Apogee SI-411 User manual

APOGEE INSTRUMENTS, INC. | 721 WEST 1800 NORTH, LOGAN, UTAH 84321, USA
TEL: [phone] | FAX: [phone] | WEB: APOGEEINSTRUMENTS.COM
OWNER’S MANUAL
INFRARED RADIOMETER
Models SI-411, SI-421, SI-431, and SI-4H1
(including SS models)

TABLE OF CONTENTS

DECLARATION OF CONFORMITY
EU Declaration of Conformity
This declaration of conformity is issued under the sole responsibility of the manufacturer:
Apogee Instruments, Inc.
721 W 1800 N
Logan, Utah 84321
USA
for the following product(s):
Models: SI-411, SI-421, SI-431, SI-4H1
Type: Infrared Radiometer
The object of the declaration described above is in conformity with the relevant Union harmonization legislation:
2014/30/EU Electromagnetic Compatibility (EMC) Directive
2011/65/EU Restriction of Hazardous Substances (RoHS 2) Directive
Standards referenced during compliance assessment:
EN 61326-1:2013 Electrical equipment for measurement, control and laboratory use –EMC requirements
EN 50581:2012 Technical documentation for the assessment of electrical and electronic products with respect to the
restriction of hazardous substances
Please be advised that based on the information available to us from our raw material suppliers, the products manufactured by
us do not contain, as intentional additives, any of the restricted materials including cadmium, hexavalent chromium, lead,
mercury, polybrominated biphenyls (PBB), polybrominated diphenyls (PBDE).
Further note that Apogee Instruments does not specifically run any analysis on our raw materials or end products for the
presence of these substances, but rely on the information provided to us by our material suppliers.
Signed for and on behalf of:
Apogee Instruments, May 2016
Bruce Bugbee
President
Apogee Instruments, Inc.

INTRODUCTION
All objects with a temperature above absolute zero emit electromagnetic radiation. The wavelengths and intensity of radiation
emitted are related to the temperature of the object. Terrestrial surfaces (e.g., soil, plant canopies, water, snow) emit radiation
in the mid infrared portion of the electromagnetic spectrum (approximately 4-50 µm).
Infrared radiometers are sensors that measure infrared radiation, which is used to determine surface temperature without
touching the surface (when using sensors that must be in contact with the surface, it can be difficult to maintain thermal
equilibrium without altering surface temperature). Infrared radiometers are often called infrared thermometers because
temperature is the desired quantity, even though the sensors detect radiation.
Typical applications of infrared radiometers include plant canopy temperature measurement for use in plant water status
estimation, road surface temperature measurement for determination of icing conditions, and terrestrial surface (soil,
vegetation, water, snow) temperature measurement in energy balance studies.
Apogee Instruments SI series infrared radiometers consist of a thermopile detector, germanium filter, precision thermistor (for
detector reference temperature measurement), and signal processing circuitry mounted in an anodized aluminum housing, and
a cable to connect the sensor to a measurement device. All radiometers also come with a radiation shield designed to minimize
absorbed solar radiation, but still allowing natural ventilation. The radiation shield insulates the radiometer from rapid
temperature changes and keeps the temperature of the radiometer closer to the target temperature. Sensors are potted solid
with no internal air space and are designed for continuous temperature measurement of terrestrial surfaces in indoor and
outdoor environments. SI-400 series sensors output a digital signal using SDI-12 protocol version 1.3.

SENSOR MODELS
The four FOV options and associated model numbers are shown below:
SI-431 SI-421 SI-411 SI-4H1
Model
Output
SI-400 Series
SDI-12
SI-100 Series
Voltage
Sensor model number and serial number are
located on a label near the pigtail leads on the
sensor cable. If you need the manufacturing date
of your sensor, please contact Apogee Instruments
with the serial number of your sensor.

