- Research Article
- Open Access
Development of a Testbed for Wireless Underground Sensor Networks
© A. R. Silva and M. C. Vuran. 2010
- Received: 2 June 2009
- Accepted: 27 November 2009
- Published: 10 January 2010
Wireless Underground Sensor Networks (WUSNs) constitute one of the promising application areas of the recently developed wireless sensor networking techniques. WUSN is a specialized kind of Wireless Sensor Network (WSN) that mainly focuses on the use of sensors that communicate through soil. Recent models for the wireless underground communication channel are proposed but few field experiments were realized to verify the accuracy of the models. The realization of field WUSN experiments proved to be extremely complex and time-consuming in comparison with the traditional wireless environment. To the best of our knowledge, this is the first work that proposes guidelines for the development of an outdoor WUSN testbed with the goals of improving the accuracy and reducing of time for WUSN experiments. Although the work mainly aims WUSNs, many of the presented practices can also be applied to generic WSN testbeds.
- Sensor Node
- Wireless Sensor Network
- Volumetric Water Content
- Burial Depth
- Transitional Region
Wireless Underground Sensor Networks (WUSNs) are a natural extension of the wireless sensor network (WSN) phenomenon to the underground environment. WUSNs have been considered as a potential field that will enable a wide variety of novel applications in the fields of intelligent irrigation, border patrol, assisted navigation, sports field maintenance, intruder detection, and infrastructure monitoring . Despite their potential, very few field experiments [2–4] have been realized, which delays the proliferation of WUSN applications. Recent models for the wireless underground communication channel are also proposed but few field experiments was realized to verify the accuracy of the models [2, 3, 5]. One possible explanation for the lack of a significant number of field experiments for WUSNs is that such experiments proved to be extremely complex and present novel challenges compared to the traditional wireless environment. Moreover, constant changes in the outdoor environment, such as the soil moisture, can contribute to the problems related to the repeatability and comparisons between WUSN experiments.
the time reduction for the realization of WUSN experiments through the use of a WUSN testbed,
the improvement of the accuracy,
an easier and standardized way to compare results from experiments realized in different WUSN testbeds,
establishment of a standard methodology for WUSN measurements.
The rest of this paper is organized as follows: In Section 2, an overview of a WUSN testbed and its physical layout are presented. In Section 3, diverse aspects to be controlled in a WUSN experiment, such as the digging process, the soil composition, the soil moisture, the antenna orientation, and the transitional region are discussed. In Section 4, detailed guidelines to preserve the quality and accuracy of the experiments, even when sensor nodes are used as RF measurement tools, are presented. The overall architecture of a WUSN testbed and the aspects of its software are provided in Section 5. The preparation for the experiments and the results of an outdoor WUSN testbed are presented in Section 6. Finally, the conclusions are discussed in Section 7.
Underground-to-underground (UG2UG) Link: the communication occurs entirely using the soil medium, as illustrated in Figure 1(a).
Underground-to-aboveground (UG2AG) Link: the sender is a buried sensor node and the receiver is an aboveground device, as illustrated in Figure 1(b).
Aboveground-to-underground (AG2UG) Link: the sender is an aboveground device and the receiver is a buried sensor node, as illustrated in Figure 1(c).
Accordingly, a WUSN testbed must support experiments in these communication scenarios. The testbed architecture for UG2UG experiments is presented in Section 2.1. The extension of the testbed to support aboveground nodes is discussed in Section 2.2.
2.1. UG2UG Testbed
A WUSN testbed must allow an easy configuration of the physical deployment aspects. As shown in Figure 1, these deployment parameters reflect the location of the sensor nodes. The parameter , also called burial depth, is defined as the distance between the center of the antenna of the buried sensor node and the surface of the soil. The distance above the ground , used in the UG2AG and AG2UG scenarios, is the distance between the center of the antenna of the aboveground device and the surface of soil. Finally, the parameter is the horizontal internode distance between the sender and the receiver nodes. Therefore, from the communication perspective, the antenna is the element of interest. In fact, the actual locations of the sensor, processor, and transceiver modules are not considered in defining the physical distances of a WSUN testbed experiment, only the antenna. However, preliminary tests show that metallic objects nearby the antenna of a node can significantly impact the results of WUSN experiments. Therefore, the actual position of a node's module, such as a soil moisture sensor, may change the results, and this scenario must be avoided or informed in the report of the experiment.
