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Dehumidifiers Għall-Mużewijiet, Arkivji u Libreriji video

Dehumidifiers Għall-Mużewijiet, Arkivji u Libreriji

240L Deehumidifier għall-Mużewijiet

Deskrizzjoni

Dehumidifiers għall-Mużewijiet, Arkivji


Karatteristiċi ewlenin:

1. Applikazzjoni ta 'erja kbira: kapaċità kbira ta' tneħħija tal-umdità, adattata għal domanda ta 'deumidifikazzjoni ta' erja kbira, ċiklu kbir ta 'riħ

 

2, medda ta 'umdità ultra-wiesgħa: 20% -90% medda ta' umdità ultra-wiesgħa, tista 'tissodisfa l-ħtiġijiet ta' siti differenti ta 'dehumidifikazzjoni, tista' tirrispondi b'mod flessibbli għal ambjenti estremi

 

3, appoġġ drenaġġ kontinwu: pajp tad-drenaġġ estern, aċċess dirett għall-pajp tad-dranaġġ, drenaġġ konvenjenti

 

4, dehumidifikazzjoni intelliġenti: fiha ċipep intelliġenti, dehumidifikazzjoni intelliġenti awtomatikament skont l-umdità ambjentali attwali, ma hemmx għalfejn tara

 

5, ġudizzju intelliġenti tal-ħsara: iddetermina awtomatikament il-post tal-ħsara u r-rispons fuq l-iskrin LCD għall-manutenzjoni

 

6, ħin taż-żewġ naħat: jista 'jistabbilixxi l-ħin tal-but u l-ħin tal-għeluq skont ir-rekwiżiti tax-xogħol, faċli biex jopera


Ritratti tal-Prodott:

Dehumidifiers for Museums, Archives and Libraries

Dehumidifiers for Museums, Archives and Libraries

Parametri dettaljati:

Mudell DH-5168C
Tneħħija ta 'umdità 168L / D jew 7L / H
Sors ta 'enerġija 380V / 50HZ
Input ta 'Qawwa Rata 3.2KW
Kurrent tal-qawwa 6.2A
Temperatura tax-Xogħol 5-38 ℃
Jiċċirkola l-Arja 1600M3 / h
Refriġerant R22 / R407C
Piż nett 108Kg
Piż gross 118Kg
L-applikazzjoni tal-Ispazju 150 ± 200 m2
Dimensjoni tal-Prodott 405x605x1620mm
Ippakkjar Dimensjoni 485x655x1680mm
Tagħbija Qty 33pcs / 20ft
Perjodu ta 'produzzjoni 10 ijiem
Garanzija Sena

Applikazzjoni għal Dehumidifier fil-Mużewijiet, Arkivji u Librerija

Il-kunċett ta 'umdità (umdità assoluta u umdità relattiva) ġeneralment huwa involut fl-istudju ta' studji ambjentali tal-mużew. Sabiex tinftiehem l-umdità, jeħtieġ li tinftiehem ir-relazzjoni bejn l-umdità relattiva u l-umdità assoluta. L-arja ta 'madwarna fiha ċertu ammont ta' fwar tal-ilma, li jissejjaħ arja mxarrba; l-arja teoretikament ħielsa mill-fwar ta ’l-ilma tissejjaħ arja xotta. Umdità assoluta hija l-proporzjon tal-massa tal-fwar tal-ilma fl-arja mal-volum totali tal-arja umda. Hija miżura tal-ammont ta 'fwar tal-ilma fl-arja.

 

Taħt ċerti kundizzjonijiet ta 'temperatura, il-proporzjon tal-kontenut tal-ilma fl-arja mal-kontenut tal-ilma li fih il-fwar tal-ilma fl-arja jilħaq il-punt ta' saturazzjoni huwa dak li s-soltu nsejħu umdità relattiva. Meta l-umdità fl-arja tilħaq l-ogħla livell, tissejjaħ saturazzjoni. L-umdità relattiva f'dan il-każ hija 100%.

 

L-ammont ta 'ilma li jista' jinħażen fl-arja huwa affettwat mit-temperatura. Iktar ma tkun għolja t-temperatura, iktar ikun l-ilma. Għalhekk, l-umdità assoluta (kontenut ta 'ilma) ma tinbidilx. Iktar ma t-temperatura tkun għolja, inqas tkun l-umdità relattiva. Jekk il-piż tal-fwar tal-ilma fl-arja huwa kostanti u t-temperatura tinbidel, l-umdità relattiva tista 'tvarja ħafna.

 

Pereżempju, għal mużewijiet f’ambjent semi-miftuħ, kollezzjonijiet inklużi artifacts tal-metall jistgħu jkunu esposti għal temperatura ogħla u umdità relattiva matul l-esibizzjoni, imma għal xi raġuni l-artifatti jiġu mċaqalqa f’ambjent f’temperatura baxxa, minħabba l-bidla ta ’ f'temperatura ta ’temperatura, il-fwar ta’ l-ilma madwar l-artefatti tal-metall jikkondensa f’kundizzjonijiet kesħin, u jikkawża “kondensazzjoni”. Il-fenomenu tal- "kondensazzjoni" tal-fwar tal-ilma fuq il-wiċċ tal-artifatti tal-metall huwa kawża importanti tal-korrużjoni tal-artifatti tal-metall.