SPECIFICATIONS
Calibration Traceability
Apogee SI series infrared radiometers are calibrated to the temperature of a custom blackbody cone held at
multiple fixed temperatures over a range of radiometer (detector/sensor body) temperatures. The temperature of
the blackbody cone is measured with replicate precision thermistors thermally bonded to the cone surface. The
precision thermistors are calibrated for absolute temperature measurement against a platinum resistance
thermometer (PRT) in a constant temperature bath. The PRT calibration is directly traceable to the NIST.
Spectral Response
SI-411
SI-421
SI-431
SI-4H1
Input Voltage Requirement
5.5 to 24 V DC
Current Drain
0.6 mA (quiescent),1.3 mA (active)
Calibration Uncertainty (-20 to 65 C),
when target and detector temperature are
within 20 C
0.2 C
0.2 C
0.3 C
0.2 C
Calibration Uncertainty (-40 to 80 C),
when target and detector temperate are
different by more than 20 C
(see Calibration Traceability below)
0.5 C
0.5 C
0.6 C
0.5 C
Measurement Repeatability
less than 0.05 C
Stability (Long-term Drift)
less than 2 % change in slope per year when germanium filter is maintained in a
clean condition (see Maintenance and Recalibration section below)
Response Time
0.6 s, time for detector signal to reach 95 % following a step change; fastest data
transmission rate for SDI-12 circuitry is 1 s
Field of View
22º half angle
18º half angle
14º half angle
32º horizontal half
angle; 13º vertical
half angle
Spectral Range
8 to 14 µm; atmospheric window (see Spectral Response below)
Operating Environment
-45 to 80 C; 0 to 100 % relative humidity (non-condensing)
Dimensions
23 mm diameter; 60 mm length
Mass
190 g (with 5m of lead wire)
Cable
5 m of two conductor, shielded, twisted-pair wire; additional cable available in
multiples of 5 m; santoprene rubber jacket (high water resistance, high UV stability,
flexibility in cold conditions); pigtail lead wires
Spectral response of SI series infrared
radiometers. Spectral response (green line) is
determined by the germanium filter and
corresponds closely to the atmospheric window
of 8-14 µm, minimizing interference from
atmospheric absorption/emission bands (blue
line) below 8 µm and above 14 µm. Typical
terrestrial surfaces have temperatures that yield
maximum radiation emission within the
atmospheric window, as shown by the blackbody
curve for a radiator at 28 C (red line).

DEPLOYMENT AND INSTALLATION
The mounting geometry (distance from target surface, angle of orientation relative to target surface) is
determined by the desired area of surface to be measured. The field of view extends unbroken from the sensor to
the target surface. Sensors must be carefully mounted in order to view the desired target and avoid including
unwanted surfaces/objects in the field of view, thereby averaging unwanted temperatures with the target
temperature (see Field of View below). Once mounted, the green cap must be removed. The green cap can be
used as a protective covering for the sensor, when it is not in use.
An Apogee Instruments model AM-210 mounting bracket is recommended for mounting the sensor to a cross arm
or pole. The AM-210 allows adjustment of the angle of the sensor with respect to the target and accommodates
the radiation shield designed for all SI series infrared radiometers.

Field of View
The field of view (FOV) is reported as the half-angle of the apex of the cone formed by the target surface (cone
base) and the detector (cone apex), as shown below, where the target is defined as a circle from which 98 % of the
radiation detected by the radiometer is emitted.
Sensor FOV, distance to target, and sensor mounting angle in relation to the target will determine target area.
Different mounting geometries (distance and angle combinations) produce different target shapes and areas, as
shown below.
A simple FOV calculator for determining target dimensions based on infrared radiometer model, mounting height,
and mounting angle, is available on the Apogee website: http://www.apogeeinstruments.com/using-your-apogee-
instruments-infrared-radiometer/.

