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Use of MEMS accelerometers/inclinometers as a geotechnical monitoring method for ground subsidence.


Due to the fast development of Micro Electro Mechanical Systems (MEMS) and the reduction of sensor cost, size and energy consumption in the last two decades, Wireless Sensor Networks (WSN) integrated with MEMS sensors have progressively been adopted into wide areas such as target tracking (Bitsch Link et al., 2010a), health monitoring (Wang and Balasingham, 2010) and environmental monitoring (Martinez et al., 2006; Cho et al., 2008). Besides, there has been an increasing concern in wireless monitoring that are embedded with MEMS during geotechnical activity (Lynch and Loh, 2006); applications have covered structural health monitoring of underground coal mines (Li and Liu, 2009), bridges (Kim et al., 2007), railways and rail vehicles (Nejikovsky and Keller, 2000; Shafiullah et al., 2007) and pipelines (Stoianov et al., 2007) construction. Aiming to enable a high-qualified, low-cost real-time surveillance system during geotechnical processes, the Department of Engineering Geology and Hydrogeology and Department of Communication and Distributed Systems at RWTH Aachen University have collaborated to develop a MEMS embedded wireless monitoring system called "X-SLEWS", which include a three-axis accelerometer and a two-axis inclinometer in each mote and is capable of measuring and sending tilting information with a settable frequency to the base station via a wireless network (May et al., 2013). As a broadly used sensor type in geotechnical monitoring system, accelerometer measures not only dynamic acceleration forces caused by vibrating or moving, but also static forces like the constant gravity pointing to the Earth, which principally agrees with the inclinometer. As the output of an accelerometer or inclinometer represents the weight of the Earth gravitational field along the axis, the tilting angle of the axis with respect to the horizontal plane is simple to obtain via a sine function (Fig. 1).

The X-SLEWS is currently designed for surface surveillance, which lead us to find the possibility of measuring ground deformation during underground excavation as a suitable deployment case. With the increasing population density in urban space, subsurface structures like tunnels have become an effective means to comply with the metropolitan requirement. Underground excavation accompanied with ground stress redistribution can cause damage to surface or subsurface structures, thus structural health monitoring is taken necessarily during construction process to prevent damages or accidents. In the aspect of land subsidence monitoring, there are varieties of methods available to measure the settlement, which include vertical extensometers, geodetic survey using Global Positioning System (GPS) or conventional leveling methods, and Interferometric Synthetic Aperture Radar (InSAR); some of the related applications are given here (Bitelli et al., 2000; Buckley et al., 2003; Tomas et al., 2010). Thanks to the booming market of smartphones and video game consoles (Lane et al., 2010; Maenaka, 2008), nonmechanical experts have progressively gained the experience of the application of accelerometers or inclinometers. Aiming at integrating the MEMS embedded X-SLEWS into geotechnical monitoring activity, we conducted a one-day measurement on the ground at the construction site of the South Hongmei Road super high way tunnel in Shanghai, by means of collecting data from three wireless sensor nodes equipped with MEMS accelerometers and inclinometers, in order to detect ground deformation caused by underground excavation. In this paper, we provide an indirect subsidence measuring methodology, which considers the change of inclination at the surveying point rather than the absolute displacement. The rest of this paper is organized as follows: First we give a brief description of the wireless sensor network and field deployment; and then we explain the data processing methodology of how to retrieve the path of the normal vector of the sensor board over time; finally, we perform a deformation analysis based on the normal vector we deduced along with the ideas about future work regarding this method.


The X-SLEWS is a joint project under the collaboration of the Department of Engineering Geology and Hydrogeology and Department of Communication and Distributed Systems at RWTH Aachen University intending to provide a flexible platform for wireless sensor networks (May et al., 2013) (Fig. 2). The idea is generalized from the project of Sensor-based Landslide Early Warning System (SLEWS) (Fernandez-Steeger et al., 2009), which has also been applied to monitor ground subsidence in an open pit mine (Femandez-Steeger et al., 2013) besides landslide surveillance. Instead of using previous SLEWS nodes provided by ScatterWeb as a black box, we implemented the popular open-source operating system TinyOS that is targeted at sensor network applications on the X-SLEWS platform.


