A development of accurate and detailed description of soil reaction to dynamic loading requires the use of high-precision laboratory measuring equipment. Although currently available technologies create vast opportunities for extending observations and measurements, most of the laboratory devices (Li et al., 2013) for soil dynamic properties determination are designed for taking measurements only of some resultant value at one point of a tested specimen. To simplify the interpretation of test results radical assumptions are made about the distribution of a measured behavioral aspect throughout the specimen. For example, in the torsional shearing (TS) test specimen, deformation is measured at one point near the upper end of the specimen, where the torque is applied. The distribution of torsional deformation along the specimen's height is assumed to be linear. The measured resultant values (displacements) represent the state of the material throughout the whole specimen and are used in calculations of mechanical parameters (e.g., stiffness parameters). The testing procedure is automated, and the approach is convenient to use in practice. However, it provides little or no information about the material's behavior inside or at other points on the surface of the specimen. It is a known fact (Wichtmann & Triantafyllidis, 2020) that measuring of deformation at one point of a material does not specify the deformation distribution throughout the whole volume of the material. For the purpose of results’ interpretation, certain assumptions need to be adopted.
Displacements can be measured on the surface of a soil specimen using contact or contactless measurement techniques, like LVDT (Linear Variable Differential Transformer) sensors (Huawen, et al., 2019), fiberoptic sensors (Xu, 2017), optical methods (Iskander, 2010) including photogrammetry and particle image velocimetry (PIV) (White, et al., 2003), (Gill & Lehane, 2001), chemiluminescent sensors (Kuang, 2018), or optical flow (Srokosz, et al., 2021). And inside a specimen, using X-ray tomography or magnetic resonance imaging (Desrues, et al., 2006), (Tyrologou, et al., 2005), (Kong, et al., 2018) which is often too expensive, economically unjustified and available only for the best-equipped geotechnical laboratories.
The resonant column (RC) along with the TS tests are currently considered most accurate for laboratory determination of shear modulus
Unlike many laboratory devices, the RC/TS apparatus (model WF8500, used in this study) has a design that allows for introducing modifications (Anestis & Surendra, 1990), (Bae & Bay, 2009). The internal, polycarbonate cylinder has numerous sockets, grommets, and a lot of free space that allow for the installation of additional components without radical modifications. In Srokosz, et al., (2021), the authors installed 5 accelerometers to the specimen's surface in order to observe and analyze specimen vibration on several levels along the specimen's height. The accelerometers attached to the specimen's surface detected some additional dynamic effects, which were not visible in standard test results. The shape of the disturbances resembled a standing wave effect, so it might be suggested that wave reflection and interference can affect the final result. Especially if the waves would interfere near the resonant frequency value. However, many wave propagation and interaction phenomena can contribute to the observed anomalies.
To continue the investigation of local vibration disturbances in the specimen, in this study the authors proposed a new multipoint measurement system. In the proposed modification of the standard device, 48 small neodymium magnets are attached to the lateral surface of the specimen. The magnets’ placement creates a regular grid of measuring points: 48 Hall sensors fixed to the internal cylinder and their location corresponds with the arrangement of the magnets. Hall sensors react to the changes in magnetic field caused by the movement of the magnets and produce an analog signal proportional to those changes. The measurement is contactless, so the influence on the specimen deformation is minimized. The obtained results allowed to conduct a qualitative analysis of the specimen vibration on the whole side surface. Some local vibration disturbances were observed that are not compliant with the theoretic model for RC test results interpretation and that could not be detected with the standard device's equipment.
Noncohesive soil specimens were used for the experiments in this study. The choice of the tested material (silica sand) was based on Wichtmann's habilitation thesis (Wichtmann, 2016), who used this type of soil to perform tests in RC. Wichtmann performed about 650 RC tests with additional measurement of the pressure wave propagation velocity (P-wave) on noncohesive soil specimens with 65 different grain size curves. One of them has been reproduced for the purposes of this work.
