Journal of Experimental Botany, Vol. 47, No. 304, pp. 1699-1707, November 1996 Journal of Experimental Botany Validating sap flow measurement in field-grown sunflower and corn1 Y. Cohen 24 and Y. Li3 2 Department of Environmental Physics and Irrigation, Agricultural Research Organization, The Volcani Center, PO Box 6, Bet Dagan 50250, Israel 3 Xinjiang Institute of Geography, Chinese Academy of Science, Urumqi, Xinjiang, People's Republic of China Received 2 November 1995; Accepted 28 June 1996 Abstract Introduction Sap flow measurement has been widely used recently in studying plant response to the environment, but results have not always been satisfactory. The possibility that the non-uniform distribution of the conducting elements in the stem cross-sectional area introduces error in the measurements was examined. The heat pulse method, combined with anatomical observations of the stem at the point of sap flow measurement, was applied in corn and sunflower, to study the interaction between anatomical structure and sap flow distribution. The probability of the temperature sensor being in contact with conducting elements was strongly affected by its insertion depth into the stem; the measured heat pulse velocity for a given transpirational flux was correlated with the number of conducting elements in contact with the sensor. Consequently, the calibration coefficient is affected by the position of the thermocouple junction in relation to the conducting elements. This dependence of apparent heat pulse velocity on density of conducting elements suggests that thermal equilibration in species with large stems may not be achieved within the limited time of heat dissipation. The relationship between sap flow and leaf area of single plants was used to test the consistency and the accuracy of the sap flow measurements. The ratio of measured to potential transpiration was used to validate the use under field conditions, of the calibration coefficient determined in potted plants. When lysimeter systems are not available, measurement of sap flow in the stem becomes an alternative method for determining canopy transpiration under field conditions. The accuracy of water uptake estimates based on sap flow measurement depends on two scales of integration: on a single plant level the integration is affected by variability in the distribution of the conducting elements in the stem cross-sectional area; and on a community level integration should be made to account for the variability among plants (Dugas, 1990; Cohen, 1994). Both levels were examined in this study, the first under greenhouse and laboratory conditions, and the second in the field. The single plant level of the integration was studied by means of the heat pulse method. The correlation between stem anatomical structure and heat pulse velocity was examined in potted plants of two herbaceous species with large stem diameter. The heat pulse method was selected in this study because it is easily adapted to field conditions. The technique has been applied previously to herbaceous species with small stem diameter; it involves a calibration coefficient that varies between species and is assumed to be dependent on stem anatomical structure (Cohen, 1994). Use of the equations describing the heat dissipation in wood with moving sap requires that the stationary wood and the moving sap act together like a single medium moving at a uniform speed (Marshall, 1958). The effect of stem anatomical structure on the deviation of computed sap flow from the theoretical value was recognized in conifer trees by Marshall (1958). Later it has been shown that variation in the cross-sectional distribution of sap flow causes inconsistent results in some Key words: Heat pulse, transpiration, LAI, potential transpiration. 1 4 Contribution from the Agricultural Research Organization, the Volcani Center, Bet Dagan, Israel. No. 1694-E, 1995 series. To whom correspondence should be addressed. Fax: +972 3 9604017. C Oxford University Press 1996 1700 Cohen and Li herbaceous species (Baker and Nieber, 1989; Ishida et al., 1991). For instance, the vascular system in mature dicot plants consists of a ring of bundles in the periphery of the stem (Esau, 1960). In young dicot stems or at the top of the stem, the bundles are distinct and form strands, whereas at lower levels they merge to form a continuous ring (Knowles, 1978). Monocot species, on the other hand, have widely spaced vascular bundles, which are not restricted to one circle in transection, but are scattered throughout the section (Sass, 1977). With such an uneven distribution of the vascular system, it is likely that in a species with a large stem diameter (corn, sunflower), the sensor, which occupies only a small proportion of the stem cross-sectional area, measures