Fully Automatic Soil Freezing Process TesterModel: BTU-FHA-1 Description- Equipment name: Fully Automatic Soil Freezing Process Tester
- Model: BTU-FHA-1
- Overview: Used to study temperature field changes, frost heave amount,
frost heave force, and water migration during soil freezing. It can
simulate frost heave under different temperature gradients and
hydraulic heads. Suitable for frozen soil engineering, subgrade
frost heave prevention research, etc.
- Core functions:
- Independent temperature control at top and bottom ends with
programmable waveforms (sine, square, triangle, linear, etc.).
- Measures axial frost heave force and displacement (stress control
or strain control).
- Water supply system simulates groundwater recharge and measures
water migration volume during freezing.
- Built‑in 18 temperature/humidity sensors and acquisition channels
for precise temperature field distribution inside the specimen.
Test Standards (International)Based on the equipment’s capabilities (soil freezing, frost heave,
water migration, temperature gradient), the following international
standards are applicable: | Standard No. | Standard Name (English) | Corresponding Test | | ASTM D5918 | Standard Test Method for Frost Heave and Thaw Weakening Sensitivity
of Soils | Frost heave susceptibility, heave amount | | ASTM D6035 | Standard Test Method for Determining the Effect of Freeze‑Thaw on
Hydraulic Conductivity | Freeze‑thaw effect on permeability | | ASTM D7099 | Standard Terminology Relating to Frozen Soil and Rock | Reference terminology | | ASTM D7300 | Standard Test Method for Laboratory Determination of Strength
Properties of Frozen Soil | Frozen soil strength | | ISO 23912 | Geotechnical investigation and testing — Frost heave test | Frost heave test | | EN 13286‑46 | Unbound and hydraulically bound mixtures — Part 46: Determination
of frost heave | Frost heave determination (European) | | GB/T 50123‑2019 | Standard for Geotechnical Testing Method — Frozen soil section | Frost heave ratio, temperature field measurement |
Note: Frost heave tests typically follow ASTM D5918(open‑system water‑supplied frost heave) or ASTM D6035 (freeze‑thaw cycling). Specification (Technical Parameters)| Parameter | Specification | | Specimen size | Φ100 mm × H200 mm; temperature sensors every 10 mm along height | | Max. axial force | 10 kN, accuracy ±0.1% FS | | Axial displacement measurement | 0–100 mm, resolution 0.001 mm, accuracy ±0.1% FS | | Strain control | Max. displacement 100 mm; shear speed 0.0001 – 9.99999 mm/min,
stepless speed regulation | | Stress control | Axial stress 0–1 MPa, arbitrarily controllable | | Water supply system | Pressure 0–1 MPa, accuracy ±1 kPa, resolution 1 kPa; volume 0–200
ml, resolution 0.001 ml, accuracy ±0.03 ml | | Lower temperature control | -20°C to +90°C, accuracy ±0.1°C; programmable waveforms (sine,
square, triangle, linear mixing); supports both computer software
control and display panel programming | | Upper temperature control | -5°C to +90°C, accuracy ±0.1°C; same programmable waveforms; two
control modes | | Acquisition module | 18 temperature/humidity sensors and acquisition channels | | Computer control & acquisition system | Collects temperature status; allows setting of different test
stages and end conditions; can perform frost heave amount and frost
heave force tests under different temperature differences; measures
soil temperature field evolution and water migration under
different hydraulic heads during freezing |
Detail- Independent top/bottom temperature control: Top and bottom can be set to different temperatures to simulate
real air temperature vs. ground temperature gradients (e.g., colder
bottom as cold source).
- Programmable temperature waveforms: Supports sine, square, triangle, linear, and mixed waveforms –
simulates natural processes like diurnal temperature variations or
cold waves.
- High‑precision water supply system: Measures water migration volume during freezing with 0.03 ml
accuracy – can distinguish water uptake by the freezing front.
