Sources and rates of potassium for sweet orange production

Fontes e doses de potássio na produção de laranjeira

SOIL AND PLANT NUTRITION

Sources and rates of potassium for sweet orange production

Fontes e doses de potássio na produção de laranjeira

José Antonio Quaggio^I; Dirceu Mattos Junior^II,*; Rodrigo Marcelli Boaretto^II >

^IIAC – Centro de Solos e Recursos Ambientais, C.P. 28 – 13020-902 – Campinas, SP – Brasil

^IIIAC – Centro de Citricultura Sylvio Moreira, C.P. 04 – 13490-970 – Cordeirópolis, SP – Brasil

ABSTRACT

Fruit yield and quality of citrus trees (Citrus spp.) is markedly affected by potassium (K) fertilization. Potassium chloride is the major source of K, even though other sources are also available for agricultural use when crops are sensitive to chloride or where potential for accumulation of salts in soils exists. Only few studies addressed the effect of K sources on yield and quality of citrus fruits. Therefore, the present study was conducted to evaluate K₂SO₄ and KCl fertilizer sources at 0, 100, 200, and 300 kg ha^–1 per year K₂O on fruit yield and quality of 'Pêra' and 'Valencia' sweet orange trees in the field. The experiments were carried out in a 4 × 2 factorial design under randomized complete blocks, with four replicates from 2001 to 2004. Fruit yield increased with increased K fertilization. Nutrient rate for maximum economic yield of 'Pêra' was 200 kg ha^–1 of K₂O and for 'Valencia', 270 kg ha^–1 of K₂O. Differences were attributed to higher production and K exportation by fruits of 'Valencia'. Fruit mass also increased with increased K fertilization what decreased total soluble solids in juice, and which correlated with leaf K concentrations for 'Valencia' (r = 0.76; p < 0.05). Leaf Ca, Mg and B concentrations decreased with K rates. Additionally, leaf Cl increased up to 440 mg kg^–1 with KCl rates, even though no negative effects occurred either on fruit yield or quality of trees.

Key words:Citrus sinensis (L.) Osbeck, chloride, sulfate, mineral nutrition, nutrient management

RESUMO

Produtividade e qualidade da produção de citros (Citrus spp.) é largamente influencia pela adubação com potássio (K). O cloreto de potássio é a principal fonte K como fertilizante, embora outras fontes estejam disponíveis para uso agrícola e que são de interesse para culturas sensíveis ao cloreto ou cultivadas em solos com potencial para acúmulo de sais. Poucos pesquisadores avaliaram o efeito de fontes de K na produção e qualidade de frutas cítricas. Assim sendo, avaliaram-se fontes de K₂SO₄ e KCl nas doses de 0, 100, 200 e 300 kg ha^–1 por ano de K₂O na produção e qualidade de frutos em pomares de laranjeiras 'Pêra' e 'Valência'. Os experimentos foram instalados em delineamento fatorial do tipo 4 × 2, com quatro repetições e conduzidos no período de 2001 a 2004. A produtividade da laranjeira aumentou com a adubação potássica. O máximo rendimento econômico para a adubação com K na laranjeira 'Pêra' foi obtido na dose de 200 kg ha^–1 de K₂O, enquanto, na laranjeira 'Valência' foi de 270 kg ha^–1 de K₂O. As diferenças foram atribuídas ao maior nível de produção e exportação de K pelos frutos de 'Valência'. A massa do fruto também aumentou com o incremento nas doses de K o que determinou as perdas de sólidos solúveis totais no suco. Esta foi correlacionada com as concentrações de K nas folhas da laranjeira 'Valência' (r = 0,76; p < 0,05). A concentração de Ca, Mg e B nas folhas diminuíram com as doses de K. A concentração de Cl nas folhas aumentou até 440 mg kg^–1 com o incremento nas doses de KCl, entretanto, não foram observados efeitos adversos na produção e na qualidade dos frutos.

Palavras-chave:Citrus sinensis (L.) Osbeck, cloro, sulfato, nutrição mineral, manejo nutricional

Introduction

Fertilizers are required to support adequate mineral nutrition of citrus and to ensure high crop productivity in low fertility tropical soils. Fruit yield and quality of citrus trees depends largely on nitrogen (N) and potassium (K) fertilization (Cantarella et al., 2003; Alva et al., 2006), elements which represent the greatest quantity of nutrients exported through harvest (Bataglia et al., 1977; Mattos Jr. et al., 2003). Furthermore, under abiotic stress conditions as salinity or drought, N and K may contribute to reduce excess absorption of sodium (Na) and chloride (Cl) by citrus trees because of the competitive root uptake observed between NO₃^–/Cl^– and K⁺/Na⁺ (Gimeno et al., 2009).

