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poster - International Conference of Agricultural Engineering

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2. Materials and Methods<br />

The study was performed at the Las Tiesas experimental farmland <strong>of</strong> the Agronomic<br />

Technical Institute <strong>of</strong> the Province <strong>of</strong> Albacete, over a reference crop (Festuca arundinacea<br />

Schreb) grown over a surface area <strong>of</strong> 1 hectares, and during a comparative period <strong>of</strong> forty<br />

days, from September 10th to October 19th <strong>of</strong> 2011.<br />

Concerning the calculation <strong>of</strong> the ET, two different methods were used:<br />

a) A weight lysimeter <strong>of</strong> 2.3x2.7x1.7m installed at the centre <strong>of</strong> the parcel (see<br />

figure 1), which is endowed with the required equipment to perform a complete<br />

water balance and to evaluate with precision both water deliveries (rain and<br />

irrigation) and losses (evapotranspiration and deep drainage).<br />

b) The FAO-56 Penman-Monteith equation (Allen et al., 1998) by using the<br />

meteorological data acquired by a weather station placed at the reference<br />

crop.<br />

Figure 1. Lysimeter at the Las Tiesas experimental farmland <strong>of</strong> the Agronomic Technical<br />

Institute <strong>of</strong> the Province <strong>of</strong> Albacete<br />

In order to carry out the comparative study between thermocouples and RTDs for<br />

estimating the ET, a fully equipped Bowen station was installed (see figure 2). This station<br />

was endowed with a NR-LITE net radiometer (Campbell Sci. Inst., USA), placed at 2m above<br />

ground level, an A100 cup anemometer (Campbell Sci. Inst., USA), a RAIN-O-MATIC<br />

pluviometer (Campbell Sci. Inst., USA), two HFP01 soil heat flow plates (Hukseflux, Holanda)<br />

and a CS616 water content reflectometer (Campbell Sci. Inst., USA).

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