a heat pulse velocity which differs from the average value for the entire stem area. An important question related to this aspect is, what would be the effect of the density of the vascular system on the time required to equalize the temperatures of the stationary tissue and the flowing sap, following a heat pulse? It is assumed that the higher thermal conductivity of the stainless steel needle, relative to that of the stem tissue, allows reasonable averaging of the temperature over the length of the needle. The objective of the present study was to test this assumption for corn and sunflower. Integration of the community level depends on the variability among plants in the field. The measurement procedures and the calibration coefficients which had been determined in potted plants were applied in the field, to evaluate the effect of plant variability on the estimation of canopy transpiration. In previous studies this variability had been addressed by selecting plants with a wide range of stem diameter or plant leaf area, two parameters which were usually considered to be related to plant transpiration rate (Kanemasu et al., 1976; Tanner and Jury, 1976; Al-Kaisi et al., 1989). The objective of the present study was to validate the extrapolation of measured single plant sap flow to canopy transpiration, with plant leaf area used as a parameter reflecting the variability between plants. Materials and methods where k (mm2 s ') is the thermal diffusivity of the stem and tm is the time at which the temperature at the upper sensor reaches a maximum. A more detailed explanation of an alternative use of equations 1 and 2 has been presented previously (Cohen et al., 1993). The sap flux in the stem, 7, is defined as Ji = [(pc)/(j>lCi)]v (3) where />, and c, are the density and specific heat of the liquid, and p and c are the density and specific heat of the wood, respectively. The determination of p and c is destructive, therefore, in contrast to the case of trees, their evaluation in the measured plant is not possible during the heat pulse velocity measurement. On the other hand, slight variations between plants and changes in the volume fractions of water and woody matrix in the course of the day are common in herbaceous plants (Kitano and Eguchi, 1989). However, sap flow measurements by the heat balance methods assume a fixed value of stem thermal conductivity, despite the variation induced by stem water content fluctuations (Sakuratani, 1984, Ishida et al., 1991). In this procedure the sap flow is computed from the heat pulse velocity, stem area, and a calibration coefficient which combines p and c values, the effect of the implantation wound size, and the structure of the xylem conducting area. The consistency of this coefficient for a given species, irrespective of plant age, and time of day, as found in our previous studies of cotton, soybean, corn (Cohen et al., 1988, 1993) and pepper (unpublished data), suggests that the effect on sap flux of diurnal changes in p and c is not significant. The probe block used for the heat pulse velocity measurement consists of a line heating element and two temperature sensors mounted on a phenolic fibre plate, 40 x 20 x 8 mm. The heating element and the sensors are made from hypodermic stainlesssteel needles of 0.5 mm o.d. and 0.25 mm i.d. and a detailed description of the probe has been given by Cohen et al. (1988). The insertion depth of the thermocouple needle was determined by placing pertinax (polyphenol) spacers of 2.3 mm width between the probe block and the stem. When 0, 1 or 2 spacers were used, the insertion depths were 7.8, 5.5 or 3.2 mm, respectively. A previously described transpiration model (Fuchs et al, 1987) was used to compute the potential transpiration (Tp). Inputs to this model were global radiation (Kipp and Zonen, Delft, Netherlands), air temperature and humidity (Model 201, Campbell Scientific, Logan, UT, USA) and wind speed (Model 014A, Met One, Sunnyvale, CA, USA), measured at 2.5 m above the soil surface in an automated meteorological station. Data were scanned every 10 min, averaged for 60 min intervals, and recorded with a battery-powered datalogger (CR21, Campbell Scientific). Potential transpiration Tp (m s" 1 ) was calculated by using the Penman equation (Monteith, 1965): (4) Measurements The heat pulse velocity (v) was measured as described previously (Cohen et al., 1988). For low or moderate sap flow rates v was estimated as = (Xl-X2)/2t0 (1) where Xx and X2 are the distances from the heater to the thermocouple junctions above (9 mm) and below (4 mm) the heater, respectively; t0 is the elapsed time from pulse emission to the first recurrence of the initial temperature difference. For high sap flow rates the accuracy of t0 estimation is unacceptable, therefore, v was estimated as (2) Where s is the slope of the saturation vapour pressure curve (kPa°C"'), y is the psychrometric constant (kPa°C~'), /?