Dona Aña ET Studies By A. Salim Bawazir, Ph.D. and J. Phillip King, Ph.D., P.E Civil and Geological Engineering Department NMSU, Las Cruces, NM This project is funded by the Lower Rio Grande Water Users Organization and administered by the New Mexico Water Resources Research Institute
Study Goal and Objective Quantify, using diverse data, the consumptive use of water by crops in the Rincon and Mesilla Valleys Measure Evapotranspiration (ET) of the Pecan Goal
Objective Study Goal and Objective Identify major crops in the valleys that have been thoroughly researched such as Cotton and Alfalfa etc. Use historical crop yields and weather data to estimate ET based on Penman method (Jensen et al., 1990)- Penman method Vs. SCS Modified Blaney - Criddle Method Measure actual ET of Pecan
Crop Acreage and Yield Data compiled from 1986 to 1995 and summarized by Elephant Butte Irrigation District (EBID) El Paso County Water Improvement District #1 (EPWCID#1) Middle Rio Grande Conservancy District (MRGCD) Other Data Compiled and summarized from 1987 to 1997 Mesilla Valley (New Mexico) Mesilla Valley (Texas) Rincon Valleys
Crop Acreage Variability from 1978 through 1999 In the Mesilla and Rincon Valleys
2003 EBID Crop Mix
ET Estimates Leyendecker Plant Science Research Center, about 24 km (15 miles) south of Las Cruces (lat 32 o 12'4.44" N, long 106 o 44'32.88" W; elevation 1168 m). Horticulture Weather Station is located about 3.2 km (2 miles) east of Mesilla (lat 32 o 16′43.02′ N, long 106 o 46′15.6″ W; elevation 1183 m).
Relative Humidity Ambient Temp
Solar Rad.
Alfalfa: Kc = 4.05E E-03(GDD) E-07(GDD) E-11(GDD) 3 Pecan: Kc = 2.93E E-03(GDD) E-07(GDD) E-10(GDD) 3 Cotton: Kc = 4.24 E E-03(GDD) E-07(GDD) E-10(GDD) 3 Crop Coefficient Based on Heat Units Example: Penman Equation: Blaney-Criddle Equation: Penman-Sammis:
Pecan ET Based on Penman Equation and Cummulative Growing Degree Days In the Mesilla and Rincon Valleys
4.83*4.75*(4.86) Summary of Crop ET in the Mesilla and Rincon Valleys
PECAN (ET) ?
ALTERNATIVE ET METHODS Eddy covariance methods – 3DECS and OPEC Systems LIght Detection And Ranging - lidar (Raman Water-Vapor Lidar) Heat Pulse Technique (Transpiration) Gas Exchange – Stomata Conductance Others
Monitor Groundwater Soil Moisture Meteorological Remote Sensing ALTERNATIVE ET METHODS
Eddy Covariance
Net Radiation Soil Heat Storage Sensible Heat Latent Heat Land Surface The Energy Budget:
Meteorological Penman-Montieth FAO-56 Equation Modified Penman Equation
Crop Coefficient
NORTH
SOUTH
WEST
EAST
PECAN TREE CANOPY APROXIEMETLY 16M (52FT)
ONE PROPELLER EDDY COVARIANCE SYSTEM (OPEC)
WIND SPEED AND DIRECTION
Q.7 NET RADIOMETER
CSAT KH20 3D SONIC ANEMOMETER & KRYPTON HYGROMETER A highly sensitive three-dimensional sonic anemometer (3D-CSAT3) and a krypton hygrometer (KH2O) were also installed at a height of m (60.5 ft) as check for OPEC system from June 11 DOY 162) through July 31, 2001 (DOY 212).
THERMO- COUPLE PROPELLER OPEC SYSTEM
GROUNDWATER MONITORING USING WATERLOGGER
Sample Results - OPEC System
GRAPH 1A
GRAPH 1-A
PECAN GROUNDWATER DEPTH (June and July) Irrigation
Measured ET of Pecan
More Work and Future Goals Improvement in weather data collection – Net radiation Continue to collect Pecan ET measurements Young Pecan ? Leaf Area Index for Pecan Measure Soil Moisture Remote Sensing Estimate amount of water applied – for management Real Time Data Collection