Irrigation Systems & Methods — Interactive 2D/3D Teaching Visualizer

Irrigation Systems & Methods — Interactive Visualizer

Every parameter is teacher-adjustable. Drag inside any 3D view to orbit · scroll to zoom.

Family tree

How irrigation methods are classified

Water can reach the root zone in four ways — flowing over the soil, sprayed through air, dripped at the plant, or supplied below ground.

Suitability engine

Which method fits this field?

Score out of 100 from soil, slope, water, labour, capital, crop and salinity. Bars update live.

Water balance

What each method costs you in water

MethodField application efficiency EaGross depth/dayStream neededWater/season (100 d)

Gross depth = ETc ÷ Ea · Stream = gross depth × area ÷ operating hours (assumed 8 h/day).

3D field

Water advancing down the field

The blue front moves exactly as the volume-balance simulation predicts. Scrub time or press play.

drag to orbit · scroll to zoom
t = 0 min
2D analysis

Advance–recession curve & infiltrated depth profile

Advance curve Recession curve Stored in root zone Deep percolation Deficit (under-irrigated)
Ea = Vstored / Vapplied  ·  DU = Zlow quarter / Zavg  ·  opportunity time τ(x) = trecession(x) − tadvance(x)
Cross-section

Wetting pattern across the furrow / border

Sandy soils push water down (narrow, deep bulbs) so furrows must be closer; clays spread water sideways.

3D field

Overlapping spray patterns

Sprinklers must overlap: a single circle under-waters its own edge. The floor colour is the depth of water actually landing.

drag to orbit · scroll to zoom
q = Cd·A·√(2gH)  ·  I = 3600q/(SlSm) mm/h  ·  CU = 100(1 − Σ|xi−x̄| / n·x̄)
2D analysis

Single-sprinkler profile and the overlap sum

Blue = water from one sprinkler at distance r. Gold = total depth after neighbours overlap. Flat gold line = uniform irrigation.

Discharge and throw both rise with √H, but drop size falls — high pressure with a small nozzle turns the jet into wind-blown mist.

3D field

Wetting bulbs under the emitters

Only part of the soil is wetted — that is the whole point of drip, and the reason its efficiency is so high.

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q = k·hx L/h  ·  EU = 100(1 − 1.27Cv/√n)·qmin/qavg  ·  Vsoil = Vwater/Δθ
2D analysis

Bulb shape by soil, and emitter response to pressure

Same litres of water, five soils. Sand drains down; clay spreads wide. Bulb width sets the maximum emitter spacing.

x = 0 is a perfectly pressure-compensating emitter (flat line — best for sloping fields); x = 1 is a fully turbulent long-path emitter.

3D field

The boom sweeps a circle

Outer spans travel much faster and must therefore discharge far more water per metre than the inner ones.

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d = 3600·Q·T/(πR²) mm  ·  vedge = 2πR/T m/h  ·  peak rate = d·vedge/w mm/h
2D analysis

Why the outer nozzles are the big ones

Discharge needed per metre of boom Instantaneous application rate Soil infiltration rate

Where the gold curve rises above the red line, water arrives faster than the soil can take it — that is where runoff and wheel-track rutting start.

3D field

Water delivered below the surface

Nothing evaporates from a dry surface, and no weeds germinate between the rows — but the wetting bulb must still reach the roots.

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2D section

Soil profile — bulbs, roots, capillary fringe

Wetted bulb Root zone Water table & capillary fringe Dry soil
Soil-water bucket

When to irrigate, and how much

AW = (FC − PWP)/100 · ρb · D  ·  RAW = p · AW  ·  interval = RAW / ETc  ·  gross = RAW / Ea
Method comparison

Same crop, same field, eight methods

MethodEaGross depthWater per irrigationSet time at your streamSeason use (100 d)

Bars show water saved per season against wild flooding, for the field area you set.

Interactive teaching aid — irrigation systems & methods · all models are simplified for classroom use Built for PiyushAI Edtech · piyushai.com