„ is the net radiation observed by the foliage (J m~ 2 s~'), p is the density of air (kg m~ 3 ), cis the specific heat of air(J k g " 1 0 C ~ ' ) , e,-e, is the air-water vapour pressure deficit (kPa). The resistance for water flux from the canopy ru, was computed as: in which r, is the aerodynamic resistance (s m" 1 ), rb is the boundary layer resistance (s m " 1 ) , and SLA1 is the sunlit leaf area index. Sap flow in sunflower and corn The net radiation Rr, was computed after Fuchs et al. (1987): RB = (0.55YfxKxSLA/-RLN (6) where n is an empirical factor between 0 and 1 that accounts for radiation entrapment resulting from multiple scattering between sunlit leaves, K is the direct component of global radiation, and RLN is the net thermal radiation. A constant value of 0.5 was assigned to n. The factor / equals 0.5 divided by the cosine of sun angle from the zenith. Other inputs to the model were the leaf area index, crop height, row width, and leaf width. Calibration Calibration and field tests were conducted in corn (Zea mays L. cv. Jubilee) and sunflower (Helianthus annuus L.). For calibration, plants were grown in pots 250 mm in diameter and 300 mm in depth, filled with a mix of sand and peat and located in a plastic-covered shelter measuring 20 x 6 x 2.5 m. The pots were wetted daily, and nutrient solution was added as required. Heat pulse velocity measurements were carried out in plants of different ages and the computed flow rates were compared with the rates of water loss, measured by automatically weighing the pot to the nearest 0.1 g every 15 min. At the end of the calibration period (2-3 d for each plant), the plant was removed from the pot, the soil was carefully washed from the root system and the plant was transferred for 24 h to a new pot containing a dilute safranin solution. Thin cross-sections of the stem, about 0.2 mm thick, were taken near the point of probe insertion and examined under a microscope. The number of bundles in corn and sunflower stems was determined in 25-30 microscopic fields of 2.3 mm diameter each. For instance, in a corn stem of 18 mm diameter, 15 microscopic fields were examined in the first annulus at a depth of 0-2.3 mm below the bark, seven fields in the second annulus, 2.3-4.6 mm below the bark, four fields in the third annulus, 4.6-6.9 mm below the bark, and four fields in the central part of the stem. 1701 irrespective of their location relative to the dripper. The row spacing was 1 m and the plant population density was close to 3.6 x 10" plants ha" 1 . The plot contained 18 rows, each 15 m long. Two irrigation treatments were applied: 330 and 156 mm of water applied at weekly intervals for the whole season. The experimental design comprised randomized blocks, with four replicates. The probes for heat pulse velocity measurement were installed on the second internode of the stem, to a depth of 5.5 mm, using one pertinax spacer. One probe was installed in each of 20 plants (10 plants per treatment) and heat pulse velocity was measured simultaneously in the 10 plants of one treatment every 15 min, so that the sap flow of each treatment was monitored at 30 min intervals. Stem diameter measurements were taken on installation and removal of the probes. Before installation of the probes, stem diameters of all plants in a 6 m row length in each treatment were determined. The stem diameter distribution of the sample was used to select 10 plants with a diameter distribution matching that of the sample, for heat pulse velocity measurements. The number of plants per unit area and the average computed sap flow rate of the individual plant (kg h" 1 ) were used to calculate the canopy transpiration (T) per unit ground area (mm h " 1 ) . A battery-powered data logger (CR7X, Campbell Scientific) was used to monitor the sensors and control the relays operating the heaters. The maximum distance between the data logger and the measured plants was 5 m. At the end of the measurement period, after removal of the probes, the plants were cut below the lowest leaf, for determination of the leaf area in the laboratory, with an optical area meter (Delta T Devices, Burwell, Cambridge, England). Two neutron probe access tubes were installed in each side of the sprinkler line to a depth of 1.5 m, at distances of 2, 4, 7, and 10 m from both sides of the sprinkler line. Probe readings were taken at 0.3 m depth intervals 2, 4 and 6 d after each irrigation event. Leaf water potentials were measured with a pressure chamber (Arimad-2, Kibbutz Kfar Charuv, Israel) between 10.00 and 12.00 h on four sunlit leaves from each row, 2, 4 and 6 d after each irrigation event. Field