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Settlement Monitoring

Hydrostatic level gauges across three measurement principles and three range bands — 0.01 mm resolution, ranges to 2000 mm — plus layered settlement gauges for subgrade consolidation, covering everything from routine foundation pits to precision engineering.

SCST 01/02 · RLS · HYDROSTATIC + MAGNETOSTRICTIVE
SCST hydrostatic level gauge with precision-machined chamber and tubing connectors
Overview

Sub-millimeter settlement, from one pit to a whole district

Hydrostatic leveling networks measure each point's settlement relative to a stable reference cell using the connected-vessel principle. SoilCreate offers three sensing principles — differential-pressure, magnetostrictive and ultrasonic — so the right physics is matched to each project's range and accuracy needs. On most structures they are deployed together with our tiltmeter series for a complete deformation picture.

  • Three principles, three range bands

    From 0–200 mm best-value monitoring to 0–2000 mm extra-large range and ultra-high-accuracy non-contact measurement.

  • 0.01 mm-class resolution

    Resolves the slow, small settlements that decide whether a structure is safe — long before they are visible.

  • RS485 to DAQ & cloud

    Every gauge feeds the SoilCreate data loggers and Monitoring Cloud for automated, unattended operation.

0.01 mm
Resolution / Accuracy
0–2000 mm
Maximum Range
3
Measurement Principles
RS485
Bus Output
How it works

One Liquid Loop, One Stable Reference

Every gauge in the network is joined at the bottom by a liquid line and at the top by a separate air line, forming a system of communicating vessels: at rest, all liquid surfaces settle to one common level H₀. When monitoring point i settles, its sensor moves down relative to that shared surface and the liquid column above it grows — the cell reads ΔPᵢ = ρ·g·(H₀ − z_sensor,i), so settlement is sᵢ = (ΔPᵢ − ΔPᵢ,₀) / (ρ·g). The glycol working fluid (≈1050 kg/m³) carries a density temperature correction ρ(T) = ρ₀[1 − β(T − T₀)], β ≈ 4×10⁻⁴/°C.

structure 被测结构 Δh settled point 发生沉降的测点 H₀ common liquid level 公共液面 gauge 1 测点 1 gauge 2 — taller column 测点 2——液柱增高 gauge 3 测点 3 reference cell 基准罐 stable bedrock — must not move 稳定基岩——长期不动点 air line Φ8 mm PU — routed separately 通气管 Φ8mm PU——独立铺设 liquid line Φ10 mm PU — connects every cell 通液管 Φ10mm PU——串联所有储液罐 ΔP = ρ·g·Δh → s = (ΔP − ΔP₀) / (ρ·g)
Settlement of any point appears as a taller liquid column relative to the shared surface H₀ — which is why the reference cell sits on bedrock that must not move, and why liquid and air lines are routed separately. Until the reference is verified by periodic leveling surveys, every "settlement value" is relative, not absolute.

Everything is relative to the reference

Hydrostatic leveling outputs settlement relative to the reference cell. If the reference itself moves, the whole network drifts with it — so the reference goes on long-term stable bedrock and its own stability is re-verified by periodic leveling surveys. When all points drift in the same direction at once, suspect the reference first.

The magnetostrictive variant: absolute position

SCST02 reads its float magnet by time-of-flight on a magnetostrictive alloy waveguide (FeNi, TbDyFe): a microsecond current pulse meets the magnet ring's axial field, and the Wiedemann effect launches a torsional strain wave traveling at ≈2850 m/s toward a detection coil (inverse Wiedemann / Villari effect). Position is x = v·Δt — 100 ps timing resolves 0.3 µm, drift stays under 5 ppm/°C, and because position is absolute, the reading is retained through power loss.

Hydrostatic level gauges

Three Principles, One Family

Differential-pressure for best value, magnetostrictive for extra-large range, ultrasonic for the most demanding accuracy — together they cover the full spectrum of settlement projects.

Parameter Differential-Pressure (SCST01) Magnetostrictive (SCST02) Ultrasonic
PrincipleConnected-vessel differential pressureMagnetostrictive time-of-flight, absolute positionNon-contact ultrasonic
Range0–200 mm0–2000 mmapprox. 100 mm
Resolution / accuracy0.01 mm resolution0.01 mm accuracyUltra-high accuracy
OutputRS485RS485RS485
Key strengthBest value for moneyExtra-large range; reading retained on power lossNo contact with the liquid surface
Best forFoundation-pit settlementLarge-area precision settlement: metro operation, building clustersPrecision engineering settlement

Engineered So the Data Can Be Trusted

Most hydrostatic-leveling failures happen at installation, not in the sensor. Our delivery process enforces the details that keep a network honest for years.

Independent liquid & air lines

Liquid and air tubes are always routed separately — sharing one conduit causes siphoning and silently invalidates the whole network. We never compromise on this.

Reference cell on stable ground

Every settlement value is relative to the reference cell, so it is installed on long-term stable bedrock and periodically re-verified by leveling surveys.

Temperature-corrected fluid

Readings carry a fluid-density temperature correction, and antifreeze concentration is re-checked on a 1–2 year cycle for cold-climate reliability.

Layered settlement gauge · RLS

See How Each Soil Layer Consolidates

Surface settlement tells you how much; layered settlement tells you where. Magnet rings embedded at target depths track each stratum independently — essential for subgrade filling, surcharge preloading and construction above shield tunnels.

  • 1
    Magnet rings anchored to the soil

    Each ring is set at a target depth with opening claws that grip the surrounding stratum — so it moves with the soil, not with the access tube.

