Potencial hídrico e trocas gasosas em cana-de-açúcar irrigada com águas salinas

rbeaa Revista Brasileira de Engenharia Agrícola e Ambiental Rev. bras. eng. agríc. ambient. 1415-4366 1807-1929 Departamento de Engenharia Agrícola - UFCG RESUMO Em Pernambuco, estado da região nordeste do Brasil, nas áreas litorâneas, devido à intrusão da água do mar, as águas utilizadas para irrigação da cana-de-açúcar podem apresentar altos teores de sais e causar sérios problemas no solo e na planta. Com o presente trabalho objetivou-se avaliar os efeitos da salinidade da água de irrigação sobre a fisiologia da cana-de-açúcar, variedade RB867515, irrigada sob cinco níveis de salinidade de 0,5; 2,0; 3,5; 5,0 e 6,5 dS m-1 com delineamento inteiramente casualizado com quatro repetições em lisímetros de drenagem. A pesquisa foi conduzida no período de dezembro de 2014 a junho de 2015, na Universidade Federal Rural de Pernambuco (UFRPE). Os níveis de salinidade foram obtidos pela diluição de NaCl e CaCl2 à água de abastecimento local (CEw = 0,5 dS m-1). Nas folhas foram feitas leituras de condutância estomática, transpiração e fotossíntese aos 140, 229 e 320 dias após o plantio (DAP) e do potencial hídrico aos 137, 243 e 318 DAP. O aumento da salinidade da água de irrigação inibiu todas as variáveis nas respectivas idades das plantas e com maior intensidade nas primeiras avaliações (140 e 229 DAP) para condutância estomática e transpiração. A fotossíntese e o potencial hídrico apresentaram maiores reduções lineares na última coleta de dados (320 e 318 DAP) respectivamente. O aumento da salinidade da água de irrigação prejudicou o potencial hídrico e as trocas gasosas nas folhas de cana-de-açúcar RB867515. Introduction Brazil is the largest global producer of sugarcane (CONAB, 2017) and in Pernambuco most of the production occurs in the coastal areas. In these areas, due to seawater intrusion, irrigation waters may have high salinity level and cause serious problems of production. In these situations, the effects of salts on plants cause restrictions in CO2 assimilation, decline in chlorophyll content, leading to losses in photosynthesis, among other metabolic alterations (Munns & Tester, 2008; Chaves et al., 2009). High concentration of salts in the soil reduces the osmotic potential, compromising water absorption by plants, especially in sensitive species. Sugarcane is a glycophyte moderately sensitive to salts (Sengar et al., 2013; Kumar et al., 2014) and, when subjected to salinity, its evapotranspiration is reduced, especially in the initial stages of cultivation (Santana et al., 2007). Water stress, which can be originated from the effect of salinity (Mortele et al., 2006), has effect on canopy architecture, playing an important role in the yield, because the canopy intercepts light, affecting the processes of photosynthesis and transpiration (Smit & Singels, 2006; Trentin et al., 2011). Water potential in the leaf is very important to understand the water relations in the plant and between plant and external environment (soil and atmosphere) (Correia, 2014). This potential provides a relative index of the water stress to which the plant is subjected, identifying various physiological alterations, in which the most affected process is cell growth, followed by photosynthesis (Taiz et al., 2017). Salinity hampers gas exchanges in glycophyte plants in general, including the physiology of sugarcane (Souto Filho et al., 2014; Andrade et al., 2015). In this context, this study aimed to evaluate the effects of irrigation water salinity on the responses of gas exchange and water potential in irrigated sugarcane, variety RB867515, using water with increasing salinity levels. Material and Methods The study was carried out at the Irrigated Agricultural Station Prof. Ronaldo Freire de Moura, located in the Department of Agricultural Engineering (DEAGRI) of the Federal Rural University of Pernambuco (UFRPE), Campus of Recife, at 8° 1’ 5” S, 34° 56’ 48” W and altitude of 6.5 m, according to the SAD 69 (South American Datum) system. The lysimeters used had capacity for 1000 L each, external diameter of 1.38 m and height of 0.745 m, buried at 0.65 m depth, with an edge of 0.10 m above soil surface to avoid the entry of rainwater or irrigation water, from runoff. These lysimeters were equidistantly placed at 1.20 m in both directions and the internal