experiments Data were collected from experimental sites at the Volcani Center in Bet Dagan (32°01' N, 34°50/ E, 25 masl) and at Kibbutz Yefa'at in the Yizre'el Valley (32°40' N, 35° 13' E, 50 masl). The experiment in Bet Dagan was conducted during the summers of 1990 and 1994 in a 0.4 ha corn plot. The soil is classified as a sandy loam soil (Rhodoxeralf by USD A designation) with 10% clay and 85% sand. The plot measured 30 x 140 m, with row spacing of 1 m and a plant density of 6-8 m" 1 . Two irrigation lines with sprinkler discharge of 8 mm h " 1 at a pressure greater than about 150 kPa were placed along the plot at a distance of 12 m from the sides to provide a central overlap of 6 m. Irrigation was applied at weekly intervals, and the amount of water applied to the plot averaged 0.7 of the weekly total pan evaporation. The water application rate varied with distance from the line source, from zero on rows near the plot border to 1.8 times the pan evaporation in the central rows, where the supplies from the two irrigation lines overlapped. The experiment in the Yizre'el Valley was conducted during the summer of 1994, with sunflowers in a 0.5 ha plot located within a large commercial field. The soil, classified as vertic or typic aquic chromoxerent, consists of 60% clay, 35% silt and 5% sand. Drip irrigation systems were used, with one line of drippers per row, in-line spacing of 1 m between drippers and a nominal water discharge of 2.3 1 h ~' from each dripper. Plants were selected for heat pulse velocity measurement Results The results of measurements of transpiration (T) of the plants in the plastic-covered shelter and apparent heat pulse velocity measurements, taken simultaneously at 15 min intervals are shown in Fig. 1. Heat pulse velocity was measured by two sensors installed in the same corn plant at the second and fourth internodes, to 5.5 and 7.8 mm depth, respectively, on opposite sides of the stem. The product of apparent heat pulse velocity and stem cross-sectional area (av) at the point of measurement was highly correlated with T determined by weight loss, irrespective of the sensor depth in the stem. The slopes of the regression lines in Fig. 1, for sensors inserted to 5.5 and 7.8 mm depths were 1.57 and 1.88, respectively. As described previously (Cohen et al., 1993) the slope is taken as a calibration coefficient for a given species. Slope and correlation coefficient values of the linear regressions between Tand av of six calibrated corn plants of different stem diameters, with similar sensor installation configurations as shown in Fig. 1, are given in Table 1. 1702 Cohen and Li Table 2. Bundle density and number of bundles in contact with 2.3 mm sensor segments at various depths beneath the bark of corn stem of 17.5 mm diameter 0.15i -. 0.12 Depth beneath bark (mm) sensor depth 5.5 mm T = -0.001 + 1.57 av R 2 » 0.93 sensor depth 7.8 mm T = 0.0004 + 1.88 av 0-2.3 4.6-6 9 2.3-4.6 p D 0.06 0.27 0.40 0.27 - 1.69 1 93 2.17 2.41 2.14* B, P D B. P D B. 1 94 2.22 2.49 2.77 2.45* 0.14 0.71 0.15 _ - 0.72 0.96 1 20 _ 0.96* 0.83 1 11 1.38 _ 1.10* 0 75 0.25 _ _ - 0.48 0 72 0.54* 0.55 0 83 0.62* R 2 = 0.95 0.03 0.06 0.09 0.12 0.15 * weighted average. P probability of appearance of particular density D (bundles mm" 2 ). B, number of bundles in contact with the sensor av (kg h plant ) Fig. 1. The relationship between transpiration (7*) determined by weight loss and the product of heat pulse velocity and the stem area (av) measured by two sensors installed at different depths in the corn stem. Table 1. Slope and correlation coefficient (R 2 ) of the linear regressions between the product of heat pulse velocity and stem area (av) and transpiration (T) in corn plants of different stem area: two sensors were inserted to 5.5 and 7.8 mm depths on opposite sides of the stem Stem area 113 154 177 201 227 283 Average SD Sensor at 5.5 mm depth Sensor at 7.8 mm depth Slope R 2 Slope R2 64 .62 .53 .61 .59 .56 .59 0.057 0.91 0.90 0.94 0.89 0.92 0.94 2.11 1.72 2.14 2.02 1.93 1.84 1.96 0.148 0.97 0.94 0.89 0.88 0.92 0 86 With the sensor inserted to a 5.5 mm depth, the slope of the linear regression was smaller and less variable than with insertion to a 7.8 mm depth. The relative position of the sensors, i.e. whether the deeper insertion was at the upper or lower position on the stem did not affect the slope. In another group of six plants, with two probes inserted in the same stem, both to a depth of 5.5 mm, an average slope of 1.57 was obtained for both sensors with standard deviation (SD) of 0.048. The linear regression slopes obtained for plants into which probes were inserted to a 3.2 mm depth were much lower than those shown in Table 1, but the variability among plants or among different orientations of the stems was high. Therefore, the