A Differential Psychrometer for Continuous Measurements of Transpiration 1 R. 0. Slatyer and J. F. Bierhuizen2 CSIRO Division of Land Research and Regional Survey, Canberra, A.C.T., Australia Introduction Transpiration is frequently measured by enclosing plants, or portions of plants, in transparent chambers and determining the change of humidity of a stream of air before and after passing through the enclosure (2, 4). Although this procedure should not be used to estimate probable transpiration rates under natural conditions, unless adequate precautions are taken to ensure that the microenvironment within the chamber does not differ significantly from that in the reference locations or that its specific characteristics can be measured and appropriate corrections made (9), it is particularly suitable for specific studies of the transpiration process. Recently, in developing an apparatus for simultaneous and continuous determinations of transpiration and photosynthesis involving differential airstream measurements of waiter vapor and CO2 concentration, Bierhuizen and Slatyer (1) incorporated a differential psychrometer, based on a design of Wylie (10). This instrument has been found to be particularly suitable for transpiration research (7, 8) and its characteristics and performance are outlined below. Materials and Methods A differential psychrometer can be considered as a pair of matched wet bulb thermometer elements enclosed in tubes, through which individual streams of air, identical except for vapor pressure, are passed at a common temperature T. Both streams originate from a single source which provides a nominally constant water vapor pressure eb by prior vapor saturation in water at a predetermined temperature. A sample from the main air stream is passed directly through 1 tube of the differential psychrometer. The remainder of the stream first passes through the transpiration chamber and in the process becomes enriched with water vapor, emerging with a new water vapor pressure eaA3 A sample from this stream is then passed through the other tube of the psychrometer. After leaving the psychrometer the air can be released or passed through equipment such as an infra-red gas analyser for differential measurements of CO2 concentration. It can be assumed that the pressure drop through the system is negligible and, since the environments of the 2 wet bulbs and their rates of ventilation are practically the same, that the psychrometric constant will be the same for both. If the actual wet bulb temperatures are given by Twa and Twb, and the corresponding saturation vapor pressures by ewa and ewb, then the standard psychrometric equation can be written: I (ewa-ea) = A ( -Twa) (eWb - eb) = A (T- Twb) II where A is a form of the psychrometric constant proportional to atmospheric pressure. For full ventilation and at a pressure of 755 mm of mercury it has a value of 0.500 mm of mercury per degree C. Subtracting equation I from II and substituting A e for (ea - eb) one can obtain III Ae = A (Twa - Twb) + (ewa - ewb) which gives, on rearrangement Ae = (A Twa + ewa) - (ATwb + ewb) IV It is apparent that equations III and IV provide 2 methods of calculating Ae. From equation III, for example, by measuring ATw = (Twa - Twb) with a differential psychrometer and obtaining the saturation vapour pressures ewa and e, b corresponding to the actual wet bulb temperatures from meteorological tables (3, 5, 6) Ae can be readily obtained. Alternatively, from equation IV, by tabulating (ATw + e5,) as a function of Tw, Ae can be readily calculated from measurements of Twa and Twb. Typical values of Ae for TUWb = 20, 25, 30 and 350, and ATw ranging from 1 to 100 are given in table I. Errors in the values adopted for psychrometer environment temperature, T, have been shown by Wylie (10) to have a small effect (less than 1.0 % per degree error in T, for T, in the range 0-30o) on the calculated value of Ae. Received April 21, 1964. 2 Present address: Institute of Land and Water Management Research, Wageningen, Netherlands. 3 The subscripts b and a refer to the air stream before and after passing through the test chamber, respectively. 