 

Barra minn hekk, l-umdità tal-ambjent li fih jitqiegħed il-ġbir hija kbira wisq, li tagħmel il-kollezzjonijiet b'reżistenza fqira tal-ilma, bħall-karta, il-kulur tal-pitturi jiskura, u huwa suxxettibbli għall-tikek tal-moffa; u jekk l-umdità tkun baxxa wisq, l-injam u l-laker se jixxaqqaq. . Għalhekk, il-kontroll tal-kontenut tal-umdità u t-temperatura tal-atmosfera fil-mużew huwa pjuttost importanti.

 

Illum, ħafna mużewijiet u galleriji tal-arti f'pajjiżhom u barra mill-pajjiż bdew jużaw regolaturi tal-umdità atmosferika, assorbituri tal-umdità, eċċ. Biex jaġġustaw l-umdità tal-kamra tal-wirja u tal-maħżen, u rċevew ċerti riżultati.

The concept of humidity (absolute humidity and relative humidity) is usually involved in the study of museum environmental studies. In order to understand the humidity, it is necessary to understand the relationship between relative humidity and absolute humidity. The air around us contains a certain amount of water vapor, which is called wet air; the air that is theoretically free of water vapor is called dry air. Absolute humidity is the ratio of the mass of water vapor in the air to the total volume of humid air. It is a measure of the amount of water vapor in the air.  Under certain conditions of temperature, the ratio of the water content in the air to the water content at which the water vapor in the air reaches the saturation point is what we usually call relative humidity. When the moisture in the air reaches the highest level, it is called saturation. The relative humidity in this case is 100%.  The amount of water that can be stored in the air is affected by the temperature. The higher the temperature, the more the water is. Therefore, the absolute humidity (water content) does not change. The higher the temperature, the lower the relative humidity. If the weight of water vapor in the air is constant and the temperature changes, the relative humidity may vary greatly.  For example, for museums in a semi-open environment, collections including metal artifacts may be exposed to a higher temperature and relative humidity during the exhibition, but for some reason the artifacts are moved to In a low temperature environment, due to the change of temperature, the water vapor around the metal artifacts will condense under cold conditions, causing
The concept of humidity (absolute humidity and relative humidity) is usually involved in the study of museum environmental studies. In order to understand the humidity, it is necessary to understand the relationship between relative humidity and absolute humidity. The air around us contains a certain amount of water vapor, which is called wet air; the air that is theoretically free of water vapor is called dry air. Absolute humidity is the ratio of the mass of water vapor in the air to the total volume of humid air. It is a measure of the amount of water vapor in the air.  Under certain conditions of temperature, the ratio of the water content in the air to the water content at which the water vapor in the air reaches the saturation point is what we usually call relative humidity. When the moisture in the air reaches the highest level, it is called saturation. The relative humidity in this case is 100%.  The amount of water that can be stored in the air is affected by the temperature. The higher the temperature, the more the water is. Therefore, the absolute humidity (water content) does not change. The higher the temperature, the lower the relative humidity. If the weight of water vapor in the air is constant and the temperature changes, the relative humidity may vary greatly.  For example, for museums in a semi-open environment, collections including metal artifacts may be exposed to a higher temperature and relative humidity during the exhibition, but for some reason the artifacts are moved to In a low temperature environment, due to the change of temperature, the water vapor around the metal artifacts will condense under cold conditions, causing














































The concept of humidity (absolute humidity and relative humidity) is usually involved in the study of museum environmental studies. In order to understand the humidity, it is necessary to understand the relationship between relative humidity and absolute humidity. The air around us contains a certain amount of water vapor, which is called wet air; the air that is theoretically free of water vapor is called dry air. Absolute humidity is the ratio of the mass of water vapor in the air to the total volume of humid air. It is a measure of the amount of water vapor in the air.  Under certain conditions of temperature, the ratio of the water content in the air to the water content at which the water vapor in the air reaches the saturation point is what we usually call relative humidity. When the moisture in the air reaches the highest level, it is called saturation. The relative humidity in this case is 100%.  The amount of water that can be stored in the air is affected by the temperature. The higher the temperature, the more the water is. Therefore, the absolute humidity (water content) does not change. The higher the temperature, the lower the relative humidity. If the weight of water vapor in the air is constant and the temperature changes, the relative humidity may vary greatly.  For example, for museums in a semi-open environment, collections including metal artifacts may be exposed to a higher temperature and relative humidity during the exhibition, but for some reason the artifacts are moved to In a low temperature environment, due to the change of temperature, the water vapor around the metal artifacts will condense under cold conditions, causing

It-tags Popolari: dehumidifiers għal mużewijiet, arkivji u librerijiĊina, manifatturi, fornituri, fabbrika, bejgħ bl-ingrossa

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