Potassium also affects external fruit characteristics, since those become larger and coarser as the K supply increases; on the other hand, K deficiency reduces number and fruit size of all citrus varieties and decreases soluble solids content of juice (Alva et al., 2006). Therefore, optimization of fruit quality for either fresh consumption or frozen concen trated orange juice production is supported by adequate nu trient management (Quaggio et al., 2005; Obreza et al., 2008).

Potassium chloride is the major source of K, even though other sources such as potassium sulfate and potas sium nitrate are also available for agricultural use. These later are usually more expensive but are preferred for crops that -are sensitive to chloride, as citrus (Bañuls and Primo-Millo, 1992), or for those grown where potential for accumulation of salts in soils exists (Laegreid et al., 1999); other characteristics may also favor the use of the same via fertigation.

Koo and Reese (1972) evaluated the effect of K sources on yield and quality of citrus fruits, which were primarily con-ducted in very coarse textured Entisols. Because of differences on anion retention in the soil colloidal complex associated to increased interest on the use of alternative K-sources for citrus production, this work compared the effect of sources and rates of K on fruit yield and quality of two orange cultivars, and established the effects of sulfur and chloride supply on the chemical characteristics of soils and nutritional status of trees.

Material and Methods

Field experiments were conducted with 5-year-old sweet orange trees grown in commercial groves located in two citrus producing regions of the State of São Paulo, Brazil, from 2000 to 2004. The first site, Santa Cruz do Rio Pardo (southern region of the State; 22º48'50" S, 49º22'40" W), Brazil, is characterized by occurrence of mild temperatures and very low water deficit along the year (mean annual temperature < 23ºC and rainfall = 1,760 mm), with a inherent low fertility, sandy to medium textured soil with the following chemical characteristics: organic matter (OM) = 13.8 g dm^–3; pH(0.01 M CaCl₂) = 4.3; K (resin extracted) = 0.6 mmol_c dm^–3; cation exchange capacity (CEC) = 43.9 mmol_c dm^–3 and soil base saturation (V) = 34.5%. Oranges produced on this site {'Pêra' sweet orange [Citrus sinensis (L.) Osb.] on Rangpur lime

(C. limonia Osb.)} are mostly destined to the fresh fruit market. The second site, Matão (central-north region of the State; 21º35'50' S, 48º26'10" W), Brazil, presents higher temperatures and frequent drought periods during the winter season (mean annual temperature ≥ 23ºC and rainfall of 1,350 mm); the soil had the following chemical characteristics: OM = 18.5 g dm^–3; pH(0.01 M CaCl₂) = 4.8; K (resin extracted) = 0.7 mmol _c dm^–3; CEC = 57.5 mmol _c dm^–3 and V = 39%. Fruits ['Valencia' sweet orange (C. sinensis) on Rangpur lime] are destined for frozen concentrated orange juice (FCOJ) production. Both experiments were conducted without irrigation.

Experiments were carried out in a 4 × 2 factorial design under randomized complete blocks, with four replicates, to evaluate the effects of K rates (0, 100, 200, and 300 kg ha^–1 per year K₂O) and sources (K₂SO₄ and KCl) on fruit yield and quality of oranges. Each experimental plot of the 32 plots consisted of four rows with five uniform trees per row, summing up 20 trees. Only the six central trees within each plot were used for sampling and yield control. Fertilizer amounts for each treatment were hand applied to the soil surface in three split applications, on both sides of trees (on 150 cm wide bands, 50 cm away from tree trunk), from early spring to late summer.

Fruit yield was measured annually by summing up the mass of fruits, if more than one harvest per year occurred. Fruit samples (n = 15) were collected at maturation for fresh mass of fruits and percent juice content (based on mass fraction) evaluation as well as juice quality, by determining total soluble solids concentration (TSS), acidity, and total soluble solids/acidity ratio (Redd et al., 1986). The amounts of TSS content per orange box (40.8 kg) and per area (kg ha^–1) were calculated. Four to six-month-old spring flush leaves were annually sampled from fruiting terminals and analyzed for total nutrient concentrations according to Bataglia et al. (1983). Soil samples were annually collected from the 0-0.2 m depth layer and analyzed according to methods described by Raij et al. (2001).

Rates of K for maximum economic fruit yield were estimated as follows: dY/dX = C/F, where: Y = fruit yield (t ha^–1); X = K rate (kg ha^–1 of K₂O); C = cost of K fertilizer (1.00 US$ kg^–1 of K₂O) and F = price of fruits (120.00 US$ t^–1 of oranges). Data were tested for significant differences among treatments using the analysis of variance (ANOVA) with the GLM procedure of the SAS^® System (1996). Selected variables were adjusted by regression and correlation model analyses using the PROC REG and the PROC CORR procedures of the SAS^®, respectively.

