Elsevier

Field Crops Research

Volume 168, November 2014, Pages 86-100
Field Crops Research

Water relations of two contrasting sugarcane genotypes

https://doi.org/10.1016/j.fcr.2014.08.008Get rights and content

Highlights

  • Sugarcane transpiration can be estimated reliably with heat balance sap flow technology.

  • High-fibre sugarcane used more water than traditional cane because it had a higher leaf area index.

  • Transpiration rates declined sooner in traditional cane than in high-fibre cane, in response to water stress.

Abstract

High-fibre sugarcane (energy-cane) cultivars have generated a lot of interest as candidates for bio-fuel production in marginal areas, especially when cellulosic ethanol is also considered. However, a better understanding is required of how much water would be used during cultivation and of their response to drought in terms of water relations. The aim of the study was to investigate the water relations of a high-fibre sugarcane hybrid (Saccharum spp F1 hybrid, 04G0073, referred to as G73) under well watered and drought stress conditions, and compare it with that of a traditional sugarcane cultivar (Saccharum spp, cultivar N19). This would help with a better understanding of the underlying physiology of differences in water use and drought response between high-fibre and traditional sugarcane. The trial consisted of four plots which were planted in a rainshelter facility at Mount Edgecombe, South Africa in October 2011. Two plots received adequate water for the duration of the trial (well-watered treatments), while the other two received no water after 10 February 2012 (water stress treatments), except for the unintended intrusion of water into the root zone on 3 March 2012. The experiment ended on 7 May 2012. Volumetric soil water content was measured with a neutron water meter and daily sap flow was recorded using the non-intrusive heat-balance method. Leaf water potential (ψL) was measured periodically with a pressure chamber, while stomatal conductance was measured periodically with a LiCor 6400. The study has shown that the heat balance method (constant heat source) of measuring sap flow velocity is a suitable technique for estimating transpiration rate in sugarcane. Transpiration rates of well-watered G73 were higher (11%) than that of well-watered N19, presumably due to a higher green leaf area index (GLAI) (6%). There was no evidence to suggest that parameters for calculating maximum evapotranspiration using the Penman-Monteith or FAO method need to be adjusted for high-fibre varieties. Transpiration rates of N19 were reduced sooner and at higher levels of soil water status, than that of G73, as water stress levels increased. G73 had the ability to maintain higher stomatal conductance (gs) than N19 at the same soil water status level, even though leaf water potential was similar between the genotypes. Higher transpiration rates of stressed G73 plants facilitated extended extraction of water from a drying soil profile, which could be a detrimental trait in marginal areas where long dry spells are common. Reduced rates of transpiration and water extraction from the soil profile through stomatal control could be a desirable trait for survival and optimal biomass production in marginal areas. G73 had higher biomass yield (12%) and WUE (10%) under well-watered conditions compared with N19 but water stress reduced both yield and WUE of G73 by 44% and 24%, respectively. The data obtained from the current study will be used for deriving crop parameters for sugarcane crop models with regards to energy-cane genotypes and may be useful in identifying marginal areas suitable for energy-cane cultivation.

Introduction

Sugarcane is acknowledged as an important bio-energy crop (Tew and Cobill, 2008, Olivério and Ferreira, 2010) that could contribute to the growing need for renewable energy. Sugarcane is high yielding (Waclawovsky et al., 2010) and has been shown to use resources (land, water, nitrogen and energy) efficiently (Gerbens-Leenes et al., 2009, De Vries et al., 2010). Bio-ethanol can be produced from the fermentation of soluble sugars in stems, while 2nd generation technology enables the production of ethanol from cell wall sugars derived from cellulose and hemicellulose in stem and leaf fibre (de Souza et al., 2013, Diasa et al., 2009, Ragauskas et al., 2006, Waclawovsky et al., 2010). This will greatly enhance the potential ethanol output from sugarcane and at the same time address concerns regarding ethanol production from food crops in high potential production areas (de Souza et al., 2013; Waclawovsky et al., 2010). Cellulosic ethanol technology also opens up the possibility to produce ethanol from high-fibre, low-sucrose energy cane (Alexander, 1985).