  • 2
    Manual probe reading

    A reed-switch probe lowered down the access tube locates each ring to ±1 mm — a simple, economical routine for short-term construction monitoring.

  • 3
    Vibrating-wire automation

    A vibrating-wire option upgrades resolution to 0.05 mm and removes site visits entirely — built for long-term, remote operation.

  • 4
    Layer-by-layer consolidation curves

    Depth-resolved settlement time series show exactly which stratum is still consolidating — the evidence engineers need to release the next construction stage.

Dimension Magnet-Ring Manual Vibrating-Wire Automated
Accuracy±1 mm±0.05 mm
Site visitsWeekly readingsNone — fully remote
Installation effortLowModerate
Best forShort-term constructionLong-term operation

Typical deployments: expressway subgrade, airport runways, surcharge-preloading programs and ground above shield-tunneling drives.

Selection guide

Settlement & Tilt: Pick the Right Product in One Glance

Settlement and tilt are usually monitored together on the same structure. This matrix covers both — tiltmeter details are on the Tiltmeter Series page.

Application Scenario Recommended Product Why
Foundation-pit settlementDifferential-Pressure Level Gauge (SCST01)Best value for money
Large-area precision settlementMagnetostrictive Level Gauge (SCST02)Extra-large 0–2000 mm range
Precision engineering settlementUltrasonic Level GaugeUltra-high accuracy, non-contact
Layered subgrade consolidationLayered Settlement Gauge (RLS)Depth-resolved, layer-by-layer settlement
Dilapidated building / tower tiltWireless Tiltmeter (LoRa)Cable-free deployment, long battery life
High-support formwork / tunnelWired Tiltmeter (RS485)Higher accuracy, continuous acquisition
Bridge tilt monitoringWireless Tiltmeter (NB-IoT)More reliable remote transmission
Installation

The Install Gates That Keep a Network Honest

None of these checks can be done at the factory — each one is confirmed on site, item by item, before the system goes live.

  • 1
    Keep every cell within range of the loop

    Mount the reservoirs so height differences stay inside the sensor's range — beyond it, the differential-pressure output saturates.

  • 2
    Route liquid and air lines separately

    Never share one PU conduit. A shared line creates a siphon: air squeezes the liquid column into interrupted flow and the whole network fails at once. This rule has no exceptions.

  • 3
    Put the reference cell on stable bedrock

    All values are relative to the reference — install it on long-term stable bedrock and re-verify its stability with periodic leveling surveys.

  • 4
    Fill to level and purge air

    Inject working fluid until every reservoir level is in place. A cell with trapped air bubbles reads erratically — re-bleed until the reading stabilizes.

  • 5
    Set the antifreeze verification cycle

    Check or replenish antifreeze concentration every 1–2 years — concentration drifts with evaporation and refills, and an under-strength fluid freezes in cold climates. Check before winter, not after the first freeze.

Magnetostrictive cells: three boundaries

The magnet ring slides over the waveguide but must never touch it — contact damages the alloy waveguide and scraps the unit. Keep clear of welders, variable-frequency drives and heavy-current cables, and flag-and-exclude data logged during welding work. A single waveguide runs to 7.5 m at most; beyond that, switch to a segmented scheme. All three are confirmed at selection stage — discovering them on site usually means changing the model.

Layered settlement (RLS): set right before grouting

Pre-embed the access tube in the borehole at its design position. Slide each magnet ring over the outside of the tube with its claws opened to grip the surrounding stratum — an unanchored ring follows the casing, not the soil, and every "settlement" it reports is false. Record each ring's as-built depth against its stratum number before sealing the hole — a depth mismatch is the most fatal error in later data interpretation. On the vibrating-wire version, equalize the external spring pre-tension across points, or initial values carry a systematic offset into the whole history.

FAQ

Field Questions, Straight Answers

Compiled from our after-sales records and the fault tables in the field manuals.

All points are drifting in the same direction — is the whole site settling?
More likely the reference cell itself is settling. Every value in the network is relative to it, so a moving reference drags all readings the same way. Re-verify the reference with a leveling survey and, if confirmed, re-select a stable reference location.
One point's reading keeps jumping around.
Air bubbles trapped in that cell. Re-bleed the cell until the reading stabilizes.
Readings respond sluggishly to known movement.
A blocked or over-bent liquid line. Clear the tube and ease the bend radius along the run. If a 4–20 mA channel reads exactly zero, check for reversed polarity or a broken wire with a multimeter.
What maintenance does the liquid loop need — especially in cold climates?
Verify or replenish antifreeze concentration on a 1–2 year cycle: concentration drifts with evaporation and refills, and an under-strength fluid freezes in winter. In cold regions, check before each winter rather than reacting to a freeze. Readings also carry the working fluid's density temperature correction.
Our magnetostrictive gauge jitters or spikes — is it broken?
Check the site log before suspecting the sensor. Sustained jitter points to strong electromagnetic interference — add shielding and re-route cabling away from welders and VFDs. A single spike usually coincides with welding or VFD transients: flag and exclude that period. No change at all suggests the magnet ring has detached; an outright invalid output means the waveguide is damaged and the unit is replaced as a whole.
A layered-settlement magnet ring suddenly shows a centimeter-level shift.
Don't alarm on a single reading. After rain, moisture in the probe can false-trigger the reed switch and mimic a sudden sink — dry the probe and re-measure. If an entire hole never moves, the casing is settling or the rings never gripped the soil: re-install. If a single ring reads in reverse, re-check the tape-cable depth markings. Re-measure first, check records second, conclude last.