Results and Discussion

Potassium fertilization affected fruit yield in both experimental sites, but no significant effects were observed for K sources in the long term study. A more marked response on fruit yield occurred in Matão, with 'Valencia', where the average orange production increased after four harvest seasons from 35 to 50 t ha^–1 per year with an increase in K₂O rate from 0 to 300 kg ha^–1 (Figure 1A and 1B). At both sites the initial K concentration in the soil was low (< 0.7 mmol _c dm^–3); linear relationships for soil exchangeable K were observed with K rates (Figure 1A and 1B; p < 0.05). Fruit yield correlated with increased availability of K in the soil to approximately K = 2.7 mmol _c dm^–3, which is similar to the critical level established for citrus trees (Quaggio et al., 1998); furthermore depressive effects of K fertilization on fruit yield were verified with soil exchangeable K higher than 2.9 mmol_c dm^–3 (Quaggio et al., 2008).

Maximum fruit yield of 'Pêra' was obtained with 242 kg ha^–1 of K₂O (Figure 1A), while fruit size was maximized with 282 kg ha^–1 of K₂O (Figure 2A). Similarly, fruit yield of 'Valencia' was obtained with 302 kg ha^–1 (Figure 1B) and maximum fruit size with 248 kg ha^–1 of K₂O (Figure 2B). In a research with seven year-old 'Marsh' grapefruit trees, Koo and Reese (1972) demonstrated that fruit yield increased with increase in K₂O application up to 188 kg ha^–1, with further increase in K₂O rate to 282 kg ha^–1 and had no positive effect on fruit yield. In another study, Reese and Koo (1975) also verified that the fruit yield of different orange variety trees increased similarly with K supply. Therefore, citrus responses to K supply occur in good agreement when grown in soils of low exchangeable-K, which are characteristic of the areas either of the present studies or of central Florida (USA).

The K₂O rate for maximum profit was obtained with approximately 200 kg ha^–1 for 'Pêra' and 270 kg ha^–1 for 'Valencia'. 'Valencia' is usually more productive than 'Pêra' (Pio et al., 2005) and have fruits which are expected to export more K (2.0 kg t^–1) than those of the later and other early season orange varieties (1.5 kg t^–1) (Bataglia et al., 1977). Therefore, the nutrient demand of the 'Valencia' grove and consequently the response to K fertilization was more meaningful.

Fruits for both varieties were large, with approximately 220 g for 'Valencia' and 180 g for 'Pêra', which despite the size still increased 7-8 % in mass with K fertilization in both sites (Figure 2A and 2B), in correspondence to previous data reported by Quaggio et al. (2006). There were no differences in fruit mass due to K sources, the effect of which was also observed for 'Marsh' grapefruit trees fertilized with either KCl or K₂SO₄ (Koo and Reese, 1972). In addition, in this study K fertilization affected the number of fruits per tree which was 25% greater in Matão and only 7% greater in Santa Cruz both compared to the non-fertilized treatments (Figure 2B).

Characteristics of fruit quality of 'Pêra' oranges were not affected by K fertilization for averaged values in Santa Cruz do Rio Pardo during 2001-2004 (Table 1). Exception occurred in 2003, when total soluble solids varied with the fertilizer source, and a 7% increase in the amount of TSS per box of oranges fertilized with K₂SO₄ was observed (data not shown). Trees were subjected to an exceptional drought stress in that year, when excess accumulation of salts in the soil probably occurred during short periods and impaired normal plant development and fruit maturation. The increase in TSS per area (400 kg ha^–1 TSS with K₂O rates varying from 0 to 300 kg ha^–1) was mostly related to the increase in fruit production obtained in the same site (Table 1). Even though TSS of fruits might decrease with increased fruit size (Quaggio et al., 2006), in the present study a decrease of 0.2

0.3 kg per box of TSS between 0 and 300 kg ha^–1 K₂O was observed in the 'Valencia' grove, which was due to a decrease in the content of juice rather to a decrease in the quality of the juice as TSS was not affected by fertilizer sources (Table 2). On the other hand, the variation in fruit yield positively affected TSS per area in both experimental sites (Tables 1 and 2). This is explained by the effect K presents on fruit mass, which is primarily associated to an increase in fruit peel thickness. A negative relationship was established between production of TSS (y) and fruit mass of 'Valencia' oranges (x) (y = -0.0084x + 4.33; r = 0.76, p < 0.05). Similar results were obtained in N, P and K fertilization experiments conducted in the field with lemon (Quaggio et al., 2002) and oranges (Quaggio et al., 2006). Such effect and other of increasing levels of fertilizers on fruit yield and quality were summarized by Obreza et al. (2008).

