RU2524544C2 - Method of forced scattering of atmospheric clouds by condensing vaporous moisture of their upper layer - Google Patents

Method of forced scattering of atmospheric clouds by condensing vaporous moisture of their upper layer Download PDF

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Publication number
RU2524544C2
RU2524544C2 RU2012145878/13A RU2012145878A RU2524544C2 RU 2524544 C2 RU2524544 C2 RU 2524544C2 RU 2012145878/13 A RU2012145878/13 A RU 2012145878/13A RU 2012145878 A RU2012145878 A RU 2012145878A RU 2524544 C2 RU2524544 C2 RU 2524544C2
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Russia
Prior art keywords
upper layer
clouds
steam
atmospheric
vaporous moisture
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RU2012145878/13A
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Russian (ru)
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RU2012145878A (en
Inventor
Леонид Григорьевич Фадеев
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Леонид Григорьевич Фадеев
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Abstract

FIELD: agriculture.
SUBSTANCE: invention relates to meteorology. The method of forced scattering of atmospheric clouds comprises condensation of vaporous moisture of the upper layer of clouds by touching vaporous moisture of the upper layer of atmospheric clouds by the heated by independent steam temperature of +100÷120°C with the cold atmosphere above the upper cloud layer. At that the independent steam is sprayed inside the upper layer by the moving device equipped with steam generator with electric water heating, producing such steam in sufficient quantity.
EFFECT: proposed method provides environmentally clean rain falling and enables to reduce the cost of the method by eliminating expensive chemical reagents.

Description

Изобретение относится к отрасли природопользования.The invention relates to the field of environmental management.

Известен принцип конденсации горячего пара из парообразного состояния в жидкое путем его соприкосновения с холодной поверхностью, например с холодной внутренней поверхностью пароприемников, применяемых в промышленности для питания теплообменников (Справочник кожевника, с. 193. Издание “Легкая промышленность”, 1985 г.).There is a known principle of condensation of hot steam from a vapor state into a liquid state by contacting it with a cold surface, for example, with the cold inner surface of steam receivers used in industry for powering heat exchangers (Handbook of a Tanner, p. 193. Light Industry, 1985).

Целью данного изобретения является использование данного принципа конденсации пара, применительно к атмосферным облакам, путем превращения влаги их верхнего слоя из парообразного состояния в жидкое, способного стимулировать выпадение дождя из всего объема облаков.The aim of this invention is the use of this principle of condensation of steam, in relation to atmospheric clouds, by converting the moisture of their upper layer from a vaporous state to liquid, capable of stimulating rain from the entire volume of clouds.

При этом функцию холодной поверхности пароприемника станет выполнять холодная атмосфера над облаками.In this case, the function of the cold surface of the steam receiver will be performed by the cold atmosphere above the clouds.

Чтобы произошла конденсация влаги верхнего слоя облаков, необходимо разогреть их верхний слой с низкой температурой до более повышенной температуры.In order for moisture condensation of the upper layer of clouds to occur, it is necessary to heat their upper layer with a low temperature to a higher temperature.

Данная цель достигается разогревом влаги верхнего слоя атмосферных облаков независимым горячим паром с температурой +100÷120°C, производимым парогенератором, путем кипячения воды индивидуальными электрокипятильниками и распыляемого через распределительную гребенку внутри определенной площади верхнего слоя атмосферных облаков движущимся устройством, укомплектованным оборудованием, производящим горячий пар в достаточном количестве.This goal is achieved by heating the moisture of the upper layer of atmospheric clouds with independent hot steam with a temperature of + 100 ÷ 120 ° C, produced by the steam generator, by boiling water with individual electric boilers and sprayed through a distribution comb inside a certain area of the upper layer of atmospheric clouds with a moving device equipped with equipment producing hot steam in sufficient quantity.

