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Farkesht technical guide

Irrigation methods, and choosing correctly between them

The gap between the worst method and the best one is half the field’s water. This dossier puts the five families side by side: where the water goes, what pressure each needs, which conditions each suits, and how any of them has to be scheduled.

Efficiency gap, worst to best method
50%
Typical drip head pressure
1.5bar
Minimum filtration for drip
120mesh

Updated August 20, 2026Farin Kesht Taban Co.

Five families

The shape of the water in the soil is the real difference

An efficiency table tells you drip beats flood. It does not tell you why. Each method’s wetting pattern does.

  • Root depth40–60 %

    Surface and flood

    Basin, border and furrow. Almost no capital cost, but most of the water passes below the roots.

  • Root depth65–85 %

    Sprinkler

    Solid set, wheel-move or centre pivot. Even coverage, but part of the water evaporates or drifts before it lands.

  • Root depth75–85 %

    Micro-irrigation

    Micro-sprinklers and bubblers under the canopy. For orchards and sandy soils, where a single emitter wets too little.

  • Root depth85–95 %

    Surface drip

    Laterals on the surface with emitters. A contained wetted bulb per plant: least wetted area, least weed pressure.

  • Root depth90–95 %

    Subsurface drip

    Laterals buried in the root zone. The surface stays dry, so evaporation nearly disappears — given the right filtration and flushing.

Efficiency, operating pressure and capital cost of the five irrigation methods
MethodApplication efficiencyOperating pressureCapital cost
Surface and flood40–60 %0–0.3 bar1 of 4
Sprinkler65–85 %2.5–4.5 bar2 of 4
Micro-irrigation75–85 %1.5–2.5 bar3 of 4
Surface drip85–95 %1–2.5 bar3 of 4
Subsurface drip90–95 %1–2.5 bar4 of 4

These efficiencies are ranges, not verdicts. A drip system at the wrong pressure with no filter can perform worse than a well-levelled flood field: a good method installed badly is a bad method.

Water audit

Of every 100 litres, how much reaches the crop?

The losses are not interchangeable and neither are their remedies: evaporation is a scheduling and nozzle question, deep percolation is a run-length and soil question, runoff is a levelling question.

  • Surface and flood50 %
    50 %Reaches the crop: 50 %Evaporation and drift: 10 %30 %Deep percolation: 30 %Runoff: 10 %
  • Sprinkler75 %
    75 %Reaches the crop: 75 %18 %Evaporation and drift: 18 %Deep percolation: 5 %Runoff: 2 %
  • Micro-irrigation80 %
    80 %Reaches the crop: 80 %12 %Evaporation and drift: 12 %Deep percolation: 6 %Runoff: 2 %
  • Surface drip90 %
    90 %Reaches the crop: 90 %Evaporation and drift: 4 %Deep percolation: 5 %Runoff: 1 %
  • Subsurface drip93 %
    93 %Reaches the crop: 93 %Evaporation and drift: 1 %Deep percolation: 5 %Runoff: 1 %
  • Reaches the crop
  • Evaporation and drift
  • Deep percolation
  • Runoff
Figures are the mid-point of each method’s range under ordinary design and operation; what a particular field achieves is established by measuring that field.

Hydraulic design

Four numbers that make or break a design

Two systems built from identical pipe and identical emitters can deliver completely different efficiency. The difference is these four figures.

90%
Emission uniformity (EU)

The minimum a new drip block should return on a field test.

20%
Allowable pressure variation

Spread across one block; beyond this, uniformity starts to fall away.

2%
Maximum lateral fall

Past this slope, pressure-compensating emitters stop being optional.

8h
Maximum block run time

The basis of blocking: source flow divided by block demand sets how many blocks there are.

No design is drawn before the source flow and pressure are measured. Most failing systems we are called to have the right pipe and the wrong source.

Selection

Which method for which conditions

Method selection does not start with the crop, it starts with the constraint: the slope, the water quality, how much water there is, and the soil texture.

