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Brazilian Archives of Biology and Technology

Print version ISSN 1516-8913On-line version ISSN 1678-4324

Braz. arch. biol. technol. vol.50 no.4 Curitiba July 2007

http://dx.doi.org/10.1590/S1516-89132007000400005 

AGRICULTURE, AGRIBUSINESS AND BIOTECHNOLOGY

 

Shoot and root responses of Trifolium vesiculosum to boron fertilization in an acidic Brazilian soil

 

 

Nerilde FavarettoI, *; Antônio Carlos Vargas MottaI; Cristina BarcikI; Sebastião Brasil Campos LustosaII; Jucinei José CominIII

IDepartamento de Solos e Engenharia Agrícola; Universidade Federal do Paraná; Rua dos Funcionários, 1540; nfavaretto@ufpr.br; mottaacv@ufpr.br; 80035-050; Curitiba - PR - Brasil
IICentro de Ciências Agrárias e Ambientais, Universidade Estadual do Centro-Oeste; Campus de Guarapuava; Rua Presidente Zacarias, 875; C.P. 3010; 85015-430; Guarapuava - PR - Brasil
IIIDepartamento de Engenharia Rural; Universidade Federal de Santa Catarina; Bairro Trindade; 88040-970; Florianópolis - SC - Brasil

 

 


ABSTRACT

To analyze the influence of boron fertilization on shoot and root growth of Trifolium vesiculosum (arrowleaf clover), an acid soil profile (60 cm depth with 67% Al saturation) was recreated in a column (three layers of 20 cm each). Lime and fertilizer (P and K) were incorporated into the top 20 cm. The treatments consisted of six boron rates where boric acid was mixed throughout the profile. Addition of boron to soil with low pH and high Al increased the root and shoot growth, independent of the rate applied. Boron inhibited Al toxicity, but no effect was observed in the root length when Al was not present in the soil. It was also observed that there was more root growth below the plow layer (0-20 cm,) suggesting better root distribution in the soil profile which could be important for the plant growth, especially under drought conditions.

Key words: Root and shoot growth, boron, aluminum, acidic soil


RESUMO

Estudos têm mostrado que o boro (B) afeta o crescimento das raízes em solo ácido reduzindo a toxidez do alumínio (Al). Para analisar a influência do boro no crescimento da parte aérea e raízes do Trifolium Vesiculosum (trevo vesiculoso) um perfil de solo ácido (60 cm de profundidade com 67% de saturação de Al) foi recriado em uma coluna (três camadas com 20 cm cada). Calcário e adubos (P e K) foram incorporados na camada de 0-20 cm. Os tratamentos consistiram de seis doses de boro sendo o ácido bórico incorporado em todo o perfil. A adubação com boro em solo com baixo pH e elevado Al aumentou o crescimento da parte aérea e raízes, no entanto, independente da dose aplicada. Boro pode inibir a toxidez de Al, porém não observou-se efeito no comprimento de raízes sem a presença de Al no solo. Observou-se também um grande aumento no crescimento de raízes abaixo da camada arável (0-20 cm), fornecendo uma melhor distribuição de raízes no perfil do solo, o que pode ser importante para o crescimento da planta especialmente em condição de seca.


 

 

INTRODUCTION

The development of root system involves complex belowground interactions. The chemical conditions of the soils have a great influence on the root growth. It is well known that high levels of aluminum (Al) inhibits the root growth. In agriculture, especially in the tropics, aluminum toxicity is one of the main factors that limits crop production in acid soils. Soil acidity and consequently Al toxicity in the upper soil layers can be easily corrected by liming, however, due to slow mobility of lime material, surface application without some degree of mixing are not effective in correcting subsoil acidity. Neutralization of subsoil acidity through deep incorporation is possible, but it increases cost and in some situations, no beneficial effects on crop production are observed (Tisdale et al., 1993).

