Well Design Principles
Fundamental principles for designing water wells that are productive, sustainable, and protected.
Design Objectives
A well must accomplish five goals simultaneously:
- Access the aquifer: Penetrate the water-bearing formation sufficiently to achieve the desired yield
- Maintain borehole integrity: Prevent collapse through proper casing and grouting
- Protect water quality: Seal out contaminated shallow groundwater and surface water
- Maximize yield: Optimize screen length, slot size, and gravel pack for the formation
- Enable maintenance: Design for pump installation, testing, rehabilitation, and eventual abandonment
Open Hole vs. Screened Wells
- Open hole (barefoot): No casing or screen in the aquifer zone — used in hard rock formations where the borehole is self-supporting. Lower cost but no formation control. Risk of collapse in weak zones.
- Screened well: Perforated casing or screen installed across the aquifer — required in unconsolidated formations (sand, gravel). Higher cost but controlled entry, better yield, longer life.
Diameter Selection
| Application | Typical Diameter | Rationale |
|---|---|---|
| Domestic | 100-150 mm (4-6") | Accommodates submersible pump, adequate yield |
| Agricultural | 200-300 mm (8-12") | Higher pump capacity for irrigation |
| Municipal | 300-600 mm (12-24") | Large pumps, redundancy, test equipment access |
| Monitoring | 50-100 mm (2-4") | Minimal disturbance, sampling access only |
The well casing ID should be at least 50 mm (2") larger than the pump bowl OD to allow for pump installation, cable routing, and future rehabilitation access.
Watch: Well Design Principles Explained
Fundamental principles for designing productive, sustainable water wells.
Watch on YouTube ↗Well Screens & Filters
Selecting the right screen type, slot size, and gravel pack for optimal well performance.
Screen Types
Wire-Wrapped Screens
Precisely spaced wire wrapped around a cage of longitudinal support rods. The V-shaped wire creates an inward-enlarging slot that resists clogging — particles that pass the outer opening flow freely inward.
- Slot sizes: 0.10-3.00 mm (0.004"-0.120")
- Open area: 40-60% — excellent hydraulic efficiency
- Material: Stainless steel (304 or 316), galvanized steel, PVC
- Cost: Highest — but best long-term performance
Perforated PVC
PVC casing with factory-drilled holes or slots. Economical for domestic wells where cost is the primary concern.
- Slot sizes: 0.5-3.0 mm (0.020"-0.120")
- Open area: 5-15% — lower hydraulic efficiency
- Cost: Lowest — 30-50% of wire-wrapped cost
Bridge Slot Screens
Heavy-duty screens with stamped bridge-shaped openings. Designed for gravel-pack wells where strength and durability are paramount.
Table of Contents
- Design Objectives
- Open Hole vs. Screened Wells
- Diameter Selection
- Screen Types
- Slot Sizing Rules
- Gravel Pack Design
- Screen Length & Placement
- Sanitary Seal Purpose
- Grout Materials
- Grouting Procedure
- Purpose
- Development Methods
- Development Verification
- Pump Types
- Submersible Pump Installation
- Overview
- Construction Methods
- Lining Methods
- Sanitary Protection
- Advantages & Limitations
- What Is an Artesian Well?
- Conditions for Artesian Flow
- Pressure Management
- Wellhead Pressure Ratings
- Artesian Aquifer Management
- Artesian Well Design
- Fundamentals of Groundwater Flow
- Pumping Tests
- Interpreting Results
- Advanced Aquifer Testing
- Numerical Modeling (MODFLOW)
- Depth Categories
- Artesian Wells
- Drilling Challenges at Depth
- Why Dewatering?