Suitability matrix: field condition against irrigation method
Suitability matrix: field condition against irrigation methodSurfaceSprinklerMicroDripSubsurface
Steep groundNot recommendedSuitableSuitableSuitableSuitable
Saline waterNot recommendedNot recommendedNot recommendedSuitableSuitable
Scarce or rotational waterNot recommendedNot recommendedSuitableSuitableSuitable
Sandy soilNot recommendedNot recommendedSuitableSuitableSuitable
Strong windSuitableNot recommendedNot recommendedSuitableSuitable
Row cropsSuitableSuitableNot recommendedSuitableSuitable
OrchardsSuitableNot recommendedSuitableSuitableNot recommended

The table shows technical suitability, not the best option. Drip suits saline water because it keeps salt off the leaves — but that same water still needs its own leaching schedule.

Scheduling

When to irrigate, and how much

The best system in the world is wasted on a calendar schedule. Soil water is spent at a rate the weather sets, and it is put back just before the allowable depletion line is crossed.

  • Field capacity
  • Allowable depletion
  • Stress zone
  • Irrigation event
Drawn from a six per cent daily depletion against a fifty per cent allowable depletion; the real rate comes from that field’s daily ET and rooting depth.
  • Crop water demand

    ETc = ET₀ × Kc

    Reference evapotranspiration multiplied by the crop coefficient for that growth stage. The output is millimetres used per day.

  • Depth and interval

    d = (θfc − θ) × Zr ÷ Ea

    The deficit back to field capacity, times rooting depth, divided by system efficiency. The output is the net depth per event.

Water quality

What actually blocks an emitter

Emitter clogging almost always has one of three causes: suspended particles, chemical precipitation, or biological growth. The bands below are the range in which the hazard is low.

  • Suspended solids

    0–50 mg/L

    0200 mg/L

    Sand and silt particles; removed by mechanical filtration.

  • Total dissolved solids

    0–500 mg/L

    02,000 mg/L

    What later precipitates as carbonate and sulphate scale.

  • Water pH

    5.5–7 pH

    09 pH

    Above 7.5 the likelihood of calcium precipitation rises sharply.

  • Iron

    0–0.1 mg/L

    01.5 mg/L

    Oxidises into orange scale and feeds bacterial slime.

  • Manganese

    0–0.1 mg/L

    01.5 mg/L

    Like iron, but a black deposit and harder to shift.

  • Bacterial population

    0–10,000 /mL

    050,000 /mL

    Biological slime; controlled by periodic chlorination.

Filtration a drip system needs

The working rule: the filter must stop anything larger than a tenth of the emitter passage.

  • Screen filter

    120 mesh130 µm

    Cheap and simple; suits well water carrying mineral particles.

  • Disc filter

    130 mesh120 µm

    Higher holding capacity; for water with a moderate organic load.

  • Media filter

    200 mesh75 µm

    For surface water, reservoirs and algae, with backflushing.

No filter replaces flushing the lateral ends. A scheduled flushing routine, with acid or chlorine injection, is part of the design — not an emergency measure.

Questions

What growers ask about choosing a system

The six that come up most.

Which irrigation method is best?

That is the wrong question. The method follows your constraint: with scarce water and sandy soil, drip; with levelled ground and plentiful cheap water, improved surface can be the better economics. Establish the constraint first, then the method.

Is drip always worth it?

Where water is limited or expensive, almost always. But the real cost of drip is not the pipe: the filter station, the fertigation injection and the flushing routine are part of the system, and leaving them out blocks it within two seasons.

Which method suits saline water?

Drip or subsurface drip, because salt never lands on the leaf and continuous moisture keeps the concentration down in the root zone. In exchange, salt accumulates at the edge of the wetted bulb and you need periodic leaching.

Why do our emitters keep blocking?

Three common causes: the wrong filter or an unwashed one, chemical precipitation in high-pH water, and bacterial growth. A water analysis says which — without it, replacing emitters only postpones the problem.

Can an existing flood system be converted to drip?

Yes, but conversion does not start with buying pipe. Source flow and pressure are measured first, then the blocking is designed; in most cases the existing source cannot irrigate the whole area at once and the system has to be laid out in shifts.

How do I know how much water I am applying?

A meter at the head and a simple emitter discharge test. Until the delivered volume is measured, any discussion of efficiency is guesswork.

Want to know which method will actually work on your land?

We start with a water analysis and a measurement of the source flow. After that, choosing the method is the easy part.