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poster - International Conference of Agricultural Engineering

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model was introduced to estimate the air flow turbulence. Using the wind velocity predicted<br />

by this model, the vapor pressure and air temperature in the vicinity <strong>of</strong> the soil surface were<br />

estimated by the numerical model describing the air heat and vapor transfer in the microadvective<br />

condition. The energy budget on the soil surface was estimated using the wind<br />

velocity, vapor pressure, and air temperature simulated by these models. The soil water<br />

content and temperature were predicted using the simulation model describing the water and<br />

heat transfer in the soil. Using the energy budget, the accuracy <strong>of</strong> this model was verified by<br />

a wind tunnel.<br />

2. Methodology<br />

2.1. Analysis <strong>of</strong> airflow field around an isolated crop<br />

The governing equations describing the wind flow around an isolated crop can be written as<br />

follows:<br />

∂u<br />

∂v<br />

+ = 0<br />

∂x<br />

∂z<br />

∂u<br />

∂u<br />

∂u<br />

1 ∂p<br />

∂ ⎛<br />

+ u + v = − + ⎜ K<br />

∂t<br />

∂x<br />

∂z<br />

ρ ∂x<br />

∂x<br />

⎝<br />

∂v<br />

∂v<br />

∂v<br />

1 ∂p<br />

∂ ⎛<br />

+ u + v = − + ⎜ K<br />

∂t<br />

∂x<br />

∂z<br />

ρ ∂z<br />

∂x<br />

⎝<br />

a<br />

a<br />

∂u<br />

⎞ ∂ ⎛<br />

⎟ + ⎜ K<br />

∂x<br />

⎠ ∂z<br />

⎝<br />

∂v<br />

⎞ ∂ ⎛<br />

⎟ + ⎜ K<br />

∂x<br />

⎠ ∂z<br />

⎝<br />

a<br />

a<br />

∂u<br />

⎞<br />

⎟ − C<br />

∂z<br />

⎠<br />

∂v<br />

⎞<br />

⎟ − C<br />

∂z<br />

⎠<br />

where u and v are the wind velocity in horizontal and vertical directions (m·s -1 ), ρ is the air<br />

density (=1.293kg/m 3 ), p is the air pressure (g·m -1·s -2 ), K a is the eddy diffusion coefficient<br />

(m 2·s -1 ), C m is the resistance coefficient by crop canopy, S is the leaf area density(m 2·m -3 ) , t<br />

is the time, x is the fetch, and z is the height.<br />

Eddy coefficient described in eqs. (2) and (3) can be estimated as follows:<br />

K<br />

a<br />

2 ∂u<br />

= λ<br />

m<br />

(4)<br />

∂z<br />

The parameter λ m , inside and outside <strong>of</strong> the crop canopy can be represented as the following<br />

equations, respectively.<br />

3<br />

2κ<br />

λ<br />

m in<br />

= (5)<br />

C m<br />

S<br />

( z − )<br />

λ = κ<br />

(6)<br />

m out<br />

d 0<br />

The parameter <strong>of</strong> inside <strong>of</strong> the crop canopy λ m in can be estimated as follows:<br />

( z − d ) 0 m in : = κ ( z − )<br />

κ > λ<br />

m in<br />

d 0<br />

m<br />

m<br />

S<br />

S<br />

u<br />

u<br />

2<br />

2<br />

+ v<br />

+ v<br />

λ (7)<br />

2<br />

2<br />

v<br />

u<br />

(1)<br />

(2)<br />

(3)<br />

κ z > λ<br />

m<br />

in<br />

: λ = κz<br />

(8)<br />

m in<br />

2.2. Heat and vapor transfer under micro-scale advection<br />

The equations that describe the air heat and vapor transfer in the advective condition can be<br />

written as follows:

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