k
r
|
Radial hydraulic conductivity |
Individual roots or root segments |
m MPa−1 s−1
|
L
r (Doussan et al., 2006; Huang & Nobel, 1994; North & Peterson, 2005) |
Usually not directly measured, but calculated using k
root and k
x measurements, based on the model of Landsberg and Fowkes (1978). |
k
x
|
Specific axial hydraulic conductance |
Individual roots or root segments |
m4 MPa−1 s−1
|
K
h (Doussan et al., 2006; Huang & Nobel, 1994; North & Peterson, 2005); K
x (Ahmed et al., 2018); L
x (Frensch & Steudle, 1989; Melchior & Steudle, 1993) |
The ability of roots to transport water longitudinally |
k
x_cs
|
k
x normalized by cross sectional area |
Individual roots or root segments |
m2 MPa−1 s−1
|
K
s (Choat et al., 2012; Pratt et al., 2007) |
k
x data for woody species is very commonly reported on a cross sectional area basis (sapwood, stele, total root cross section) |
k
root
|
(Total) root hydraulic conductivity |
Individual roots or root segments |
m MPa−1 s−1
|
L
pr (Boursiac, Protto, et al., 2022; Kim et al., 2018; Steudle, 2000a); L
p (Gambetta et al., 2017; Huang & Nobel, 1994; Lambers & Oliveira, 2019; North & Peterson, 2005) |
The total water transport capacity of an individual root or a root segment. It can be separated into its radial and axial components. Often assumed to be an approximation of k
r in the literature (i.e., water transport only limited by k
r, not by k
x
|
K
rs
|
Whole root system conductance |
Entire root system |
m3 MPa−1 s−1
|
K
root (Cai et al., 2022); L
p (Lambers & Oliveira, 2019); L
pr (Kim et al., 2018; Steudle, 2000a), L
0 (Boursiac, Protto, et al., 2022; Maurel et al., 2010; Tyerman et al., 2017) |
The water transport capacity of the entire root system. |
K
rs_norm
|
K
rs normalized by a measure of the root system size |
Entire root system |
Depends on normalization |
|
Most common normalizations found in the literature include:Root surface area: K
rs_area (m MPa−1 s−1);Root fresh or dry weight: K
rs_weight (m3 MPa−1 s−1 g−1);Root length: K
rs_length (m3 MPa−1 s−1 m−1); Root volume: K
rs_vol (m3 MPa−1 s−1 m−3) |