- Multi‑point temperature measurement along height: Sensors every 10 mm (approx. 20 points) – precisely maps
temperature field evolution inside specimen.
- Dual control modes: Both strain‑controlled (constant displacement rate) and
stress‑controlled (constant load) – flexible for different boundary
conditions.
- Fully automatic stage‑based testing: Software can define test stages (e.g., pre‑cool →
constant‑temperature freezing → thaw → re‑freeze) and end
conditions (e.g., heave threshold or time limit).
Application- Highway & railway subgrade: Frost heave prevention, evaluation of subgrade soil frost
susceptibility.
- Pipeline engineering: Anti‑frost‑heave design for buried pipelines in permafrost
regions.
- Canal & hydraulic engineering: Frost heave damage mechanisms of lined canals.
- Building foundations in cold regions: Stability of shallow foundations and piles under freeze‑thaw
cycles.
- Artificial ground freezing construction: Simulating temperature field and water migration during freezing
method.
- Climate change research: Effects of repeated freeze‑thaw on soil mechanical properties.
- Urban underground space: Frost heave impact on subway tunnels and utility tunnels.
Advantages- Independent programmable top/bottom temperature control: Realistically simulates differential air/ground temperatures; can
generate arbitrary temperature waveforms.
- High‑resolution displacement and water supply measurement: Displacement 0.001 mm, water volume 0.001 ml – captures
micro‑scale frost heave initiation and water migration processes.
- Multi‑sensor temperature field reconstruction: 18 sensors distributed along height – obtains internal
temperature distribution, not just a single point.
- Dual control modes (stress/strain): Allows either constant‑rate compression or constant frost heave
force – closer to field conditions.
- Fully automated test sequence: Multi‑stage (cooling, constant temperature, warming, re‑freezing)
and auto‑stop conditions can be pre‑set – unattended operation.
- Wide temperature range: From -20°C to +90°C – suitable for frost heave, high‑temperature
drying/shrinkage, and heat transfer tests.
What To Choose (Selection Guide)- Mainly studying frost heave amount & water migration→ Standard configuration with water supply system and multi‑point
temperature sensors is sufficient.
- Need to simulate complex temperature fluctuations (e.g., diurnal,
cold waves)→ Must include programmable waveform function (already included in
this model).
- Need to measure frost heave force (stress control)→ This model supports stress control (0–1 MPa), can measure frost
heave force.
- Can specimen size be changed?– This model is fixed at Φ100×H200 mm; custom sizes require
contacting the manufacturer.
- Need to also measure soil moisture distribution?– This model provides 18 humidity sensors to measure water content
profile.
- Need automatic freeze‑thaw cycles?– Software can set multiple cycles automatically.
Process FlowExample:Constant‑temperature frost heave test(bottom -10°C, top +2°C, unidirectional freezing) - Specimen preparation: Remoulded or undisturbed soil, compact to target density and
water content – Φ100×H200 mm.
- Install sensors: Insert temperature/humidity sensors every 10 mm along height;
connect to data acquisition.
- Mount specimen in apparatus: Place into pressure cell or insulating sleeve; connect top and
bottom temperature plates; connect water supply system.
- Set test parameters:
- Bottom temperature: -10°C, Top temperature: +2°C (or sine wave).
- Water supply pressure: e.g., 10 kPa (simulates groundwater level).
- Axial loading mode: stress control (e.g., 0.1 MPa to simulate
overburden) or strain control .
- Start freezing: Software automatically cools; records temperature at each point,
frost heave displacement, water supply volume, axial force over
time.
- Check end conditions: e.g., frost heave amount reaches 5 mm, or 72 hours of freezing
completed.
- End test: Stop temperature control; after thawing, remove specimen;
photograph or weigh if needed.
- Data analysis: Plot temperature field profiles, frost heave vs. time curves,
cumulative water migration curves; calculate frost heave ratio,
frost heave force, etc.
|