A hole is designated only for the senders: the hole, which is used to place the sender node(s), that is, the sender hole, must have direct line-of-sight with all other holes. In other words, no other hole or obstacle can exist between the sender holes and the other holes. It is possible to have multiple senders in the same sender hole. However, only one sender can be active at a given moment.
At the senders hole, no receivers are allowed: if receivers are placed at the same hole as the sender, one of them can be a potential communication obstacle to the other. For instance, if the nodes Sender A, Receiver 1, and Receiver 2 are buried, in this order, in the same hole, the Receiver 1 will be an obstacle for the propagation of waves from the Sender to the Receiver 2.
direct line-of-sight between sender and receiver without any artificial obstacle,
simultaneous experiments for different internode distances and, optionally, different burial depths,
high accuracy in the results through the redundancy in the measurements.
The use of multiple nodes in the same hole, as suggested in Figure 2(d), deserves special attention. In this case, the testbed would be actually based on a 3D-grid which is a natural option to speed up the experiments. However, the placement of a sensor nearby the antenna of another underground node can interfere with the experiment results. Preliminary tests are necessary to verify if this interference will potentially occur before deciding for the use of a 3D-grid in the underground setting. In the experiments in , the use of multiple nodes at the same hole was not possible due to the interference issues. Therefore, in that case, every hole in the layout contains only one sensor and the underground part of the testbed was constrained to a 2D-grid.
It is possible to extend the testbed in Figure 3(a) to support multiple senders at different holes. However, the complexity of this new layout can be pretty high, and the implementation of a unique and general purpose testbed can be very difficult. One alternate solution is to create additional testbeds for this kind of experiments. One example of application of this new testbed is the transmission contention experiments. In Figure 3(b), the layouts of the -sender and -sender cases are shown.
2.2. Testbed Extension: Aboveground Nodes
The surface of the paper pipe must be aligned with the soil surface, as shown in Figure 4(a).
The propagation of the antenna cannot be disturbed by the paper pipes filled with soil (discussed in Section 3.1), as shown in Figure 4(b). The mentioned paper pipes can be used, but the antenna must be positioned in a way that it points to the direction of the aboveground device(s), as shown in Figure 4(a).
The hole must have a direct line-of-sight (without obstacles) to the aboveground device(s), as shown in Figure 4(c).
- (iv)The aboveground nodes devices can be easily installed using a 10?cm-length buried PVC pipe in conjunction with a wood stake. It also possible to build a grid of aboveground devices, as shown in Figure 4(c).
All the devices and schemes presented in this section speed up the realization of our experiments. Without these schemes, the same experiments would last more than times. At the same time, the accuracy of these experiments is not compromised.
In this section, the factors that impact the realization of WUSN experiments are presented. The challenges of burying and unburying sensor nodes are presented, and the use of paper and plastic pipes is described in Section 3.1. The analysis of the soil texture and soil moisture of the WUSN testbed is included as an essential part of the results of the experiments in Section 3.2. The errors caused by the antenna orientation and the use of sensor nodes to make RF measurements are discussed in Sections 3.3 and 3.4. Finally, the issues related to the transitional region of WUSNs are presented in Section 3.5.