The hardware layout of the sensor node is divided into two components: the base board that contains the parts required for basic operation of the node, and the add-on board that is deployed with sensors and offers additional functions. Specifically, the base board includes the microcontroller, the power supply circuitry and a socket for the radio module; the add-on board is allocated with a SD card socket for optional data storage as well as a 3-axis accelerometer and two orthogonal 1-axis inclinometers for geotechnical use. Both of the sensors are high performed MEMS sensors with a sensitivity of 0.0637[degrees]/count for the accelerometer and 0.00179[degrees]/count for the inclinometer. The XBee radio module family is chosen as the radio component based on its variety of radio frequencies and promising performance for long-distance radio transmission during a previous project (Bitsch Link et al., 2010b). The sensor node is powered by three 3.6 volt batteries, and the microcontroller or peripheral components could be provided with an appropriate supply voltage via a voltage regulator. All the sensed data will be stored into the SD card on the add-on board as well as be transmitted to the network's gateway--also the base station, which consists of a node and a Raspberry Pi and periodically updates and broadcasts the clock to all connected nodes. This design ensures no loss of data, even when the network is temporally weak or disconnected, data of each sensor node can be read later from the SD card.


The data received at the base station is stored in a plain text log file and formatted as:

2013-01-15T19:11:00.027989+0800 > $1358239557|101|1|10@1358230555|ACC|1|-82|988|80 2013-01-15T19:11:00.043215+0800 > $1358239557|101|1|10@1358230555|BATT|4028 2013-01-15T19:11:00.055838+0800 > $1358239557|101|1|10@1358230555|INC|-17156|-59718

Which can be separated by the delimiters ">", "|" and "@" and read from left to right as the timestamp from the Linux-based Raspberry Pi, the timestamp of the receiving time of the data from the sensor node that belongs to the base station, the node ID of the sensor node that creates the message, the node ID of the first recipient in the path to the base station ("1" represents for the base station), 10 times of the estimated number of required transmission during delivery, the gathering time of the data according to the sensor node, and the sensed data with respect to different categories. Concretely, the acceleration data of 3 axes of accelerometer are given behind the abbreviation "ACC", following with a temperature measured by an embedded thermometer; the number behind "BATT" shows the current voltage from the external power supply; "INC" leads a spontaneous data set from the two orthogonal inclinometers. To ensure the digital accuracy after transmission, the units of the data from the accelerometer, the battery and the inclinometer are chosen as mm/[s.sup.2],mV and [micro]m/[s.sup.2] .

For the described experiment, the X-SLEWS network was deployed on the surface above underground excavation for a tunnel in Shanghai for one day. The data collected were processed step by step according to the methodology that is going to be discussed in the following.


In the case of geotechnical monitoring such as ground subsidence, we require the inclination angle and the azimuth of the detected tilting surface, the values of which can be expressed from the normal vector of the sensor board plane. To obtain the normal vector rather than three tilt angles along sensor axes, we have implemented the rotation matrices that refer to inertial navigation method into the processing of data (Jekeli, 2001). The method is presented in four sub-steps as below.


Inertial Navigation System (INS) is a navigation aid that combines a computer and sensors to successively calculate the position, orientation and velocity of a moving object without the need for external references (Jekeli, 2001), which is commonly used by vehicles like ships, aircrafts, and guided missiles. The use of rotation matrices is the key to realize coordinate transformation, which helps the vehicle to trace targets from its own navigation system and is much significant during relative movement. To start with, the Euler Orientation Cosine Matrix is briefly introduced here.

We define a coordinate system O[X.sub.0][Y.sub.0][Z.sub.0], which is transformed to a new coordinate system OX'Y'Z' by rotating a roll angle [phi], a pitch angle [THETA] and a yaw angle [psi] around x-, y- and z- axis respectively (Fig. 3). The roll, pitch and yaw rotation matrices that are used to deduce a rotated vector are listed as follows:




There are 6 possible orders for the rotation of the coordinate system and principally they are equally valid. Following different rotation orders, the expressions of gravitational vector in the new coordinate system are correspondingly distinctive. However, the roll and pitch can only be solved by the orders of Z-Y-X or Z-X-Y since a spatial vector has two degrees of freedom (Pedley, 2013). Taking the Z-Y-X order for instance, after being rotated successively around z-, y- and x-axis, the rotated vector of Earth gravitational field (0,0,-1) can be expressed as:



