Development of a muon radiographic imaging electronic board system for a stable solar power operation
© The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences; TERRAPUB 2010
Received: 29 October 2008
Accepted: 28 March 2009
Published: 22 February 2010
Cosmic-ray muon radiography is a method that is used to study the internal structure of volcanoes. We have developed a muon radiographic imaging board with a power consumption low enough to be powered by a small solar power system. The imaging board generates an angular distribution of the muons. Used for realtime reading, the method may facilitate the prediction of eruptions. For real-time observations, the Ethernet is employed, and the board works as a web server for a remote operation. The angular distribution can be obtained from a remote PC via a network using a standard web browser. We have collected and analyzed data obtained from a 3-day field study of cosmic-ray muons at a Satsuma-Iwojima volcano. The data provided a clear image of the mountain ridge as a cosmic-ray muon shadow. The measured performance of the system is sufficient for a stand-alone cosmic-ray muon radiography experiment.
Recent technological advances in cosmic-ray muon radiography (Nagamine et al., 1996) has enabled scientists to better determine the internal structure of a volcano. Cosmic-ray muons, which are characterized by small horizontal angles at sea level, are high-energy particles that can penetrate through a volcano. The amount of energy lost by muons while passing through matter is dependent on the density of that matter. The resultant angular distribution of the muons can then be used to calculate the density profile of a volcano and, consequently, its internal structure. Therefore, a cosmic-ray muon radiography detection system is needed to determine the paths of these muons and to count the events. Various volcanoes have recently been observed by a detection system using a nuclear emulsion film (Tanaka et al., 2007a, b, c). In terms of space limitations associated with these systems near volcanoes, however, a compact system would be useful. However, we are not able to use this system for real-time observations, and real-time readings may facilitate the predictions of volcanic eruptions. A system for real-time observation requires readout electronics. A number of systems already exist for this purpose (Tanaka et al., 2001, 2003, 2005), but since these systems are designed based on NIM (U.S. NIM Committee, 1990) and CAMAC (IEEE, 1982) system, power consumption is large and the systems require commercial power supplies. It is, therefore, difficult to construct such systems near volcanoes. In order to overcome this difficulty, we have developed a power-effective readout board with a power consumption that can be fed by a small solar power system.
2. Detection System
Here we briefly discuss a detection system for cosmic-ray muon radiography before going in a detailed discussion of the readout board.
The detection system detects cosmic-ray muons penetrating through a volcano, determines the paths of these muons, and generates the angular distribution of the muons as a histogram.
All signals of the photomultipliers are processed by the readout system, which consists of a readout board, Ethernet bridges, and a personal computer (PC). The readout board processes the signals from the detector, generates a histogram as a web page, and works as a web server. The detector and readout part are connected through a computer network with the Ethernet bridges. The generated histogram can be obtained from the remote PC using a web browser. This board plays a central role in this system (see following section). In addition, all devices, except for the readout board, are commercial products, and there are many commercial products at reduced price which can be used for this application. Thus, a cost-effective and high-performance system can be easily constructed.
For communication, a wired or wireless local area network (LAN) can be employed. In cases in which a small solar power system and wireless bridges are used, it is possible to construct a remote observation station near a volcano. This is a major advantage of this system. The low power consumption requirement allows the utilization of a small solar power system—a very important factor in the development of this system. For an observation system near a volcano, the system requires a power supply capability of about 600 W. When the sunlight is taken into account, an effective average power of about 60Wcan be obtained. Another important factor to be considered in the development of this system is the fact that near a volcano access could be limited, thereby constraining the size of the station. The construction costs of the station can be reduced by keeping the station small and using light-weight elements. In order to resolve these issues, we have developed a specific readout board. For this system, the goal was to have a reduced power consumption board (several watts) compared to the effective available average power. The second goal was to have a single module of reduced size and weight (several hundreds grams).
3. Readout Board
The readout board is discussed in detail in this section. As already mentioned, the board processes the incoming signals from detectors and generates a histogram. The PC can read the histogram from the readout board with a web browser.
The detector signals are received by the comparators and are digitized after they have been compared with threshold voltages. The event filter selects candidate muon events for which the muon path can be constructed and generates information data on the paths. The data consist of a detection time and detection positions of the two counters. A histogram that depicts the angular distribution of the selected events is generated by the histogram generator using the path information. The network processor handles network protocols (Stevens, 1994) to access the histogram from a remote PC using a web browser. The network protocols used for this purpose are Ethernet, Internet Protocol (IP), Transmission Control Protocol (TCP), Hyper Text Transfer Protocol (HTTP), and Hyper Text Markup Language (HTML). The Ethernet PHY converts signals to meet Ethernet specifications. The FPGA circuits are discussing in more detail in the following sections.
3.1 Event filter
The event filter selects events that can be used to construct the muon paths and generates path information.
3.2 Histogram generator
The histogram is generated in a 32-bit-width internal memory of the FPGA. The path information, 10 bit in width and generated by the coincidence unit, is used as the address for access to the internal memory. The data according to the address are counted up when an event is detected. These data are read by the network processor described in the next section, using a remote PC.