Таким образом, разогретая парообразная влага верхнего слоя атмосферных облаков, вступая в соприкосновение с холодной атмосферой над ними, начнет конденсироваться, превращаясь в водяные капли, которые, пронизывая нижние слои облаков, вызовут выпадение из них дождя, очищая небосвод.Thus, the heated vaporous moisture of the upper layer of atmospheric clouds, coming into contact with the cold atmosphere above them, begins to condense, turning into water droplets, which, penetrating the lower layers of the clouds, will cause rain to fall out of them, cleansing the sky.

В итоге произойдет разгон облаков на площади, обработанной движущимся устройством.As a result, clouds will disperse in the area treated by the moving device.

Для осуществления способа принудительного разгона атмосферных облаков путем конденсации парообразной влаги их верхнего слоя мной предлагается “Устройство для доставки оборудования, производящего горячий пар, и его распыления в верхних слоях атмосферы”, на которое подана отдельная заявка.To implement a method of forced dispersal of atmospheric clouds by condensation of vaporous moisture in their upper layer, I propose a “Device for the delivery of equipment producing hot steam and its atomization in the upper atmosphere”, for which a separate application has been submitted.

Claims (1)

Способ принудительного разгона атмосферных облаков путем конденсации парообразной влаги их верхнего слоя, характеризующийся тем, что осуществляют соприкосновение парообразной влаги верхнего слоя атмосферных облаков, разогретой независимым паром температурой +100÷120°C с холодной атмосферой над верхним слоем облаков, при этом независимый пар распыляют внутри верхнего слоя движущимся устройством, укомплектованным парогенератором с электрическим разогревом воды, производящим такой пар в достаточном количестве. The method of forced dispersal of atmospheric clouds by condensation of the vaporous moisture of their upper layer, characterized in that the vaporous moisture of the upper layer of atmospheric clouds is contacted, heated by an independent steam with a temperature of + 100 ÷ 120 ° C and a cold atmosphere above the upper layer of clouds, while the independent vapor is sprayed inside the top layer with a moving device, equipped with a steam generator with electric heating of water, producing such steam in sufficient quantities.
RU2012145878/13A 2012-10-26 2012-10-26 Method of forced scattering of atmospheric clouds by condensing vaporous moisture of their upper layer RU2524544C2 (en)

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RU2524544C2 true RU2524544C2 (en) 2014-07-27

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Citations (5)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
SU497983A1 (en) * 1974-06-04 1976-01-05 Центральное Конструкторское Бюро Гидрометеоролического Приборостроения Method of release of liquid reagents into the atmosphere
RU2017399C1 (en) * 1991-06-18 1994-08-15 Демидов Валентин Михайлович Method for formation and induction of rain
RU2234831C1 (en) * 2003-09-26 2004-08-27 Ишков Юрий Григорьевич Method of initiating rain preferably during dry summer period
RU2373693C1 (en) * 2008-04-10 2009-11-27 Сергей Владимирович Бологуров Method of local impact on atmosphere and device for its implementation
US20100001089A1 (en) * 2008-07-01 2010-01-07 Arturo Vazquez Serrano Methods and systems for promoting precipitation from moisture-bearing atmospheric formations

Patent Citations (5)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
SU497983A1 (en) * 1974-06-04 1976-01-05 Центральное Конструкторское Бюро Гидрометеоролического Приборостроения Method of release of liquid reagents into the atmosphere
RU2017399C1 (en) * 1991-06-18 1994-08-15 Демидов Валентин Михайлович Method for formation and induction of rain
RU2234831C1 (en) * 2003-09-26 2004-08-27 Ишков Юрий Григорьевич Method of initiating rain preferably during dry summer period
RU2373693C1 (en) * 2008-04-10 2009-11-27 Сергей Владимирович Бологуров Method of local impact on atmosphere and device for its implementation
US20100001089A1 (en) * 2008-07-01 2010-01-07 Arturo Vazquez Serrano Methods and systems for promoting precipitation from moisture-bearing atmospheric formations

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