In this sub-step, based on the equivalent relations between sensor output value and the corresponding components of g' vector, the roll [phi] and pitch [THETA] can be resolved and rotation matrices are hereby obtained. To begin with, it is worth noting that the weight of the Earth's gravitational field g aligned along the positive semi-axis will result in a negative readout on the accelerometer. This is caused by the working principle of MEMS accelerometers and can be explained with the help of a sketch (Fig. 4). The accelerometer is sensitive to g and the linear acceleration, both of which can lead a deflection on the proof mass that is suspended by restoring springs from a fixed sensing plate. The capacitance between the fingers of the proof mass and the sensing plate can be converted into an output on behalf of the weight of g. When the linear acceleration direction points downward, because of the inertia from the spring, the mass proof will drift upward relative to the fixed comb; in contrast, when the gravitational field or such static force directs downward, the variation of the mass proof will point downward as well, which goes oppositely to the first case. Since the scale of the sensor is calibrated according to the deflection generated by linear acceleration, the output of the weight of gravity that is aligned with the positive direction will provide a negative value.

As a result, the vector of the Earth's gravitational field is exported as (0,0,1) instead of (0,0,-1).

Similarly, the components of [g'.sub.x,y,z] correspondingly equal to the magnitude of the normalized accelerometer reading [G.sub.p] ([G.sub.px], [G.sub.p,y], [G.sub.p,z]) after multiplying -1, which can be presented as:



Solving equation (6), the roll [phi] and the pitch [THETA] can be expressed as:

tan [phi] = []/ [G.sub.pz] (7)

sin [THETA] = -[G.sub.px]/[square root of ([G.sup.2.sub.px] + [] + [G.sup.2.sub.pz])] (8)

In the case of a small rotation of the sensor (less than 90[degrees]), a 2-axis inclinometer is enough to deduce the roll [phi] and the pitch [THETA]. When acquiring these values by way of inclinometers, since the two outputs cannot be normalized, the equations (7) and (8) will be replaced as:

sin [phi] = [] [square root of (1-[G.sup.2.sub.px])] (9)

sin [THETA] = -[G.sub.px] (10)

Even though we can resolve the roll value p and the pitch value [THETA] , we cannot get the solution for yaw [psi] without an additional type of sensor like a magnetometer or a gyroscope. Considering the relatively simple deformation mode in geotechnical projects and the slight relevance to construction safety, we take the yaw [psi] that represents the rotation around z-axis equaling as zero for now, thus all the rotation angles are fixed and the rotation matrices have been obtained.


After retrieving the expression of rotation matrices, we operate the matrices inversely and intend to convert the normal vector from the transformed coordinate system into a description according to the old one. Taking the upward direction that perpendicular to sensor board plane as the normal direction, following the Z-Y-X order, the equation that describes the correlation between initial normal vector [V.sub.n] and the converted normal vector (0, 0, 1) in the rotated coordinate system can be expressed as:



As the rotation matrices [R.sub.z] ([psi]), [R.sub.y] ([THETA]) and [R.sub.z] ([phi]) are unit orthogonal matrices (1), it satisfies the principle that the transpose equals to its inverse. Hence equation (12) could be also written as




The normal vector represents the tilt direction and the tilt angle of the sensor board, which moves along with the monitored objects during geotechnical events. However, before stability analysis or deformation analysis, the expressions of normal vectors from distinct sensor nodes should be firstly unified.


We deployed the wireless sensor network on the surface at the construction site above South Hongmei Road super high way tunnel in Shanghai, and retrieved data by the accelerometer and inclinometer with a collecting frequency of 0.1 Hz from 10:54:25 to 17:03:00 on January 27th in 2013. Figure 5 presents the deployment and surroundings in the field. The shield machine was supposed to pass through the deployment site 41.65 meters underground during the test, so that we were able to observe the real-time ground settlement caused by excavation. Figure 6 shows the positional relationship between MEMS sensors and the tunnel underground and Figure 7 shows a planar sketch of the distribution of the sensor nodes and illustrates the steps within the process of data analysis. Five sensor nodes were separately placed with a distance of 10 to 20 meters each side on the surface along with or perpendicular to the excavating direction (Fig. 7(a)). All of the five located sensors worked well during measurement, but only three sensors recorded full data because of hardware problems. After resolving the normal vectors [V.sub.norm] by equations (9) and (10) and formula (15) (Fig. 7(b)), we unified these vector expressions in a unified Cartesian coordinate system via rotation matrices (Fig. 7(c)) and then projected the normal vectors which are above the same or parallel tunnel cross section(Fig. 7(d)).