1 1051 Description The requirements of the apparatus were that it should be of small size and possess long-term stability so that it could be incorporated in a gas circuit for Downloaded from on June 14, 2017 - Published by www.plantphysiol.org Copyright © 1964 American Society of Plant Biologists. All rights reserved. 1052 PLANT PHYSIOLOGY continuous studies of transpiration and photosynthesis. Because it was desirable for some determinations to be made at very low rates of air flow, and because transpiration and photosynthesis rates may change rapidly in response to a change in environmental conditions, it was also important that the instrument should be fully sensitive even at flow rates of less than 0.5 liter/min and that it should have a rapid response time of significantly less than 1 minute. A diagrammatic sketch of the instrument (already used by Bierhuizen and Slatyer, 1) is given in figure 1. The 2 air streams, with water vapor pressure ea and eb are first brought to a common reference temperature T by passing them through a pair of copper coils, soldered together and immersed in a thermostatically controlled water bath. The coil outlets are connected directly to the psychrometer tube inlets so that the temperature of the air around the elements is effectively the same as bath temperature T. Insulation of the psychrometer is also aided by constructing it from a solid block of acrylic plastic (plexiglas or perspex). The air streams pass out of the copper coils, through the psychrometer (entry is via orifices to induce turbulence in the air flow past the wet bulb elements) and then through calibrated flowmeters. Flow is regulated by valves on the inlet side of the transpiration chamber and total flow through the chamber can be measured by the differences between the flowmeter reading on the common inlet tube and the amount diverted through the tube b. Horizontal insertion of the wet bulb elements into the psychrometer was adopted partly for convenience in manipulation and partly because it facilitated adequate depth of wet bulb insertion behind the tip of the wick. Each w-et bulb consisted of a 44 gauge copper- constantan thermojunction which was threaded through a central hole in the plexiglas mounting and allowed to project 2 to 3 mm. The projecting tip was thinly covered with dissolved plexiglas to protect the junction chemically, seal the hole and provide mechanical support. Fine mesh knitted wet bulb sleeving, previously boiled in very dilute alkali solution and then thoroughly rinsed and stored in distilled water, was then drawn over the tip, along the narrow section of the thermocouple mounting, and extended into wet bulb reservoirs located directly below the psychrometer proper. The open end of the sleeving projected 2 to 3 mm beyond the thermocouple and was closed with a loop of cotton thread. The use of 0-rings enables each wet bulb unit to be positioned accurately and simply yet easily removed for inspection and maintenance. To facilitate easy threading of the wet bulb sleeving through the access hole leading from the 2 wet bulb reservoirs to the psychrometer tubes, this part of the assembly was attached to a brass plate which could be quickly and easily removed when the wet bulbs were being introduced or adjusted. Each wet bulb reservoir could also be removed separately for refilling. The vertical height from water level to thermocouple was kept as small as possible. It seldom exceeded 2 cm. The constantan wires of each thermocouple were connected together to form the differential psychrometer and, in addition, were connected to a common constantan reference junction which was located in the water bath and so maintained at temperature T. The output of each wet bulb thermocouple and the differential output was then connected to a multichannel DC potentiometric recorder with a full scale sensitivity of 1 mv. The output of the thermocouples, 43 ,tv per degree C, permitted output corresponding to a PERSPEX BLOCK THERMOCOUPLE MOUNTING BY 2 O-RINGS '' r y SECURED re E T R INL t~~~~~~~~~~~~~~~~~LA WIRES gyITHERMOCOUPLE WATER RESERVOIR FOR WICK SURROUNDING WET BULB Fig. 1. Diagrammatic sketch of differential psychrometer. Note that both thermocouple elements are wet bulbs. One element is shown without wet bulb sleeving to provide details of construction. In use each element is inserted into the psychrometer until the wick is directly over the water reservoir. Downloaded from on June 14, 2017 - Published by www.plantphysiol.org Copyright © 1964 American Society of Plant Biologists. All rights reserved. 