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Dehumidifiers Untuk Muzium, Arkib Dan Perpustakaan video

Dehumidifiers Untuk Muzium, Arkib Dan Perpustakaan

240L Dehumidifier untuk Muzium

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Description/kawalan

Dehumidifiers untuk Muzium, Arkib


Ciri-ciri utama:

1. Aplikasi kawasan besar: kapasiti dehumidifikasi yang besar, sesuai untuk permintaan dehumidifikasi kawasan besar, kitaran angin yang besar

 

2, kelembapan ultra-lebar: 20% -90% kelembapan ultra-lebar, boleh memenuhi keperluan tapak dehumidification yang berbeza, boleh memberi respons fleksibel kepada persekitaran yang melampau

 

3, menyokong saliran berterusan: paip longkang luar, akses terus ke paip pembetung, saliran mudah

 

4, dehumidification pintar: mengandungi cip pintar, dehumidification secara automatik mengikut kelembapan alam sekitar semasa, tidak perlu menonton

 

5, penghakiman kesalahan pintar: secara automatik menentukan lokasi dan maklum balas pada skrin LCD untuk penyelenggaraan

 

6, masa dua hala: boleh menetapkan masa boot dan masa tutup mengikut keperluan kerja, mudah dioperasikan


Foto Produk:

Dehumidifiers for Museums, Archives and Libraries

Dehumidifiers for Museums, Archives and Libraries

Parameter Terperinci:

Model DH-5168C
Kelembapan Penyingkiran 168L / D atau 7L / H
Sumber kuasa 380V / 50HZ
Input Kuasa Rated 3.2KW
Kuasa Semasa 6.2A
Suhu Kerja 5-38 ℃
Beredar Air 1600M3 / h
Penyejuk R22 / R407C
Berat bersih 108Kg
Berat kasar 118Kg
Memohon Ruang 150 ~ 200m2
Dimensi Produk 405x605x1620mm
Dimensi Pembungkusan 485x655x1680mm
Memuatkan Qty 33pcs / 20ft
Tempoh pengeluaran 10 hari
Waranti 1 tahun

Permohonan Dehumidifier di Muzium, Arkib dan Perpustakaan

Konsep kelembapan (kelembapan mutlak dan kelembapan relatif) biasanya terlibat dalam kajian muzium kajian alam sekitar. Untuk memahami kelembapan, perlu memahami hubungan antara kelembapan relatif dan kelembapan mutlak. Udara di sekeliling kita mengandungi sejumlah wap air, yang dipanggil udara basah; udara yang secara teorinya bebas wap air dipanggil udara kering. Kelembapan mutlak adalah nisbah jisim wap air di udara ke jumlah keseluruhan udara lembap. Ia adalah ukuran jumlah wap air di udara.

 

Di bawah keadaan tertentu suhu, nisbah kandungan air di udara ke kandungan air di mana wap air di udara mencapai titik tepu adalah apa yang biasanya kita panggil kelembapan relatif. Apabila kelembapan di udara mencapai tahap tertinggi, ia dipanggil tepu. Kelembapan relatif dalam kes ini adalah 100%.

 

Jumlah air yang boleh disimpan di udara dipengaruhi oleh suhu. Semakin tinggi suhu, semakin banyak air. Oleh itu, kelembapan mutlak (kandungan air) tidak berubah. Semakin tinggi suhu, semakin rendah kelembapan relatif. Sekiranya berat wap air di udara adalah malar dan perubahan suhu, kelembapan relatif mungkin berbeza-beza.

 

Sebagai contoh, untuk muzium dalam persekitaran yang terbuka separuh, koleksi termasuk artifak logam mungkin terdedah kepada suhu dan kelembapan relatif lebih tinggi semasa pameran, tetapi untuk sebab tertentu artifak dipindahkan ke Dalam persekitaran suhu yang rendah, disebabkan perubahan suhu, wap air di sekeliling artifak logam akan mengembun di bawah keadaan sejuk, menyebabkan "pemeluwapan". Fenomena "pemeluwapan" wap air pada permukaan artifak logam adalah punca utama pengaratan artifak logam.

 

Di samping itu, kelembapan persekitaran di mana koleksi diletakkan terlalu besar, yang membuat koleksi dengan rintangan air yang lemah, seperti kertas, warna lukisan gelap, dan terdedah kepada bintik-bintik acuan; dan jika kelembapan terlalu rendah, kayu dan lacquers akan retak. . Oleh itu, mengawal kandungan kelembapan dan suhu atmosfera di muzium adalah sangat penting.

 

Pada masa kini, banyak muzium dan galeri seni di rumah dan di luar negara telah mula menggunakan pengawal selia kelembapan atmosfera, penyerap kelembapan, dan lain-lain untuk menyesuaikan kelembapan bilik pameran dan gudang, dan telah menerima keputusan tertentu.

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

Cool tags: dehumidifiers untuk muzium, arkib dan perpustakaanChina, pengeluar, pembekal, kilang, borong

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