Rainwater harvesting and artificial groundwater recharge ...
On-Going Research to Estimate Groundwater Recharge in ......On-Going Research to Estimate...
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On-Going Research to Estimate Groundwater Recharge in Agricultural Areas of the Mesilla Valley
Salim Bawazir1 and Alexander “Sam” Fernald2
Graduate Students: Kevin Boyko3 and Jusep Artola3
Project Collaborators: J. Phillip King1 , Zohrab Samani1, Juan Solis1+
Project Funded by the USGS-Transboundary Aquifer Assessment Program (TAAP) through NM WRRI
1 Faculty, Civil Engineering Dept., NMSU;1+ PhD candidate, Civil Engineering Dept., NMSU2 Faculty Watershed Management and Director of NM Water Resources Research Institute3 Water Science and Management Program, NMSU
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Background
• Mesilla Valley Aquifer (Mesilla Bolson) is a trans-boundary aquifer shared between New Mexico, Texas and Mexico
• Significant portion of the drinking water supply for the City of El Paso and Juarez
• Main source of drinking water for residents of Mesilla Valley
• Main source of irrigation water during dry years
• The aquifer is vital for the sustainability of the agricultural industry, economic development and the quality of life in Southern New Mexico, El Paso, and Juarez
• The long-term management and sustainability of the Aquifer depend on understanding the dynamic of the aquifer
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Project Objectives:
- Measure Evapotranspiration (ET) of one of the major crops (i.e. Alfalfa) in the Mesilla Valley
- Measure ET of fallow farm field- ET of fallow ground has not been well quantified in
the hydrologic budget; Often considered “miniscule” and therefore considered “zero”
- Use Ground level ET measurements to verify remote sensing ET Models [Mesilla Valley ET]
- Estimate groundwater recharge based on irrigation practices
Upper (Top) Boundary Layer (i.e. ET) of Groundwater model has often been assumed
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MeasurementLocations
Salopek: 84 acres (34 ha)
Willies: 87 acres (35.2 ha)
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Leyendecker Climate Station(NMSU: Leyendecker Plant Science Station)
Willies Farm – Alfalfa (Eddy Covariance System and Climate Station)
Eddy Covariance System
Climate Station
Soil Moisture Profile
Depth to Groundwater
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Salopek Fallow Farmland –Alfalfa (Eddy Covariance System and Climate Station)
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Preliminary Results:
Recharge to Groundwater: 1.0 - 1.5 ft
ET of alfalfa = 4.6 ft (1403 mm)
Precipitation = 11 in or 0.92 ft (277 mm)
Irrigation Applied = 5.67 ft (1729 mm)
N= 271 days of data collection
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Willie’s Farm; Measured ET Values and Remote Sensing REEM ET Estimates
2/25/2017 Measured = 2.03 mm REEM Satellite Model = 2.00 mm (avg.)3/13/2017 Measured = 4.9 mm REEM Satellite Model = 4.00 mm (avg.)
Improving Remote Sensing ET Models (REEM and SSEBop) is in Progress for the Mesilla Valley
2/25/2017
Remote Sensing Model Estimates –Sample of REEM Estimates
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Thank you