3.1. The Digging Process
Burying and unburying sensor nodes are very time-consuming tasks in underground settings. For instance, in our experimental testbed, almost hours were necessary to dig a single 20 cm-diameter, m-depth hole, even with the use of an electric power auger. Therefore, an initial consideration about the dimensions of the holes is necessary. Besides the time issue, the larger a hole is, the larger is the modification of the soil density at that area, and this parameter affects the signal attenuation caused by the soil [4, 6]. A second aspect is related to the depth of the hole. The majority of the WUSN applications will not require burial depths higher than 1 m [1, 4, 5, 7]. Therefore, the WSUN testbed considered in this section assumes a burial depth smaller than 1 m. The process of digging deeper holes is only feasible with special machines. On the other hand, for shallow holes, there are many simple and manual digging tools available in the market considering that the diameter of the hole is restricted to up cm. In the case of our testbed, the required minimum diameter is 7.5 cm due to the dimensions of the sensor node. Therefore, 8 cm-diameter holes were dug with power augers. The difficulty to bury a sensor node also highlights an important aspect for the success of WUSN applications: the deployment of hundreds or thousands of these devices needs to be relatively simple. In this sense, sensor nodes with cylindrical form and a tiny diameter ( to 4 cm) are required.
The paper/plastic pipe helps to preserve the physical structure of the hole for multiple experiments. However, to perform the experiments, the sensor should also be covered with soil. Therefore, the reuse of a hole for multiple experiments is still a problem. A possible solution for this issue is the use of paper pipes filled with soil. In our testbed, additional 7.5 cm-diameter paper pipes are used for this purpose. These new paper pipes contain the same soil which is taken out from the digging process. These pipes, with both ends sealed, can have different lengths, helping to make experiments for different burial depths.
3.2. Soil Texture and Soil Moisture
Example of a soil analysis report.
Besides the soil texture, the water content (WC), or soil moisture, is other parameter to be included in every WUSN experiment report. However, differently from the soil texture, which is very stable for the same site, the WC is dynamic and depends on the environment and the weather. Moreover, the WC also varies as a function of the burial depth [3, 10]. These facts are important because the WC can significantly modify the results of an experiment, as suggested in [3–5, 7].
There are two basic methods to measure the amount of water in the soil: soil water content and soil water potential measurements . The soil water potential measurement, expressed in bars units, is related to the energy status of the soil water. Tensiometer and electrical resistance sensors are some examples of soil sensors that can be used to gather water potential measurements. This method provides a more realistic measurement of the actual plant water stress and, therefore, has a significant value for irrigation purposes. On the other hand, the soil water content measurement provides an effective measurement of the portion of water in the soil sample. This aspect has a direct relation with the dielectric properties of the soil  and, consequently, impacts the underground wireless communication behavior [3–5, 7].
The soil water content (WC) can be expressed in two forms: gravimetric water content (GWC) and volumetric water content (VWC). A method called oven drying method is usually used to calculate the GWC . This method consists of separating and weighing a sample of the soil. Then, this soil sample is completely dried in an oven and it is weighed again. The difference in the weights divided by first measurement represents the VWC in the soil sample, a number varying from to . Having the GWC value, the VWC can be obtained by 
where VWC and GWC are the volumetric water content and gravimetric water content of the soil sample, respectively, is the soil density in g/cm3, is the water density (1 g/cm3 at ), is the mass of the soil sample in g, and is the volume of the soil sample in cm3.
Despite its simplicity, the direct evaluation of the VWC using the gravimetric method is not practical for the WUSN testbed for three reasons. First, the gravimetric method implies that a soil sample must be regularly removed from the testbed and this continuous process is time-consuming and destructive. Second, the conversion of GWC to VWC given by (1) depends on the bulk soil density parameter. This density changes for different burial depths and its measurement requires additional attention . As a result, the good accuracy of the GWC measurement can be compromised in the VWC conversion. Finally, it is not possible to have a significant number of measurements of the VWC on a long-term experiment. For instance, if we would like to analyze the effects of the rainfall over the WUSN communication, the presence of a person continuously taking soil samples would be required. Instead, the use of soil moisture sensors that can dynamically take VWC measurements is required in the testbed. Some examples of these sensors are the time domain reflectometer (TDR) and capacitance-based devices . Recent work in WUSN shows the successful use a capacitance-based sensor, ECH2O EC-5  sensor [3, 12, 13], for water content measurements.