Besides Al toxicity, boron (B) deficiency is another important factor that inhibits the root growth (Marschner, 1995; Castro et al., 2003). Studies have shown that boron fertilization can decrease the effect of Al toxicity (LeNoble et al., 1996a, 1996b; Lukaszewski and Blevins, 1996). According to LeNoble et al. (1996a), it is possible that Al inhibits root growth by inducing boron deficiency and that the boron requirement for optimal root growth under acidic and high Al conditions may be higher than the requirement under low Al levels. In soil, boron is considered a mobile element, easily reaching subsoil layers. Thus, leaching of surface applied boron could increase the boron level in the subsoil, thereby increasing the depth of the root growth (Smith et al., 1993; LeNoble et al., 1996b). However, the narrow concentration range between boron deficiency and toxicity requires special care in boron fertilization (Gupta et al., 1985; Marschner, 1995; Grassi Filho et al., 2004). Among the sources of boron in soil, organic matter plays an important role, thus, plants growing in sandy soils tend to develop boron deficiencies because of very low organic reserves (Gupta et al., 1985; Luchese et al., 1994).

Plants have different requirements and usually dicotyledons are more exigent than monocotyledons. In plants, boron is classified as an immobile element, consequently symptoms of deficiency in the shoots are noticeable on the youngest leaves, and the internodes are shorter giving the plants a bushy or rosette appearance (Gupta et al., 1985; Marschner, 1995).

In southern Brazil, many forage species have been introduced, including Trifolium vesiculosum, Savi (arrowleaf clover), a winter annual legume. For good development the soil pH should be between 5 and 6 and boron may be needed in sandy soils to enhance the root growth (Hoveland and Evans, 1995). According to Gupta et al. (1985), the optimum hot-water extractable boron level in soil for clover growth was generally greater than 0.5 mg kg-1.

The overall objective of the present study was to determine if boron applied at different rates could reduce subsoil Al toxicity in Trifolium vesiculosum crop. The hypothesis was that boron could decrease the effect of Al toxicity on the root growth mainly.

 

MATERIALS AND METHODS

This experiment had six treatments (boron rates), arranged in a completely randomized design with six replicates and was conducted at the greenhouse complex of the Soil Department of the Federal University of Paraná State, Curitiba, Brazil. The soil profile was recreated in white plastic columns (20 cm diameter, 63 cm long) with three layers of soil (0-20, 20-40 and 40-60 cm) here referred as the A, B, and C layers, respectively. The soil used was removed (also in three layers) from a grassland field in Ponta Grossa, Paraná. The soil was a "Cambissolo álico" with medium texture, high Al content, and low pH, organic matter and nutrients. The chemical and physical properties of each layer are presented in Tables 1 and 2.

Soil particle and bulk density were determined by the hydrometer and cylinder methods, respectively, according to EMBRAPA (1997). The pH was determined in CaCl2 0.01 M; H+Al via SMP solution; Ca, Mg and Al extracted by KCl 1N; P and K via Mehlich I; total organic C by colorimetry (Pavan et al., 1992); Fe, Mn, Cu, and Zn by HCl 0.1 N (Hildebrand, 1977); and B by BaCl2 using the microwave technique of Abreu et al. (1994).

The upper soil layer (0-20 cm) was limed (4.3 Mg ha-1) according to the base saturation recommendation (IAC, 1996) and fertilized with 320 and 140 kg ha-1 of P2O5 (phosphate monocalcium) and K2O (potassium sulfate and chlorite), respectively. Since this experiment was conducted in the pots, the P and K addition was double the value recommended for the field clover by Comissão de Fertilidade do Solo-RS/SC (1994). Liming and fertilization were conducted one month before and at the day of planting, respectively. The chemical condition of soil in layer A (0-20 cm) at planting was the following: pH CaCl2 (5); Al3+, H++Al3+, Ca2+, Mg2+, K+, and CEC (0, 4, 2.1, 1.6, 0.24 and 7.9 cmolc dm-3, respectively); Al saturation and base saturation (0 and 50% respectively). The second and third layers did not receive lime and P and K fertilizer. All three layers received the same amount of B (boric acid) according to the respective treatments (0, 0.25, 0.5, 0.75, 1 and 2 kg ha-1 of B).

After the fertilization, each pot received 10 arrowleaf clover (Trifolium vesiculosum) seeds inoculated with rhyzobium. After seedling establishment (30 days), pots were thinned to four plants per pot. Plants were watered periodically with deionized water. The experiment was conducted until flowering (4.5 months). Aboveground biomass was sampled, cleaned with deionized water and dried for the determination of weight and nutrient concentration. Boron concentration was determined on sieved (2 mm) biomass samples for all the experimental units via dry digestion according to Hildebrand (1977).