There are indications that high-fibre energy cane (F1 hybrid crosses of Saccharum spp. with its wild relatives (S. spontaneum, Erianthus spp. and Miscanthus spp.) or crosses between F1 hybrids and Saccharum spp. (BC1 generation hybrids)) produces higher biomass yields than traditional cultivars (Alexander, 1985, Silva et al., 2007, Kim and Day, 2011) and better tolerates harsh environmental conditions (Tew and Cobill, 2008). This makes them an ideal feedstock for bio-ethanol production (Canilha et al., 2012). High-fibre energy cane could therefore be used for biomass production in marginal production areas where resource levels are low, such as low rainfall areas or areas with poor soils. Higher biomass yields can only be achieved by increased capture of resources (mainly radiation and water) and/or by increased conversion efficiency of captured resources to biomass. It is therefore important to better understand water relations of high fibre sugarcane, and particularly how they use water and cope with dry conditions in comparison with conventional sugarcane. This information is needed for reliable determination of the feasibility of growing high-fibre sugarcane for biomass production in marginal areas. Water relations of traditional sugarcane has been researched extensively (Hsiao, 1973, Inman-Bamber and de Jager, 1986a, Inman-Bamber and de Jager, 1986b, Abayomi and Lawal, 1998, Ali et al., 1999, Singels et al., 2000, Singels and Inman-Bamber, 2002, Inman-Bamber and Smith, 2005, Smit and Singels, 2006, Koonjah et al., 2006, Silva et al., 2007). In contrast, very little is known about the physiology of high-fibre sugarcane, especially with respect to water relations. In an excellent review of sugarcane water relations, Inman-Bamber and Smith (2005) reported on water use determination, and the role of leaf area, leaf water potential, and stomatal conductance on water use and drought tolerance. Transpiration rate is determined by energy exchanges at the cropped surface (atmospheric and crop factors) and internal energy gradients in the soil-plant-atmosphere system (Inman-Bamber and Smith, 2005). Stomata on the leaves respond to these factors in order to regulate transpiration through the stomatal aperture. This control is represented in the Penman-Monteith equation (Monteith, 1981) as bulk surface resistance (Allen et al., 1998), or alternatively, canopy conductance (gc). The relationship between gc and stomatal conductance (gs) is given by (McGlinchey and Inman-Bamber, 1996):gc=gs0.5GLAIwhere GLAI is green leaf area index.

Meinzer and Grantz (1989) demonstrated that gc only regulates transpiration when crops are water-stressed using the decoupling coefficient (Ω) which describes the relationship between gc and aerodynamic conductance for water vapour transfer (ga). Inman-Bamber and Smith (2005) maintained that, because of this, full canopy transpiration rate of well-watered crops will differ little between cultivars.

Grantz and Meizner (1991) suggested that stomata responded to vapour pressure gradients and photon flux density. Smith et al. (1999) and Grantz and Meizner (1990) suggested that stomata also responded to hormonal root signals under drought stress. Saliendra et al. (1991) and Inman-Bamber and de Jager (1986b) found that some cultivars closed stomata at much higher leaf water potentials (ψL) than others, suggesting that this relationship is cultivar-specific. Smit and Singels (2006) found that cultivar NCo376 maintained higher gs for longer and at lower soil water contents than drought susceptible cultivar N22, as an imposed water stress event unfolded. However, the gs vs ψL relationship was similar for these two cultivars. Olivier and Singels (2003) found that N22 was more sensitive to water stress than N25 and N14, showing a much larger cane yield reduction when irrigation was reduced by 50%.

Inman-Bamber and Smith (2005) identified early stomatal closure, osmoregulation and reducing effective leaf area through leaf rolling and accelerated leaf and stalk senescence as drought adaptation traits in sugarcane. Blum (1996) and Chaves et al. (2003) found that drought tolerant genotypes reduce transpiration under dry conditions through early stomatal closure thereby conserving soil moisture and allowing plants to maintain an adequate water status to sustain critical physiological and biochemical processes. However, stomatal closure often leads to a decline in biomass accumulation because carbon assimilation (photosynthesis) is also reduced (Sinclair et al., 1994).