The WC measurements must be collected frequently to confirm that the same WC value is present during the experiments. This is specially recommended when a set of experiments is partitioned into many different sessions and distinct days. This continuous need of taking WC measurements during a set of experiments is another reason for the use of soil moisture sensors as part of the testbed infrastructure. The soil texture and the WC must be informed together in the experiments reports. The comparisons between experiments realized in different testbeds are only feasible including with these parameters in the analysis.
3.3. Antenna Orientation
Usually, the antenna orientation is not a very critical factor for over-the-air wireless communication experiments. However, considering the extreme attenuation due to the soil propagation, the antenna orientation is an additional constraint to be considered in the deployment of WUSNs, specially for multihop underground networks, where the communication range varies based on the antenna orientation. Accordingly, the experiments in a WUSN testbed can be easily compromised if the antenna orientation is not carefully adjusted.
The original antenna of a Mica2 mote is a standard one-quarter wavelength monopole antenna with 17 cm-length. It is well known that this type of antenna does not exhibit a perfect omni-directional radiation pattern. Therefore, it is expected that changes in the antenna orientation cause variations on the signal strength of the receiver node. These variations are specially significant when the underground scenario is considered. The experiments are performed at a transitional region (defined in Section 3.5), that is, nearby the boundaries of the underground communication range.
In Figure 6(b), the packet error rate (PER) is shown as a function of the node orientation. When the relative angle varies from 90° to 340°, the PER increases and the orientation of a node has a significant impact on the communication success. When the antenna orientation is between and , the communication between the nodes is not possible.
To avoid the interference of the antenna orientation over the experiments results, it is important to choose a unique antenna orientation for all experiments in a WUSN testbed. In our experiments, only the 0° orientation (Figure 6(a)) is used in order to eliminate the effects of the antenna orientation. Naturally, for every combination of sensor node type and its antenna, different antenna polarizations and orientations can be adopted as the default configuration for all experiments. Accordingly, an experiment similar to the one shown in Figure 6 must be performed to maintain the accuracy of the results and also to provide the recommendation of the best configuration for the sensor deployment.
3.4. Misalignment of RF Measurements
In an ideal wireless testbed, the best accurate tools are selected to be used as the instrumentation for the RF measurements. However, this is not usually the case for WUSN testbeds for two reasons. First, it is a common approach in WUSNs to use the sensor nodes to cooperate and provide the most reliable and efficient communication solution. Therefore, sensor nodes are expected to be also used as network instrumentation. Second, if a special and more accurate instrument, such as a spectrum analyzer, is used at the receiver side of the experiment, the grid idea cannot be applied and multiple tests must be performed one-by-one. The natural consequence is the increase of the time to conclude the experiments.
Usually, the nodes present different receiver sensitivities . This fact can cause the mentioned misalignment problem and the accuracy of the experiments can be compromised. Considering this, a balanced approach adopted in a WUSN testbed is to continue using the sensor nodes as part of the RF instrumentation, but selecting only a subset of the nodes. The selected nodes for an experiment are the ones previously qualified to perform the RSS measurements. Therefore, before using the sensor nodes for the WUSN experiments, they are tested in typical WSN scenarios, using over-the-air tests, in a process called qualification test. The reason for this test is explained by the following example.
Suppose that we want to test receiver nodes, all placed in the same hole at different burial depths. The results from this experiment can only be validated if these nodes present similar RSS measurements for an over-the-air test, using the same internode distance. If this is the case, the distinct underground measurements provided by the nodes at different burial depths are actually related to the burial depth effects and not a difference caused by their receiver sensitivities.
