M. Raviv et al., Optimization of transpiration and potential growth rates of 'Kardinal' rose with respect to root-zone physical properties, J AM S HORT, 126(5), 2001, pp. 638-643
Citations number
20
Categorie Soggetti
Plant Sciences
Journal title
JOURNAL OF THE AMERICAN SOCIETY FOR HORTICULTURAL SCIENCE
Physical characteristics of two media were studied concerning water availab
ility to roots, as reflected in specific transpiration rate, stomatal condu
ctance, and specific growth rate of very young leaflets of 'Kardinal' rose
(Rosa x hybrida L.), grafted on Rosa canina L.'Natal Brier'. Plants were gr
own in UC mix [42% composted fir bark, 33% peat, and 25% sand (by volume)]
or in coconut coir. Water release curves of the media were developed and hy
draulic conductivities were calculated. Irrigation pulses were actuated acc
ording to predetermined media moisture tensions. Transpiration rate of plan
ts was measured gravimetrically using load cells. Specific transpiration ra
te (STR) was calculated from these data and leaf area. STR and stomatal con
ductance were also determined using a steady-state porometer. Specific grow
th rate (R-SG) of young leaflets was calculated from the difference between
metabolic heat rate and respiration rate, which served as an indicator for
growth potential. Low STR values found at tensions between 0 and 1.5 kPa i
n UC mix suggest this medium has insufficient free air space for proper roo
t activity within this range. Above 2.3 kPa, unsaturated hydraulic conducti
vity of UC mix was lower than that of coir, possibly lowering STR values of
UC mix-grown plants. As a result of these two factors, STR of plants grown
in coir was 20% to 30% higher than that of plants grown in UC mix. STR of
coir-grown plants started to decline only at tensions around 4.5 kPa. Yield
(number of flowers produced) by coir-grown plants was 19% higher than UC m
ix-grown plants. This study demonstrated the crucial role of reaching suffi
cient air-filled porosity in the medium shortly after irrigation. It also s
uggests that hydraulic conductivity is a more representative measure of wat
er availability than tension.