Freescale Semiconductor FRDM-FXS-MULTI 데이터 시트
MPL3115A2
Sensors
12
Freescale Semiconductor, Inc.
5
Terminology
5.1
Resolution
The resolution of a pressure sensor is the minimum change of pressure that can be reliably measured. The usable resolution
of the MPL3115A2 is programmable, enabling the user to choose a compromise between acquisition speed, power consumption,
and resolution that best fits the application. To simplify the programming, the data is always reported in the same format with
differing number of usable bits.
and resolution that best fits the application. To simplify the programming, the data is always reported in the same format with
differing number of usable bits.
5.2
Accuracy
5.2.1
Offset
The offset is defined as the output signal obtained when the Reference Pressure (a vacuum for an absolute pressure sensor)
is applied to the sensor. Offset error affects absolute pressure measurements but not relative pressure measurements. An alti-
tude measurement is the pressure value in comparison to sea level, a Barometric measurement is the pressure value read by
the sensor, i.e. a measurement of total pressure seen (e.g. 70 kPa), or total height (e.g. 3000 m) above sea level. A change in
the offset will affect the pressure value or height seen above sea level as it shifts the sea level ‘base reference’. An absolute
pressure measurement is not the same as relative pressure measurement, where the pressure is compared when raising or low-
ering pressure in shorter intervals. This would be a walk up a hill, measuring the pressure and altitude difference from start to
finish. In the relative case, the offset shifts are shared in the two absolute measurements and negate each other during the pres-
sure calculation. For the MPL3115A2, the long term offset shift can be removed by adjusting the pressure or altitude offset cor-
rection. This adjustment is provided to override the factory programmed values to compensate for offsets introduced by
manufacturing and mounting stresses. It is highly recommended that this is utilized to realize the full accuracy potential of the
device.
tude measurement is the pressure value in comparison to sea level, a Barometric measurement is the pressure value read by
the sensor, i.e. a measurement of total pressure seen (e.g. 70 kPa), or total height (e.g. 3000 m) above sea level. A change in
the offset will affect the pressure value or height seen above sea level as it shifts the sea level ‘base reference’. An absolute
pressure measurement is not the same as relative pressure measurement, where the pressure is compared when raising or low-
ering pressure in shorter intervals. This would be a walk up a hill, measuring the pressure and altitude difference from start to
finish. In the relative case, the offset shifts are shared in the two absolute measurements and negate each other during the pres-
sure calculation. For the MPL3115A2, the long term offset shift can be removed by adjusting the pressure or altitude offset cor-
rection. This adjustment is provided to override the factory programmed values to compensate for offsets introduced by
manufacturing and mounting stresses. It is highly recommended that this is utilized to realize the full accuracy potential of the
device.
5.2.2
Linearity
Linearity compares the slope of the measurement data to that of an ideal transfer function. It refers to how well a transducer’s
output follows the equation Pout = Poff + Sensitivity x P straight line equation over the operating pressure range. The method
used by Freescale to give the linearity spec is the end-point straight line method measured at midrange pressure.
used by Freescale to give the linearity spec is the end-point straight line method measured at midrange pressure.
5.2.3
Absolute Pressure
Absolute pressure sensors measure an external pressure relative to a zero-pressure reference (vacuum) sealed inside the
reference chamber of the die during manufacturing. This standard allows comparison to a standard value set such that
14.7 psi = 101325 Pa = 1 atm at sea level as a measurement target. The absolute pressure is used to determine altitude as it
has a constant reference for comparison. Measurement at sea level can be compared to measurement at a mountain summit as
they use the same vacuum reference. The conversion of absolute pressure to altitude in meters is calculated based on US Stan-
dard Atmosphere 1976 (NASA). Note that absolute pressure is not linear in nature to altitude; it is an exponential function. The
value of altitude, in increments of 0.0625 meters, can be read directly from the MPL3115A2, or the value of pressure in
0.25 Pascal (Pa) units.
14.7 psi = 101325 Pa = 1 atm at sea level as a measurement target. The absolute pressure is used to determine altitude as it
has a constant reference for comparison. Measurement at sea level can be compared to measurement at a mountain summit as
they use the same vacuum reference. The conversion of absolute pressure to altitude in meters is calculated based on US Stan-
dard Atmosphere 1976 (NASA). Note that absolute pressure is not linear in nature to altitude; it is an exponential function. The
value of altitude, in increments of 0.0625 meters, can be read directly from the MPL3115A2, or the value of pressure in
0.25 Pascal (Pa) units.
5.2.4
Span
Span is the value of full scale output with offset subtracted, representing the full range of the pressure sensor. Ideally the span
is a specification over a constant temperature. The MPL3115A2 uses internal temperature compensation to remove drift. Span
accuracy is the comparison of the measured difference and the actual difference between the highest and lowest pressures in
the specified range.
accuracy is the comparison of the measured difference and the actual difference between the highest and lowest pressures in
the specified range.
5.3
Pressure/Altitude
The MPL3115A2 device is a high accuracy pressure sensor with integrated data calculation and logging capabilities. The al-
titude calculations are based on the measured pressure, the user input of the equivalent sea level pressure (to compensate for
local weather conditions) and the US Standard Atmosphere 1976 (NASA) to give the altitude readings. Pressure is given in Pas-
cals (Pa), and fractions of a Pa. Altitude is given in meters (m) and fractions of a meter. The altitude is calculated from the pres-
sure using the equation below:
local weather conditions) and the US Standard Atmosphere 1976 (NASA) to give the altitude readings. Pressure is given in Pas-
cals (Pa), and fractions of a Pa. Altitude is given in meters (m) and fractions of a meter. The altitude is calculated from the pres-
sure using the equation below:
Where p
0
= sea level pressure (101326 P
a
) and h is in meters. The MPL3115A2 uses this value since the offset register is
defined as 2 Pascals per LSB.
h
44330.77 1
p p
0
⁄
)
0.1902632
} OFF_H (Register Value)
+
(
–
{
=