- Dewatering Methods
- Permeability Estimates
Slot Sizing Rules
D10 = grain size at which 10% of sample is finer (by weight)
Gravel Pack D50 = 4-6 × Aquifer D50
Example: If aquifer D50 = 0.3 mm (medium sand), then gravel pack D50 = 1.2-1.8 mm, slot size = 0.5-0.8 mm
Gravel Pack Design
A gravel pack is placed in the annular space between the well screen and the borehole wall in unconsolidated formations. It serves two purposes:
- Filtration: Prevents fine formation material from entering the well
- Hydraulic improvement: Increases the effective well diameter and improves flow into the screen
Screen Length & Placement
- Length: Screen should be placed across the full saturated thickness of the aquifer for maximum yield
- Open area: Design for entrance velocity <0.03 m/s (1 ft/s) to minimize turbulence and head loss
- Position: Screen bottom should be 1-3 m above the borehole bottom (sump) to allow sediment accumulation
- Overlap: If multiple screens are used, ensure minimum 3 m overlap with the producing zone
| Formation Type | Screen Type | Gravel Pack? | Slot Size |
|---|---|---|---|
| Hard rock (open hole) | None | No | N/A |
| Fine sand | Wire-wrapped | Yes — critical | 0.25-0.50 mm |
| Medium sand | Wire-wrapped | Recommended | 0.50-1.00 mm |
| Coarse sand | Wire-wrapped / perforated | Optional | 1.00-2.00 mm |
| Gravel | Perforated | No | 2.00-3.00 mm |
Watch: Well Screens & Filter Pack Design
How to select and install well screens for optimal yield and sand-free water.
Watch on YouTube ↗Grouting & Sealing
Protecting groundwater quality through proper well seals.
Sanitary Seal Purpose
A sanitary seal prevents surface contamination from migrating down the borehole along the casing. Without a proper seal, surface water carrying bacteria, chemicals, and sediment can flow directly into the aquifer through the annular space between the casing and borehole wall.
Grout Materials
| Material | Depth | Properties | Best For |
|---|---|---|---|
| Bentonite chips | 0-10 m | Swells 10-15× in water, impermeable | Primary seal, standard wells |
| Neat cement | 0-30+ m | High strength, heat of hydration | Deep seals, structural support |
| Cement grout | 0-30+ m | Pumpable, high strength | Deep grouting, mine shafts |
| Bentonite-cement mix | 0-15 m | Swelling + strength | Flexible seal in variable conditions |
| Clay grout | 0-5 m | Low cost, moderate sealing | Temporary seals, test wells |
Grouting Procedure
- Pre-grout inspection: Use a caliper log or CCTV to verify borehole diameter and condition
- Clean the annulus: Remove drilling mud and debris from the annular space with air or water
- Place chips (bentonite): Drop dry bentonite chips slowly while maintaining water level — chips settle and swell
- Pump grout (cement): Pump from bottom up through tremie pipe to displace water and prevent bridging
- Verify seal: After 24-48 hours, check for water movement through the seal (dielectric test or pipe-log)
Most jurisdictions require a minimum seal depth of 3-6 m below ground surface, extending at least 1.5 m into bedrock or below the deepest contaminated zone. Some states require sealing below all known contaminated aquifers — check local regulations.
Well Development
Techniques to maximize well yield by removing fine materials from the aquifer near the screen.
Purpose
Development removes drilling damage, fine sediment, and drilling fluids from the well screen and surrounding formation. A properly developed well can yield 2-5× more water than an undeveloped well. Development is one of the most critical steps in well construction — it directly determines the well's long-term performance.
Development Methods
Airlift Development
Compressed air is injected through small-diameter tubing (airline) suspended inside the well. The air creates a two-phase mixture that rises rapidly, pulling water and fine sediment from the aquifer. The most effective development method for most wells.
- Procedure: Inject air for 15-30 minutes, let well rest 30 minutes, repeat 3-5 cycles
- Success indicator: Water clears from turbid to transparent over multiple cycles
Surging
Alternating positive and negative pressure pulses to mobilize fines. A surge block (rubber disk) is rapidly moved up and down inside the casing, creating alternating flow directions through the screen.
Jetting
High-pressure water directed at screen openings from a jetting tool lowered inside the well. Effective for cleaning individual screen sections but time-consuming for long screens.
Over-Pumping
Sustained high-rate pumping (1.5-2× design yield) to draw fines into the well. Requires a temporary surface pump and sediment settling tanks. Effective but generates large volumes of turbid water that must be disposed of properly.
