Evapotranspiration (ET), calculated using the Penman-Monteith (FAO-56) formula, needs hourly weather data (or 15 or 30 minute intervals, but not daily).
The ET is calculated in each interval, and the total mm is summed for each day for graphing, or for use in other formulas.
The calculations are in accordance with FAO Irrigation and Drainage Paper 56 Crop evapotranspiration - Guidelines for computing crop water requirements.
The Penman-Monteith Method HOWELL T.A, EVETT S.R.
Select a weather station logger with daily data, use, and add a new calculated sensor. Select formula: ET0 Daily (FAO 56)
Station is optional. It enables minor corrections for station altitude, height, latitude and longitide to be applied
Values need to be entered into a text file - eg:
Station: Goanna will get values from file
Crop factor defaults to a value of 1. The value graphed = ET * CropFactor.
A file can be specified that allows the crop factor to vary with date.
Crop Factor: cotton.fac
1 Aug, 0.30
1 Sep, 0.35
1 Oct, 0.4
1 Nov, 0.5
1 Dec, 1.0
1 Jan, 1.05
1 Feb, 1.0
1 Mar, 1.0
1 Apr, 1.0
1 May, 1.0
Adjust allows ET to be the FAO56 standard for a short crop (Cn=900, Cd=0.34), or a high crop (Cn=1600, Cd=0.38). see here.
The water balance (or cheque-book) method is to calculate the water left in the soil each day by subtracting the daily value of ET, and adding any irrigations or rainfalls.
M-Log can do the calculattions with either , or as a separate calculated sensor.
The top blue line is total water content in the profile calculated from soil moisture sensors at different depths.
The vertical bars are probable gains, with the estimated gain amounts (5mm, 15mm, etc) shown as a vertical green bars.
The blue line at the bottom is ET from an NZ scheduling service (???).
The red line is total water content calculated using the ET values.
The starting value is set to be the first measured water content (about 310mm om 24 Oct).
Each day the calculated water content is decreased by the ET value.
After each gain the calculated water content is increased by the estimated gain amount.
If the calculated water content is close to or above the full point, the water content is set equal to the full point.
The ET values could be from a commercial service e.g. iWater, downloaded automatically by M-Log each day, or from a weather station.
As well as allowing colours ,e ct to be set, a calculated sensor also allows the gains to come from a rain sensor, or a sensor recording applied irrigations.
Data courtesy Fruition NZ.
The total mm through the plant in the season can be calculated by totalling the daily water us. This can be used to estimate of yield, or to calculate yield per Ml. see here.
Extra or calculated ???
M-Log calculates the next irrigation, and can also calcuate all irrigations required for the rest of the season.
The total water content can be calculated for the whole season.
The last reading was on 20 Feb, and M-Log is then calculating the ideal irrigation schedule for the remainder of the season using ET from a ???
Scheduling can start from last RZ calculated from ETTotal, or a user set RZ1 using drag/drop. Only one prediction line can be plotted at a time: calculated, user or historical. also sets that this et will be used for scheduling Et for remainder od fseason taken from 'historical', of not set from last measured, ig not set from user, if not set = 5 mm/day. the date of next flood irrigation can be 'fixed' drag/drop of user rate for predictions
Use, select the calculated RootZone sensor, and on the tab 'Plot to end of season'.
The upper and lower limits are set on thetab. The limits are defined in an RDI file, and can be either...
If Use for scheduling is not checked the FULL or REFILL values are used.
The ET used to calculate the schedule is the 'historical' sensor used to calculate the next irrigation selected on the M-Log will automatically adjust the year.tab. It can be a sensor in a weather station or an ET file. The weather data can be from any year -