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water contents were almost greater than 12%. The surface soil water content reached about<br />

34% (vol. %). The low water contents centered at the depth 10–50 cm and radial distance 0–<br />

60 cm illustrated that the root water uptakes were intensive in this area. The agreement<br />

between the simulations and measurements was excellent.<br />

Radial distance from the trunk (cm)<br />

0 20 40 60 80 100 120 140 160<br />

0<br />

Radial distance from the trunk (cm)<br />

0 20 40 60 80 100 120 140 160<br />

44 0<br />

40<br />

44<br />

40<br />

Soil depth (cm)<br />

20<br />

40<br />

60<br />

80<br />

Soil water content (vol. %)<br />

36<br />

32<br />

28<br />

24<br />

20<br />

16<br />

12<br />

8<br />

Soil depth (cm)<br />

20<br />

40<br />

60<br />

80<br />

Soil water content (vol. %)<br />

36<br />

32<br />

28<br />

24<br />

20<br />

16<br />

12<br />

8<br />

100<br />

August 26 - Measured<br />

4<br />

100<br />

August 26 - Simulated<br />

4<br />

Radial distance from the trunk (cm)<br />

0 20 40 60 80 100 120 140 160<br />

0<br />

Radial distance from the trunk (cm)<br />

0 20 40 60 80 100 120 140 160<br />

44 0<br />

40<br />

44<br />

40<br />

Soil depth (cm)<br />

20<br />

40<br />

60<br />

80<br />

Soil water content (vol. %)<br />

36<br />

32<br />

28<br />

24<br />

20<br />

16<br />

12<br />

8<br />

Soil depth (cm)<br />

20<br />

40<br />

60<br />

80<br />

Soil water content (vol. %)<br />

36<br />

32<br />

28<br />

24<br />

20<br />

16<br />

12<br />

8<br />

100<br />

September 2 - Measured<br />

4<br />

100<br />

September 2 - Simulated<br />

4<br />

FIGURE 1: Two-dimensional maps <strong>of</strong> measured and simulated water content values.<br />

Consequently, most <strong>of</strong> the tree root activity, as indicated by temporal and spatial changes in<br />

soil water, was also concentrated in the surface soil layer. Water content pr<strong>of</strong>iles also<br />

revealed that deeper/younger parts <strong>of</strong> the root systems did not extract water as efficiently as<br />

shallower/older roots, suggesting a significant axial resistance could exist in deeper roots<br />

(Pierret et al. 2006). All these observations converge and indicate that a precise description<br />

<strong>of</strong> root water uptake requires the integration <strong>of</strong> data about soil and root hydraulic properties<br />

as well as root spatial distribution. In order to study all these aspects <strong>of</strong> soil–root interplay on<br />

water uptake, modeling can help, in conjunction with experimental work, to test these<br />

hypotheses on water transfer in the soil–root system (Garrigues et al. 2006).<br />

References<br />

Clothier, B. E., & Green, S. R. (1994). Rootzone processes and the efficient use <strong>of</strong> irrigation<br />

water. Agric Water Manag 25:1–12.<br />

Clothier, B. E. (1989). Research imperatives for irrigation science. J Irrigation Drainage Eng<br />

115(3):421–448.<br />

Coelho, E. F., & Or, D. (1999) Root distribution and water uptake patterns <strong>of</strong> corn under<br />

surface and subsurface drip irrigation. Plant Soil 206: 123–136.<br />

Green, S., & Clothier, B. (1999). The root zone dynamics <strong>of</strong> water uptake by a mature apple<br />

tree. Plant Soil 206: 61–77.<br />

Kjelgren, R., Goldhamer, D. A., Uriu, K., & Weinbaum, S. A. (1985). Almond tree response to<br />

variable nitrogen fertilization rates through low volume sprinklers. In: Proceedings <strong>of</strong> the<br />

3rd<strong>International</strong> drip/trickle irrigation congress, Fresno, vol 2.

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