Development Verification
- Specific capacity test: Measure yield vs. drawdown — compare to pre-development values
- Sand content test: Water should contain <1 mg/L of suspended solids (<1 ppm)
- Turbidity: <5 NTU after development (ideally <1 NTU)
Watch: Well Development Methods
Surging, airlift, jetting, and over-pumping techniques to develop a well after drilling.
Watch on YouTube ↗Pump Selection & Installation
Choosing and installing the right pump for your well conditions.
Pump Types
| Type | Depth Range | Flow Rate | Efficiency | Best For |
|---|---|---|---|---|
| Submersible | 10-300+ m | 1-150 L/s | 60-80% | Most drilled wells — industry standard |
| Jet (deep well) | 10-80 m | 0.5-15 L/s | 30-50% | Domestic supply, simple installation |
| Centrifugal (surface) | 0-10 m suction | 5-200 L/s | 60-85% | Surface supply, booster stations |
| Hand pump | 0-50 m | 0.05-0.5 L/s | N/A | Rural/off-grid, village water supply |
| Progressive cavity | 0-100 m | 0.5-50 L/s | 50-70% | High-viscosity fluids, sandy water |
Submersible Pump Installation
The submersible pump is the most common choice for drilled water wells. It consists of a motor (hermetically sealed, oil or water-filled) coupled to a multi-stage centrifugal pump.
- Setting depth: Minimum 5-10 m below the lowest anticipated water level (drawdown + safety margin)
- Motor type: Water-filled (lower cost, easier maintenance) vs. oil-filled (better lubrication, higher temp tolerance)
- Power supply: Single-phase (1-3 HP for domestic) or three-phase (3-100+ HP for agricultural/municipal)
- Variable frequency drive (VFD): Adjusts motor speed to match demand — saves energy, reduces wear, prevents water hammer
TDH = Hstatic + Hdrawdown + Hfriction + Hdischarge
Pump Power Required:
P = (Q × TDH × ρ × g) / (η × 1000)
P = power (kW), Q = flow (m³/s), ρ = density, g = 9.81, η = pump efficiency
Watch: Choosing the Right Well Pump
Submersible vs jet pumps: selection criteria, sizing, and installation considerations.
Watch on YouTube ↗Hand-Dug & Large-Diameter Wells
Traditional well construction methods still used worldwide for community water supply.
Overview
Hand-dug wells are the oldest form of groundwater access, still serving billions of people in developing regions. While drilled wells are preferred for deep aquifers, hand-dug wells remain practical for shallow water tables (0-15 m) where large diameter provides adequate storage and low-cost construction is essential.
Construction Methods
Manual Excavation
- Hand digging: Workers excavate using picks, shovels, and buckets — typically 2-person teams
- Cribbing: Timber or concrete ring supports prevent wall collapse during excavation
- Depth limit: Usually 6-12 m due to safety constraints and water table depth
- Diameter: 1-3 m — provides significant water storage (4-7 m³ per meter depth)
Caisson / Shaft Sinking
- Open caisson: Concrete ring sections sink under their own weight as soil is excavated from inside
- Steined shaft: Brick or stone lining built progressively as excavation advances
- Depth capability: Up to 30 m with proper techniques and ground conditions
- Diameter: 1-4 m — larger than drilled wells, provides natural storage
Machine-Assisted
- Backhoe excavation: Large equipment for initial overburden removal, then hand finishing
- Auger bailing: Truck-mounted auger for 0.6-1.2 m diameter holes to 15 m
- Bucket auger: Manual or powered auger for intermediate size (0.3-0.6 m)
Lining Methods
| Material | Diameter | Depth | Cost | Lifespan |
|---|---|---|---|---|
| Concrete rings | 0.8-2.0 m | 10-20 m | Low | 30-50 years |
| Ferrocement | 0.6-1.5 m | 10-15 m | Very low | 20-30 years |
| Brick masonry | 1.0-3.0 m | 10-20 m | Low | 30-50 years |
| Stone lining | 1.0-2.5 m | 8-15 m | Very low | 20-40 years |
| Timber cribbing | 1.0-2.0 m | 5-10 m | Low | 10-20 years |
Sanitary Protection
Hand-dug wells are highly vulnerable to surface contamination. Critical protections include:
- Concrete apron: 1.5-2 m radius, sloped away from well, minimum 100 mm thick
- Well head protection: Raised collar (300-500 mm above ground) with removable cover
- Setback distances: Minimum 15 m from latrines, 30 m from septic systems
- Covered top: Secure lid with access hatch — prevents debris and animal entry
- Drainage channel: Directs spilled water away from well head
The most widely deployed hand pump in the world — installed in over 4 million wells across South Asia and Africa. Designed for 45-60 m depth, delivers 0.5-1.0 L/s with moderate effort.使用寿命 15-20 years with regular maintenance. Spare parts available globally.