measurements by insertion to a 3.2 mm depth were excluded from the analysis. The number of bundles in contact with the sensor (Bt) in each of three measured sections of a 17.5 mm diameter corn stem is given in Table 2. B, was taken as bundle density (D) multiplied by the stem area occupied by the sensor (2.3 x 0.5= 1.15 mm2). The probability (P) of appearance of D expresses the proportion of the stem area with a particular D to the total area of the stem section. In the section nearest to the bark the bundle density was higher than in deeper sections, therefore, the weighted average number of bundles in contact with the sensor was 2.7 as compared with 0.69 in the annulus at a depth of 4.6-6.9 mm below the bark. Excluding slight variations between plants, the bundle arrangement shown in Table 2 were repeated in all other measured mature corn plants. Variations in bundle density among different stem orientations were not significant (not shown in Table 2). The sensor position within the cross-sectional area of a 19 mm diameter corn stem, and the location of the thermocouple in the needle are shown in Fig. 2, in which the probability of a 2.3 mm-long sensor section being in contact with various numbers of conducting bundles, as calculated from all examined plants is also given. The probability that a sensor section extending from 0-2.3 mm Depth tmneath bark Imm) A | Thermocouple junction | 0-2.3 0.8 0.6 0.2 0.0 0 1 2 3 4 NUMBER OF BUNDLES IN CONTACT WITH THE SENSOR Fig. 2. Sensor position within the cross-sectional area of a 19 mm diameter com stem and the probability of a sensor being in contact with various numbers of conducting bundles. Sap flow in sunflower and corn depth below the bark will be in contact with one, two, three or four bundles is 0.04, 0.57, 0.37 or 0.02, respectively. With increasing depth beneath the bark, the number of bundles in contact with the sensor diminishes markedly. In a sunflower stem, the conducting system forms a nonsymmetrical ring of bundles located adjacent to the bark and not more than about 3 mm beneath it. In a stem of 16 mm diameter, the continuity of the ring of conducting elements is often interrupted by non-conducting tissue, but in a young stem of 10 mm diameter completely separate coloured blocks of various diameters were observed. The slopes and correlation coefficients of the linear regressions between T and av of six calibrated sunflower plants of different stem diameters with sensors inserted to a depth of 5.5 mm below the bark on opposite sides of the stem are given in Table 3. The slope value was 0.73 (or 0.72) with a standard deviation of 0.054 (or 0.048). The similarity between the two sides in the slope values suggests that there is little orientational variability in the sunflower stem. Insertion of the sensors to a depth of 7.8 mm in another group of six sunflower plants yielded a poor relationship between T and av; the slopes of the linear regressions were between 1.01 and 1.41, and they varied widely among plants and between the two sides of the stem (Table 4). Tables 1, 3 and 4 indicate that stem diameter had no effect on the regression slopes (calibration coefficient), although it might be expected that the density of the conducting tissue would change with age. The findings also suggest that the tangential distribution of bundles in the stems of both species may be considered uniform. In contrast, the radial distribution of the bundles is not uniform, therefore, the calibration coefficient depended on insertion depth. Field measurements of sap flow were made in 1990 with sensors at depths of 5.5 and 7.8 mm, but only the data from 5.5 mm depth will be considered here. During 1994, heat pulse sensors were inserted into corn and sunflower stems to a 5.5 mm depth. Figure 3 shows the Table 3. Slopes and correlation coefficient (R 2 ) of the linear regressions between the product of heat pulse velocity and stem area (av) and transpiration in sunflower plants of various stem areas: two sensors were inserted to a 5.5 mm depth on opposite sides of the stem Stem area (mm 2 ) 64 106 125 158 211 232 Average SD Side A Opposite to side A Slope R1 Slope R2 0.81 0.72 0.73 0.66 0.79 0.68 0.73 0.054 0.83 0 89 0.94 0.91 0.92 0.95 0.77 0.73 0.80 0.66 0.72 0.69 0.72 0.048 0.84 0.83 0.88 0.94 0.93 0.96 1703 Table 4. Slopes and correlation coefficient of the linear regressions between the product of heat pulse velocity and stem area (av) and transpiration (T) in sunflower plants of various stem areas: two sensors were inserted to a 7.8 mm depth on opposite sides of the stem Stem area (mm 2 ) 76 117 137 149 167 206 Average SD Side A Opposite to side A Slope R1 slope R1 1.34 1.01 1.41 1.09 1.28 1.15 1.21 0.141 0.92 0.87 0.93 0.91 0.84 0.