Abstract:
Water is considered as a critical resource for agriculture and supplying the
right amount in the right time is essential for healthy plants and optimum
productivity. This objective can be met only through scientific water management
and judicious water application, which in turn requires proper scheduling of
irrigation events. For most of the agricultural crops a relationship can be found
between evapotranspiration and climate by introducing a crop coefficient (K c ),
which is the ratio of crop evapotranspiration (ET c ) to reference crop
evapotranspiration (ET o ). Hi-tech horticultural systems use protected cultivation
with soil and soil less media as substrates. Evapotranspiration in open field and
inside of polyhouse will differ due to the micro climatic variation. Water balance
components in the mini lysimeter will be influenced by the atmospheric condition
and the media used in the mini lysimeter. At present water requirement for open
field vegetable cultivation is adopted as such as in polyhouse cultivation. Hence
there is a need to study the consumptive use of crops in soil and soilless media
inside the polyhouse.
Field experiment on the comparative evaluation of evapotranspiration
parameters in a naturally ventilated polyhouse for alternate growing media was done
in a Naturally ventilated polyhouse in the research plot of the Department of
Irrigation and Drainage Engineering, in KCAET campus, Tavanur. In the study,
Non-Weighing Mini-Lysimeters were used to determine evapotranspiration
parameters and to develop crop-coefficient curves for Okra for soil and soil less
media. The study compares the data for soil and soil less media in order to quantify
the properties of these medias on evapotranspiration. ET 0 was estimated by Penman
montieth equation using CROPWAT model. Studies on crop morphological
parameters indicated that plant growth and yield parameters were higher for soil
media than soil less.
Seasonal average ETc values of Okra for soil and soil less media were 4.23
and 3.1mm/day. The calculated values of Kc for the initial, mid and late seasonstages were 0.98, 1.5and 0.74 in soil. Soil less media values were 0.72, 1.16 and 0.5
for different stages respectively. It was observed that soil less Kc values were lower
than the soil. This may be due to the higher water holding capacity of the soil less
media, which resulted in lesser evapotranspiration. The results implied that water
requirement is lower for soil less media compared to soil.
The results of this study can be used as a guideline in the computation of
water requirement of soil and soil less in polyhouse for Tavanur region. If the poly
house irrigation is scheduled in such a way as to apply the right quantity of water
enough to meet the evapotranspiration requirements of crops, considerable water
saving can be achieved.