Advantages & Limitations
- Advantages: Low cost (10-20% of drilled wells), local materials and labor, large storage, easy maintenance, community ownership
- Limitations: Shallow depth only, contamination risk, labor-intensive construction, lower yield, limited to soft formations
- Best for: Rural communities, shallow water tables, developing regions, emergency water supply
Watch: How to Drill a Well by Hand
Traditional hand-dug well construction methods still used in developing regions worldwide.
Watch on YouTube ↗Artesian Well Management
Understanding and managing wells that flow under natural pressure from confined aquifers.
What Is an Artesian Well?
An artesian well taps a confined aquifer where groundwater is under pressure sufficient to rise above the top of the aquifer. If pressure is enough to reach the surface without pumping, it is a flowing artesian well.
Conditions for Artesian Flow
- Confined aquifer: Aquifer bounded above and below by impermeable layers (aquitards)
- Recharge area: Outcrop at higher elevation where water enters the aquifer
- Hydraulic head: Potentiometric surface above the ground level at the well site
- Pressure gradient: Water rises due to elevation difference between recharge area and well
h = Z_recharge - Z_well
h = pressure head (m), Z = elevation above sea level
Flow Rate from Artesian Well:
Q = K × A × (h / L)
Same as Darcy's Law but driven by natural artesian pressure
Pressure Management
Free-Flowing Wells
When artesian pressure exceeds ground level, water flows continuously without pumping:
- Flow control valve: Gate valve or needle valve to regulate discharge
- Pressure gauge: Monitor residual head — declining pressure indicates aquifer stress
- Flow meter: Track total extraction for water balance management
- Waste prevention: Never allow unrestricted flow — wasteful and can cause erosion
Subsurface Safety Valves
For high-pressure artesian wells, safety valves prevent uncontrolled blowout:
- Tubing-retrievable safety valve: Installed on tubing — wireline serviceable
- Wireline-retrievable valve: Quick replacement without pulling tubing
- Surface safety valve (SSV): Emergency shutdown at wellhead
- Downhole safety valve (DHSV): Closes automatically if surface control is lost
Wellhead Pressure Ratings
| Pressure Class | Rating | Typical Application |
|---|---|---|
| Low pressure | 0-7 bar (0-100 psi) | Domestic artesian wells |
| Medium pressure | 7-35 bar (100-500 psi) | Municipal supply, moderate head |
| High pressure | 35-105 bar (500-1500 psi) | Deep artesian, geothermal |
| Ultra-high pressure | 105-210 bar (1500-3000 psi) | Deep basin, oil-field associated |
Artesian Aquifer Management
- Water level monitoring: Piezometer network tracks potentiometric surface
- Extraction limits: Sustainable yield must not reduce artesian pressure
- Recharge management: Artificial recharge to maintain pressure in stressed aquifers
- Multi-well coordination: Interference between artesian wells reduces individual yields
- Compaction risk: Over-extraction can cause irreversible aquifer compaction and land subsidence
The world's largest artesian aquifer underlies 1.7 million km² of central Australia. Drilled since 1880s, thousands of bores tap pressurized water from 200-1500 m depth. The Australian government's Great Artesian Basin Sustainability Initiative has capped over 1,000 free-flowing bores to conserve water and maintain pressure.