For the purpose of a concise evaluation of the ground deformation, we derive tilt angles and azimuths of the sensors deployed on the surface through inverse trigonometric functions (Fig. 8). As the data collecting rate of the sensor is quite high, to get rid of interferences and side effects, we use the moving average to smooth the time series and find the tendency over time. Moving Average (MA) is a type of Finite Impulse Response (FIR) filter helping us to define the trend and recognize the changes in the trend (Nelson, 1983); the initial data points are being analyzed by way of creating a series of averages of different subsets of the full data set. Figure 9 (a) and Figure 9 (b) show the plots of dip angles of normal vectors in the cross section and the azimuth values of nodes N101, N102 and N105 over time with a 361-term moving average curve, and the plots in blue indicate the vibration caused by underground excavation. The excavating process has caused ground motion as well as output outliers. Hereby we analyze the data on the basis of the moving average curve for the sake of a reduction side effect and interferences. The amplified moving averages are shown in Figure 10. Generally speaking, the curves of moving average of the dip angles from each node present approximate variations over time, which is related to the proceeding of the excavation. The variations of azimuths from the three nodes reveal a tendency that the projection on the ground above the digging center has the maximum settlement. The detailed analysis is shown below.


Concerning the dip angle values, all of the three sensor nodes show an undulation. Sugiyama et al. (1999) summarized the following five primary types of ground deformation caused by shield tunneling, which are described as:

* Step 1: Preceding settlement before the shield machine arrives.

* Step 2: Deformation of ground towards the face due to stress relief.

* Step 3: Settlement during passage of the shield.

* Step 4: Subsidence due to the tail void between shield and lining.

* Step 5: Succeeding settlement due to consolidation.

Due to these five components, the ground deformation will appear a periodically settlement along with the process of the construction (Fig. 11). Since the accelerometer and inclinometer record the tilt angle of the sensor board with respect to horizontal plane, the retrieved data will not show the gradually increasing settlement over time as in Figure 11, but a tilt-return-tilt cycle that can be briefly displayed in Figure 12. When the shield arrives beneath the sensor node, the sensor will tend to the settlement center and measure a gradually increasing inclination; as the deformation expands, the surface under the sensor will become comparably flat and thus the tilt angle will restore to a certain extent; while the shield machine moving forward, a succeeding settlement will occur and the sensor node will incline to the subsidence center again. According to the distance to the digging center and the slight differences of soil property , the level of ground subsidence at distinct location will be different, which can explain why all the three nodes show a trend of undulation but not simultaneously wave crests and thoughs.


The azimuth, which stands for the angle between x positive semi-axis and the projection of normal vector in XOY plane (counterclockwise is positive), would show a variation to the initial direction because of the vibration and subsidence caused by excavation. From Figure 10 we can see all the azimuths from three nodes have relatively monotonous changes over time. The variations can be concisely expressed from a top view in Figure 13, where the projected normal vectors [V'.sub.nom], in the XOY plane of the three nodes change their direction. For nodes N101 and N105, the [V'.sub.norm] rotate 1.3969[degrees] and 0.9612[degrees] to the digging center, this leads to the conclusion that the subsidence above the tunnel is comparatively larger than that on both sides; hence the sensors that are deployed on both sides of the tunnel will tend to the excavation center, and the azimuth in the XOY plane will rotate to the settlement center via the shortest path (Fig. 13). However, the node N102 rotates 7.3613[degrees] to the inverse direction to the digging center. There is lack of thread to explain this phenomenon, but since this node was located right above the tunnel, the relatively stronger vibration caused by excavation would have affected the performance of this sensor.


