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Engenharia Agrícola

Print version ISSN 0100-6916

Eng. Agríc. vol.32 no.2 Jaboticabal Mar./Apr. 2012

http://dx.doi.org/10.1590/S0100-69162012000200010 

SOIL AND WATER ENGINEERING

 

Development of experimental structure and influence of high CO2 concentration in maize cro

 

Desenvolvimento de estrutura experimentale influências da alta concentração de CO2 na cultura do milho

 

 

João B. Lopes da SilvaI; Paulo A. FerreiraII; Eduardo G. PereiraIII; Luís C. CostaIV; Glauco V. MirandaV

IEngº Agrícola e Ambiental, Professor, Doutor em Engenharia Agrícola, Universidade Federal do Piauí, Campus Bom Jesus, silvajbl@yahoo.com.br
IIEngº Agrônomo, Professor, Ph. D. em Engenharia de Água e Solo, Universidade Federal de Viçosa, pafonso@ufv.br
IIIBiólogo, Professor, Doutor em Fisiologia Vegetal, Universidade Federal de Viçosa, Câmpus Florestal, egpereira@gmail.com
IVMatemático, Professor, Ph. D. em Agrometeorologia, Universidade Federal de Viçosa, l.costa@ufv.br
VEngº Agrônomo, Professor, Doutor em Genética e Melhoramento, Universidade Federal de Viçosa, glaucovmiranda@gmail.com

 

 


ABSTRACT

Maize is a C4 plant that shows few or no response to high [CO2]. Thus, this study aimed to analyze the photosynthetic rate and yield of maize under high [CO2] and develop open-top chambers (OTC) to create an atmosphere enriched with CO2. The experiment was conducted between October 2008 and March 2009. The OTCs were developed in modular scheme. Measurement of photosynthetic rates, transpiration, stomata conductance, grain yield and dry matter were performed. The experimental design was randomized blocks with four replications and three treatments: P1 - plants grown in OTC with 700 ppm [CO2], P2 - plants grown in OTC with environmental [CO2], and P3 - control, cultivated in open field. The results were analyzed by ANOVA and Tukey's test (Pr< 0.05). The chambers can reduce by 25% the photosynthetically active radiation and increase the air and leaf temperatures. Plants under high [CO2] (P1) showed the highest photosynthetic rates and the lowest stomata conductance and transpiration. The total weight of grains (g) and dry mass of shoots (g) showed no increases for P1, despite their higher photosynthetic rates.

Keywords: open-top chambers, climate change, Zea mays L.


RESUMO

O milho é uma planta C4 que apresenta pouca, ou nenhuma, resposta às elevadas [CO2]; assim, neste trabalho, objetivou-se analisar respostas fisiológicas e produtivas da cultura do milho sob alta [CO2], e desenvolver câmaras de topo aberto (CTA) para criar uma atmosfera enriquecida com CO2. O experimento foi conduzido entre outubro de 2008 e março de 2009. As CTAs foram desenvolvidas em esquema modular. Foram realizadas medições da taxa fotossintética, transpiração, condutância estomática, produção de grãos e matéria seca. O delineamento experimental foi em blocos casualizados, com quatro repetições e três tratamentos: P1 - plantas cultivadas em CTA a [CO2] de 700ppm; P2 - plantas cultivadas em CTAcom [CO2] ambiente; e P3 -plantas cultivadas em campo aberto, testemunhas. Os resultados obtidos foram submetidos à análise de variância e teste de Tukey (Pr<0,05). As câmaras reduzem em 25% a Radiação Fotossinteticamente Ativa e aumentam a temperatura do ar e das folhas, em relação ao ambiente externo. As plantas sob alta [CO2] (P1) apresentaram as maiores taxas fotossintéticas e as menores condutâncias estomáticas e transpiração. O peso total dos grãos (g) e a matéria seca da parte aérea (g) não apresentaram incrementos para P1, apesar das maiores taxas fotossintéticas.

Palavras-chave: câmaras de topo aberto, mudanças climáticas, Zeamays L.