drainage system was composed of 50-mm-diameter corrugated pipe, covered with a geotextile to prevent soil particles from entering the drain. A 0.2 m3-layer of crushed stone was placed above the drain and a geotextile was laid above the crushed stone also to serve as a filter. Above the geotextile, each lysimeter received 1070 kg of dry soil. The experimental design was completely randomized with 4 replicates, totaling 20 experimental plots. The studied salinity levels were: T1 = 0.5; T2 = 2.0; T3 = 3.5; T4 = 5.0 and T5 = 6.5 dS m-1, obtained by the addition of NaCl and CaCl2 at molar ratio of 1:1 (Ca:Na), respectively, in the water from the local supply system of the UFRPE (ECw = 0.5 dS m-1), using the quantities necessary to achieve the ECw levels of the respective treatments, according to Rhoades et al. (2000) Eq. 1: Q = 640 E C w (1) where: Q - quantity of salts (mg L-1); and, ECw - desired value of water electrical conductivity (dS m-1). For the control (T1), only water from the local supply system was used, with no addition of salts. The sugarcane variety RB867515 was used and its cuttings came from the Sugarcane Experimental Station of Carpina (EECAC-UFRPE); each lysimeter was planted with six cuttings, with two buds each. In the initial stage of the experiment, irrigations were performed using water from the local supply system, applying 4 mm every two days in all lysimeters, to ensure sprouting and establishment of the plants. At 60 days after planting (DAP), daily irrigations began using the respective saline waters based on crop evapotranspiration (ETc), calculated as the product between reference evapotranspiration (ETo) and crop coefficient (kc). ETo was obtained according to the climate data of an automatic meteorological station (Campbell Scientific, CR1000/CFM100/OS100) located in the area, which provided the result using the Penman-Monteith equation (Allen et al., 1998). The kc used corresponded to the phenological stage of the plant, according to the Food and Agriculture Organization of the United Nations – FAO (Allen et al., 1998). A drip irrigation system was used, with four pressure-compensating emitters per lysimeter, spaced at 0.30 m, with mean flow rate measured in the field of 4.2 L h-1 per emitter. Irrigation was not applied on days in which rainfall was equal to or higher than crop evapotranspiration. At 137, 243 and 318 DAP, leaf water potential was analyzed using the Scholander Chamber. Analyses were conducted in the early morning before the sunrise, when the plant is in equilibrium with the surrounding environment. At 140, 229 and 320 DAP, gas exchange was evaluated: stomatal conductance, photosynthesis and transpiration, using an infrared gas analyzer (IRGA LI-6200). Readings were taken between 11 and 13 h, a time of intense sunshine and high evapotranspiration demand, on a typical day without nebulosity, to avoid instabilities caused by rapid variations in solar radiation. All analyses were carried out in one leaf per lysimeter, physiologically active and not shaded, in the +3 leaf, according to the numbering proposed by Kuijper (Dillewijn, 1952). The data were subjected to analysis of variance by F test (p < 0.05 and < 0.01) and regression, using the statistical program SISVAR (Ferreira, 2014), and one analysis was performed for each DAP. Results and Discussion The increment in water salinity linearly inhibited stomatal conductance at rates of 0.0222, 0.0155 and 0.0143 (mol m-2 S-1) per unit increase in irrigation water electrical conductivity, regardless of the ages evaluated, but always with greater intensity along plant ages, following the order: 140 > 229 > 320 DAP (Figure 1). Figure 1 Stomatal conductance in sugarcane, RB867515 variety, subjected to different salinity levels at 140, 229 and 320 days after planting Osmotic stress reduces water availability to plants and, consequently, can inhibit gas exchanges and growth (Munns & Tester, 2008). Comparatively, stomatal conductance was higher in plants irrigated with water from the local supply system (0.5 dS m-1) than in plants irrigated with more saline waters (Figure 1), at all times evaluated. At the three times evaluated (140, 229 and 320 DAP), the increase in the concentration of the saline waters led to greater reduction in stomatal conductance, due to the attempt of the plants to adapt to the stress condition. According to