As an example of a qualification test, one sensor node is assigned with the role of broadcasting (over the air) a total of packets, bytes each, to a set of nodes located in the same physical position and exactly with the same antenna orientation. The transmit power used by the sender node must be small in order to allow the RSS/PER comparison at critical conditions. Usually, we use 10 dBm as the transmit power of the sender and 5 m as the internode distance between the sender and the set of nodes under qualification process. After the test, the results are collected from each node and only the subset of nodes that have similar PER and average RSSI, as previously defined, are selected to participate in the experiment. However, as expected, this kind of approach has at least two drawbacks. First, the process is very time-consuming and must be repeated every new day/session of experiments. Second, usually it is not possible to use all the available nodes for the experiment, which means that the grid is constrained by the number of qualified nodes. For instance, in our experiments, using Mica2 motes, generally only % of the available nodes were qualified for each day of experiments. Surprisingly, the qualified nodes are not always the same nodes. The use of sensor nodes as instrumentation for RF measurements requires a huge effort in order to maintain the accuracy of the results. Also, the total number of nodes to be available for a WUSN testbed is significantly higher than the actual number of nodes used in the experiments.
3.5. Transitional Region of WUSNs
It is well known that in traditional wireless communication (air channel), there is a region where the reliability of the signal varies, until the point where the communication ceases. It was reported that this issue is highly accentuated in WSNs and this critical region is called the transitional region . However, results from preliminary UG2UG experiments show that the underground transitional region is significantly smaller than its air channel counterpart . As already commented, the main problem with wireless underground communication is the very high signal attenuation caused by the soil [1, 4, 5, 7]. At the same time, usually sensor nodes present low power RF transceivers. The combination of these factors results in a very small width of the transitional region. This fact causes problems in realizing WUSN experiments and it is one of the main reasons for the small number of experiments in this area.
The identification of the transitional region in a WUSN environment, which defines the limits of the communication range, is tied to the burial depth of the nodes, the soil texture, and the WC. For instance, in some of our UG2UG experiments, the transitional region presented a width of less than % of the maximum internode distance. More specifically, with a maximum internode distance of 100 cm and a transmit power of +5 dBm, the transitional region is located between 85 cm and 95 cm . As expected, such small distance is very critical: an imperceptible slight movement in one direction, when burying the node, causes the change from a good communication region to a transitional region. Therefore, if the tests are being realized very close to the transitional region, a careless manipulation of the sensors can cause significant interferences in the results.
Considering all the presented facts, the recommendation is to limit all the experiments to a secure region which is not the transitional region. Restricting the experiments in a secure region is a way to preserve the quality and accuracy of the WUSN experiments. For instance, if WC experiments are realized in the transitional region, it will not be clear if the RSS and PER results uniquely reflect the WC effects or if the results are also affected by the instabilities of the transitional region. On the other hand, for instance, experiments realized at % of the maximum internode distance present very stable results and the repeatability and comparisons between experiments are feasible in this secure region . Naturally, the exception for this guideline is when the maximum internode distance and the transitional region are the aspects under investigation in the experiments.
Many aspects or variables that can potentially interfere with the quality of the WUSN experiments are considered in this section. Guidelines are provided to minimize the issues or completely eliminate the interference of one or multiple variables. The qualification phase is particularly very important due to the well known differences in the transceiver performances of low-cost sensor nodes. However, even with a qualified set of nodes, the interpretation of the results can still be affected by the way the RF measurements are realized. Guidelines to realize such measurements are provided in the next section.
A WUSN testbed is generally used to provide the infrastructure necessary for the realization of comparisons between experimental results and the predictions made by theoretical models. However, it has been reported that sensor nodes are being used to make RF measurements, usually the RSS . This is usually necessary and desirable because many communication protocols take advantage of the use of the sensor node as an RF measurement tool to make decisions related to multihop schemes, topology, localization, and so forth. However, it is possible to identify some issues related to the use of sensor nodes for such measurements. In Section 4.1, a methodology to avoid the issues caused by the limitations of the sensor node receiver circuitry is presented. In Section 4.2, guidelines to correctly estimate the path loss exponent are provided.
