Skip to main content

Table 3 Parameter estimates and coefficients of determination (R 2) of the relationship between environmental variables and daily transpiration rate (E, mm day−1) per tree height class during 2008

From: Environment and tree size controlling stem sap flux in a perhumid tropical forest of Central Sulawesi, Indonesia

Tree height class (m)

E vs. Dmean

E vs. R

E vs. SWC

E = a (1-exp(−bDmean))

E = E = b0 + b1R

E = b0 + b1SWC

  

E = b0 + b1SWC + b2SWC2

a

b

R 2

P

b 0

b 1

R 2

P

b 0

b 1

b 2

R 2

P

<10

0.009

1.762

0.86

<0.001

−0.0003

0.0003

0.55

<0.001

0.014

−0.0002

0.12

<0.001

10–20

0.086

1.629

0.75

<0.001

−0.0024

0.0025

0.47

<0.001

0.133

−0.0002

0.12

<0.001

20–30

0.114

2.894

0.80

<0.001

0.0039

0.0043

0.59

<0.001

−1.265

0.0586

−0.0006

0.07

<0.001

>30

0.763

5.159

0.69

<0.001

0.2364

0.0243

0.45

<0.001

−10.543

0.4807

−0.0052

0.07

<0.001

  1. The relationship between E and vapour pressure deficit (D mean, kPa) followed an exponential form for all tree height classes. The relationship between E and solar radiation (R, MJ m−2 day−1) was better fitted to a first-order polynomial in all tree height classes. The relationship between E and soil water content (SWC, %) was better explained by a first-order polynomial in the smaller tree height classes and by a second-order polynomial in the taller trees