Crop water relations studies rely heavily on the determination of crop water use. Water use from an unstressed, fully canopied sugarcane crop can be estimated from weather data using the FAO56 approach which relates crop evapotranspiration (ETc) to grass reference evapotranspiration (ETo) using a crop coefficient (Kc) (Allen et al., 1998). Values of Kc for fully canopied sugarcane range from 1.1 to 1.5, depending on climatic conditions, with a typical value of 1.25 (Allen et al., 1998, Inman-Bamber and McGlinchey, 2003). Actual ETc can also be estimated using the energy balance (e.g. Inman-Bamber and McGlinchey, 2003, Olivier et al., 2010), lysimetry (e.g. Thompson and Boyce, 1967, Olivier and Singels, 2012) or soil water balance (e.g. Singels et al., 2000, Rossler et al., 2013, Olivier et al., 2013) approach. A drawback of these methods is that the two components of ETc, namely evaporation from the soil (E), and transpiration (T) from the crop canopy, cannot be separated.

Crop transpiration can be estimated by monitoring the flow rate of stem sap through heat balance techniques. This method has not been used as widely in sugarcane as in other crops. Chabot et al. (2002) used steady state heat balance sap flow measurements to estimate the contribution of a water table to sugarcane water use. They found that transpiration from sap flow measurements exceeded transpiration measured with a lysimeter by 13.5%. Chabot et al. (2005) found that sugarcane transpiration determined from sap flow exceeded reference evapotranspiration by 35% and ascribed this to errors associated with sap flow sensors as well as to the process of scaling up from stem level to canopy level. In this study stem sap flow per unit leaf area was scaled up to canopy level using leaf area index estimated from stem diameter. The sap flow technique was also used by Nassif and Marin (2013).

The aim of the study was to investigate the water relations of a high-fibre sugarcane hybrid under well watered and drought stress conditions, and compare it with that of a traditional sugarcane cultivar. This would help with gaining a better understanding of the underlying physiology of differences in water use and drought response between high-fibre and traditional sugarcane. It is hoped that this would help in deciding the feasibility of growing high-fibre sugarcane in marginal areas for bio-energy production.

The specific objectives were to estimate crop evaporation (referred to as transpiration) from sap flow measurements using the steady state heat balance method, and relate this to plant canopy characteristics (green leaf area, stomatal conductance and leaf water potential), atmospheric conditions (reference evapotranspiration and vapour pressure deficit) and soil water status. A secondary objective of the study was to quantify the potential productivity of the two genotypes under water stressed and well-watered conditions by recording biomass yield and water use efficiency over the growing period.

Section snippets

Experimental details

The study was conducted at the South African Sugarcane Research Institute (SASRI) rainshelter (29°42′40″S, 31°02′35″E). Two contrasting sugarcane genotypes (N19 a high sucrose cultivar, and 04G0073, a high-fibre sugarcane F1 hybrid chosen on limited crop performance yield data, from now on referred to as G73) were planted on October 2011 at 1.25 m row spacing. Fertiliser was applied according to standard recommendations to ensure nutrient sufficiency. The trial was divided into four plots (six

Weather

Weather conditions during the experiment are shown in Fig. 1. The mean minimum (Tmin) and maximum temperatures (Tmax) during the first stress period were 20.9 and 29 °C. During the second stress period, the mean Tmin had decreased to 16.6 °C, while the mean Tmax was 27 °C. Tmin during the second stress period was lower than the optimum range for sugarcane growth (20 to 30 °C) reported by Inman-Bamber and Smith (2005). The mean ET0 (ET0 as defined by Allen and Pruitt, 1991) was 3.98 and 2.98 mm d−1

Relationship between TSAP and soil water supply and atmospheric demand

TSAP of G73 was reduced below well-watered values when RASWC dropped below about 0.5 (Fig. 14). A similar analysis for N19 was not possible because TSAP of the stressed treatment never fully recovered to that of well-watered values during the recovery period.

Fig. 15 shows the relationship between TSAP and ET0 for the control treatments. On average N19 transpired at rates of about 61% of ET0, while G73 transpired at rates of about 71% of ET0. Although this difference is not statistically

Conclusion

The study has shown that the heat balance method (constant heat source) of measuring sap flow velocity is a suitable technique for estimating transpiration in sugarcane under non-stressed conditions. The instrumentation was relatively easy to install and operate, over an extended time period, without damaging stalks or requiring frequent refitting. It produced consistent hourly estimates of sap flow in different stalks. When scaled up to a per unit area level, transpiration estimates of

Acknowledgements

We acknowledge Yuriy Tsupko for the trial design, and the South African Sugarcane Research Institute Technical Team for measurement assistance. Prof. Mike Savage of the University of KwaZulu-Natal gave valuable advice on sap flow data processing. Aresti Paraskevopoulos assisted with the leaf area calculations.

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