Monitoring soil moisture. For more efficient irrigation

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Monitoring soil moisture For more efficient irrigation Bano Mehdi Advanced Integrated Water Resources Management course Bridgetown, September 26, 2007

Past drought adaptations in Canada included: Increasing irrigation, but in times of low water, or no water, not always viable since irrigation needs often exceed supply Planting native grasses for fodder Planting drought resistant crops, such as lentils Diversification of farm systems Implementing conservation tillage to keep soil moisture More efficient irrigation, such as scheduling irrigation according to soil moisture

Available soil moisture SATURATION FIELD CAPACITY PERMANENT WILTING POINT

Soil-water conditions GRAVITATIONAL WATER SATURATION (0 cbar) FIELD CAPACITY (-30 cbar) PLANT AVAILABLE WATER WILTING POINT (-1500 cbar)

Plant available water

Irrigation needs Precipitation deficit surplus Potential ET April May June July Aug Sept. Oct. Nov.

Irrigation scheduling Irrigation scheduling is deciding when and how much to irrigate based on physical measurements that estimate crop water use and the soil-water status The scheduling depends on soil moisture levels and crop evapotranspiration. This technique can require investment costs, as technical equipment is sometimes used to monitor soil moisture levels

Irrigation scheduling Irrigation scheduling will not reduce losses on-farm from leaking pipes or equipment. It will however help to conserve water by guiding the grower to apply only the right amount required for optimum crop growth throughout the growing season. The timing of application is closely monitored through soil moisture measuring equipment, either in realtime, or through manually read equipment, or downloadable data onto a computer.

Benefits of irrigation scheduling Local (farm) benefits Municipal benefits Sector (agriculture) benefits Water savings on farm Energy savings Higher quality of produce Potential higher crop yields More timely water application to crops When used with fertigation, can lead to greater nutrient use efficiency by crop, and nutrient application savings Water savings at the municipal level Energy savings by reducing the demand on equipment, such as water pumps for example. Improved water quality for the environment by meeting in stream flow requirements for ecosystems Water savings in the agricultural sector Technology transfer and training in the areas of monitoring soil moisture and irrigation scheduling Potential yield increases and crop quality improvement in the horticultural sector Potential adaptation strategies to drought and climate change for growers Increased and advanced knowledge base in water savings Establish a road map to training and extension materials which will accelerate producer and agri-business uptake of the technology available

Monitoring soil moisture for irrigation o o o o needs: Project objectives Provide efficient and timely applications of water to crops Provide growers with water management tools Test equipment in conjunction with growers Obtain grower feedback

Monitoring equipment for soil moisture for irrigation Soil Moisture Depths #Sensors Data Comments Sensor installed (cm) collection Fieldscout TDR 20 1 Portable instrument Data is viewed immediately and recorded Manual 20, 50 2 Manual read Read directly in the field Tensiometers WaterMarks 15, 30, 45 3 Watchdog400 datalogger Data is downloaded, then viewed on computer Capacitance probe 15, 30, 50 1 probe, 3 sensors website Real-time viewable on web site

TDR, permanent and portable TDR: time-domain reflectrometry determines soil volumetric water content. The principal of measurement is based on measuring the travel time of an electromagnetic wave along a waveguide between the two probes. A built in GPS system is able to pin-point the measured sites which is helpful for resampling. Permanent TDR and Datalogger Permanent TDR and datalogger Portable TDR with GPS

Tensiometers, manual and automatic Tensiometers: are installed permanently at the depth of the root zone. They provide a reading of the soil water suction, or tension, caused by the soil water moving away from the ceramic cup (in a drying soil), or moving towards the ceramic cup (in a wetted soil). The water tension is related to the soil water that is available to plants.

Watermarks (gypsum blocks) Watermarks: installed permanently in the soil, and determines volumetric water content which is displayed. It works on the same principal as the tensiometer, it measures the electrical resistance to current flow between electrodes embedded in gypsum; as the gypsum dries the electrical resistance increases between the rods. Watchdog 400 with Watermarks

Capacitance probes C-probes: is inserted into the ground for the duration of the growing season and consists of capacitance sensors attached to a probe column. It can measure volumetric moisture content at up to 6 depths in the soil. Data is transmitted via radio telemetry every 15 minutes to a base station. The output is in millivolts, soil moisture is interpreted from a graph with the software.

Courtesy of Rufa Doria

Project to predict irrigation needs Water Balance Model I=ET-PPT- RO P + SMC Part of the project involves using C-probes to monitor soil moisture Tools for producers to determine when to irrigate Doria, 2006