 

 

INTRODUCTION

Since 1958, when systematic measurements of CO2 at Mauna Loa, Hawaii, began, CO2 concentrations increased more than 17% and it may reach 600 ppm by 2020 (TAIZ & ZEIGER, 2004). In general, [CO2] 200-400 ppm higher than normal produces stimuli in growth and production of C3-type plants, but not in C4-type crops, because increase in the [CO2] have little effect on photosynthetic rates of C4 plants, due to the mechanism that increases the [CO2]on the site of action of Rubisco from these plants (ZISKA & BUNCE, 2006).

Maize (Zea mays L.) is a C4 plant that generally tends to present little or no additional growth in response to elevated [CO2] (GHANNOUM et al., 2000). Here, LEAKEY et al. (2004) argue that the effects of high [CO2] in plants are not sufficiently understood to allow for future predictions of climate change. RUDORFF et al. (1996) did not observe increases in grain yield of [CO2] of 500 ppm in open-top chambers. Similar results were reported by Kim et al. (2007) working with high-[CO2] chambers. However, LEAKEY et al. (2004) observed that maize under high [CO2] showed a maximum of 41% increase in CO2 assimilation, with an average of 10%, with the maximum value occurring during periods with less rain. These increments are due to the high intracellular concentration of CO2 at low stomatal conductance and reduced transpiration. In experiments with open-top chambers (SAMARAKOON & GIFFORD, 1996), maize plants under water stress and high [CO2] showed an increase of 50% growth compared to well-watered plants under environmental [CO2]. PRINS et al. (2007) also obtained positive responses for corn growth at high [CO2].

Because maize is a crop with high nutritional and economic values, more research is needed to quantify the impacts of climate change on this culture. Thus, this study aimed to analyze some of the physiological responses and quantify the yield of maize under CO2-enriched atmosphere, but also to develop open-top chambers to enable the enrichment of the air with CO2.

 

MATERIALS AND METHODS

The experiment was carried out in drainage lysimeters at the campus of the Federal University of Viçosa (UFV), Viçosa-MG, between October 2008 and March 2009. To enrich the air with CO2, open-top chambers were developed, based on COSTA (2003), LOBO (2003) and SOUZA (2007). The developed chambers consisted of rectangular modules to monitor plant growth, with side doors to facilitate data collection (Figure 1). A hood was also added to allow control of the water in the chamber environment. The chambers were made of steel structure and the sides were covered with a transparent plastic film.

The air injection system in the chambers was made of a centrifugal fan, in which the airflow was directed into the chamber by perforated PVC pipes for homogeneous air distribution. CO2 was stored in cylinders at a rate regulated by primary pressure gauge coupled to a high-pressure solenoid valve. The solenoid valve also controlled plant day time exposure to CO2 between 6 am and 6 pm with timers. Next to the chambers, the flow was again regulated with a fine adjustment valve. [CO2] in the chambers was monitored and adjusted every other day with environment [CO2]-meter, model Testo 535.

Lysimeters with 1.0 x 1.4 m section and 0.8 m depth were filled with Red-Yellow Dystrophic Latosol, of very clayey textural class (70% clay, 9% silt, 12% coarse sand, and 9% fine sand). Soil acidity correction was carried out in this substrate with lime (80%PRNT) at a dose of 3 t ha-1. Two fertilizations were also carried out during the experiment, being the first with 8-28-16 NPK at the time of planting and the second as top fertilization, 20-05-20NPK at the dose of 800 kg ha-1. The maize cultivar used was 'AG9010', with spacing of 0.20 m between plants and 0.50 m between rows, totaling 14 plants per lysimeter.

The plants were irrigated with dripping tapes to maintain the soil at field capacity (FC, 33.62%), with the soil water content monitored by a TDR (time domain reflectometry) with probes positioned at 0.20 and 0.40 m depth.

Environmental, physiological and phenological data were collected. Environmental data were gathered daily at every hour with an automatic portable weather station, Davis Vantage-Promodel. At the station, data were collected for photosynthetically active radiation (PAR) and temperature in the environment and inside the chambers. Also, it was used a pyranometer to measure the PAR radiation inside the chambers.

