponential equation, it is assumed that the appropriate rate (from which an increase in the value of y does not justify the increase in the rate) displays a value of "y" equal to 90% of the absolute value of the amplitude between "y0" and "ymax". The statistical program SigmaPlot 10.0 was used to perform the statistical analysis and generate graphs.

 

Results and Discussion

The potassium fertilization did not alter the concentrations of P, Ca, S, B or Cu, in leaf which displayed mean values of 2.04, 16.4, 1.75 g kg-1, 67.9 and 5.85 mg kg-1, respectively (Table 2). The Mn concentration was adjusted to an exponential model, and its increase was extremely low, starting at a concentration of 127.7 mg kg-1 for a K rate of 50 mg dm-3 (Table 2). The Mg concentration in the leaves decreased with increasing K rates (Table 2), possibly as a function of the antagonistic effect between K and Mg (Meurer, 2006) that attenuates Mg absorption when the K concentration in the soil solution increases (Fonseca & Meurer, 1997).

 

 

The foliar N concentration decreased with increasing potassium fertilization (Table 2). Nitrogen most notably interacts with K, so the stimulus to growth produced by the addition of one of these nutrients can lead to a deficiency of the other via dilution (Cantarella, 2007). In fact, this effect was observed in the present study, once increasing K concentrations lead to a linear increase of the dry matter (DM) of the leaves (y = 30.40+0.0674x, R2 = 0.19, significant at 0.05) and a decrease in the foliar N concentration (Table 2).

Linear increases in concentrations in the leaves were observed for Fe (maximum of 131.1 mg kg-1), Zn (maximum of 19.7 mg kg-1) and K (varied from 6.0 to 13.4 g kg-1) with increased K fertilization (Table 2). These values, particularly the foliar K concentration obtained with the rate of 160 mg dm-3 (13.7 g kg-1), approach those observed by Laviola & Dias (2008) in completely opened physic nut leaves and in the fructification phase. Lima et al. (2011a) studied the redistribution of macronutrients in physic nut leaves with distinct phenological stages and verified a K concentration of 37 g kg-1 in the growing leaves, 22 g kg-1 in the mature leaves and 13 g kg-1 in the leaf litter (recently fallen leaves).

The distinct foliar nutrient concentrations found in the literature for the species are due, mainly, to the fact that a standard which leaf (position and plant age) of physic nut should be collected remains lacking. In the present study, the foliar nutrient concentrations represent the average of all leaves of a plant in initial development; thus, any comparison with other results could be imprecise. In this scope, Lima et al. (2011a) confirmed that the leaves from positions 2 and 3 from the apex (considering only the completely expanded leaves) seem to be the most appropriate for analyzing the N, P, K, S, Cu, Fe, Mn and Zn concentrations. However, the appropriate mineral concentrations in the leaves for the species remain undefined, which also limits further comparisons and/or discussions.

Although an increase of foliar K concentration was observed (Table 2), this did not result in increases in height (average value of 92.1 cm), stem diameter (average value of 3.2 cm), DM of the petioles+stem (average value of 79.2 g plant-1), root DM (average value of 25.2 g plant-1) or total DM of physic nut (average value of 140.3 g plant-1). This could be attributed to the fact that physic nut possibly absorbed more K than necessary, commonly known as "luxury consumption" (Meurer, 2006), which is characterized by an increase in mineral concentrations in the tissues without an induction of a response in growth (Pavinato et al., 2009). However, it is important to emphasize that the K stored into the leaves possibly would be used later, once it is very important for the fructification phase (Meurer, 2006; Laviola & Dias, 2008).

Laviola & Dias (2008) confirmed that in the production phase the K requirement by physic nut increases. This happens because the K works at the transportation of phloem photoassimilates, being an important nutrient for the fruit formation (Marschner, 1995). This same result also raises the hypothesis that physic nut, in its initial stages of development, does not require a large amount of K. Oliveira et al. (2012) also noted that potassium fertilization did not affect the growth and yield in the first and second year of physic nut cultivation in the field.