CABLE CONNECTORS
Apogee started offering in-line cable connectors on
some bare-lead sensors in March 2018 to simplify the
process of removing sensors from weather stations for
calibration by not requiring the full cable to be
uninstalled back to the data logger.
The ruggedized M8 connectors are rated IP67, made of
corrosion-resistant marine-grade stainless-steel, and
designed for extended use in harsh environmental
conditions.
Inline cable connectors are installed 30 cm from the
head
(pyranometer pictured)
Instructions
Pins and Wiring Colors: All Apogee connectors have six
pins, but not all pins are used for every sensor. There
may also be unused wire colors inside the cable. To
simplify data logger connection, we remove the unused
pigtail lead colors at the data logger end of the cable.
If you ever need a replacement cable, please contact us
directly to ensure ordering the proper pigtail
configuration.
Alignment: When reconnecting your sensor, arrows on
the connector jacket and an aligning notch ensure
proper orientation.
Disconnection for extended periods: When
disconnecting the sensor for an extended period of time
from a station, protect the remaining half of the
connector still on the station from water and dirt with
electrical tape or other method.
A reference notch inside the connector ensures
proper alignment before tightening.
When sending sensors in for calibration, only send the
short end of the cable and half the connector.
Tightening: Connectors are designed to be firmly
finger-tightened only. There is an o-ring inside the
connector that can be overly compressed if a wrench is
used. Pay attention to thread alignment to avoid cross-
threading. When fully tightened, 1-2 threads may still
be visible.
Finger-tighten firmly

OPERATION AND MEASUREMENT
All SI-400 series radiometers have an SDI-12 output, where target and detector temperatures are returned in
digital format. Measurement of SI-400 series radiometers requires a measurement device with SDI-12 functionality
that includes the M or C command.
VERY IMPORTANT: Apogee changed all wiring colors of our bare-lead sensors in March 2018 in conjunction
with the release of inline cable connectors on some sensors. To ensure proper connection to your data device,
please note your serial number or if your sensor has a stainless-steel connector 30 cm from the sensor head then
use the appropriate wiring configuration below.
Wiring for SI-400 Series with Serial Numbers range 0-3056
Wiring for SI-400 Series with Serial Numbers 3057 and above or with a cable connector
Black: Ground (for sensor signal and input
power)
Red: Power In (4.5-24 V DC)
White: SDI-12 Data Line
Clear: Shield/Ground
Red: Power In (4.5-24 V DC)
Black: SDI-12 Data Line
Clear: Ground (shield wire)

Sensor Calibration
Apogee SI series infrared radiometers are calibrated in a temperature controlled chamber that houses a custom-
built blackbody cone (target) for the radiation source. During calibration, infrared radiometers (detectors) are held
in a fixture at the opening of the blackbody cone, but are thermally insulated from the cone. Detector and target
temperature are controlled independently. At each calibration set point, detectors are held at a constant
temperature while the blackbody cone is controlled at temperatures below (12 C), above (18 C), and equal to the
detector temperature. The range of detector temperatures is -15 C to 45 C (set points at 10 C increments). Data
are collected at each detector temperature set point, after detectors and target reach constant temperatures.
All Apogee SDI-12 infrared radiometer models (SI-400 series) have sensor-specific calibration coefficients
determined during the custom calibration process. Coefficients are programmed into the microcontroller at the
factory. Calibration data for each sensor are provided on a calibration certificate (example shown on following
page).
Calibration overview data are listed in box in upper left-hand corner, temperature errors are shown in graph, and
calibration date is listed below descriptions of calibration procedure and traceability.