Root samples were collected from each layer and cleaned with water using a set of sieves with screen openings of 2 and 0.2 mm. The separation of clover roots from the organic debris was done by hand using tweezers. Afterwards, the roots were stored in plastic bags containing 50% ethanol and placed in a freezer (0 °C). The variables measured were root dry weight, length and medium ratio. The root mass was determined after oven drying the samples at 60 °C until constant weight was attained. Root length was determined according to Tennant (1975) using the following equation: C=N*fc, where: C was the length (cm), N was the number of intersections and fc was a correction factor. The screen used for counting the root intersections had 1 cm2 square grids with an fc value of 0.7857. The total length in each layer was calculated from a 0.5 g subsample of wet mass. The medium ratio was calculated according to Shenk and Barker (1978) using the following equation: r = (mf/(c*p))0.5, where: r was the medium ratio, mf was the wet weight and p was a constant. During the root sampling, soil samples were collected from each layer to determine boron concentration.

Analyses of variance and mean comparison were made using SAS software. Soil and root variables were analyzed using a split plot model where rate of boron correspond to the whole plot and layer to the subplot; other variables were analyzed as one factor in a complete randomized model. Preliminary statistical analyses indicated that some variables had to be transformed in order to achieve the requisites for an analysis of variance. A regression between the log (standard deviation) and log (mean) was performed for each variable to define which transformation should be used (Box et al., 1978). When necessary, the data were transformed, but presented in their original form.

 

RESULTS AND DISCUSSION

Plant growth

The shoot dry weight increased up to 130% with boron fertilization. The smallest mean (5.03 g, treatment without boron) was significantly different from means of all boron applied rates (Fig. 1). In agreement with these results, Haby et al. (1993) and Smith et al. (1993) reported a significant increase in the clover shoot growth when boron was applied to an acid sandy soil from Texas. The maximum increase (11.52 g) was obtained from 0.5 kg ha-1 application of B, however, no significant differences were observed among boron rates, except on 0.75 kg ha-1 of B (Fig. 1). Since all the treatments received lime in the upper soil layer and that they had high Al levels in the subsoil, results indicated that boron could reduce the effects of Al on aerial growth. LeNoble et al. (1996b) observed that high Al in the subsoil inhibited shoot growth of alfalfa, but they did not report significant differences in treatments with supplemental boron.

 

 

As expected, the level of boron in plant tissue increased linearly with boron fertilization (Fig.1). The maximum value (50 mg kg-1) was for the pots treated with 2 kg ha-1 of B and the smallest (35 mg kg-1) for the controls (no boron applied).

According to Gupta et al. (1985), dicots (e.g., clover), required more boron than monocots. For white clover in association with ryegrass, the critical level of boron in tissue was 25-35 mg kg-1 (Dunlop and Hart, 1987), and for red clover, concentrations less than 20 mg kg-1 were related to boron deficiency symptoms (Gupta et al., 1985). Deficiencies in the field occurred when boron levels in the plant was less than 15 mg kg-1 (dry weight basis) while boron concentration between 20 and 200 mg kg-1 were adequate for the growth. Boron toxicity under field conditions generally occurred when plant concentrations exceed 200 mg kg-1. However, these were only general guidelines, and plants responded differently depending on many factors, including species and soil conditions (Gupta et al., 1985; Marschner, 1995). In this experiment, symptoms of deficiency and toxicity were seen in both the control and the 2 kg ha-1 of B treatments. However, the levels of boron in the plant tissue (35 to 50 mg kg-1) would have been considered adequate.

Root growth

Root dry weight

Root dry weight in each layer was significantly higher in the treatments with applied boron compared to the control with no B (Fig. 2), indicating that boron promoted root growth (Smith et al., 1993; Lukaszewski and Blevins, 1996). However, no statistical difference was observed among the rates of boron applied. LeNoble et al. (1996b) observed higher dry weight for treatments with boron applied throughout a subsoil having a high Al level, but they reported statistical differences only at the 90-120 cm depth. The soil aluminum status could explain the difference since LeNoble et al. (1996b) used soil with lower Al saturation compared with that used in this experiment.

