Background of Study. Background of Study Background of Study Potential use of low cost drip irrigation technology in upland watersheds for dry season.

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Presentation transcript:

Background of Study

Background of Study Potential use of low cost drip irrigation technology in upland watersheds for dry season cropping Use of drip is gaining popularity in developing countries ( e.g. use of IDE Easy drip in SEA watersheds through SANREM) Maximization of crop yield depends on irrigation water distribution uniformity Choice of operating head compounded by topographic condition

Basic Issue What operating head to employ to maximize water distribution uniformity under sloping conditions?

OBJECTIVE To determine the effect of hydraulic head and slope on the water distribution uniformity of the IDE ‘Easy Drip Kit’ and consequently develop mathematical relationships to characterize the effect of slope and head on water distribution uniformity

METHODOLOGY 100 sq. m IDE Easy drip kit (10 m x 10 m) Submain Slopes: 0%, 10%, 20%, 30%, 40% and 50% (Sl = 0%) Operating Head: 1.0 m, 2.0 m and 3.0 m Sampled from 11 emitters per lateral for a total of 110 samples Direct volumetric measurement for emitter discharge 3 trials per setting At least 54 laboratory experiments

Experimental Set-up for Testing the IDE Drip Irrigation System College of Engineering & Agro-industrial Technology, University of the Philippines Los Baños

Experimental Set-up for Testing the IDE Drip Irrigation System College of Engineering & Agro-industrial Technology, University of the Philippines Los Baños

Experimental Set-up for Testing the IDE Drip Irrigation System College of Engineering & Agro-industrial Technology, University of the Philippines Los Baños

Sampling and Data Collection

Evaluation of Water Distribution Uniformity Christiansen’s Coefficient of Uniformity UC = (1-D/M)100 where: UC = coefficient of uniformity (%) D = average of the absolute values of the deviation from the mean discharge M = average of discharge values

Evaluation of Water Distribution Uniformity Merriam and Keller’s Emission Uniformity EU = (qLQ/qmean)100 where: EU = emission uniformity (%) qLQ = average of the lowest quarter of the observed discharge values qmean= average of observed discharge values

RESULTS

Typical emitter discharge variation along the lateral of the IDE drip kit at 0% slope

UC and EU at various Heads at 0% slope

Effect of Head on UC at Various Slopes

Effect of Head on EU at Various Slopes

Effect of Slope on UC at Various Heads

Effect of Slope on EU at Various Heads

Linear Regression Model* Linear Regression Models for UC as a Function of Head at Various Slopes Slope (%) Linear Regression Model* R2 Y=1.50X + 65.02 0.233 10 Y=19.90X + 15.06 0.975 20 Y= 8.67X + 24.09 0.995 30 Y = 8.32X + 20.25 0.927 40 Y=4.14X + 12.98 0.722 50 Y = 1.35X + 8.37 0.997 * Y = coefficient of uniformity, UC (%) X = head (m)

Linear Regression Model* Linear Regression Models for UC as a Function of Slope at Various Heads Head (m) Linear Regression Model* R2 1.0 Y= -0.95X + 54.69 0.850 2.0 Y= -1.15X + 68.57 0.987 3.0 Y= -1.27X + 77.91 0.943 * Y = coefficient of uniformity, UC (%) X = submain slope (%)

Observed and Predicted UC vs. Head at 0% Submain Slope

Observed and Predicted UC vs. Head at 10% Submain Slope

Observed and Predicted UC vs. Head at 20% Submain Slope

Observed and Predicted UC vs. Head at 30% Submain Slope

Observed and Predicted UC vs. Head at 40% Submain Slope

Observed and Predicted UC vs. Head at 50% Submain Slope

Observed and Predicted UC vs. Slope at 1.0 m Head

Observed and Predicted UC vs. Slope at 2.0 m Head

Observed and Predicted UC vs. Slope at 3.0 m Head

CONCLUSION Water distribution uniformity of the 100 sq m IDE Easy drip kit proved to be influenced by operating head and submain slope UC and EU increase with increasing head for all slopes A head of 3.0 m may be considered as optimum from both hydraulic and practical considerations for all slopes UC and EU decrease with increasing slope for all heads UC and EU decrease tremendously for slopes > 30%

CONCLUSION For 0% slope, a head differential of 0.5 m does not cause significant change in UC or EU UC is linearly related to either head or slope Linear regression models proved to be adequate to characterize the relationship between UC and head and between UC and

RECOMMENDATION To minimize non-uniformity of water distribution, control valves or pressure regulators may be installed along the submain IDE may consider including affordable pressure regulators for use of the drip kit in steep slopes Emitter clogging should be addressed to prevent occurrence of minimal or zero emitter discharge Further studies are recommended to address water distribution uniformity issues

Acknowledgements This project was funded by USAID for SANREM-CRSP awarded to Virginia Tech, North Carolina A&T State University and University of the Philippines Los Baños Foundation, Inc. Paper presentation was made possible through the support from DA-BAR and SEARCA Engrs. Arthur Fajardo and Noel Gordolan and everyone who helped in data gathering

Thank You!

Contact Information Dr. Victor B. Ella Associate Professor and Dean College of Engineering and Agro-industrial Technology University of the Philippines Los Banos College, Laguna, PHILIPPINES E-mail: vbella@up.edu.ph or vbella100@yahoo.com Tel/fax: (049)-536-2873