SDI-12 Interface
The following is a brief explanation of the serial digital interface SDI-12 protocol instructions used in Apogee SI-400
series infrared radiometers. For questions on the implementation of this protocol, please refer to the official
version of the SDI-12 protocol: http://www.sdi-12.org/specification.php (version 1.4, August 10, 2016).
Overview
During normal communication, the data recorder sends a packet of data to the sensor that consists of an address
and a command. Then, the sensor sends a response. In the following descriptions, SDI-12 commands and
responses are enclosed in quotes. The SDI-12 address and the command/response terminators are defined as
follows:
Sensors come from the factory with the address of “0” for use in single sensor systems. Addresses “1 to 9” and
“A to Z”, or “a to z”, can be used for additional sensors connected to the same SDI-12 bus.
“!” is the last character of a command instruction. In order to be compliant with SDI-12 protocol, all commands
must be terminated with a “!”. SDI-12 language supports a variety of commands. Supported commands for the
Apogee Instruments SI-400 series infrared radiometers are listed in the following table (“a” is the sensor address.
The following ASCII Characters are valid addresses: “0-9” or “A-Z”).
Supported Commands for Apogee Instruments SI-400 Series Infrared Radiometers
Instruction Name
Instruction Syntax
Description
Send Identification Command
aI!
Send Identification Information
Measurement Command
aM!
Tells the Sensor to take a Measurement
Measurement Command w/ Check
Character
aMC!
Tells the Sensor to take a Measurement and return it
with a Check Character
Change Address Command
aAb!
Changes the Address of the Sensor from a to b
Concurrent Measurement Command
aC!
Used to take a measurement when more than one
sensor is used on the same data line
Concurrent Measurement Command w/
Check Character
aCC!
Used to take a measurement when more than one
sensor is used on the same data line. Data is returned
with a check character.
Address Query Command
?!
Used when the address is unknown to have the sensor
identify its address
Get Data Command
aD0!
Retrieves the data from a sensor
Make Measurement Command: M!
The make measurement command signals a measurement sequence to be performed. Data values generated in
response to this command are stored in the sensor's buffer for subsequent collection using “D” commands. Data
will be retained in sensor storage until another “M”, “C”, or “V” command is executed. M commands are shown in
the following examples:
Command
Response
Response to 0D0!
aM! or aM0!
a0011<cr><lf>
Target temperature
aM1!
a0012<cr><lf>
Target temperature and sensor body temperature
aM2!
a0012<cr><If>
Target millivolts and sensor body temperature
aMC! or aMC0!
a0011<cr><lf>
Target temperature w/ CRC
aMC1!
a0012<cr><lf>
Target temperature and sensor body temperature w/ CRC
aMC2!
a0012<cr><If>
Target millivolts and sensor body temperature w/CRC

where a is the sensor address (“0-9”, “A-Z”, “a-z”) and M is an upper-case ASCII character.
The target temperature and sensor body temperature are separated by the sign “+” or “-“, as in the following
example (0 is the address):
Command
Sensor Response
Sensor Response when data is ready
0M!
00011<cr><lf>
0<cr><lf>
0D0!
0+23.4563<cr><lf>
0M1!
00012<cr><lf>
0<cr><lf>
0D0!
0+23.4563+35.1236<cr><lf>
0M2!
00012<cr><If>
0<cr><If>
0D0!
0+1.0+35.1236<cr><If>
where 23.4563 is target temperature, 1.0 is target millivolts, and 35.1236 is detector (sensor body) temperature.
Concurrent Measurement Command: aC!
A concurrent measurement is one which occurs while other SDI-12 sensors on the bus are also making
measurements. This command is similar to the “aM!” command, however, the nn field has an extra digit and the
sensor does not issue a service request when it has completed the measurement. Communicating with other
sensors will NOT abort a concurrent measurement. Data values generated in response to this command are stored
in the sensor's buffer for subsequent collection using “D” commands. The data will be retained in the sensor until
another “M”, “C”, or “V” command is executed:
Command
Response
Response to 0D0!
aC!
a00101<cr><lf>
Target temperature
aC1!
a00102<cr><lf>
Target temperature and sensor body temperature
aC2!
a00102<cr><If>
Target millivolts and sensor body temperature
aCC!
a00101<cr><lf>
Target temperature w/ CRC
aCC1!
a00102<cr><lf>
Target temperature and sensor body temperature w/ CRC
aCC2!
a00102<cr><If>
Target millivolts and sensor body temperature w/CRC
where a is the sensor address (“0-9”, “A-Z”, “a-z”, “*”, “?”) and C is an upper-case ASCII character.
For example (0 is the address):
Command
Sensor Response
0C!
000101<cr><lf>
0D0!
0+23.4563<cr><lf>
0C1!
000102<cr><lf>
0D0!
0+23.4563+35.1236<cr><lf>
0C2!
000102<cr><If>
0D0!
0+1.0+35.1236<cr><If>
where 23.4563 is target temperature, 1.0 is target millivolts, and 35.1236 is detector (sensor body) temperature.
Change Sensor Address: aAb!
The change sensor address command allows the sensor address to be changed. If multiple SDI-12 devices are on
the same bus, each device will require a unique SDI-12 address. For example, two SDI-12 sensors with the factory
address of 0 requires changing the address on one of the sensors to a non-zero value in order for both sensors to
communicate properly on the same channel:

