Estimate watering time using area, depth, and flow. Add breaks, moves, and cycle soaking. Get consistent results and reduce wasted watering time.
Calculator Inputs
Example Data Table
| Scenario | Area | Depth | Flow | Efficiency | Zones | Estimated elapsed |
|---|---|---|---|---|---|---|
| Raised beds | 18 m² | 12 mm | 7 L/min | 0.75 | 3 | ~45–60 min |
| Small lawn patch | 40 m² | 8 mm | 10 L/min | 0.65 | 4 | ~55–75 min |
| Container garden | 8 m² | 15 mm | 5 L/min | 0.80 | 2 | ~35–50 min |
Formula Used
How to Use This Calculator
Shallow rooted greens often respond well to 6–10 mm per session, while fruiting vegetables typically need 12–20 mm when temperatures rise. For lawns, 8–15 mm per watering encourages deeper roots than frequent light sprays. Use the depth field to match your goal and keep notes by season. If you are unsure, start at 10 mm and adjust using soil feel tests after each week.
Hand watering flow changes with nozzle settings and hose length, so measure at the exact setup you will use. Time how long it takes to fill a 10 liter bucket, then convert to liters per minute by dividing 10 by minutes. Repeat twice and average the values. This reduces error and keeps the time estimate stable across different days and pressures. Record bucket volume and timing in a log so recalculations are immediate later.
Efficiency represents how much applied water actually reaches the root zone. Calm, close range watering on flat beds can reach 0.80–0.90. Wind, splashing on foliage, sloped ground, or runoff can drop results to 0.50–0.70. If you see puddling before infiltration, lower efficiency and use cycle limits. Conservative settings prevent under watering and improve planning reliability.
Splitting the garden into zones helps distribute attention and prevents over watering one area while rushing another. Use bed edges, plant groups, or sprinkler reach as boundaries. The calculator divides active time across zones, so you can set a repeatable routine such as three minutes per bed. Keep zones similar in size when possible, or adjust by watering priority for new plantings and heat stress.
Clay soils and compacted paths often accept water slowly, causing runoff when watering is continuous. Set a cycle limit, then allow a soak period so water moves downward before the next pass. Two cycles of five minutes with an eight minute soak can outperform one ten minute run. This approach improves uniformity, reduces surface losses, and shortens the time spent correcting dry spots.
FAQs
Increase depth modestly, usually 12–20 mm for most beds. Also reduce frequency to promote deeper roots. Use soil checks to confirm moisture below the surface.
Fill a known bucket size and time it. Divide liters by minutes to get liters per minute. Repeat and average for better accuracy.
Not all water reaches the soil due to wind, runoff, and overspray. Efficiency corrects for those losses so the calculated time delivers the intended soil moisture.
Use them on clay, slopes, or compacted areas where runoff starts quickly. Short cycles with soak pauses improve infiltration and reduce wasted surface water.
Group areas with similar water needs and access. Keep zone sizes manageable so each section gets consistent attention and similar timing during every routine.
Recheck flow and area inputs, then consider reducing depth or increasing efficiency with calmer technique. Improving infiltration with mulch can also reduce required watering time.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.