'Magnetic Map Building' to the already invented method

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Magnetic Map Building for Mobile Robot Localization Purpose Danilo Navarro Universidad de Oriente Departamento de Ingenierı́a Eléctrica Barcelona - Venezuela dnavarro@cantv.net

Abstract

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Robotic mapping addresses the problem of modeling environments through mobile robots sensors. The Resulting maps are commonly used for robot localization and navigation. Using a compass in mobile robotics is not frequently considered because it has a significant disadvantage: the data it provides can be easily contaminated by surrounding electromagnetic noise or by large ferrous structures. This makes the compass unreliable for heading determination in indoor environments. This paper addresses construction of an environmental magnetic map with a mobile robot, and how to use such map to determine the robots local heading. We present a novel approach that characterize indoor environments as a magnetic field function. A mobile robot gathers data from a low cost compass as it moves around. This method models the robots working area by means of a simple representation which is time persistent and does not require specialized sensors. Thus, we propose a methodology based on 2D interpolation aimed at determining the robots heading on the working area. Real test results showed the method is suitable for the partial correction of the robots position.

1. Introduction Mobile robot positioning decomposes into two stage: orientation estimation, followed by localization estimation[7]. Localization is strongly influenced by wrong heading estimate. Therefore, sensors providing absolute direction are extremely important in robot navigation. A low cost sensor that offers this possibility is the magnetic compass. Using a compass in mobile robotics is considered by some investigators[3, 4, 6, 9]. Suksakulchai et al[8] propose a method that extracts landmarks from compass data and uses it for mobile robot localization. Their method consists in exploring a corridor while collecting and storing the information about the changes observed by the compass. Afterwards, with the robot moving through the same corridor, data is collected from the compass and its correspondence to the stored data is ana-

978-1-4244-2728-4/09/$25.00 ©2009 IEEE

Gines Benet Universidad Politécnica de Valencia Informática de Sistemas y Computadoras Valencia - España gbenet@disca.upv.es

lyzed by means of a technique of sequential data adjustment using discreet least squares. Few compass-equipped robot have been reported because the compass use has a significant disadvantage: the data it provides can be easily contaminated by surrounding electromagnetic noise or by large ferrous structures. In practice, this makes the compass unreliable for heading determination in indoor environments. Despite this fact, the electronic compass continues being of interest as a support instrument for highlevel processes in indoor mobile robotics, due to its low cost and very good relative precision. So, this paper addresses the task of constructing an environment magnetic map with a mobile robot, and how to use such map to determine the robots local heading. We present a novel approach, which characterize indoor environments as a magnetic field function. A mobile robot gathers data from a low cost compass as it moves around. The robot starts exploring the surroundings and at the same time gathers data of the magnetic field components, Hx , Hy , registered by the compass at defined locations on the working area. This way, the collected data forms a grid that represents the magnetic field present in the explored environment. Applying the proposed method, the robots working area is modeled by means of a simple representation that is time persistent and does not require of specialized sensors, or specialized processes for modeling or calibration. Finally, we propose a method based on 2D interpolation aimed at determining the robots heading on the working area.

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2. Environment magnetic field modeling The Earth’s magnetic field intensity is between 0.5 and 0.6 gauss, and can be modeled like a magnetic dipole whose field lines are originated in a point near the Earth geographical south and finish in a point near the Earth geographical north. The magnetic field direction and intensity are represented by a vector of three components Hx , Hy , Hz . The Earths magnetic field intensity is between 0.5 and 0.6 gauss, and can be modeled as a magnetic dipole whose field lines originate in a point near the Earths geographical south and end in a point near the Earths geographical north. The magnetic field direction

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