Artesian Well Design
- Casing: Full-length steel casing to surface — withstands artesian pressure
- Wellhead: Flanged connection rated for maximum expected pressure
- Packer: Isolates artesian zone from overlying formations
- Screen: Selective screening in artesian aquifer zone only
- Cement: Full cement job to prevent upward pressure migration through annulus
Well Hydraulics & Aquifer Testing
Understanding groundwater flow, aquifer properties, and pumping tests that quantify well performance.
Fundamentals of Groundwater Flow
Water moves through aquifers driven by hydraulic gradients. Darcy's Law describes this relationship:
Q = discharge (m³/s), K = hydraulic conductivity (m/s), A = cross-sectional area (m²), dh/dL = hydraulic gradient (dimensionless)
Pumping Tests
Constant-Rate Pumping Test
The gold standard for aquifer characterization. A production-size pump runs at constant discharge while water levels are monitored in the pumping well and observation wells at regular intervals.
- Duration: 24-72 hours minimum (some tests run weeks for large-scale aquifer characterization)
- Monitoring: Water level measurements at 1, 2, 5, 10, 20, 30, 60 min, then hourly
- Data analysis: Drawdown vs. log-time curves matched to type curves (Theis, Cooper-Jacob, Hantush)
Step-Drawdown Test
Used to determine well efficiency and optimal pumping rate. The well is pumped at 3-5 progressively higher rates, each sustained until drawdown stabilizes.
s = total drawdown (m), B = formation loss coefficient, C = well loss coefficient, Q = pumping rate
Well efficiency = (theoretical drawdown / actual drawdown) × 100%
Slug Test
A low-cost alternative for estimating hydraulic conductivity. A known volume of water is suddenly added (rising head) or removed (falling head) and the recovery is measured.
Interpreting Results
| Result | Indication | Action |
|---|---|---|
| High T (>500 m²/day) | Productive aquifer | Large-diameter well feasible |
| Low T (<50 m²/day) | Low permeability | Consider stimulation (fracturing, acidizing) |
| Steady state reached quickly | Strong recharge boundary | Good long-term yield potential |
| No steady state after 72 hr | No recharge boundary | Limited sustainability — reduce pumping rate |
| Rapid recovery | High storativity | Good buffer against drought |
Units: m³/day/m of drawdown — declining trends over time indicate well deterioration or aquifer depletion
Watch: Well Hydraulics & Aquifer Testing
Understanding Darcy's Law, pumping tests, and aquifer parameters for well design.
Watch on YouTube ↗Advanced Aquifer Testing
Step-Drawdown Test
Incremental pumping at increasing rates to establish well efficiency and optimal operating point:
- Procedure: Pump at 4+ flow rates (25%, 50%, 75%, 100% of capacity), each step 1-2 hours
- Data: Drawdown vs. flow rate — plot to determine specific capacity and well losses
- Well efficiency: E = (H_s / s_w) × 100% — ratio of theoretical to actual drawdown
- Optimal rate: Design for 70-80% of well efficiency to minimize turbulence and encrustation
s = BQ + CQ²
s = total drawdown (m), B = formation loss coefficient, C = well loss coefficient, Q = pumping rate
Slug Test
Quick, low-cost test for hydraulic conductivity — ideal for low-yield or contaminated wells:
- Procedure: Instantaneously add/remove water (slug) and monitor water level recovery
- Analysis methods: Bouwer-Rice (unconfined), Hvorslev (confined), Cooper-Bredehoeft-Papadopulos
- Duration: 5-30 minutes per test — much faster than full pumping tests
- Advantages: No pumping equipment needed, works in low-yield wells, minimal water disturbance
Interference Testing
Multi-well testing to determine aquifer connectivity and storage properties:
- Pumping well: One well pumped at constant rate
- Observation wells: 2-4 wells at different distances monitored for drawdown
- Transmissivity: Calculated from delayed drawdown at observation wells
- Storage coefficient: Determined from time-drawdown analysis at multiple distances
- Anisotropy: Different yields in different directions indicate fractured or layered aquifer
Numerical Modeling (MODFLOW)
The industry-standard groundwater flow model developed by USGS:
- Purpose: Simulate groundwater flow, predict well impacts, optimize well placement
- Data requirements: Aquifer geometry, boundary conditions, hydraulic properties, recharge rates
- Applications: Well field design, capture zone analysis, saltwater intrusion modeling, climate impact assessment
- Software: MODFLOW-2005, MODFLOW-6, with GUIs like MODFLOW-SURFACT, Visual MODFLOW, PMWIN
Capture Zone Analysis
- Definition: The area contributing water to a well over a specified time frame
- 10-year capture zone: Area that contributes water reaching the well within 10 years — critical for source water protection
- Methods: Analytical (Toth, Bear), numerical (MODPATH particle tracking)
- Protection zones: Inner zone (0-2 years): no activity. Outer zone (2-10 years): restricted activity. Broader zone (10-25 years): land use planning
Use MODFLOW when: (1) multiple wells interact, (2) complex boundary conditions exist, (3) regulatory agencies require quantitative impact assessment, (4) saltwater intrusion or contamination transport is a concern, or (5) long-term sustainability analysis is needed. For simple single-well assessments, analytical methods (Theis, Cooper-Jacob) are sufficient.
