1993
DOI: 10.1016/0022-1694(93)90130-2
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Measuring water use efficiency of Eucalypt trees with chambers and micrometeorological techniques

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Cited by 61 publications
(31 citation statements)
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“…From their analysis of the aerodynamic parameters, they calculated that hourly rates of CO 2 exchange were similar to those for other natural vegetation, reaching a net uptake rate of CO 2 at midday of 0.1-0.7 mg m À2 s À1 and a net loss of CO 2 at night of 0-3 mg m À2 s À1 , but they did not report rates of water vapour exchange. At a site in Kioloa State Forest, New South Wales, McIlroy and Dunin (1982) and Denmead et al (1993) used the eddy flux technique and measurements of the gradients of water vapour and CO 2 above a 10 m-tall, 11-year-old stand dominated by E. maculata. Rates of transpiration were high (>4 mm per day) in early summer, falling to lower values (about 2 mm per day) in autumn and corresponding daily rates of carbon dioxide uptake were 30 and 20 g m À2 , equivalent to 0.7 and 0.5 mg m À2 s À1 for a 12 h day, similar to those reported by Leuning and Attiwill (1978).…”
Section: Transpirationmentioning
confidence: 99%
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“…From their analysis of the aerodynamic parameters, they calculated that hourly rates of CO 2 exchange were similar to those for other natural vegetation, reaching a net uptake rate of CO 2 at midday of 0.1-0.7 mg m À2 s À1 and a net loss of CO 2 at night of 0-3 mg m À2 s À1 , but they did not report rates of water vapour exchange. At a site in Kioloa State Forest, New South Wales, McIlroy and Dunin (1982) and Denmead et al (1993) used the eddy flux technique and measurements of the gradients of water vapour and CO 2 above a 10 m-tall, 11-year-old stand dominated by E. maculata. Rates of transpiration were high (>4 mm per day) in early summer, falling to lower values (about 2 mm per day) in autumn and corresponding daily rates of carbon dioxide uptake were 30 and 20 g m À2 , equivalent to 0.7 and 0.5 mg m À2 s À1 for a 12 h day, similar to those reported by Leuning and Attiwill (1978).…”
Section: Transpirationmentioning
confidence: 99%
“…In Western Australia, the use of large ventilated chambers placed around individual trees was pioneered to estimate transpiration for periods of up to a year or more (Greenwood et al, 1985). While this approach provided useful comparative information about transpiration between species or treatments, errors can occur in transferring the data to trees growing in open conditions because the presence of the chamber changes leaf energy balance (Leuning and Foster, 1990) except when evaporation approaches the equilibrium rate (Dunin and Greenwood, 1986), or when estimating water-use efficiency (Denmead et al, 1993).…”
Section: Transpirationmentioning
confidence: 99%
“…Nonetheless, representative fluxes can be inferred from these progressions by fitting nonlinear regressions that describe fluxes at the initial time of chamber closure Anthony et al 1995;Wagner et al 1997;Kutzbach et al 2007;Langensiepen et al 2012;Pihlatie et al 2013). More relevant disturbances include alteration of radiation by the chamber walls, and ventilation affecting both air mixing and aerodynamic and leaf boundary-layer resistances (Denmead 1984;Leuning and Foster 1990;Denmead et al 1993;Le Dantec et al 1999;Hooper et al 2002;Steduto et al 2002;McLeod et al 2004;Christiansen et al 2011). Further major sources of systematic errors include: i) chamber leakage, potentially causing flux underestimation (Held et al 1990;Grau 1995;Steduto et al 2002;Rodeghiero et al 2007;Denmead 2008); ii) inaccurate determination of effective chamber volume (Jassal et al 2012); iii) condensation of water vapour on chamber walls (Pérez-Priego et al 2010); iv) water dilution, particularly when the gas analyser does not compute the dry CO 2 molar fraction, as is the case for some Licor instruments (e.g., Li840/ Li840A, Li820).…”
Section: Introductionmentioning
confidence: 99%
“…Firstly, WUE can be described as a ratio of CO 2 uptake and transpiration in the process of photosynthesis (Polster, 1950;Bierhuizen and Slatyer, 1965;Holmgren, 1965;Tanner and Sinclair, 1983). In this case we are talking about so called water-use effi ciency of photosynthesis (WUE Ph ) or sometimes referred to as WUE I -instantaneous WUE because of the time resolution (Bierhuizen and Slatyer, 1965;Zur and Jones 1984;Baldocchi et al, 1987;Denmead et al, 1993;Lindroth et al, 1994;Cienciala and Lindroth, 1995;Larcher, 2003). For ecological, agricultural and forestry purpose, however, the ratio of dry matter production to water consumption over longer period is more informative than temporary gas exchange ratios.…”
mentioning
confidence: 99%