Table 1 Diffusion test conditions and the estimated diffusion coefficients for D2O, K+, Cs+, and I− in sugi xylem (sapwood and heartwood).
From: Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water
Sample | Test conditions | Tracer initial condition | |||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
La | Ab | Vc | D2O | Stable K+ | Stable Cs+ | Stable I− | |||||
CHd | CLe | CH | CL | CH | CL | CH | CL | ||||
m | m2 | m3 | ‰ | ‰ | mg L−1 | mg L−1 | ng L−1 | ng L−1 | ng L−1 | ng L−1 | |
Sapwood-1 | 0.022 | 1.13 × 10–4 | 0.0013 | 4700 | − 66.11 | 365 | 0 | – | – | – | – |
Sapwood-2 | 0.022 | 1.13 × 10–4 | 0.0013 | 3399 | − 65.9 | 314 | 0.16 | 496,500 | < 5 | 492,900 | < 5 |
Heartwood-1f | 0.022 | 1.13 × 10–4 | 0.0013 | 4344 | − 62.74 | 374 | 0.19 | 419,050 | < 0.5 | – | – |
Heartwood-2 | 0.022 | 1.13 × 10–4 | 0.0013 | 4345 | − 62.35 | 374 | 0.33 | 419,050 | < 0.2 | – | – |
Heartwood-3 | 0.022 | 1.13 × 10–4 | 0.0013 | 3399 | − 66.4 | 314 | 0.16 | 496,500 | < 5 | 508,500 | < 5 |
Heartwood-4 | 0.022 | 1.13 × 10–4 | 0.0013 | 1910 | − 66.4 | 176.5 | 0.16 | 279,030 | < 5 | 273,950 | < 5 |
Sample | Slope of the regression lines | Estimated diffusion coefficients | Sampling time | ||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
D2O | K+ | Cs+ | I− | D2O | K+ | Cs+ | I− | t > 3·ϕg·L2/D | |||
– | – | – | – | m2 s−1 | m2 s−1 | m2 s−1 | m2 s−1 | days | |||
Sapwood-1 | 0.4505 | 0.0111 | – | – | 2.81 × 10–10 | 8.90 × 10–11 | – | – | 38 | ||
Sapwood-2 | 0.3246 | 0.0091 | 0.0089 | 0.0085 | 2.80 × 10–10 | 8.48 × 10–11 | 5.26 × 10–11 | 5.05 × 10–11 | 38 | ||
Heartwood-1 | 0.8284 | 0.063 | 0.0247 | – | 5.35 × 10–10 | 4.93 × 10–10 | 1.73 × 10–10 | – | 19 | ||
Heartwood-2 | 0.2198 | 0.0087 | 0.0003 | – | 1.42 × 10–10 | 7.59 × 10–11 | 2.46 × 10–12 | – | 70 | ||
Heartwood-3 | 0.2386 | 0.0076 | 0.0029 | 0.001 | 2.06 × 10–10 | 7.06 × 10–11 | 1.70 × 10–11 | 5.75 × 10–12 | 49 | ||
Heartwood-4 | 0.2065 | 0.0098 | 0.0025 | 0.0019 | 3.15 × 10–10 | 1.63 × 10–10 | 2.65 × 10–11 | 2.03 × 10–11 | 32 |