The physiological data collected were: photosynthetic rate (A), transpiration (E) and stomata conductance (Gs), collected at flowering (60 days after planting - DAP) and at the phase of grain formation (90 DAP). Measurements were performed between 8 am and 11 am on the 10th leaf of each plant, with a portable photosynthesis analyzer (IRGA - Infra Red Gas Analyzer), LCi model, with an external radiation source system, 1,200 µmol m-2 s-1 and environmental conditions inside and outside the chambers (temperature, [CO2] and relative humidity). The phenological data collected were: plant height, leaf temperature, shoot dry weight, and yield. Leaf temperature was collected daily at 8 am, 11 am, 2 pm and 5 pm, using an infrared thermometer. For yield evaluation, the following variables were analyzed: total grain weight per plot, weight of thousand grains, and number of grains per spike.

The experimental design used was randomized complete block design (RBD) with four replications. The treatments were: P1 - plants grown in open-top chambers with [CO2] to 700 ppm; P2 - plants grown in open-top chambers with environmental [CO2], and P3 - plants grown in open air, control.

The variables were analyzed using simple descriptive statistics (mean, standard deviation and coefficient of variation) for further analysis of variance (ANOVA). For comparison among the treatments, the Tukey's test at 5% probability (Pr<0.05) was applied.

 

RESULTS AND DISCUSSION

Microclimate changes in the developed open-top chambers

The addition of modules into the open top chamber developed (Figure 2) optimized CO2 consumption, reducing the experimental cost to obtain an atmosphere with high [CO2], for increasing the CO2 flow, through the injection system and environmental airflow control (Figure 3) which was increased with the addition of modules.

Significant differences were observed for PAR (MW m-2 day-1) among the treatments (Table 1), 25.41% reduction of radiation inside the chambers (P1, P2) as compared to radiation outside the chambers (P3). The maximum and average temperatures of external and internal environments of the chambers showed significant differences between treatments (Tables 1 and 2). Higher temperatures were expected in P1, given that higher [CO2] in the environment causes major microclimate changes, but in fact P2 showed higher values (Table 2).

This demonstrates that in the chamber, the key factor to increase temperature is water vapor, which is originated from the high humidity in the chamber due to the higher P2 plant transpiration (Table 2). Despite the small differences in values of average temperatures between P1 and P2, 0.42ºC, the same did not occur for the maximum values, 1.04ºC. These results indicate that the cameras altered the microclimate, increasing the average daily temperature in more than 2ºC, and the maximum temperature in over 7ºC in comparison to the environment. These results corroborate with the observations by AINSWORTH & LONG (2005) and LONG et al. (2005).

Physiology, growth and yield in the maize crop

There were significant differences between treatments in both measurements of photosynthetic rate (A) and stomatal conductance (Gs) (Table 1). Although the net photosynthesis (A) did not present statistical difference in the second measurement between P1 and P2 (Table 2),plants subjected to P1 treatment showed higher photosynthetic rates in the two measurements, 27.03 and 32.02% respectively higher than P3, thus responding positively to the increase of [CO2]. This result indicates that C4-type plants may respond to increased [CO2] in the environment, unlike the findings by TAIZ & ZEIGER (2004) and ZISKA & BUNCE (2006), who reported that C4 plants do not benefit from increased [CO2] in the atmosphere. Nevertheless, PRITHCARD & AMTHOR (2005) mentioned that the C4 plants benefit from increases of [CO2], although not directly increasing the photosynthetic rate, but through the reduction in stomatal conductance (Gs) and transpiration (Table 2). Moreover, WAND et al. (1995), LEAKEY et al. (2004) and SOUZA (2007) found similar increases in photosynthetic rates of C4 plants. Conversely, KIM et al. (2007) found no stimulation in photosynthetic maize plants grown at high [CO2].

Transpiration (E) showed significant differences only in the second measurement (Table 1). Possibly, the first measurement showed no significant differences due to the high coefficient of variation (CV), 28.62%, as the differences between P1 and P2 were similar between the two measurements, 1.5 mmolm-2 s-1. The reduction of perspiration (E) in plants under high [CO2], was due to reduction of stomatal conductance (Gs), which also caused these plants (P1) to present higher leaf temperatures (Table 2), as it reduced heat exchange with the environment, increasing the leaf temperature, a fact that corroborates observations reported by DAVIES (2006), KÖNER (2006) and LARCHER (2006). Increase in leaf temperature should be beneficial because it increases the photosynthetic rate. However, this benefit was not observed, since P2 and P3 showed no significant differences (Table 2), although leaf temperatures in P2 were higher than that of P3, and P2 photosynthetic rates are 8.85% and 7.25% higher in relation to P3 in the first and second measurement, respectively.