 

 

Increased root dry weights of 74-88, 100-198, and 498-693% were observed for the respective first, second, and third layers where boron was applied compared to the control. Thus, enhancement of root growth due to boron application occurred throughout the whole soil profile. Large increases in root dry matter with boron application was also reported by LeNoble et al. (1996b) who found a 300% increase at the 90-120 cm depth. Changes in root dry weight at the 0-20 cm depth was not expected due to soil acidity correction, suggesting a natural lack of B.

Measurement of dry weight by the layer provided information about root behavior with depth. Results showed that the roots grew mainly in the A layer, decreasing gradually with depth. The dry weight in layers A, B, and C was 2.80, 0.40 and 0.33 g, respectively. Considering total root growth (3.53 g) independent of the applied boron, layers A, B and C constitute 79.3, 11.3 and 9.4% of the total, respectively. The contribution of each layer within each rate of boron applied is shown in Fig. 3. Boron application resulted in better root distribution since only 12% of root dry matter was found in the B and C layers without boron as compared to 19- 25% with boron.

 

 

Root length

Root length was significantly higher in the treatments with boron applied, compared to the control treatment (without B) only in layers B and C (Fig. 4). The A soil layer (0-20 cm) was limed and fertilized with P and K, thus no Al was present in this layer. The lack of differences among the treatments showed that supplemental boron affected the root length only in the high Al layers. LeNoble et al. (1996b) reported that boron applied throughout a high Al profile promoted significant increases in the root length and dry weight at the 90-120 cm depth. Increased root lengths of 7-29, 196-266, and 629-940% were observed for the respective first, second, and third layers where boron was applied compared to the control. This indicated that root length responded more to boron application than root dry weight, especially in the second and third layers (20-60 cm). Similarly, LeNoble et al. (1996b) noted higher increases in root length density compared to dry root weight with depth. This could be explained by an increase in the total number of lateral roots as was noted by Smith et al. (1993).

 

 

Root length by the depth showed the same trend as the root dry weight, with the highest concentration occurring in the upper 20 cm. The average root length in layers A, B, and C was 37776, 7901, and 6486 cm, respectively. Considering total root growth (52163 cm) independent of boron applied, layers A, B, and C constituted 72.4, 15.2 and 12.4% of the total, respectively. Fig. 3 shows the contribution of each layer within each rate of boron applied. As observed for the root dry matter, the boron application resulted in better root length distribution since only 10% of the root length was found in the B and C layer in the treatment without boron compared to 27-33% with boron.

Previous reports indicated that higher root growth in the sub-surface soil compared to plow layer, resulted in a more even root distribution in the soil profile when gypsum (Souza and Ritchey, 1986; Farina et al., 2000) and boron (LeNoble et al., 1996b) were applied. This suggested that boron application could help the plant to resist drought and to use nutrients within the subsoil (Souza and Ritchey, 1986). This could explain the better seedling establishment, growth and survival of clover noted by Smith et al. (1993). The increase in root dry mass and length below the plow layer (0-20 cm) highlighted the importance of boron under high Al levels which could aid plants under stress conditions.

Root ratio

In the length measurement, the taproots were not considered, while with dry weight they were considered. Thus, apparently boron was more important for diameter than length. However, this was not observed in the present results. Root ratio did not show interaction between the soil layers and boron rates. Differences were observed only among the layers, and as expected, the values were higher in the layer A compared to the layers B and C.

Soil

As expected, the boron level increased linearly according to the rate applied to the soil for all the layers (Fig. 5). However, higher levels of boron were detected in the C layer compared to the others. This was probably due to the boron contribution from the upper soil layers since the sorption of boron to soil was weak (Pavan and Correa, 1988), resulting high mobility, especially in the sandy soil (Gupta et al., 1985; Marschner, 1995). The amount of boron recovered from the A, B, and C layers was 72, 76, and 102% of the boron applied to the soil, respectively. The recovery was calculated using the angular coefficient from the regression between boron in the soil and the rate of boron applied to each layer. These results confirmed the high recovery of boron application from the fertilizer as well as the leaching effect (Gupta et al., 1985).

 

 

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Received: November 01, 2005;
Revised: August 04, 2006;
Accepted: March 12, 2007.

 

 

* Author for correspondence

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