% .12 .39 .21 .13 .41 .09 .23 0.149 0.83 0.88 0.94 0.91 0.95 0.89 0.8 distance from sprinkler line (m) c CD 1 0.6 73 0.4 Q_ < 0. T80 182 184 186 188 DAY OF YEAR 190 19 Fig. 3. Daily sap flow of corn plants at various distances from the sprinkler line. daily sap flow of corn for various distances from the sprinkler line, measured in 1994; since the water amount decreased with distance from the sprinkler line, leaf area and sap flow decreased accordingly. The figure indicates the capability of the method to measure small day-to-day differences in sap flow as well as differences between rows and between dry and wet soils. The values in Fig. 3 are averages over five plants for each distance from the sprinkler line. The relationship between sap flow of 10 plants, taken at 1 m from the sprinkler line, and their leaf area is shown in Fig. 4. The parameters of the linear regression for the data points in the figure and of regressions for other groups of 10 plants, taken at distances of 1, 4, 7, and 10 m from the line, are given in Table 5. There is a clear linear link between sap flow rate and LAI for LAI values of up to 3.9, which may be deduced from the closeness of the regression slope values for the three longer distances from the sprinkler line, and also from the high correlation coefficients (R2). On the other hand, the slope of the linear regression at 1 m distance, with an LAI of 4.9 was lower than those of the plants at longer distances from the sprinkler line. It indicates that the LAI of the plant 1704 Cohen and Li Table 5. LAI and regression parameters of the linear relationship between sap flow of individual corn plants and leaf area of plants at various distances from sprinkler line Distance from line (m) LAI (mean of 10 plants) I 4 7 10 Regression parameters 4.9 3.9 2.8 I 2 0.4 0.6 0.8 2 LEAF AREA (m plant') Fig. 4. The relationship between sap flow and leaf area for 10 corn plants, taken at 1 m distance from the sprinkler line. at 1 m distance was above the threshold level at which the sap flow per unit area diminishes because of attenuation of radiation by the canopy. It may also be explained by ageing of the leaves, with some older portions becoming non-functional in water vapour exchange. The low correlation coefficient of the linear regression at 1 m from the line also suggests wide variability in exposure to radiation. A high correlation between sap flow and leaf area in individual plants was also found in sunflower (Fig. 5). The maximum leaf area of water-stressed sunflower plants (irrigation of 150 mm) was nearly 0.4 m2 per plant compared with 1 m 2 in well-irrigated plants (230 mm). For this reason the maximum LAI was 3.1 and 2.2, respect- 1^ • l/rigrton with 150 mm SE of coefficient 0 21 0.07 0.11 0.03 0.753 0.841 0.863 0.859 0.74 0.87 0.93 0.91 0.15 0.11 0.09 011 ively, for the plots irrigated with 230 and 150 mm annually. These values of LAI are below the values obtained in well-developed stands of sunflower (Jaafar et ai, 1993). Figure 5 indicates no difference between the two irrigation treatments in sap flow per leaf unit area. To validate the use of the heat pulse method for determination of canopy transpiration, the relationship between measured transpiration and potential transpiration was studied. The comparison between the two was made only for days when there were indications that water supply to the plants was sufficient. Figure 6 shows the distribution of soil water content for a mature corn canopy, on the second day after the irrigation. The soil water content at 1-5 m distance from the sprinkler line was close to full water capacity at all depths, excluding 0.15 m. On the same day, the soil water content at greater distances from the sprinkler line was below the maximum capacity, therefore, plants could have been under differing degrees of water stress. Midday leaf water potential during the first and second days after an irrigation event at 1 -5 m distance from sprinkler line was — 1.2 ± 0.1 MPa, but at greater distances from the sprinkler line it was —1.6 ±0.15 MPa. In view of the above results it is assumed that for the first 2 d after an irrigation event, water availability to the plant was not a limiting factor for transpiration of plants located up to 5 m from the sprinkler line. No measurement of leaf conductance was carried out either in 1990 or in 1994, but in 1995 a set of intensive leaf conductance measurements was made in Z 0.20 m R - 0.73 O 0.15 o 0 O ^0.6 a. 0 R2 SF - 0.05 + 1.83 LA 1.6 C/3 Slope _ 0.30 'E " E 0.25 -—2.6 A Constant £ o.io < Irrigation with 230 mm SF - 0 1 B + 1.88 LA 0.05 R - 0.83 0.2 0.4 0.6 0.8 1.2 LEAF AREA (m 2 plant'1) Fig. 5. The relationship between sap flow and leaf area for sunflower plants irrigated by two different water amounts. ° r*—•• distance from sprinkler line (m) 1 3 5 7 10 O 0.3 D A • • 0 . 6 0 . 