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The invention relates to the field of technology intended for active influence on the atmosphere in order to disperse fogs in a controlled area (airfields, high-speed roads, open areas for various sports and entertainment events, etc.). In addition, the proposed method and device can be used for ventilation of air over a large area, including for ventilation of quarries, as well as for causing additional precipitation, reducing the likelihood of precipitation. The device for dispersing fog contains three flat structures installed with a gap between themselves and free for the passage of an air flow. The central structure is grounded. In the space between its grounded elements, corona electrodes are electrically isolated and connected to a high-voltage direct current source. The other two structures are connected to high voltage direct current sources of different polarity and are installed electrically isolated on either side of the central structure. To disperse the fog, a directional flow of electrically charged particles generated by the corona discharge is created using the above-mentioned fog dispersing device. In the process of generating a corona discharge, an additional electric field is formed, the lines of force of which pass through the area of action of the inhomogeneous electric field that generates the corona discharge, and are oriented in the direction of the flow of electrically charged particles. An increase in the efficiency of fog dispersion is achieved by dividing the process of forming a directed flow of electrically charged particles into two independent processes: the formation of electrically charged particles using a corona discharge and the effect on the formed electrically charged particles by an additional more uniform electric field, the lines of force of which are oriented towards the planned movement of particles ... The additional field can be formed with the greatest possible degree of homogeneity. The stability of a uniform electric field against a probable electric breakdown allows the formation of an additional electric field with a value of its strength greater than that of the closest analogue. The speed of movement of the flow of electrically charged particles increases, the speed of the generated wind flow increases.