The sand is classified as a poorly graded sand with a uniformity coefficient CU value of 3.0 (see
The physical parameters of soil.
silica sand | 2.65 | 0.33 | 0.41 | 0.14 | 3.0 | 0.68 | 0.41 | 1.86 |
The maximum dry density and the optimum moisture content of the sand were determined through the Standard Proctor Compaction Test. The specimens were prepared with the optimum moisture content (3.0–3.5%).
The modifications proposed in this study were introduced to the device made by Wykeham Farrance (model WF8500). It is a conventional fixed-base free top version of the apparatus (ASTM Standard, 2000). The WF8500 is an RC device with TS and free decay (FD) operation modes. The device is designed to measure soil stiffness parameters (shear modulus
The mass moment of inertia of the drive system can be calculated using geometry and special distribution of all the elements, but the procedure would be challenging and most likely affected by errors (Clayton et al., 2009). Therefore
The device works in a frequency spectrum of 10–300 Hz. The resonant frequency
In this study, a contactless displacement detection method is proposed. In the proposed modification, 48 small neodymium magnets NdFeB–N38 (10 × 5 × 2.5 mm, 1 g) are attached to the specimen's surface using adhesive tape. The placement of the magnets corresponds with the arrangement of 48 Hall sensors (Honeywell SS495A1), which are glued to the internal cylinder. The exact placement of the magnets and the sensors is presented in
The additional components added to the standard RC/TS equipment are as follows:
A polycarbonate cylinder with a regular grid of Hall sensors ( A communications interface ( A signal conditioning system (low-noise voltage stabilizers, resistor voltage dividers with high temperature stability and ultralow tolerance), 24-bit analog-to-digital converters (Microchip MCP3903), A control module (a set of microcontrollers Raspberry Pi PICO RP-2040 with dual-core processors ARM Cortex M0+ operating at a frequency of 120 MHz), A dedicated software
In the RC/TS apparatus cylindrical soil specimens are tested. All specimens have the following dimensions: A soil specimen is shaped in a latex membrane and a rigid cylindrical form. The material is compacted with a hand rammer (about 25 strokes per layer) in 5 layers. After the specimen is installed, the rigid form is disassembled and the RC/TS device chamber equipment is assembled (internal cylinder, drive system, measurement system, and external cylinder). The soil specimen is subjected to isotropic pressure of 50 kPa for 24 hours before performing an RC test. A series of preliminary RC tests is performed for torque amplitudes not exceeding 5% of the maximum torque amplitude that can be applied in RC/TS apparatus (0.01 V, 0.02 V, 0.05 V, 0.1 V, 0.2 V, and 0.5 V). The series of tests is carried out to determine the minimum and maximum value of frequency that should be applied during the tests. The resonant frequency is expected to be found in that specified range. The specimen is unloaded and the device equipment is disassembled. The magnets are attached to the membrane surface with adhesive tape. The specimen with the attached magnets is presented in The specimen is covered with the additional internal cylinder with Hall sensors installed on its internal surface. The RC/TS device chamber equipment is assembled. The soil specimen is subjected to isotropic pressure of 50 kPa for 24 hours. A series of RC tests (see point 4.) is performed to assess the influence of the magnets’ installation on the resonant frequency of the The main series of RC tests is performed for torque amplitudes in the full range (1 V–10 V in 1 V increments). Additionally, after the main series of experiments, TS tests are performed.
The RC test input parameters.
1. | 100 | 200 | 1.0 | ||
Resonant column | 2. | 50 | 80 | 180 | 2.0 |
3. | 60 | 160 | 3.0 | ||
4. | 60 | 160 | 4.0 | ||
5. | 50 | 150 | 5.0 | ||
6. | 50 | 150 | 6.0 | ||
7. | 50 | 150 | 7.0 | ||
8. | 40 | 140 | 8.0 |
After conducting the RC tests (the main experiment), TS tests were conducted with a very low frequency. As the full calibration was not performed in this study, the cyclic, slow-changing tests were necessary to assess how small deviations in the magnet–sensor distance affect the Hall sensor measurements. This information could not be obtained during the RC tests, as additional dynamic effects could be expected to occur in the material.