Command
Response
Description
aAb!
b<cr><lf>
Change the address of the sensor
where a is the current (old) sensor address (“0-9”, “A-Z”), A is an upper-case ASCII character denoting the
instruction for changing the address, b is the new sensor address to be programmed (“0-9”, “A-Z”), and ! is the
standard character to execute the command. If the address change is successful, the datalogger will respond with
the new address and a <cr><lf>.
Send Identification Command: aI!
The send identification command responds with sensor vendor, model, and version data. Any
measurement data in the sensor's buffer is not disturbed:
Command
Response
Description
"aI!"
a13Apogee SI-4mmvvvxx…xx<cr><lf>
The sensor serial number and other identifying values are
returned
where a is the sensor address (“0-9”, “A-Z”, “a-z”, “*”, “?”), mm is a the sensor model number (11, 21, 31, or H1),
vvv is a three character field specifying the sensor version number, and xx...xx is serial number.
Metadata Commands
Identify Measurement Commands
The Identify Measurement Commands can be used to view the command response without making a
measurement. The command response indicates the time it takes to make the measurement and the number of
data values that it returns. It works with the Verification Command (aV!), Measurement Commands (aM!, aM1! …
aM9!, aMC!, aMC1! … aMC9!), and Concurrent Measurement Commands (aC!, aC1! … aC9! , aCC!, aCC1! … aCC9!).
The format of the Identify Measurement Command is the address, the capital letter I, the measurement command,
and the command terminator (“!”), as follows:
<address>I<command>!
The format of the response is the same as if the sensor is making a measurement. For the Verification Command
and Measurement Commands, the response is atttn<CR><LF>. For the C Command, it is atttnn<CR><LF>. For the
High Volume Commands, it is atttnnn<CR><LF>. The address is indicated by a, the time in seconds to make the
measurement is indicated by ttt, and the number of measurements is indicated by n, nn, and nnn. The response is
terminated with a Carriage Return (<CR>) and Line Feed (<LF>).
Identify Measurement Command example:
3IMC2!
The Identify Measurement Command for sensor address 3, M2 command, requesting a CRC.
30032<CR><LF>
The response from sensor address three indicating that the measurement will take three seconds
and two data values will be returned.
Identify Measurement Parameter Commands
The Measurement Parameter Commands can be used to retrieve information about each data value that a
command returns. The first value returned is a Standard Hydrometeorological Exchange Format (SHEF) code. SHEF
codes are published by the National Oceanic and Atmospheric Administration (NOAA). The SHEF code manual can