3.3 Network processor
The network processor handles the network protocols used to access the histogram from a remote PC using a web browser. The PC can execute instructions as follows: obtain and clear histogram data, and obtain and clear data of event counters for monitor of the detectors.
The feature of this block is that those network protocols are processed by only a hardware circuit specialized for a web page. There is no CPU and no other programmable sequencers in this block. This design has advantages in terms of power consumption and operating failure rate. The protocols are generally processed by a system employing an embedded CPU with an operating system (OS). The system requires an external memory device because the size of the internal memories is too small to store a program. The use of a small number of devices contributes to a reduced power consumption and failure rate while running.
4. Tests and Results
We measured the power consumption of the readout board and observed a volcano with this system. The first image was obtained as a density profile.
A measured power consumption of the readout board is 2.5 W. This result shows that a small solar power system is enough for this application.
We have developed a muon radiographic imaging board for use in a stable solar power system. The board has a low power consumption, 2.5 W, and a small size, 35×160×160 mm, and weighs only 420 g. All detector signals are processed by a single board. A histogram of the angular distribution of cosmic-ray muons is generated on the board. A remote PC can communicate with the board and obtain the histogram through LAN using a web browser. This board enables us to employ a small solar power system and a wireless LAN system and consequently, to install a detection system near a volcano where there is no commercial power and limited access to an observation station. Using this system, we have been able to collect and analyze data from a 3-day-long cosmic-ray muon observation at Satsuma-Iwojima volcano. A clear image of the mountain ridge was obtained as a cosmic-ray muon shadow. This result shows that the performance of the system is sufficient for the experiments. We are now ready use test the cosmic-ray muon radiography system on various other volcanoes.
- IEEE, Standard Modular Instrumentation and Digital Interface System (CAMAC), IEEE-583, January, 1982Google Scholar
- Nagamine, K., M. Iwasaki, K. Shimomura, and K. Ishida, Method of probing inner-structure of geophysical substance with the horizontal cosmicray muons and possible application to volcanic eruption prediction, Nucl. Instr. Meth. A, 356, 585–595, 1996.View ArticleGoogle Scholar
- SMSC, LAN8700/LAN8700i data sheet, Rev. 1.5, October, 2007 Stevens, W. R., TCP/IP Illustrated, Volume 1: The protocols, Addison- Wesley, 1994.Google Scholar
- Tanaka, H., K. Nagamine, N. Kawamura, S. Nakamura, K. Ishida, and K. Shimomura, Development of the Cosmic-Ray Muon Detection System for Probing Internal-Structure of a Volcano, Hyperfine Inter., 138, 521–526, 2001.View ArticleGoogle Scholar
- Tanaka, H., K. Nagamine, N. Kawamura, S. Nakamura, K. Ishida, and K. Shimomura, Development of a two-fold segmented detection system for near horizontally cosmic-ray muons to probe the internal structure of a volcano, Nucl. Instr. Meth. A, 507, 657–669, 2003.View ArticleGoogle Scholar
- Tanaka, H., K. Nagamine, N. Nakamura, and K. Ishida, Radiographic measurements of the internal structure of Mt. West Iwate with nearhorizontal cosmic-ray muons and future developments, Nucl. Instr. Meth. A, 555, 164–172, 2005.View ArticleGoogle Scholar
- Tanaka, H., T. Nakano, S. Takahashi, J. Yoshida, and K. Niwa, Development of an emulsion imaging system for cosmic-ray muon radiography to explore the internal structure of a volcano, Mt. Asama, Nucl. Instr. Methods A, 575, 489–497, 2007a.View ArticleGoogle Scholar
- Tanaka, H., T. Nakano, S. Takahashi, J. Yoshida, M. Takeo, J. Oikawa, T. Ohminato, Y. Aoki, E. Koyama, H. Tsuji, and K. Niwa, High resolution imaging in the inhomogeneous crust with cosmic-ray muon radiography: The density structure below the volcanic crater floor of Mt. Asama, Japan, Earth Planet. Sci. Lett., 263, 104–113, 2007b.View ArticleGoogle Scholar
- Tanaka, H., T. Nakano, S. Takahashi, J. Yoshida, H. Ohshima, T. Maekawa, H. Watanabe, and K. Niwa, Imaging the conduit shape beneath the dome with cosmic-ray muons: the structure beneath Showa-Shinzan lava dome, Japan, Geophys. Res. Lett., 34, L22311, 2007c.View ArticleGoogle Scholar
- Uchida, T., Hardware-based TCP processor for gigabit ethernet, IEEE Tran. Nucl. Sci., 55, 1631–1637, 2008.View ArticleGoogle Scholar
- Uchida, T. and M. Tanaka, Development of TCP/IP processing hardware, IEEE Nuclear Science Symposium 2006 Conference Record, 1411-1414, 2006.Google Scholar
- U.S. NIM committee, Standard NIM Instrumentation System, DOE/ER-0457T, May, 1990.Google Scholar
- XILINX Inc., Spartan-3AN FPGA Family: Data Sheet, DS557, December, 2007.Google Scholar