For the tunnel case in Shanghai, the inclinations are very low that hardly relevant to the constructions and will not affect the usage. Besides, concerning the quantity of the retrieving data, they are not suitable to be used in proceeding analysis. First of all, the amount of sensors was quite limited and irregular. Therefore, the data provide only a limited view at one cross section and do not allow validating the observations within the progress of the construction spatially. Secondly, the measuring was only taken for one day, which is too short to monitor the whole process of ground settlement. Furthermore, as the dip angle only differed with a maximum variation of 0.04[degrees], it was indeed a test to the performance of the sensor. Even the sensitivity of the inclinometer is 0.00179[degrees]/count in small scope of variation, we must admit that errors and drifts exist and will permanently affect the accuracy of data. Lastly, according to the record from Shanghai Meteorological Bureau, the temperature during the measuring day varied from 4 [degrees]C to 10 [degrees]C. An offset caused by temperature was existed and would affect the accuracy of the measurement. In other words, we may verify the trend of the inclination of sensors by a tendency analysis, but we should not take every single value as a precise reflection of the tilt angle in this case. To refine the measuring method, we should increase the amount of sensors and prolong the measuring period, uniformly distribute the sensors parallel with and perpendicular to the longitudinal direction of the excavation, and apply numerical simulation methods for settlement predictions and back analysis.


We deployed the ad-hoc X-SLEWS wireless monitoring system at the construction site of South Hongmei Road super high way tunnel in Shanghai and conducted a one-day ground tilting measurement. The main effort of this paper is the coordinate system converting method that we used to transform the output into the normal vector of the sensor board. First of all, we made use of the rotation matrices to deduce an expression of the three weights of the Earth's gravitational field in the rotated coordinate system. Secondly, we calculated the rotating angle of [phi] and [THETA] on the basis of the equivalent relations between the output of the sensor and the expressions of the Earth's gravitational field from the first step. Besides, we took the third rotating value [psi] as zero concerning the relatively simple deformation mode and its slight relevance to construction safety. Thereby the rotation matrices were solved. After that, we applied these rotation matrices to deduce the normal vector. Furthermore, we unified the normal vector from each sensor in a uniform coordinate system to realize a concise comparison.

In the following deformation analysis, we studied the dip angle of the normal vector of nodes N101, N102 and N105 in the cross section as well as the azimuth value over time. The undulation of the plots of the dip angle is caused by the periodically subsidence during the process of shield tunneling, and their diverse crests and thoughs refer to the different soil properties and the slight distinct distances to the center. The curves of the azimuth from nodes N101 and N105 reveal that both of the sensors tend to incline to the excavating center, which is in accordance with the settlement mechanism caused by underground digging. These results enhance the idea that ground settlement can be monitored with the help of inclinometers or accelerometers by proper deployment. In the follow-up study, the deformed pattern of a surface settlement could be optimized by the fusion of an amount of distinctive types of sensors and the integration of numerical simulation methods, and a well-planned surveillance is strongly expected.

DOI: 10.13168/AGG.2014.0015

Article info

Article history:

Received 16 April 2014

Accepted 28 August 2014

Available online 8 October 2014


The field test in Shanghai was supported by Shanghai Tunnel Engineering CO., LTD. Thanks to the staff and the management, for their great arrangement and their kind suggestions before the deployment. Many thanks to Professor Youliang Chen and Xi Du from University of Shanghai for Science and Technology (USST), without their support this deployment test would have been not possible. Thanks to Xuelian Zhou and Qiuyu Song from USST for their kind help concerning the overview of construction site. Special thanks to Laiye Bi from RWTH Aachen University, for his very valuable comments and discussion while developing and deducing the described method.


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Cheng LI (1) *, Tomas M. FERNNANDEZ-STEEGER (1), Jo Agila Bitsch LINK (2), Matthias MAY (2) and Rafig AZZAM (2)

(1) Department of Engineering Geology and Hydrogeology, RWTH Aachen University, Lochnerstr 4-20, Aachen, Germany

(2) Chair of Communication and Distributed Systems, RWTH Aachen University, Ahornstr 55, Aachen, Germany

* Corresponding author's e-mail:

(1) Unit Orthogonal Matrix is a unitized square matrix, the transpose of which equals to its inverse, which can be expressed as Q = [Q.sup.-1], QQ = QQ = E, where E is the identity matrix.
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Title Annotation:Original paper
Author:Li, Cheng; Fernnandez-Steeger, Tomas M.; Link, Jo Agila Bitsch; May, Matthias; Azzam, Rafig
Publication:Acta Geodynamica et Geromaterialia
Article Type:Report
Date:Oct 1, 2014
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