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Díhéadraitheoirí Do Mhúsaeim, do Chartlanna agus do Leabharlanna video

Díhéadraitheoirí Do Mhúsaeim, do Chartlanna agus do Leabharlanna

Díleáiteoir 240L do Mhúsaeim

Cur síos

Díhéadaitheoirí do Mhúsaeim, Cartlann


Príomhghnéithe:

1. Cur i bhfeidhm limistéar mór: cumas mór dehumidification, oiriúnach le haghaidh éileamh dehumidification limistéar mór, timthriall gaoithe mór

 

2, raon taise ultra-leathan: is féidir le raon taise 20% -90% ultra-leathan, riachtanais na suíomhanna díhiodráitithe éagsúla a chomhlíonadh, is féidir leo freagairt go solúbtha do thimpeallachtaí foircneacha

 

3, tacú le draenáil leanúnach: píopa draein seachtrach, rochtain dhíreach ar an bpíopa séarach, draenáil áisiúil

 

4, dehumidification cliste: tá sliseanna cliste, beidh dehumidification Chliste go huathoibríoch de réir na taise comhshaoil atá ann faoi láthair, ní gá féachaint

 

5, breithiúnas lochtach cliste: an suíomh locht agus an t-aiseolas ar scáileán LCD a chinneadh go huathoibríoch le haghaidh cothabhála

 

6, uainiú dhá bhealach: is féidir leis an am tosaithe agus an t-am múchta a shocrú de réir na riachtanas oibre, atá éasca le feidhmiú


Grianghraif Táirge:

Dehumidifiers for Museums, Archives and Libraries

Dehumidifiers for Museums, Archives and Libraries

Paraiméadair Mhionsonraithe:

Mionsamhail DH-5168C
Deireadh Taise 168L / D nó 7L / H
Foinse Cumhachta 380V / 50HZ
Ionchur Cumhachta Rátáilte 3.2KW
Cumhacht Reatha 6.2A
Teocht Oibre 5-38 ℃
Scaipeadh Aeir 1600M3 / h
Cuisneán R22 / R407C
Meáchan Glan 108Kg
Meáchan comhlán 118Kg
Ag Cur Spáis i bhFeidhm 150 ~ 200m2
Toise Táirgí 405x605x1620mm
Toise Pacála 485x655x1680mm
Loading Qty 33pcs / 20 troigh
Tréimhse táirgthe 10 lá
Bharántas 1 bhliain

Iarratas ar Dhíthhíoltóir i Músaeim, i gCartlanna agus sa Leabharlann

Is iondúil go mbíonn coincheap na taise (taise absalóideach agus taiseachas coibhneasta) páirteach i staidéar staidéar timpeallachta iarsmalainne. D'fhonn an taise a thuiscint, is gá tuiscint a fháil ar an ngaol idir taiseachas coibhneasta agus taise absalóideach. Tá méid áirithe gal uisce san aer timpeall orainn, ar a dtugtar aer fliuch; tugtar aer tirim ar an aer atá saor ó theoiric ó ghal uisce. Is é taise absalóideach an cóimheas idir mais an ghal san aer agus toirt iomlán an aeir thais. Is tomhas é ar mhéid an ghal san aer.

 

Faoi choinníollacha áirithe teochta, is é an cóimheas idir an t-ábhar uisce san aer agus an t-ábhar uisce ag a sroicheann an gal uisce san aer an méid a thugaimid de ghnáth taiseachas coibhneasta. Nuair a shroicheann an taise san aer an leibhéal is airde, tugtar sáithiúchán air. Is é an taiseachas coibhneasta sa chás seo ná 100%.

 

Bíonn tionchar ag an teocht ar an méid uisce is féidir a stóráil san aer. Dá airde an teocht, is ea is mó an t-uisce. Dá bhrí sin, ní athraíonn an taise iomlán (cion uisce). Dá airde an teocht, is amhlaidh is ísle an taiseachas coibhneasta. Má tá an meáchan ar ghal uisce san aer tairiseach agus má athraíonn an teocht, d'fhéadfadh an taiseachas coibhneasta athrú go mór.

 

Mar shampla, i gcás iarsmalann i dtimpeallacht leath oscailte, d'fhéadfadh bailiúcháin lena n-áirítear déantúsáin miotail a bheith nochta do theocht níos airde agus taiseachas coibhneasta le linn an taispeántais, ach ar chúis éigin aistrítear na déantáin go Timpeallacht ísealteochta, mar gheall ar an athrú teocht, déanfaidh an gal uisce thart ar na déantáin miotail comhdhlúthú faoi choinníollacha fuar, rud a fhágann go mbeidh "comhdhlúthú" ann. Is é an feiniméan a bhaineann le “comhdhlúthú” gal uisce ar dhromchla na ndéantán miotail cúis thábhachtach le creimeadh déantán miotail.

 

Ina theannta sin, tá taise na timpeallachta ina bhfuil an bailiúchán rómhór, rud a fhágann go mbíonn drochbhailíocht uisce ar na bailiúcháin, mar shampla páipéar, dath na bpictiúir, agus go bhfuil spotaí múnlaithe orthu; agus má tá an taise ró-íseal, crackfaidh an t-adhmad agus na laicir. . Dá bhrí sin, tá sé fíorthábhachtach an cion taise agus teocht an atmaisféir a rialú.

 

Faoi láthair, tá tús curtha ag go leor músaem agus dánlann ealaíne sa bhaile agus thar lear úsáid a bhaint as rialtóirí taise atmaisféarach, astaitheoirí taise, srl. Chun taise an tseomra taispeántais agus an stóras a choigeartú, agus tá torthaí áirithe faighte acu.

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

Clibeanna Te: dehumidifiers do mhúsaeim, cartlanna agus leabharlannaChina, monaróirí, soláthróirí, monarcha, mórdhíola

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