1053 SLATYER AND BIERHUIZEN-MEASURING TRANSPIRATION temperature difference of up to 200 to be displayed on the recorder chart. Results Instrument performance was checked in several different ways, the most important being the examination of the effect of rate of air flow on wet bulb depression, and of the accuracy of the observed wet bulb temperature at full ventilation. The sensitivity of the instrument in terms of thermocouple output was quite satisfactory since differential temperature could be measured to better than 0.10 and, consequently, differences of less than 0.05 mg water per liter of air could be determined. For single leaves of, say, 100 cm2 area this corresponds to about 1 % of typical transpiration rates. ASPIRATION SPEED 20 10 9 The calibration data are shown in figures 2 and 3. In figure 2 rate of air flow past the wet bulb elements was calculated from the flowmeter readings and effective cross sectional area, in each tube, available for flow. Since the diameter of the element plus sleeve was 3 mm and the internal diameter of the tube 6 mm the cross sectional area was approximately 0.20 cm2. A flow rate of 500 cm3/minute in each tube was therefore represented by an air speed past the elements of the order of 25 m/minute. The figure shows that with humid air (T 30', TWeb 24.60 relative humidity 63 %) maximum wet bulb depression occurred at flow rates less than 100 cm3/minute and even with relatively dry air (T 30°, T,,b 13.30 relative humidity 4 %) it was obtained at flow rates of less than 250 cm3/minute. (cm / sec) 40 30 18- R.H. =4% 0 60 14- U 0 12- z o 0 (n (n w a. (Li ox 8OD -J 6- R.H. =63% 3 4- 2- 0] 6 1 i6o I 200 T I 300 400 I 500 RATE OF AIR FLOW (cc/ min) Fig. 2. Effect of ventilation rate on wet bulb depression using airstreams of 4 % R.H. (hollow circles) and 63 %o R.H. (solid circles). Downloaded from on June 14, 2017 - Published by www.plantphysiol.org Copyright © 1964 American Society of Plant Biologists. All rights reserved. 1054 PLANT PHYSIOLOGY *, 0 w z 15 :3 w a. w 04 cr w I- 3: m z w z a. 3. w a 30 25 2'0 DEWPOINT GIVEN BY THERMOCOUPLE 0b 1'5 MEASUREMENTS (0c) Fig. 3. Relation between observed dewpoint temperature, from thermocouple measurements, and the value giverr by the temperature of the water in which the airstream was equilibrated. Hollow circles refer to thermocouple tube a and solid circles to thermocouple tube b. In figure 3 the observed wet bulb depression, taken from recorder readings, has been used to calculate dewpoint temperature and is plotted against a range of water temperatures, Tb, in which the air stream was equilibrated. The 2 estimates agreed closely and zero stability, measured as the difference between the 2 psychrometer elements when identical streams of air were passed through both tubes of the psychrometer, was high. At the extreme relative humidities obtainable (4 % and 89 % at 300) differential output did not exceed +0.5 ,uv over a test period as long as 40 minates. The speed of response to changed humidity in the tubes was also rapid; in almost every case the rate of equilibration of the air itself appeared to be the limiting factor. An example of the use of the instrument in practice is given in figure 4. These data were collected for cotton leaves in transpiration experiments similar to those described by Slatyer and Bierhuizen (10, 11). Environmental conditions of light (6,000 ft-c), bulk air temperature (30°), windspeed (3.1 cm sec'1), and bulk CO2 concentration (0.03 %) were kept constant. Bulk air relative humidity was increased abruptly on 2 occasions from the initial value of Downloaded from on June 14, 2017 - Published by www.plantphysiol.org Copyright © 1964 American Society of Plant Biologists. All rights reserved. SLATYER AND BIERHUIZEN-MEASURING TRANSPIRATION 2 TIME (Hours) Fig. 4. Change of transpiration rate of an enclosed cotton leaf exposed to constant environmental conditions except for abrupt changes in bulk relative humidity. about 20 % so that the effective leaf-air vapor pressure difference [calculated from additional leaf temperature measurements (1)] was reduced by about 25 % and 50 % respectively. The rapid change in transpiration rate as the leaf adjusts to a new energy balance is well illustrated as is the constancy of the transpiration rate at any one humidity level. Numerous other examples of the use of the instrument can be found in the papers already cited (10, 11). Discussion 1055 e8 is the saturation vapor pressure (at temperature T) in the same units as Ae, and p is the density of water vapor in saturated air, also at temperature T. Alternatively, the initial calculation of Ae can be eliminated, and the difference between the relative humidity appropriate to (T - T,,) multiplied directly by the density of water vapor in saturated air (at temperature T) to give C. The value of C, multiplied in turn by the rate of air movement through the test chamber gives transpiration rate. The alternative procedure can be recommended for many experimental applications, especially when a limited number of values of T are used as experimental parameters. It, too, can be simplified but at the risk of introducing errors. The simplification takes advantage of the fact that the relationship between relative humidity and (T - T,) is approximately linear for moderate differences in temperature. The slope of this relationship (per cent relative humidity/degree C temperature difference) for any 1 value of T, can be obtained from standard psychrometric charts or tables. It is then multiplied by the density factor as above, and the product of the value so obtained with A/T and with rate of air movement gives the transpiration rate to within ±5 %. This error can be tolerated for many purposes and even for accurate measurements the calculation provides a useful rapid checking procedure. Summary Table I. Valutes of Ae in mm for 4 levels of TWb anid Values of ATw Ranging from 1 to 10° A differential psychrometer is described which is particularly suitable for continuous transpiration measurements of plants in experimental enclosures. The instrument is small, inexpensive to construct and maintain, and has high accuracy and precision, together with good long term stability. Response time of the instrument appears to be quicker than the equilibration of the airstream being monitored. A thermostated equilibration water bath is used so that nominally similar dry bulb temperatures exist in both the test and reference airstreams. This makes the measurements relatively tolerant of fluctuating environmental temperature and pressure. Also the use of small psychrometer tube dimensions and turbulence inducing entry orifices enable maximum wet bulb depression to be achieved at apparent aspiration speeds of < 20 cm/second corresponding to airflow rates of < 250 cm3/minute. Twb 250 Acknowledgments In order to calculate transpiration rate the values of Ae obtained from equations III or IV must be converted to water vapor concentration (mg water/ liter air) and multiplied by the rate of flow of air through the test chamber. The conversion from Ae in mm of mercury can be made using the expression C=p (Ae/e8) V where C is the water vapor concentration in mg/liter, 200 A~Tia 1 2 3 4 5 6 7 8 9 10 1.61 3.29 5.03 6.76 8.72 10.67 12.70 14.81 17.00 19.28 1.95 3.98 6.09 8.28 10.56 12.94 15.40 17.97 20.64 23.42 300 2.38 4.84 7.41 10.08 12.86 15.74 18.75 21.87 25.12 28.50 350 2.88 5.89 9.01 12.26 15.64 19.20 22.82 26.62 30.58 34.70 The authors acknowledge the considerable amount of advice and assistance provided by Dr. R. G. Wylie and his colleagues from CSIRO, Division of Physics, Sydney, throughout the period of development of this instrument. They also acknowledge the assistance of Mr. J. V. Savage who fabricated both the prototype and final version. Literature Cited 1. BIERHUIZEN, J. F. AND R. 0. SLATYER. 1964. An apparatus for the continuous and simultaneous measurement of photosynthesis and transpiration Downloaded from on June 14, 2017 - Published by www.plantphysiol.org Copyright © 1964 American Society of Plant Biologists. All rights reserved. 1056 2. 3. 4. 5. PLANT PHYSIOLOGY under controlled environmental conditions. C.S.I.R.O. Div. Land Res. Tech. Paper 24. DECKER, J. P., W. G. GAYLOR, AND F. D. COLE. 1962. Measuring transpiration of undisturbed Tamarisk Shrubs. Plant Physiol. 