The TS tests were performed with the loading path parameters presented in
The TS test input parameters.
Torsional shearing | 50 | 0.02 | 5.0 | 3 |
The RC test results obtained with the original measuring system are presented in
RC test results.
1. | 145.45 | 0.0069 | 84.51 |
2. | 125.61 | 0.0116 | 62.88 |
3. | 115.48 | 0.0144 | 53.27 |
4. | 107.60 | 0.0185 | 46.18 |
5. | 101.01 | 0.0242 | 40.69 |
6. | 96.01 | 0.0312 | 36.73 |
7. | 88.81 | 0.0388 | 31.45 |
8. | 83.19 | 0.0491 | 27.60 |
The results also confirm that repeating the experiment affects the resonant frequency in a non-negligible way.
There is a distinct relationship between the specimen's mass (and the mass moment of inertia) and the resonant frequency. The magnets attached to the specimen's surface increase the resonant frequency of the
In
Along with the series of RC tests, a TS test was conducted. A nondynamic test was necessary to assess the quality of magnet–sensor interaction. Considering the facts that
there is a nonlinear relationship between the magnet–sensor distance and the sensor's response, exceeding a critical value of magnet–sensor distance (which depends on the magnet's geometry and material) results in a complete loss of signal from the sensor, only the qualitative result analysis was performed.
The displacements of the 48 points on the lateral surface of the specimen detected by the Hall sensors during the TS test are presented in
The conducted TS test constitutes a point of reference for a proper analysis of the RC tests results. It is necessary to observe the Hall sensors’ reaction to the relatively slow movement of magnets to consider the differences in horizontal sensor–magnet distances and apply this to RC results’ analysis. It should be stressed that it has provided information about the measuring system and not about the material.
The TS test was also necessary for the following:
A phase shift correction. The phase shift in signals coming from neighboring sensors is related to the opposite orientation of the neighboring magnets’ poles. Estimation of the distance between each Hall sensor and the corresponding magnet. The results of the RC tests (
About 77% of the Hall sensors detected changes in the position of magnets The results obtained with those sensors were used for further analysis of the RC tests.
During the performed RC tests, most of the sensors detected the expected specimen reaction to the applied dynamic loading of changing frequency. The signal characteristics are similar to the standard RC proximity sensors readings, that is, there is a distinct maximum amplitude value corresponding with the resonant frequency value.
Careful analysis of the obtained data series shows that:
In several measuring points during the forced vibration a local minimum in amplitude value is detected at the time when the resonance is expected to occur (see the series A4, B5, C6, E4 and F5 marked with circles in The distribution of amplitudes along some of the vertical lines is significantly disturbed (disproportionately to the observed differences in reaction to TS loading). For example, in column no. 16 ( The fixed bottom assumption is not met. The detected changes in magnetic field strongly suggest that magnets placed near the bottom end of the specimen (see locations F3, F5 or F11) experience significant displacements.
The proposed multipoint displacement detection method allowed to observe some of the complex effects and disturbances related to mechanical wave propagation through a noncohesive soil specimen. The following main conclusions can be drawn from this study.
During the forced vibration (RC test), the vibration amplitudes distribute disproportionately along the specimen's height. In some regions (measuring points) on the specimen's surface there is an observable dampening of the amplitude at the time when the resonant frequency is detected with standard RC equipment and other Hall sensors. The effects should be studied further, and additional experiments are needed to assess the influence of other factors on the obtained results.
The performed experiments confirmed that the bottom end of the specimen cannot be considered as fixed. The points near the bottom end undergo significant displacements both during the TS and RC tests. As a consequence, the averaged strain obtained with the standard RC/TS WF8500 measuring equipment (proximity sensors, accelerometers) is affected by a non-negligible error.
It should be stressed that this article presents the results of a qualitative research. The performed experiments should be treated as a preliminary research that allowed to identify the aforementioned issues. In order to take accurate measurements of the displacements, a precise calibration of the measuring system is required.
The authors aim to develop the proposed modification of the RC/TS apparatus in future research to ensure accurate measurements of displacements that can be used for further interpretation of soil dynamic properties.