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The mechanisms involved in the natural ventilation of greenhouses

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dc.contributor.author Boulard, T en
dc.contributor.author Meneses, JF en
dc.contributor.author Mermier, M en
dc.contributor.author Papadakis, G en
dc.date.accessioned 2014-06-06T06:43:13Z
dc.date.available 2014-06-06T06:43:13Z
dc.date.issued 1996 en
dc.identifier.issn 01681923 en
dc.identifier.uri http://62.217.125.90/xmlui/handle/123456789/1095
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-0030025421&partnerID=40&md5=8057a13143e68a7c95ea3907e285bf62 en
dc.title The mechanisms involved in the natural ventilation of greenhouses en
heal.type journalArticle en
heal.publicationDate 1996 en
heal.abstract Although natural ventilation is one of the major mechanisms that controls the greenhouse climate, our understanding of the underlying processes remains insufficient to allow accur ate prediction of the rates of such exchanges. This paper deals with the physical mechanisms involved in natural ventilation of a greenhouse equipped with continuous lateral windows, and uses the following experimental procedures: • air exchange rate measurements, using tracer gas or heat and water balance techniques; • direct determination of the air and heat flows through an opening, using an eddy correlation system, comprising a sonic anemometer and a fine wire thermocouple; • measurements of mean and turbulent pressure differences at ground level between inside and outside. The methods employed allow the prediction of greenhouse air exchange rates as well as the characterization of its components: a steady effect resulting from the combination of both mean wind-related and stack effects and a turbulent effect linked to wind speed fluctuations. Local estimations of total, mean and turbulent flows are provided: a wind parallel to the greenhouse axis produces an inflow at the leeward half and an outflow at the windward half. The mean flow of sensible heat is estimated between 55% and 80% of the total flux so that the turbulent flow does not exceed 45% of the total. Local estimations of total, mean and turbulent flows are compared with air exchange rate measurements using the decay rate method and a good agreement between both approaches is demonstrated. © 1996 Elsevier Science B.V. All rights reserved. en
heal.journalName Agricultural and Forest Meteorology en
dc.identifier.issue 1-2 en
dc.identifier.volume 79 en
dc.identifier.spage 61 en
dc.identifier.epage 77 en


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