Mô đun Honeywell CC-PAIX01 51405038-275 Analog Input Module NEW AND ORIGINAL PACKAGE IN STOCK
Honeywell CC-PAIX01 51405038-275 Analog Input Module NEW AND ORIGINAL PACKAGE IN STOCK
QUICK DETAILS
- Brand :Honwell
- Model :51405038-275
- Place of Origin : USA
DESCRIPTION
- Contorl Circuit Board
- PC BOARD
- DIGITAL OUTPUT MODULE BOARD
OTHER SUPERIOR PRODUCTS
| Yasakawa Motor, Driver SG- | Mitsubishi Motor HC-,HA- |
| Westinghouse Modules 1C-,5X- | Emerson VE-,KJ- |
| Honeywell TC-,TK- | GE Modules IC – |
| Fanuc motor A0- | Yokogawa transmitter EJA- |
Planning Considerations
Implementing an ELMM solution begins by planning for the following:
• Network topology: Understand how ELMM connects to LCN.
• EUCN Planning: ELMM connects to EUCN (UCN over FTE). See UCN Planning guide for more details.
• Site Selection: Dimensions of existing LM cabinets are marginally different from Series C cabinets that
house ELMMs. Analyze this and work out the location of the new cabinet. Wiring and grounding for the
new cabinet and its hardware components must be planned. ELMM comes factory-fitted in a Series C
cabinet. If your plan is to use an existing UCN cabinet to house the ELMMs, estimate for activities for
mounting ELMM hardware and its components and wiring them.
• ELMM and C300 controllers: The number of modules needed based on your requirements, or based
on the number of LM processors being replaced.
• ELMM redundancy: ELMM supports redundancy. Plan the number of controllers and ELMMs required if
you want redundancy, or if the LMs being replaced are redundant.
• IOs: C300 communicates with an entirely different set of IOs (Series C IOs) compared to LM. Map the
existing IOs with their Series C IO or PMIO equivalents in the planning stage itself. If equivalent LM IOs
are unavailable, an engineering solution may have to be found. If you have existing remote IOs, connect
them via Series C Fiber Optics Extenders.
Other Modules
CC-PCF901 PWA MODULE, CONTROL FIREWALL 9 G3 CC C300
CC-PCNT01 PWA MODULE, C300 CONTROL PROCESSOR C300
CC-TCF901 PWA, CNTRL FIREWALL IOTA 8 PORT 1 UPLINK C300
CC-TCNT01 PWA, C300 CONTROL PROCESSOR IOTA CC C300
CC-SCMB02 MODULE ASSY, MEMORY BACKUP C300 C300
51199942-300 BATTERY PACK C300
CC-PWRR01 POWER ASSY, RED 20A W/O BBU
51199929-100 PWA SUPPLY MODULE
CC-PAIX01 PWA MODULE, HLAI G3 CE CC AI
CC-PAIH01 PWA MODULE, HART HLAI G3 CE CC
CC-TAIX11 PWA, AI IOTA RED 16 12IN CE CC
CC-TAIX01 PWA, AI IOTA 16 6IN CE CC
CC-PAOX01 PWA MODULE, AO G3CE CC AO
CC-TAOX11 PWA, AO IOTA RED 16 12IN CE CC
CC-TAOX01 PWA, AO IOTA 16 6IN CE CC
CC-PDIL01 PWA MODULE, DI 24V IO G3 CE CC DI
CC-PDIS01 MODULE, DISOE 24V ASSY G3 24V
CC-TDIL01 PWA, DI 24VAC IOTA
CC-TDIL11 PWA, DI 24V IOTA RED 32 24V
CC-PDOB01 PWA MODULE, DO 24V IO G3 CE CC DO
CC-TDOB01 PWA, DO 24V BUSS IOTA 32 24V
CC-TDOB11 PWA, DO 24V BUSS IOTA RED 32 24V
CC-PAIM01 PWA MOD, LLAMUX G3 CE CC
CC-TAIM01 PWA, PMIO LLMUX IOTA 64PT CE CC
Fluorinated Gases: Hydrofluorocarbons (HFCs), perfluorocarbons (PFCs) and sulfur hexafluoride (SF6) are synthetic, powerful greenhouse gases that are emitted from a variety of industrial processes. Fluorinated gases are sometimes used as substitutes for ozone-depleting substances (i.e., CFCs, HCFCs and halons). These gases are typically emitted in smaller quantities, but because they are potent greenhouse gases, they are sometimes referred to as High Global Warming Potential gases (High GWP gases). HFCs are 140 to 11,700 times more potent than CO2 and have atmospheric lifespans of 1–260 years. Most commercially used HFCs remain in the atmosphere less than 15 years. PFCs are 6,500 to 9,200 times more potent than CO2 and have an atmospheric lifespan of several thousand years. Sulfur hexafluoride is 23,900 times a more potent greenhouse gas than CO2 and is extremely long lived with very few sinks (EPA, 2009c).
Projected change in annual mean surface air temperature from the late 20th century (1971-2000 average) to the middle 21st century (2051-2060 average). The change is in response to increasing greenhouse gases and aerosols based on a middle of the road estimate of future emissions. Warming is larger over continents than oceans, and is largest at high latitudes of the Northern Hemisphere. These results are from the GFDL CM2.1 model but are consistent with a broad consensus of modeling results.