be found at http://www.nws.noaa.gov/oh/hrl/shef/indexshef.htm. The second value is the units of the parameter.
Additional fields with more information are optional.
The Measurement Parameter Commands work with the Verification Command (aV!), Measurement Commands
(aM!, aM1! … aM9!, aMC!, aMC1! … aMC9!), and Concurrent Measurement Commands (aC!, aC1! … aC9! , aCC!,
aCC1! … aCC9!).
The format of the Identify Measurement Parameter Command is the address, the capital letter I, the measurement
command, the underscore character (“_”), a three-digit decimal number, and the command terminator (“!”). The
three-digit decimal indicates which number of measurement that the command returns, starting with “001” and
continuing to “002” and so on, up to the number of measurements that the command returns.
<address>I<command>_<three-digit decimal>!
The format of the response is comma delimited and terminated with a semicolon. The first value is the address.
The second value is the SHEF code. The third value is the units. Other optional values may appear, such as a
description of the data value. The response is terminated with a Carriage Return (<CR>) and Line Feed (<LF>).
a,<SHEF Code>,<units>;<CR><LF>
Identify Measurement Parameter Command example:
1IC_001!
The Identify Measurement Parameter
Command for sensor address 1, C
command, data value 1.
1,RW,Watts/meter squared,incoming solar radiation;<CR><LF>
The response from sensor address 1, SHEF
code RW, units of Watts/meter squared,
and additional information of incoming
solar radiation.
Target Temperature Measurement
SI-400 series infrared radiometers have an SDI-12 output. The following equations and the custom calibration
coefficients described in this section are programmed into the microcontroller. Target temperature is output
directly in digital format.
The detector output from SI series radiometers follows the fundamental physics of the Stefan-Boltzmann Law,
where radiation transfer is proportional to the fourth power of absolute temperature. A modified form of the
Stefan-Boltzmann equation is used to calibrate sensors, and subsequently, calculate target temperature:
bSmTT D
4
D
4
T
(1)
where TTis target temperature [K], TDis detector temperature [K], SDis the millivolt signal from the detector, m is
slope, and b is intercept. The mV signal from the detector is linearly proportional to the energy balance between
the target and detector, analogous to energy emission being linearly proportional to the fourth power of
temperature in the Stefan-Boltzmann Law.

During the calibration process, m and b are determined at each detector temperature set point (10 C increments
across a -15 C to 45 C range) by plotting measurements of TT4–TD4versus mV. The derived m and b coefficients are
then plotted as function of TDand second order polynomials are fitted to the results to produce equations that
determine m and b at any TD:
0CT1CT2Cm D
2
D
(2)
0CT1CT2Cb D
2
D
(3)
Where C2, C1, and C0 are the custom calibration coefficients listed on the calibration certificate (shown above)
that comes with each SI-100 series radiometer (there are two sets of polynomial coefficients, one set for m and
one set for b). Note that TDis converted from Kelvin to Celsius (temperature in C equals temperature in K minus
273.15) before m and b are plotted versus TD.
To make measurements of target temperatures, Eq. (1) is rearranged to solve for TT[C], measured values of SDand
TDare input, and predicted values of m and b are input:
 
15.273bSmTT 4
1
D
4
DT 
(4)
Emissivity Correction
Appropriate correction for surface emissivity is required for accurate surface temperature measurements. The
simple (and commonly made) emissivity correction, dividing measured temperature by surface emissivity, is
incorrect because it does not account for reflected infrared radiation.
The radiation detected by an infrared radiometer includes two components: 1. radiation directly emitted by the
target surface, and 2. reflected radiation from the background. The second component is often neglected. The
magnitude of the two components in the total radiation detected by the radiometer is estimated using the
emissivity (ε) and reflectivity (1 - ε) of the target surface:
 
BackgroundetargTSensor E1EE 
(1)
where ESensor is radiance [W m-2 sr-1] detected by the radiometer, ETarget is radiance [W m-2 sr-1] emitted by the
target surface, EBackground is radiance [W m-2 sr-1] emitted by the background (when the target surface is outdoors
the background is generally the sky), and εis the ratio of non-blackbody radiation emission (actual radiation
emission) to blackbody radiation emission at the same temperature (theoretical maximum for radiation emission).
Unless the target surface is a blackbody (ε= 1; emits and absorbs the theoretical maximum amount of energy
based on temperature), Esensor will include a fraction (1 –ε) of reflected radiation from the background.
Since temperature, rather than energy, is the desired quantity, Eq. (1) can be written in terms of temperature
using the Stefan-Boltzmann Law, E = σT4(relates energy being emitted by an object to the fourth power of its
absolute temperature):
 
