D-G2 FUEL DISPENSER

D-G2 FUEL DISPENSER

Pump Type: Optional

Inlet Pressure : >=54kPa.

Flow rate (L/min.): 55±5

Suction Distance (m): 6(verticalmente) / 50(orizzontalmente)

FlowMeter Type : Optional

Accuracy : ±0.2%

Motor Voltage(V): 110V/220V/380V,50Hz/60Hz

Capacity(hp): 1HP(0.75kw)

Input Voltage : 110V/220V/380V,50Hz/60Hz

Nozzle: Auto Shut-off Nozzle

Environmental Condition: -40~~+55degree

Control Type: Solenold Vale Control Type

Preset: Function Provided(Small LCDIndicator)

Display(Counter): Type LCD and Bright Backlight

Digit of Volume: 0~~999,999(6 Digits),Decimal point can be changed

Digit of Amount : 0~~999,999(6 Digits),Decimal point can be changed

Digit of Unit price : 0~~9999(4 Digits),Decimal point can be changed

Digit of Total Range : 0~~99,999,999,99

Optional Display Type: LCD and Bright Backlight

Digit of Volume : 0~~99,999,999(8 Digits),Decimal point can be changed

Digit of Amount : 0~~99,999,999(8 Digits),Decimal point can be changed

Digit of Unit price: 0~~999999(6 Digits),Decimal point can be changed

Digit of Total Range: 0~~99,999,999,99

Totalizer: 1~~9,999,999

Hose :4.5m

Weight : 215kg

Dimension(L×W×H): 900*620*2180(mm)

Dimension(L×W×H)Of Qty of Container : 40ft: 45 20ft: 22

f the technological supervision department. Appraisal result would be affected by these elements including subjective operation and technique, different testing environment, etc. which possibly result in additional error.Pay much attention to fuel dispenser the following items: Maximum measuring valve and accuracy of standard measurer The cubage and volume of metal standard measurement used for fuel dispenser appraisal has regulated in procedure and regulation. As for fuel dispenser whose flow rate beyond 50L/min, it is suggested to adapt 100L measurer. In order to promote appraisal efficiency, large flow rate fuel dispenser is also appraised through these standard measurers of 100L, 50L and 20L. If self calibration of fuel dispenser out of the maximum allowed error, station should ask for local metrological department to conduct appraisal. Collision or hit is avoided as few as possibl fuel dispenser e since cubage is affected by the convex and concave of measurer surface. Vernier of measurer is fixed on measuring neck. Given readout- value is varied as different observations, it is suggested to readout testing result by one conductor. Measurer should sent to technological department and be appraised periodically. Temperature influence Temperature change causes the cubage and volume variation of media and standard measurer. Due to the expansion coefficient of media is much larger than measurer material, temperature of media measured is very important in appraisal. 1�errand would lead to 0.1% relative cubage error. Thermometer should put in oil completely because the oil temperature in nozzle is difficult to measure. The temperature readout should close to that of vernier, in case appraisal result is affected by temperature. Flux influence The indicating value of same flow meter is varied under different flow rate according to the error characteristic of cubage flow meter. The error is caused by flow meter’s leakage, which is varied from different fuel dispenser flow rate. Thereby, openness of nozzle should keep stable in appraisal progress

ling Transaction Data　　 Data ID 20 30-32 Unlocking of Locked Transaction Buffers under error　　 conditions clarified.　　 Chapter 3.11 Data Download　　 Section co fuel dispenser ntents removed.　　 Chapter 5.2 Implementation Guidelines Recommendations　　 Action after Reset or Power Off text description clarified.　　June 2005 2.21 Chapter 2.1　　 Note added covering removal of more than one nozzle.　　 Chapter 2.1.4　　 Under RELEASE_FP note added on Data Ack to return if no transaction buffer.　　 Chapter 3.3 Calculator Database　　 Data ID 5 note added about single sided dispensers.　　 Data ID 5 default value comment added.　　 D fuel dispenser ata ID 11 note added if Release_FP received with Authorised state not allowed.　　 Data ID 44 examples improved and default value added.　　 Chapter 3.7 Fuelling Point Data　　 Config_Lock made Read Write in state 1.　　 Chapter 3.8 Logical Nozzle Data　　 Comments for Meter_2_Id made similar to Meter_1_Id.　　 Chapter 3.9 Fuelling Transaction Data　　 Changed the state column so the state now refers to the Transaction Buffer　　 State Diagram and not the Point State Diagram.　　 Command Clear_Transaction Data Id 30. Comment added about clear all　　 transactions.　　 Data ID 31 Unlock reference to Communications Specification added.　　 Chapter 3.10 Error Code Data　　 Clarification of number of error codes to be returned.　　FP31_2.23 IFSF - STANDARD FORECOURT PROTOCOL fuel dispenser March 2006　　

rmohaline Circulation. The THC pulls warm salty water from the tropics northwards. It gradually loses heat as it does so and, as it approaches the Arctic, begins to sink because it is saltier, and therefore heavier, than the surrounding wate fuel dispenser r. As it sinks, it pulls in more warm water from the tropics. The deeper, colder water returns to the tropics through the Deep Southerly Return Flow, which passes by Florida, and the Subtropical Recirculation, which curls round the west coast of Africa. There are good reasons to be nervous about the Gulf Stream s future, because it has not been reliable in the past. Since the most recent ice age 20,000 years ago, it has packed up several times—most recently, it seems, around 8,200 years ago, when a sudden flood of fresh water from a North American lake tipped into the North Atlantic. The fresh water seems to have diluted the Gulf fuel dispenser Stream s saltiness and thus weakened its flow. That, fear climate-change watchers, is what could happen as the Arctic ice melts. But the models did not predict that it would start happening yet, which is why the climatological world sat up when a paper was published last year claiming that the flow appeared to be slowing. The paper, by Harry Bryden and some colleagues at Britain s National Oceanography Centre in Southampton, was based on five sets of measurements of the THC taken over half a century. The first three showed no discernible change in its speed; but results in 1998 and again in 2004 suggested a noticeable slowing, which Dr Bryden and his colleagues estimate at 30% of the current s volume. Some scientists, such as MIT s Professor Carl Wunsch, caution against drawing conclusions from so few data points. “The oceans are like the atmosphere. The system is exceedingly noisy. You get weather in the oceans like you get weather in the atmosphere. This paper is based on five crossings of the Atlantic over 47 years. It s as though you went fuel dispenser out on five different occasions in five different places in North America over