9 SOIL DEPTH (m) 1.2 1.5 Fig. 6. Soil water content as a function of soil depth for several distances from the sprinkler line, under a mature corn canopy. Sap flow in sunflower and corn corn on the same plot. Sunlit leaf conductance of about 4.5 mm s" 1 was maintained, as long as the weighted volumetric soil water content at 0.15-0.75 m depth was above 0.22 m 3 m~3. Canopy transpiration (T) was computed from sap flow and plant number per unit area. The contribution of the secondary shoots to canopy transpiration was taken into account by calculating the ratio between their leaf area and that of the whole plant. As described above, the transpiration model takes account of several plant parameters, including leaf area. In computation of Tp, therefore, values of Tp on a given day will depend on the LAI. Figure 7 presents the diurnal course of T and Tp for two groups of 10 corn plants grown in 1990, at 1 m and 5 m, respectively, from the sprinkler line, with an average of 7.8 plants per 1 m row. The LAI (based on the leaf area of the plants in which sap flow was measured) was 5.7 and 4.2 for plants at 1 m and 5 m distance, respectively. The computed Tp for 1 m distance was 9.28 mm d" 1 while that for 5 m distance was 7.15 mm d" 1 . Figure 7 shows that canopy transpiration, as computed from sap flow measurements, was closely related to Tp at both distances but lagged behind it. The T/Tp ratio on a daily basis was 0.85 or 0.82 for plants at 1 m or 5 m from the sprinkler line, respectively. The results of measured transpiration taken on other days were also closely related to Tp, with the T/Tp ratio around 0.8, as long as soil water content was close to field capacity. The close relationship between potential and measured transpiration, with a consistent ratio between the two, irrespective of plant size, indicates the high reliability of extrapolating single plant heat pulse measurement results to canopy transpiration. Discussion In both corn and sunflower, when the thermocouple junction was positioned in the vicinity of densely packed conducting elements, the measured heat pulse velocity for a given transpirational flux was higher than in areas with sparsely distributed elements. This was evident when the thermocouple junction was inserted deep into the stems of both species, where the number of conducting elements was zero or close to zero. This influence of junction position on measured heat pulse velocity explains the different calibration coefficients found for the two species and for different insertion depths into the stems. It also indicates that the relatively high thermal conductivity of the stainless steel was not sufficient to average the temperature over the length of the needle. In corn and, more likely, in sunflower stems, a section of thermocouple needle (nearest the bark) is always in contact with sap-conducting elements, because of the high density of bundles in corn and the continuous ring of active conducting tissue near the bark in sunflower. Hence, it might be expected that the thermocouple needle section would immediately detect the wave of heat carried by the sap. However, with increasing needle insertion depth, the measured heat dissipation rate decreases because of the low density of bundles in the deeper layers of the stem. The change in bundle density with depth may explain the difference in calibration coefficients between corn and sunflower. Because of the continuous ring of sap-conducting tissue in a mature sunflower stem, the thermocouple needle section near the bark is always in contact with conducting elements and is immediately heated by the moving sap, so that the measured heat pulse velocity per unit transpirational flux is high, resulting in a low calibration coefficient for sunflower. On the other hand, in corn the conducting bundles are distributed unevenly in the stem, so that the probability for the sensor to be in contact with conducting tissue is smaller than in sunflower, even near the bark, and it decreases with increasing penetration into the stem. Therefore, the measured heat pulse velocity per unit transpirational flux is low and the cahbration coefficient for corn is high. These findings imply that, following a heat pulse, a local thermal equilibrium between the stationary tissue 1.2 5 m distance from the sprinkler line ___ 1 m distance from the sprinkler line 1 £ £ 0.8 a I- 0.6 o 0.4 0.2 0 4 8 12 16 20 1705 0 4 8 12 16 2C 24 TIME OF DAY Fig. 7. Diurnal course of transpiration (7*) and potential transpiration (Tp) for plants grown at 1 m or 5 m distance from the sprinkler line. 1706 Cohen and Li and flowing liquid is established as the theory requires (Marshall, 1958). However, a thermal equilibrium over the entire area occupied by the sensor is not attainable within the time limit of the