4.1. Clipping Effect
Wireless communication channel models usually use empirically determined parameters, such as path loss exponent (PLE). In a WUSN testbed scenario, the sensor nodes can be used to take RF measurements for the estimation of such parameters. However, these measurements can introduce distortions in the results. The following case involving Mica2 motes was observed in our experiments and illustrates the problem.
Incorrect interpretation of the testbed data. The communication model can predict a RSS value and the experimental data can show a smaller result. If this smaller value is exactly the maximum nominal RSSI of the receiver, probably this is not a model mismatch.
Inaccuracy in the model prediction. If the communication model is using the testbed to obtain certain empirical parameters, such as PLE, the results of the model will be negatively affected by these incorrect measurements.
Although the first mentioned consequence is not critical because it is only related to the way the experimental data from the testbed is analyzed, the second consequence must be avoided or solved. Therefore, in the case of PLE estimation, only combinations of transmit power levels and internode distances that are clearly not affected by the clipping effect can be used. This guideline is specially important when defining the reference distance for PLE measurements . In the next section, guidelines to calculate PLE is presented with a methodology to choose the appropriate reference distance to avoid the mentioned clipping effect.
4.2. Path Loss Exponent Estimation Using Sensor Nodes
The PLE is an essential input parameter in wireless communication models. In this section, a methodology is presented to estimate the PLE using sensor nodes in a WUSN testbed.
- (i)must lie in the far-field (Fraunhofer) region. The far-field region is defined as the region beyond the far-field distance which is defined by  is the largest physical linear dimension of the antenna and is the wavelength of the RF wave in meters. For instance, for the Mica2 node operating at 433 MHz, is approximately 0.17 m and, therefore, is 8.3 cm. In this case, must be greater than 8.3 cm.
After selecting a value for the reference distance , the next step is to setup the sender at its minimum transmit power and collect the RSS measurements at the receiver. An additional RSS measurement is taken considering at this time the maximum transmit power. The difference between both measurements must be approximately the nominal difference between the maximum and minimum transmit power levels used. If this goal is not achieved, a higher value for must be chosen and the above tests must be repeated. In the experiments reported in Section 6, the distance is 10 m. Any RSS measurement for internodes distances smaller than 10 m will have an error due to the nature of the RF instrumentation used (the sensor node itself). However, if a spectrum analyzer is used, the reference distance = 1 m could be adopted without any loss of accuracy. Naturally, the value for will vary for different models of sensor nodes and their antennas. Moreover, the use of multiple receivers will improve the quality of the results in the procedures described in this section.
Take RSS measurements for distances . Configure the maximum transmit power level at the sender and take many RSS measurements for internode distances higher than . For our experiments with Mica2 motes, using +10 dBm for the transmit power, two additional distances are used for the RSS measurements: = 15 m and = 20 m.
Apply a linear regression technique to estimate PLE . Using the following equation and applying Minimum Mean Square Error (MMSE) technique , it is possible to estimate PLE ( ) to be used by the wireless communication model:
Even if the PLE is not expected to be used, the approach observed in the presented methodology represents the set of best practices for RF measurements using sensor nodes in generic WSNs. In this way, any parameter to be used in a communication model which is based on RSS measurements of sensor nodes must follow a similar approach aiming the accuracy of the investigated model. The guidelines presented in this section can be applied to any WSN experiment. In fact, their relevance with this work is mostly related to the air path of the UG2AG and AG2UG experiments.
After receiving the configuration data from the manager, the sender broadcasts the messages. After the broadcasting period, the sender informs the manager node, via radio channel, that it finished this phase. At this moment, the operator of the experiment can request the results from each receiver node via radio channel. It is also possible to select multiple senders to start a transmission contention experiment.