27: 393-97. DEUTSCHEN, W. 1955. Aspirations-PsychrometerTafeln (Friedr, Viewg, and Sohn, Braunschweig, Germany). HEATH, 0. S. AND H. MEIDNER. 1961. The influence of water strain on the minimum intercellular space carbon dioxide concentration, r, and stomatal movement in wheat leaves. J. Expl. Botany 12: 226-42. HODGMAN, C. D., R. C. WEAST, AND S. M. SELBY. 1962. Handbook of Chemistry and Physics. Chemical Rubber Publishing Company, Cleveland, Ohio. 6. LIST, R. J. 1958. Smithsonian Meteorological Tables. Smithsonian Institute, Washington, D. C. 7. SLATYER, R. 0. AND J. F. BIERHUIZEN. 1964. Transpiration from cotton leaves under a range of environmental conditions in relation to internal and external diffusive resistances. Australian J. Biol. Sci. 17: 115-30. 8. SLATYER, R. 0. AND J. F. BIERHUIZEN. 1964. The influence of several transpiration suppressants on transpiration, photosynthesis and water use efficiency of cotton leaves. Australian J. Biol. Sci. 17: 13146. 9. SLATYER, R. 0. AND I. C. MCILROY. 1961. Practical Microclimatology. UNESCO, Paris. 10. WYLIE, R. G. 1963. A new tool for transpiration experiments. C.S.I.R.O. Annual Report 1962-63, 32-3. Cation, Organic Acid, and pH Relationships in Peel Tissue of Apple Fruits Affected with Jonathan Spot 1. 2 A. E. Richmond,3 D. R. Dilley, and D. H. Dewey Department of Horticulture, Michigan State University, East Lansing, Michigan Jonathan spot is a physiological disorder of the epider,mal and hypodermal tissues of Jonathan and other apple varieties. Pentzer (8) observed that the pH of the affected tissue was higher than that of adjacent normal tissue and suggested that the spot symptom resulted from the conversion of anthocyanin color from red to blue. The affected tissue is also characterized by a marked accumulation of K, Ca and Mg (1). Wilkinson (10) suggested that K, the dominant fruit cation, may serve in a buffer system with malic acid, the dominant fruit acid, for maintaining tissue pH. Several investigators (2, 3, 10) have observed a direct relationship between the K content and titratable acidity of apple fruits. It is generally accepted that organic acids are synthesized in the cells to compensate ion balance when cation absorption exceeds anion absorption (4, 9). Recently, Johnson et al. (5) provided additional evidence that organic acid synthesis is the result rather than the cause of excess cation absorption. The relationship between cation accumulation and organic synthesis and the development of Jonathan spot on apple fruits is herein reported. 1 Received April 27, 1964. 2 Journal Article 3350 of the Michigan Agriculture Experiment Station. 3 Current Address: Department of Plant Biochemistry, University of California, Los Angeles, California. Materials and Methods Mature Jonathan apples (Malus sylvestris, Miller) were harvested and maintained in storage at approximately 00 for several months to obtain fruits with varying degrees of spot development. Discs (approximately 5 mm in diameter and 2 mm thick) of spotted tissue and adjacent normal tissue were obtained from sections of fruit peel with a cork borer. Samples of spotted and normal peel tissue were analyzed for mineral composition as described by Kenworthy (6). Quantitative analysis of the nonvolatile organic acids of spotted and normal tissue was determined by the ion exchange column chromatographic procedure of Markakis et al. (7) as modified by Dostal (2). A pH titration profile was obtained for spotted and normal peel tissue employing a 95 % ethanol extract of 2 g of tissue. Prior to titration, the extract was evaporated on a hot plate, the residue dissolved in 20 ml of water, and the solution clarified by centrifugation. Half of the supernatant solution was titrated with 0.0354N HCI to pH 2.5, while the other half was titrated to pH 8.0 with 0.0280 N NaOH. pHTitration profiles were also obtained for solutions of those acids present in 1 g of spotted and normal peel tissue after adjustment of the solution to the pH observed in the respective tissue homogenates. Downloaded from on June 14, 2017 - Published by www.plantphysiol.org Copyright © 1964 American Society of Plant Biologists. All rights reserved.
© Copyright 2026 Paperzz