Foliar concentration of K in both orange varieties increased up to 15 g kg^–1 with K fertilization (Figure 3). Koo and Reese (1972) also verified effects of fertilization on leaf K concentrations, which varied from 12 to 22 g kg^–1 in an experiment with young 'Hamlin' orange trees. Adequate levels of leaf K, 10-15 mg kg^–1 (Quaggio et al., 2005) were attained with K rates between 100 and 300 kg ha^–1 per year of K₂O. On the other hand, Ca and Mg leaf concentrations were below those considered adequate for improved fruit yield of citrus trees (Quaggio et al., 2005) with application of higher K₂O rates (Figure 4A and B). The equilibrium of exchangeable cations in the soil is proportional to the activity ratio of K for divalent cations in soil solution. Thus, increased rates of K₂O primarily cause an increase on the activity of this former element and consequently a decrease on root uptake of Ca and Mg (Jakobsen, 1993). These effects must be considered by fertilizer recommendations in order to prevent possible nutritional imbalances in the grove that will probably cause fruit yield losses. Research results have pointed out to lower Ca and Mg contents in the spring flush leaves collected from fruiting terminals in a commercial grove with six-year-old 'Murcott' tangor trees conducted on a sandy loam Oxisol. This caused the occurrence of stem dieback and reduced fruit yield because of the high rates of K applied during several years of fertilization (Mattos Jr. et al., 2003).

Leaf concentration of sulfur (S) did not change with fertilizer sources, with approximately 3.0 g kg^–1 for all tested K rates (Figure 5A and 5B). Fruit yield responses of citrus do not suffer much interference when leaf S is above 2.0 g kg^–1 (Malavolta et al., 1987), which is probably associated to the limited amount of the nutrient exported with fruit harvest (about 4.5 kg ha^–1; Mattos Jr. et al., 2007). Furthermore, S supply by pesticide and micronutrient applications in citrus groves likely hindered the effects of additional input of this nutrient with the use of K₂SO₄. An annual input of 30 to 50 kg ha^–1 of S is estimated because of management practices, and which amounts may far exceed such range if nitrogen and phosphorus fertilizers containing S are used (Mattos Jr. et al., 2007). On the other hand, chloride (Cl) concentration in the leaves of trees varied with the application of KCl fertilizer, which was up to 375 mg kg^–1 (Figure 5C and 5D). However, there were no adverse effects on fruit yield and quality of trees caused by Cl. Effects of excess Cl are expected to occur when leaf concentration is above 1000-2000 mg kg^–1 as reported for orange (Syvertsen et al., 1993), lemon (García-Sánchez et al., 2003) and mandarin trees (García-Sánchez et al., 2006); this is also greatly dependent on citrus species since lemons are more sensitive than oranges (Lloyd et al., 1989) as well as on rootstock varieties (Ruiz et al., 1997; García-Sánchez et al., 2003, 2006).

Other results of leaf analysis demonstrated a significant interaction (p < 0.05) between K and B contents of leaves in both locations, in which leaf B decreased about ten units B with increased K fertilization (Figure 6A and 6B). Such effect was also described for alfalfa (Wallace and Bear, 1949) and avocados (Jaime et al., 1992), even though no specific mechanism at the plant level was proposed to explain such results. Conversely, K uptake by plants is increased with B supply (Cooper et al., 1952; Schon et al., 1990; Obermeyer et al., 1996; Quaggio et al., 2003; Grassi et al., 2004). In this case, B facilitates K uptake probably because of increased hyperpolarization of the plasma membrane (Schon et al., 1990).

Conclusions

Potassium rates affected production of both orange varieties, even though there were no effects of KCl and K₂SO₄ sources on either fruit yield or quality in the long term study. Fruit size increased with K supply, which was associated with increased leaf K concentration. Despite K fertilization caused least differences on total soluble solids (TSS) concentration of orange juice, TSS yield per area basis increased by increasing the K rates. Leaf concentration of S did not change with potassium sources. On the other hand, chlorine levels in the leaf varied with rates of KCl. However, no adverse effects on fruit yield and quality of trees were caused by excess Cl. Increased leaf K caused decreases on leaf Ca, Mg and B. A linear increase on soil exchangeable K occurred with increased K fertilization, even though maximum fruit yield was observed at approximately K = 2.7 mmol _c dm^–3.

Acknowledgements

To FAPESP for financial support, CNPq for research fellowships and Grupo Nova America (Santa Cruz do Rio Pardo) and Cambuhy Agrícola (Matão) for field assistance.

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Received February 19, 2010

Accepted November 04, 2010

Publication Dates

• Publication in this collection
  11 July 2011
• Date of issue
  June 2011

History

• Received
  19 Feb 2010
• Accepted
  04 Nov 2010