Hose, soaker hose, or drip runtime

How long should I water a raised bed?

There is no reliable universal number of minutes. Measure the flow of the installed setup, choose the volume or geometric depth you want to represent, calculate runtime, and then check what actually happened in the bed.

Quick answer Measure first.

Runtime = target volume ÷ measured whole-zone flow. The same target can take 10 minutes with one setup and 40 minutes with another because their flow rates differ.

Why a fixed time fails

A minute is not an amount of water.

Every setup flows differently

Faucet pressure, hose length and diameter, filters, regulators, timers, fittings, emitter count, clogging, elevation, and competing household use can change delivery.

Every bed receives water differently

Soil texture and condition, mulch, slope, compaction, existing moisture, root depth, and irrigation layout affect infiltration, spread, drainage, and runoff.

Worked example—not a recommendation

A 4 × 8 foot raised bed

A 4 × 8 foot bed has 32 square feet. One inch spread geometrically over that area represents about 19.9 U.S. gallons.

19.9 gal ÷ measured flow = runtime

The one-inch target is used here only to show the arithmetic. It does not establish that this bed, crop, soil, or weather needs one inch today.

Measured whole-zone flow2.0 U.S. gal/min19.9 ÷ 2.0 = about 10 minutes
Measured whole-zone flow0.5 U.S. gal/min19.9 ÷ 0.5 = about 40 minutes
Metric example10 mm over 3 m² = 30 LAt 6 L/min, 30 ÷ 6 = 5 minutes
Metric identity1 mm over 1 m² = 1 LThis is geometric volume, not proof of root-zone delivery.
Measurement-first workflow

From the installed setup to a checked result

1. Test the setup you will actually run

Keep the faucet, hose, timer, filter, regulator, injector, fittings, and watering line in the intended configuration. A faucet-only result may not represent a connected soaker hose or drip zone.

2. Measure whole-zone flow

Use a calibrated container and repeated fill times, or an isolated meter difference. Preserve the capture point, settings, trials, and test conditions.

3. Select the calculation target

Enter a volume, or enter bed area and a geometric depth. The target is your calculation input—not a crop-specific recommendation from TerraEvidence.

4. Calculate runtime

Divide the target volume by measured flow in matching units. TerraEvidence applies no hidden crop, climate, soil, efficiency, or schedule multiplier.

5. Verify in the bed

Check several locations for wetting depth and distribution. Note runoff, dry gaps, leaks, clogged emitters, and soil moisture before deciding whether to change the next run.

Choose the matching path

Hose, soaker hose, and drip lines need the right flow basis.

Hose or sprinkler

Measure the flow with the nozzle and settings you will use. If the setup distributes water over an area, inspect coverage separately; total flow does not prove uniform application.

Run a bucket-and-stopwatch flow test

Soaker hose

Measure only the isolated soaker-hose pathway when possible. Keep hose length, size, layout, regulator context, and beginning-middle-end observations attached to the record.

Use the isolated-soaker pathway

Point-source drip

If you have an actual emitter count and a sourced per-emitter rate, calculate nominal total output. Pressure, clogging, elevation, line length, and equipment condition can still change actual delivery.

Calculate drip output

Known volume over an area

Convert an entered water volume into geometric equivalent depth, then keep distribution, infiltration, and root-zone delivery as separate questions.

Calculate applied water depth
Interpretation boundary

The runtime is arithmetic—not a watering prescription.

It represents

  • Runtime for an entered target at a measured or explicitly sourced flow
  • Calculated volume from flow × runtime
  • Geometric equivalent depth when an area is entered
  • A record tied to the tested setup and units

It does not prove

  • Whether watering is needed today
  • Plant-water requirement or watering frequency
  • Uniform distribution across the bed
  • Infiltration, runoff, drainage, or root-zone storage
  • The cause of crop stress or irrigation-system problems
Check the soil before and after watering.

Use several representative root-zone locations. Interpret the observations with rainfall, weather, crop condition, soil, and suitable local guidance rather than following the same timer setting automatically.

How to check soil moisture before watering
Reviewed 29 August 2026

University and Extension sources

These sources support measuring actual delivery, preserving setup context, and checking field conditions. TerraEvidence keeps the narrower calculation boundary stated above.

Washington State University

Shows that garden-hose flow depends on hose diameter, hose length, and dynamic supply pressure.

Garden Hose Flow Rate and Time

This educational guide does not replace local Extension advice, equipment instructions, water-use restrictions, or professional irrigation design.