heat pulse. This problem is likely to be more critical in large stems than in small ones, since the conducting system is more evenly distributed in the latter (Webber, 1938), and the metal needle occupies a proportionately larger area of the stem. Difficulties in the analysis of stem sap flow by means of heat pulse velocity measurements were found in an earlier study also, and were attributed to non-uniformity of heat dissipation in the stem (Pickard, 1973). Non-uniform radial heat dissipation in the stems of herbaceous species has been discussed in other studies also (Kitano and Eguchi, 1989; Ishida et ai, 1991). In large stems such as tree trunks, the existence of a radial gradient in convective heat pulse velocity has been recognized and been taken into account by using a multisensor temperature probe. Such a sensor facilitates independent measurements in radially narrow regions within the stem (Dye et al., 1991; Olbrich, 1991). In view of the interaction between the stem anatomical structure and the sensor configuration, the calibration coefficient should be determined individually for each species and for any given sensor configuration. While the necessity for calibration of the method for each species was stressed in our previous studies, the present results emphasize the interaction between sensor location and stem structure in determining the calibration coefficient. For instance, the importance of inserting the sensor to an exactly determined depth was not carefully considered in our previous study with corn (Cohen et al., 1993) and, consequently, the calibration coefficient varied widely among plants and was slightly higher than in the present study. The shape of the bundles in corn has been found to be fairly constant in several lines and hybrids (Sass, 1977), which indicates that the same calibration coefficient can be used for various corn varieties and environmental conditions. The findings of the present study may be used more widely in the interpretation of other sap flow methods, which use a steady-state heating of a stem section and in which temperature changes are monitored mostly at the stem surface (Sakuratani, 1984; Baker and Nieber, 1989). When the conducting system structure is similar to that in sunflower, the bark temperature variation most likely represents thermal changes caused by diurnal variations in the sap flow rate, but with a conducting system like that in corn or sorghum, the effect of changes in the heat balance of the stem section on the bark temperature strongly depends on the radial heat conductivity of the stem (Zhang and Kirkham, 1995). Since the findings in the present study indicate low heat conductivity in the tissue between the bundles, it may be expected that changes in sap velocity in bundles located away from the bark would not be detected instantaneously by means of stem-surface temperature measurements. In spite of the theoretical and technical problems described above, the heat pulse method has been found useful for monitoring canopy transpiration in field-grown cotton (Cohen et al., 1995). The present data validate the use of the method for plants with large stem diameter. Because no absolute measurement was used in the field to determine transpiration, the relationship between the sap flow and leaf area of single plants was used to test the consistency and the accuracy of sap flow measurements. The close correlation between leaf area index and 7 has been demonstrated by other researchers (Kanemasu et al., 1976; Tanner and Jury, 1976; Ritchie and Johnson, 1990). The high correlation between sap flow and leaf area found in the present study validates the use of this measurement procedure and suggests that the results were free of external environmental noise. The high correlation between potential transpiration computed by the model and transpiration measured by the heat pulse method, under non-limiting water supply, validates the use of the calibration coefficient determined for potted plants. A consistent ratio between the potential and measured transpiration, irrespective of plant size, plant age and environmental conditions, validates the extrapolation of the results of sap flow measurements in single plants to canopy transpiration. References Al-Kaisi M, Brun LJ, John WE. 1989. Transpiration and evapotranspiration from maize as related to leaf area index. Agricultural Forest Meteorology 48, 111-16. Baker JIM, Nieber JL. 1989. An analysis of the steady-state heat balance method for measuring sap flow in plants. Agricultural Forest Meteorology 48, 93-110. Cohen Y. 1994. Thermoelectric methods for measurement of sap flow in plants. In: Stanhill G, ed. Advances in bioclimatology, Vol. 3. Heidelberg: Springer-Verlag, 63-89. 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