Deep Well Dewatering Calculator
When drawdown exceeds 5-6 m, wellpoints run out of suction - size deep wells instead.
With the default inputs: Pit length 30 m · Pit width 20 m · Drawdown 6 m etc.Deep wells (with 1 spare) 4 wells
Use your own dimensions ↓Inputs
Result
| Pit area | 600m² |
| Equivalent radius | 13.82m |
| Radius of influence | 107.3m |
| Total pit inflow | 1031m³/d |
| Yield per well | 490m³/d |
| Wells required | 3wells |
| Total capacity with spare | 1960m³/d |
How this is worked out
Deep wells take over where wellpoints lose suction, roughly below 5-6 m of drawdown. Total inflow uses the large-well method: an equivalent radius r₀ = √(area/π), the Kusakin radius of influence R = 2S√(kH), then the unconfined full-penetration formula Q = 1.366·k·(2H−S)·S / lg(R/r₀). Per-well yield is the empirical q = 65π·d·L·∛k, and the well count is inflow ÷ yield rounded up plus one spare - a dewatering ring without a spare fails the moment one well pumps out or a screen clogs. H is only the dewatered depth, not the whole formation thickness.
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Reverse: known result, work out one input
Enter a target result; the other inputs stay fixed and this one is worked out.
Formula
| Equivalent radius | r₀ = √(area/π) |
| Radius of influence | R = 2S√(kH) (Kusakin, k in m/d) |
| Total inflow | Q = 1.366·k·(2H−S)·S / lg(R/r₀) |
| Per-well yield | q = 65π·d·L·∛k (d, L in m) |
| Well count | n = ⌈Q/q⌉ + 1 (spare) |
How to work it out
- Work out the equivalent radius r₀ = √(area/π), treating the whole pit as one large well.
- Estimate the radius of influence with Kusakin's R = 2S√(kH); k is permeability (m/d), H the aquifer thickness.
- Total inflow by the large-well method: Q = 1.366·k·(2H−S)·S / lg(R/r₀), with S the drawdown.
- Per-well yield by the empirical q = 65π·d·L·∛k; well count = ⌈Q/q⌉ rounded up.
- Add one spare, place wells evenly around the pit, and size pumps at 1.2× total capacity.
Where it goes wrong
- Guessing permeability - an order of magnitude off in k is an order of magnitude off in Q, and every well and pump is wrong.
- Taking the whole formation as H - count only the dewatered depth; too large an H inflates inflow and the well count.
- Skipping the spare - a clogged screen or dead pump collapses the whole system and water rises from the pit floor.
Material and cost
Deep wells run a few thousand to ten-plus thousand each (hole, screen, pump, power) - few holes but dear per unit. Wellpoints rent as a set at a few hundred to a thousand-plus a day. For deep, long programmes deep wells often come out cheaper overall: fewer holes, less attention.
On site
- Run a pumping test first to confirm k and the radius of influence - do not force experience values.
- Discharge well beyond the pit's zone of influence; never recycle water back into the hole.
- Keep observation wells separate from pumping wells and watch the level actually reach 0.5 m below formation.
Basis
- CIRIA C750 Groundwater control — design and practice (2nd edition, 2016), Section 6 (deep well systems and yield)
- EN 1997-1:2004, Section 10 (hydraulic failure and dewatering)
- BS 8004:2015, Section 9 (control of groundwater)
- IS 3764:1992 Code of Safety for Excavation Work
FAQ
When do I use deep wells instead of wellpoints?
Why add a spare well?
Cite this page
Use this format in reports, method statements or coursework. The link is permanent.
Building Calculator. Deep Well Dewatering Calculator. 2026-10-25. https://jianzhujisuan.com/en/deep-well-dewatering