The software in the manager node stores the configuration data for a given experiment, the manual annotations from the operator for that experiment, and the results from each receiver in a local file. If a receiver node receives a request for the results of an experiment but it did not have anything in its buffer, it returns a message to the manager informing no results, that is, packet error rate (PER) = %. After sending the results to the manager, the receiver erases its buffer. Also, if the receiver receives messages from a new experiment, it automatically erases the previous results which were not requested by the manager.
For the realization of long-term experiments, that is, experiments that are extended for a longer period of time, such as hours, some modifications in the previous architectural scheme are necessary. First, the operator configures the experiment informing its long-term feature. Then, a special message is sent from the manager to the sender node. This special message informs the sender that it must broadcast messages with a higher interval, for example, every minute. The message broadcasted by the sender to the receivers also has the information regarding the long-term experiment. Accordingly, the receivers will store the results into their Flash memories due to the fact that the RAM memory is not usually large enough to buffer all the results. Finally, the process of capturing the results must also be modified for the long-term experiments. If the radio channel is used for the transfer of long-term results, the process could take hours to finish. The solution is to have each receiver directly connected to the computer acting as the manager, when the dump of the experiment results is started. In fact, this is the only situation where a cable (usually USB or serial) is necessary in the WUSN testbed.
Each broadcasted message in a given experiment has a sequence number. When the receiver receives that message, it saves in its buffer a summary of the message: its sequence number and the RSSI level related to the reception of the message. The RSSI information is provided by the transceiver of the sensor node as previously discussed in Section 4. Therefore, the summary of the message has exactly the same size in the receiver's buffer irrespective of the size of the message. The sequential numbers are used to identify if the loss of packets occur. Therefore, this observation can help to identify if the experiment suffered interference during its realization. If this is the case, the experiment can be promptly repeated or the source of interference can be identified.
Soil texture. This evaluation is realized once, for a given testbed location. The soil texture report must be done for different depths, as shown in Table 1.
Water content (WC). This evaluation must be frequently performed as mentioned in Section 3.2. Moreover, it is very important to know the values of WC for different burial depths of the sensors to be tested.
Attenuation due to the use of paper/plastic pipes. This evaluation is realized once, when the WUSN testbed is being built. The fixed average RSS difference between the results with and without the pipes are recorded. If they cannot be neglected, all the RSS results from the experiments must be adjusted accordingly.
Default antenna orientation. This evaluation is realized once, for a given model of sensor node and its antenna. As mentioned in Section 3.3, the best antenna orientation are found and fixed for all experiments with that sensor.
Transitional region. The range of this value will change as a function of the soil composition, WC, frequency, and transmit power. It is necessary to know, a priori, the different values for this region according to the mentioned parameters. Therefore, experiments in the transitional region must be avoided when trying to analyze a specific aspect of the WUSN communication, as explained in Section 3.5.
The first step in the preparation for a WUSN experiment is the qualification test, exemplified in Section 3.4. After having the set of nodes to be used, the next step is the assignment of the roles for the sensor nodes. Considering that the manager node does not interfere on the results because it only triggers the start of the experiments and captures the results, the manager node can be elected randomly from the set of available nodes and there is no need to change its role. The node presenting smaller variance in its qualifying results must be selected as the sender. The same sender node can be used for all experiments in a single session. However, the use of the same sender node for different experiments sessions, for example, different days, is not recommended. As expected, the remaining qualified nodes can act as receivers. After the preparation phase, the WUSN experiments can be performed.
In Figure 11(a), the results of UG2UG experiments are presented . For this experiment and the next 2, the RSS values are shown as a function of the horizontal internode distance for different transmit power levels. The variance of the RSS values is also provided. The clipping effect mentioned in Section 4 is observed in Figure 11(a). For a transmit power of +10 dBm, the RSS reported is the same as the maximum RSS informed by the manufacturer of the Mica2 mote . As shown in Figure 11(a) and in Table 2, the maximum internode distance is found around and 90 cm for transmit powers of + and +10 dBm, and 50 cm for and 0 dBm. These results show that the transitional region, discussed in Section 3.5, is also a function of the transmit power of the sender.
