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Did You Know?
• California Farm Gate value in 2009
– ≈ 36 – 37 billion dollars
– 90% comes from products produced on irrigated lands
– California does not have a water problem, it has a salt problem
Talking Points For Interpreting Irrigation Analysis Data
• Why such a complete analysis?
• Critical elements
• Basic parts of an irrigation water analysis
• Interpreting your irrigation analysis data
• Water-born pathogens
• Soil-Plant-Water interrelations
• Units and conversions (see handout)
First
Why Such A Complete Analysis?
• To make sure the data is valid
• To make sure every critical element is examined
• To check cations and anions are in balance
• To check that electrical conductivity and total dissolved solids correlate– TDS x 0.7(conversion) = approximate E.C.
Closer look at soil N avail
Critical Elements• Chloride – Specific ion toxicity
• Boron – Specific ion toxicity
• Sodium – Should be less than 60 % of cations
• Bicarbonate – High bicarbonate water seals the soil
• Carbonate – Waters containing carbonate must have a pH > 8.3 and are usually very pure
• E.C. – Should be less than 1200 umhos/cm for salt sensitive crops
• SAR (Sodium Absorption Ratio) – Severe problems will persist above 9
Next prop to look at is pH
Anions
• These are the predominately found negative ions in irrigation water
• Meq of cations = Meq of anions
Next prop to look at is pH
Micronutrients
• These are plant micronutrients that may or may not be available
Water Pathogens
• E. Coli 157 – Bacteria derived from fecal contamination
• Salmonella – Primarily found in surface water
• Listeria – Primarily found in refrigerated conditions
Soil-Water-Plant Interrelations
• A sickly plant growing in a well drained and well fertilized soil is likely to be struggling with a pathogen or a physical disorder
• High soil Potassium promotes Magnesium deficiencies in plants
• High Magnesium soils usually have low infiltration rates
• High soil Phosphorus levels promotes low plant uptake of Iron, Zinc, Manganese, and Copper
1 of 3
Soil-Water-Plant Interrelations• Soil pH will eventually be nearly the same as the
irrigation water pH
• Soil E.C.e should be 1.5 to 2 times the water EC. If higher, check soil drainage and/or leaching conditions
• At an E.C.e above 8, the soils osmotic pressure will be too high and plants will be stressed
• At a higher E.C.e the soil solution may extract water from the plant or the fruit
2 of 3
Soil-Water-Plant Interrelations
• As soil texture becomes heavier, water and nutrient holding capacity increases
• As soil texture becomes heavier, the availability of water and nutrients decreases
• As soil pH changes nutrient availability also changes (see pH chart)
• Hard water makes soft soil
• Soft water makes hard soil
3 of 3
Adjusting the soil pH changes more than just the pH
____________________________
Another ? on Micros
The Real Benefit of Water Data
• Better crop selection
• Better salinity management
• Improved economic yields