Ka'idar Aiki
Yayin da tsarin porosity na zaren yumbu ke shiga porosity, za a sami convection na zafi a cikin tsarin canja wurin zafi don tanda mai ƙarfi ko mara kyau. Lokacin da mai gyara ya shiga saman zaren, zai inganta tsarin porosity na saman zaren kuma ya toshe canja wurin zafi mai convective, don haka rage zafin bangon waje da kuma cimma ƙarin tasirin adana kuzari.
Takaitaccen Bayani
Samfurin yana shiga cikin samfuran zare, yana samar da wani Layer mai tauri a saman wanda ya bambanta da shafi kuma ba zai taɓa fitowa akan lokaci ba.
Fa'idodi
Fesa wannan samfurin a saman zare na iya sa saman ya zama mai tauri, don haka cimma waɗannan halaye:
Yana iya inganta ƙarfin saman aiki na samfuran zare masu tsaurin ra'ayi sosai kuma yana ƙara juriya ga scouring.
Zai iya hana raguwar kayayyakin zare yadda ya kamata kuma ya rage yadda wutar ke shiga jikin tanderu.
temIndexSunan SamfuraOsmotic-Mai Ingantaccen Ƙarfafawa Mai Gyaran Gyara RS-GXJ1BD,(g/cm3)1.35-1.40Al2O3+SiO2,bayan bushewa,%≥99.5Rashin juriya,℃1650ForumKayan SamfuraRayuwar Shiryayye Watanni 6 a 0-45℃
Ƙayyadewa
| Abu | Fihirisa |
| Sunan Samfuri | Wakilin Gyaran Osmotic Mai Inganci Mai Inganci RS-GXJ1 |
| BD,(g/cm3) | 1.35-1.40 |
| Al2O3+SiO2, bayan bushewa,% | ≥99.5 |
| Rashin juriya,℃ | 1650 |
| Fom ɗin Samfuri | Ruwa mai ruwa |
| Rayuwar shiryayye | Watanni 6 a 0-45℃ |
Aikace-aikace
Babban murfin tanda, murfin ladle, tanderun dumama masana'antar sinadarai, tanderun zafi mai zafi, bututun iska mai zafi babban murhun shawagi, tanderun maganin zafi, tanderun lantarki na masana'antu, da sauransu.