Potassium fertilization promoted a linear increase in the leaf area (y = 5449.41+18.48x, R2 = 0.29, significant at 0.01) and DM of the leaves, the maximum values, obtained with a maximum K rate (160 mg dm-3), were 8,406.2 cm2 and 41.2 g, respectively. Prado et al. (2004) also noted that K (rates up to 220 mg dm-3) is important for the increase in the leaf area in passion fruit (Passiflora edulis) seedlings. These responses occurred mainly because, among the innumerable functions of K in the plant, the activation of enzymes that participate in photosynthesis and respiration, processes that participate in the metabolism of the leaf, are emphasized (Ernani et al., 2007).

The total accumulation of the most nutrients (Table 3) was kept constant most likely because the total DM was not altered. However, the linear increase in the accumulation of Ca (maximum of 1.12 g plant-1) and Mn (maximum of 25.45 mg plant-1) was verified in the physic nut plants (Table 3). Although the Mg concentration was reduced in the leaf, its total accumulation in the plant (1.4 g plant-1) did not change (Tables 2 and 3).

 

 

Commonly, high concentrations of K in the soil solution cause an imbalance in the Mg uptake. This occurs because the availability of nutrients is related not only to the concentration of cations in the soil but also to the ionic interactions between them (such as antagonistic interactions between K, Ca and Mg), which can occur both in the soil and in the plant and influence the availability and uptake of the elements (Tisdale et al., 1985). However, even with increased accumulation of Ca and K in the plants, the accumulation of Mg was not affected, most likely because Mg provided by the dolomitic limestone was sufficient to avoid imbalances in the uptake of this nutrient.

As a function of the increase of K fertilization, there was a linear increase in the total accumulation of K in the physic nut seedlings (Table 3), which reinforces the hypothesis that the plants absorbed a quantity of K greater than their need.

At the end of the experiment, larger rates of K used in fertilization increased the content of exchangeable K in the soil in a concentration-dependent manner (Figure 1A). The K rate of 160 mg dm-3 of soil elevated the content of exchangeable K in the soil from 7.8 (initial) to 80.3 mg dm-3. From the calculated rate of 86 mg dm-3, K fertilization not only increased the content of exchangeable K in the soil but also increased the non-exchangeable K (Figure 1B), which is due to the fact that different forms of K are in equilibrium in the soil (Rosolem et al., 2006). The rates of 80, 120 and 160 mg dm-3 contributed, respectively, with 0.22, 0.26 and 0.63 g of K to the stock of non-exchangeable and/or fixed K in the soil (Table 4).

 

 

 

 

When the rates of 0 and 40 mg dm-3 were used the non-exchangeable fraction of K supplied the K demand of the plants (Table 4). In the absence of K fertilization, the contribution of the non-exchangeable K fraction was 0.49 g, which represented 78% of all K absorbed by the plant. Fertilization with 40 mg dm-3, even increasing the exchangeable K content, reduced the K stock in 0.04 g the non-exchangeable fraction. These results indicate that physic nut can absorb K from the non-exchangeable fraction of the soil, which alludes to practical applications and explains, in part, the observation that physic nut exhibits a low demand for K in the initial growth phase and a low response to K fertilization. Thus, the fact that the plant be able to absorb K from the non-exchangeable fraction can mask the fertilization effects.

When the exchangeable K in the soil is low, the K from the non-exchangeable fraction contributes to the total K uptaken by the plants (Silva et al., 1995). One of the main mechanisms that facilitates this process is the capacity of the plants to absorb K at low K soil contents (Wang et al., 2011), which occurs because the exhaustion of K at the root surface generates a concentration gradient that results in release of non-exchangeable K (Hinsinger et al., 1993). However, there are more specific factors that can release non-exchangeable K, such as increases in the soil contents of NH4+ (Scherer, 1993), Ca2+, Mg2+ and Na2+ and, mainly, the exudation of organic acids by the roots (Wang et al., 2011). The primary mechanism that governs the release of non-exchangeable K by physic nut remains unknown and thus merits future studies to elucidate the potential for physic nut cultivation.

 

Conclusions

1. Higher rates of K used in fertilization allow greater uptake of K, Ca and Mn by physic nut seedlings.

2. The total dry mass production of physic nut is not altered by increases in potassium fertilization.

3. The physic nut can release and absorb K from the non-exchangeable soil fraction.

 

Acknowledgments

To FAPESP (State of São Paulo Research Foundation), for providing a scholarship to first author.

 

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Protocolo 184.13 – 05/06/2013
Aprovado em 06/12/2013

 

 

* (Autor correspondente)
1 Parte da Dissertação de Mestrado da primeira autora

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