The increases in leaf and ambient temperatures (Table 2) were not sufficient to reduce the crop cycle, although high temperatures are commonly reported to reduce it (KÖNER, 2006, MENZEL & SPARKS, 2006). This cycle reduction due to increased temperature was observed by RENATO (2009), using simulation models of crop growth of sugarcane; nonetheless this increase greatly reduced the cycle of the crop. Thus, the results of this study are important for modeling and simulation, as they help in the calibration and simulation of models, since most of them have leaf temperature as input, as the model proposed by FARQUAR et al. (1980).

Maximum plant heights were higher for plants grown inside P1 and P2 chambers (Table 2). However, this greater height was not due to increased leaf and chamber temperatures (Table 2), or even [CO2], but for PAR reduction (Table 1), which caused plant etiolation. Due to shading, P1 and P2 plants approached to VT phase (tasseling) faster, thus shortening the vegetative stage (stage V0 to V15). However, this reduction of the vegetative stage length did not reduce the plant cycle because the plants arrived together at the reproductive stage (R1); nor it reduced the leaf number, as all plants developed 15 leaves.

Only the total dry matter of shoots showed significant differences among treatments (Table 1). The total weight of grains (g), the thousand grain weight (g) and the number of grains per spike showed no significant differences, even with the highest photosynthetic rates of P1 (Table 2), thus showing that increase of [CO2] does not increase the weight of individual grains, but also it does not provide increased reproduction in experimental conditions similar to this work. This fact is in disagreement with the affirmations by JABLONSKI et al. (2002) and ZISKA & BUNCE (2006), who argued that increases in [CO2] affect reproduction, which in turn increases the number of flowers and pollen production, therefore leading to increase in the number of grains.

It was expected larger amount of dry matter and yield (total weight of the grains) in plants subjected to P1, in view of the highest photosynthetic rate in P1 (Table 2). The hypothesis for the failure to increase the dry matter and total grain weight is the average PAR reduction in the chambers, 25.41% (Table 1), because the photosynthetic rate measurements were performed with irradiance close to the saturation point (1,200 µmol m-2 s-1), thus evaluating the maximum photosynthetic capacity of the leaf. As well, measurements of photosynthesis were made on a single leaf per plant and grain yield is more related to carbon gain of the whole plant. This is in agreement with ZISKA & BUNCE (2006), who stated that only one leaf is not a good indicator for the response of photosynthesis and growth of the whole plant.

Similar results for yield (total grain weight) and dry matter, were found by RUDORFF et al. (1996), GHANNOUM et al. (2000) and KIM et al. (2007) working with open-top chambers. While SAMARAKOON & GIFFORD (1996), LEAKEY et al. (2004) and PRINS et al. (2007) found positive results for maize production at high [CO2], along with OLIVEIRA (2007) and COSTA et al. (2009) who worked with crop growth models.

 

CONCLUSIONS

The open-top chambers developed in this work change the internal microclimate, with additions of more than 2ºC in the average daily temperature, but also reduce the average PAR (Photosynthetic Active Radiation) in 25.41%, causing etiolation. The addition of modules in the open-top chamber optimizes CO2 consumption, reducing the experimental cost to obtain an atmosphere with high [CO2].

The photosynthetic rate of maize (C4) shows stimulation at high [CO2] in the environment. However, the increase in leaf temperature, of more than 2ºC on average, does not provide increased photosynthetic rate. Nonetheless, it is not sufficient to change the plant cycle length. Despite the higher rate of plant photosynthesis in environments with high [CO2], grain production did not increase, as well as there was not an increase in dry matter of the aerial system.

 

ACKNOWLEDGMENTS

The authors thank FAPEMIG for research funding, and Capes and CNPq for awarding research grants.

 

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Recebido pelo Conselho Editorial em: 21-2-2011
Aprovado pelo Conselho Editorial em: 3-12-2011

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