Deep Well & High-Pressure Systems
Engineering considerations for wells exceeding 300 m depth.
Depth Categories
| Category | Depth | Typical Aquifer | Challenges |
|---|---|---|---|
| Shallow | 0-50 m | Alluvial, unconsolidated | Contamination risk, low pressure |
| Intermediate | 50-300 m | Sedimentary, weathered rock | Moderate temperature, higher pressure |
| Deep | 300-1000 m | Deep sedimentary, fractured rock | High temperature, torque/drag, lost circulation |
| Very deep | >1000 m | Deep basin, geothermal | Extreme conditions, specialized equipment |
Artesian Wells
An artesian well taps a confined aquifer where the potentiometric surface lies above the ground surface. The water rises naturally under pressure without pumping. Flowing artesian wells require a capping device to prevent uncontrolled discharge.
Flowing artesian wells can discharge hundreds of liters per minute uncontrolled. An uncontrolled blowout can cause ground subsidence, aquifer contamination, and significant water waste. Always install a control valve and pressure gauge on artesian wells.
Drilling Challenges at Depth
- Torque and drag: At 500 m, a drill string may weigh 15-25 tonnes in air. Friction against the borehole wall adds 30-50% to the effective weight. Torque requirements can exceed 10,000 N·m.
- Temperature gradients: 25-30°C per km — at 1000 m depth, bottom-hole temperature may be 40-55°C. Affects drilling fluid properties and pump motor life.
- Lost circulation: Fractured zones can absorb entire mud volumes. Lost circulation materials (LCM) — nut plug, mica, cellophane — are required.
- Formation pressure: Deep confined aquifers may be overpressured — requiring heavier mud to prevent blowouts.
TDH = Hstatic + Hfriction + Hdischarge
Pump Power:
P(kW) = Q(m³/s) × TDH(m) × ρ × g / η
Dewatering & Construction Wells
Techniques for lowering groundwater to enable safe excavation.
Why Dewatering?
Construction below the water table requires groundwater removal to provide a dry, stable working environment. Dewatering is essential for foundations, tunnels, mining operations, and utility installations.
Dewatering Methods
| Method | Max Depth | Best Soil | Cost | Capacity |
|---|---|---|---|---|
| Wellpoint | 5-6 m/stage | Sand, gravel | Low-Medium | 1-10 L/s per point |
| Deep Well | Unlimited | All types | Medium-High | 10-100+ L/s per well |
| Eductor (ejector) | 30-45 m | Silt, fine sand | High | 1-5 L/s per unit |
| Ground Freezing | Unlimited | Any (incl. clay) | Very High | Impermeable barrier |
| Vacuum Assisted | 5-8 m | Fine sand, silt | Medium | 2-15 L/s per well |
Permeability Estimates
K = C × D₁₀²
K = hydraulic conductivity (cm/s), C ≈ 1-10 (shape factor), D₁₀ = effective grain size (mm)
Dewatering discharge often requires permits before release to waterways. Treatment (settling, pH adjustment, oil-water separation) may be required. Discharge to municipal sewer systems typically requires a separate permit and may incur surcharges.