← Hydrology & Irrigation Engineering

Tube Wells & Pumping Tests

Types of wells — open wells, strainer, cavity and slotted tube wells, shallow and deep tube wells, infiltration galleries and collector wells; well drilling methods (percussion, rotary, reverse rotary, DTH, jetting, augering); well screens, gravel packing, entrance velocity and well design; well development; pumping tests — constant rate, step drawdown (well loss and efficiency) and recovery tests; well failures, incrustation and corrosion; comparison of open and tube wells — with solved numericals.

📑 Contents (9 sections)

Last reviewed 16 Sept 2026 · 7 min read

Types of wells

Open (dug) wells

Large-diameter (usually 1–6 m) shallow wells, masonry lined, yielding from the bottom and sometimes through weep holes in the lining. Suitable for small yields from shallow unconfined aquifers; large storage helps meet peak demand. Classed as shallow (resting on a pervious stratum) or deep (resting on an impervious layer and drawing from a pervious stratum below through a bore).

Tube wells

A tube well is a long pipe (casing + screen) sunk into the ground to tap one or more water-bearing strata.

Type Description
Strainer type Screens (strainers) placed against water-bearing layers, blind pipe elsewhere; the most common type
Cavity type Draws water from a cavity formed below a strong clay (impervious) layer; the pipe ends at the bottom of the clay; flow is spherical rather than radial — requires a firm, thick confining layer
Slotted type Slotted pipe surrounded by a gravel pack (shrouding)
  • Shallow tube wells — depth usually up to about 60–70 m, small discharge, often with centrifugal pumps at the surface.
  • Deep tube wells — deeper (often 100 m and more), larger discharge, with vertical turbine or submersible pumps.

Other groundwater structures

  • Infiltration gallery — a horizontal perforated conduit laid in permeable material alongside or under a river bed; collects filtered water. For flow from one side: .
  • Infiltration well — shallow wells in river beds connected to a jack well.
  • Collector (radial) well — a large central caisson with horizontal radial laterals driven into the aquifer; very large yields near rivers.
  • Springs — natural outflow of groundwater at the surface (gravity, artesian, contact springs).

Well drilling methods

Method Principle Suitability
Cable tool (percussion) Heavy bit repeatedly lifted and dropped; cuttings removed by bailer Consolidated and unconsolidated formations; slow but simple
Hydraulic rotary (direct circulation) Rotating bit; drilling fluid (bentonite mud) pumped down the drill pipe carries cuttings up the annulus Fast in unconsolidated formations; mud supports the hole
Reverse circulation rotary Fluid flows down the annulus, cuttings pumped up the drill pipe Large-diameter wells in loose alluvium
Down-the-hole (DTH) hammer Pneumatic hammer with compressed air Hard rock — fastest in basalt, granite
Jetting High-velocity water jet washes material out Small wells in soft sand
Augering / boring Hand or power auger Shallow wells in soft soil
Driven wells Well point driven by hammering Very shallow sand aquifers

Well screens and gravel packs

  • Screen (strainer) — lets water in while retaining aquifer material. Types used in Indian practice include slotted pipes, wire-wound (continuous slot) screens and proprietary strainers; material: mild steel, stainless steel, brass, PVC/FRP (corrosion-resistant).
  • Slot size — chosen from the aquifer grain-size curve so that fines near the well are removed during development while most of the formation is retained.
  • Gravel pack (artificial pack) — graded gravel placed around the screen where the aquifer is fine and uniform; allows larger slots, increases effective well radius and reduces sand pumping.
  • Entrance velocity through the screen openings is kept low (commonly not more than about 3 cm/s) to reduce head loss, incrustation and sand movement.

Well design steps

  1. Aquifer data from test bores and logs (lithology, grain size, water quality).
  2. Housing casing diameter to accommodate the pump (normally a few cm larger than the pump bowl).
  3. Screen length — depends on aquifer thickness (confined aquifers: most of the thickness; unconfined: lower portion, commonly one-third to half).
  4. Screen diameter and open area — keep entrance velocity within limits.
  5. Slot size and gravel pack design.
  6. Sanitary seal (grout) near the top.

Well development

Removes fine material from around the screen to increase permeability and yield and to stabilise the formation:

  • Overpumping — pumping at a higher rate than design.
  • Backwashing / surging — alternate pumping and reversing flow.
  • Compressed air — intermittent air surging and air lifting.
  • Mechanical surging — surge block moved up and down.
  • High-velocity jetting through the screen.
  • Chemicals — polyphosphates to disperse clays and drilling mud; acid treatment in limestone aquifers.
  • Hydrofracturing — in hard rock, to open fractures.

Pumping tests

Test Procedure Gives
Constant-rate test Pump at constant ; record drawdown with time in pumped and observation wells , (Theis, Cooper–Jacob), boundaries, leakage
Step-drawdown test Pump at successively higher rates for equal periods Well loss, formation loss, well efficiency, optimum pumping rate
Recovery test Record residual drawdown after pumping stops (independent of pumping fluctuations)
FormulaWell losses (Jacob)

= formation (aquifer) loss (laminar); = well loss (turbulent flow through screen, pack and casing).

Plot against : straight line with slope and intercept .

Well efficiency

FormulaTheis recovery method

= residual drawdown; = time since pumping started; = time since pumping stopped. Slope per log cycle gives .

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