In Figure 11(b), the results of UG2AG experiments are shown. The receiver is positioned at the soil surface ( = 0). As shown in Figure 11(b) and in Table 2, the maximum internode distance is found to be between and 3 m, depending on the transmit power level. The results from AG2UG experiments are shown in Figure 11(c). The sender is positioned at the soil surface ( = 0). As shown in Figure 11(c) and in Table 2, the maximum internode distance is found to be between and 90 cm, depending on the transmit power level. These results are in accordance with the extreme attenuation suffered by the signal as shown in Figure 11(c) and due to the fact that the sensitivity of the Mica2 mote is around 95 dBm . Since these experiments are realized in the transitional region, the realization of them are challenging. The use of redundant nodes, as shown in Figure 2, is specially recommended in this kind of scenario.
In Figure 12(a), the effects of the soil moisture on the underground communication can be observed. The RSS values are shown as a function of the transmit power level for two soil conditions: dry (GWC = 11%) and wet (GWC = 18%). The GWC measurements followed the guidelines explained in Section 3.2. The horizontal internode distance is 30 cm and the nodes are buried at a depth of 40 cm, which is the default burial depth for all experiments mentioned here. The PER is below % in all cases. As shown in Figure 12(a), for a transmit power of 3 dBm, the additional attenuation caused by the higher WC is almost 20 dB. Using a higher transmit power, it is possible to cancel the adverse effects of the WC. Applying these results to the WUSN testbed, it is clear that even small variations of WC can significantly alter the results of the experiments. Therefore, a careful and continuous control of the WC in a WUSN testbed is essential.
In the last experiment, the temporal characteristics of the wireless underground channel are investigated. Accordingly, a -hour experiment is performed with the following parameters: the horizontal internode distance is 50 cm and the transmit power is +10 dBm. For comparison, the same experiment is repeated over-the-air in an indoor environment with an internode distance of 5 m and a transmit power of +10 dBm. In Figure 12(b), the RSS values are shown as a function of time. The PER values are omitted because they are extremely low, never higher than % . Each data point shows the average of minutes of RSS information, which corresponds to packets. In Figure 12(b), the confidence intervals of the RSS are also shown along with the average values for each point as well as the results of the over-the-air experiments. As shown in Figure 12(b), the maximum variation of the signal strength is around 1 dB. Compared to the over-the-air communication, underground wireless channel exhibits a stable characteristic with time. To perform this kind of long-term experiment, a special attention to the battery level is necessary. We used special battery packs for both sender and receiver nodes to prevent errors caused by the battery level. Also, observe that the experiment is located in a secure region (Section 3.5), allowing a clear analysis of the wireless underground channel stability under normal conditions.
The development of an outdoor WUSN testbed and the realization of WUSN experiments are challenging. This work provides a set of guidelines that result in a balanced approach between high accuracy and a practical implementation of a WUSN testbed. The basic approach behind the proposed guidelines is the identification and elimination/mitigation of each variable which significantly affects the experiment results.
A WUSN testbed architecture is presented and aspects such as physical layout and software are discussed. The use of paper and plastic pipes are considered in detail, explaining the advantages of these devices in the process of burying and unburying sensor nodes. The influences of the antenna orientation and the soil moisture are highlighted. The importance of the qualification tests and procedures to identify the transitional region in a WUSN are discussed. Finally, results from experiments with the WUSN testbed are provided. The analysis of the results exemplifies the relation between the application of the guidelines proposed in this work with the accuracy of the results.
The ultimate goal of this work is to contribute to the efforts in modeling the wireless underground communication completely and developing simulation environments. To achieve this objective, an accurate outdoor WUSN testbed is essential for the evaluation of the theoretical communication models for WUSNs.
The authors would like to thank Dr. Suat Irmak for his valuable comments throughout the development of the WUSN testbed at Clay Center, NE and Emily Casper and the UNL Landscaping Services staff for their valuable help during the experiments at City Campus.
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