Inman-Bamber et al. (2005), reduction in stomatal conductance is an important strategy of sugarcane to avoid leaf dehydration. The trend in transpiration data was similar to that of stomatal conductance, i.e., a reduction with the increment in salinity and plant age (Figure 2). Similar situation was reported by Souto Filho et al. (2014), who observed decrease in stomatal conductance and transpiration in two sugarcane varieties, SP813250 and RB92579, subjected to saline stress. These results also agree with those found by Gonçalves et al. (2010) in sugarcane varieties (SP791011, RB72454, RB98710 and RB92579) subjected to irrigation with saline waters. Figure 2 Transpiration rate in sugarcane subjected to different salinity levels at 140, 229 and 320 days after planting Based on the responses of plants over time, at the last evaluation, close to harvest, there were the lowest transpiration and photosynthetic rates, which reflect the reduction in the physiological activity of the plant at the end of its phenological cycle. Photosynthetic rate (A), as well as gas exchange variables, decreased with the increment in salinity. At 140 DAP, plants that did not receive saline water showed a photosynthetic rate of 17.8 μmol CO2 m-2 m-1, whereas in those subjected to the highest saline stress (6.5 dS m-1) the photosynthetic rate was reduced to 6.01 µmol CO2 m-2 m-1. Similar values, 5.83 μmol CO2 m-2 m-1, were obtained by Souto Filho et al. (2014) at 180 DAP in the sugarcane variety SP813250 subjected to 6.5 dS m-1. The data found at 229 DAP were close to those of the first analysis at 140 DAP, whereas at 320 DAP there was a greater reduction in the photosynthetic rate (Figure 3). Figure 3 Photosynthetic rate of sugarcane subjected to different salinity levels at 140, 229 and 320 days after planting Reductions of approximately 11, 13 and 16% in the photosynthetic rate were observed at 140, 229 and 320 DAP, respectively, per unit increase in water salinity. Andrade et al. (2015) observed reductions of 9.28% at 139 days after sprouting of sugarcane irrigated with 4.6 dS m-1 water in comparison to those under 0.9 dS m-1 water. The reductions in gas exchange variables were directly proportional to the time of cultivation. Since no leaching fractions were applied over time, probably there was an accumulation of salts in the soil, which led to reduction in water availability to plants, justifying the decline in gas exchanges. At 229 DAP, the RB867515 variety, which is known as tolerant to water stress (Silva et al., 2015), exhibited a mechanism of adaptation to saline stress, evidenced at 229 DAP, because even with reduced stomatal conductance (Figure 1), it was able to maintain photosynthetic rates similar to those of plants with 140 DAP (Figure 3), the moment in which stomatal conductance was higher. Studies conducted by Reis & Campostrini (2008) demonstrate that the photosynthetic rate can be related to stomatal movement. As observed for the other variables, the increase in the salt content of the waters linearly reduced leaf water potential (Figure 4). There were reductions of 24.50, 27.79, and 66.28% at 137, 243 and 318 DAP, respectively, as a function of the increase in water salinity, in dS m-1. The percent reductions were calculated as the ratio between the angular and linear coefficients (a/b). Figure 4 Water potential of sugarcane subjected to different levels of irrigation water salinity at 137 (A), 243 (B) and 318 (C) days after planting The reduction in water potential probably occurred because of the decline in soil water potential, both osmotic and matric, which leads to limitation in water availability to the plant. As soil water potential decreases, plants need to reduce even more their water potential for water absorption to occur, a process which frequently requires energy expenditure (Muns & Tester, 2008). Conclusions Increment in irrigation water salinity inhibited water potential, stomatal conductance, transpiration and photosynthetic capacity in the leaves of the sugarcane variety RB867515, regardless of the days evaluated. Literature Cited Allen, R. G.; Pereira, P. S.; Raes, R.; Smith, M. Crop evapotranspiration: Guidelines for computing crop water requirements. Rome: FAO, 1998. 300p. Irrigation and Dranaige Paper, 56 Allen R. G. Pereira P. S. Raes R. Smith M. 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