4
Background
4
etargT
4
Sensor T1TT 
(2)

where TSensor [K] is temperature measured by the infrared radiometer (brightness temperature), TTarget [K] is actual
temperature of the target surface, TBackground [K] is brightness temperature of the background (usually the sky), and
σis the Stefan-Boltzmann constant (5.67 x 10-8 W m-2 K-4). The power of 4 on the temperatures in Eq. (2) is valid for
the entire blackbody spectrum.
Rearrangement of Eq. (2) to solve for TTarget yields the equation used to calculate the actual target surface
temperature (i.e., measured brightness temperature corrected for emissivity effects):
 
4
4
Background
4
Sensor
etargT
T1T
T


. (3)

MAINTENANCE AND RECALIBRATION
Blocking of the optical path between the target and detector, often due to moisture or debris on the filter, is a
common cause of inaccurate measurements. The filter in SI series radiometers is inset in an aperture, but can
become partially blocked in four ways:
1. Dew or frost formation on the filter.
2. Salt deposit accumulation on the filter, due to evaporating irrigation water or sea spray. This leaves a thin
white film on the filter surface. Salt deposits can be removed with a dilute acid (e.g., vinegar). Salt
deposits cannot be removed with solvents such as alcohol or acetone.
3. Dust and dirt deposition in the aperture and on the filter (usually a larger problem in windy
environments). Dust and dirt are best removed with deionized water, rubbing alcohol, or in extreme
cases, acetone.
4. Spiders/insects and/or nests in the aperture leading to the filter. If spiders/insects are a problem,
repellent should be applied around the aperture entrance (not on the filter).
Clean inner threads of the aperture and the filter with a cotton swab dipped in the appropriate solvent. Never use
an abrasive material on the filter. Use only gentle pressure when cleaning the filter with a cotton swab, to avoid
scratching the outer surface. The solvent should be allowed to do the cleaning, not mechanical force.
It is recommended that infrared radiometers be recalibrated every two years. See the Apogee webpage for details
regarding return of sensors for recalibration (http://www.apogeeinstruments.com/tech-support-recalibration-
repairs/).

TROUBLESHOOTING AND CUSTOMER SUPPORT
Independent Verification of Functionality
The simplest way to check sensor functionality is the aM2! command. This command returns detector temperature
and detector voltage output. Detector temperature should read very near room temperature. When the aperature
of the sensor is covered with aluminum foil, the voltage output should read very near 0 mV.
If the sensor does not communicate with the datalogger, use an ammeter to check the current drain. It should be
near 0.6 mA when the sensor is not communicating and spike to approximately 1.3 mA when the sensor is
communicating. Any current drain greater than approximately 6 mA indicates a problem with power supply to the
sensors, wiring of the sensor, or sensor electronics.
Compatible Measurement Devices (Dataloggers/Controllers/Meters)
Any datalogger or meter with SDI-12 functionality that includes the M or C command.
An example datalogger program for Campbell Scientific dataloggers can be found on the Apogee webpage at
http://www.apogeeinstruments.com/content/Infrared-Radiometer-Digital.CR1.
Modifying Cable Length
SDI-12 protocol limits cable length to 60 meters. For multiple sensors connected to the same data line, the
maximum is 600 meters of total cable (e.g., ten sensors with 60 meters of cable per sensor). See Apogee webpage
for details on how to extend sensor cable length (http://www.apogeeinstruments.com/how-to-make-a-
weatherproof-cable-splice/).
Signal Interference
In instances where SI-400 series radiometers are being used in close proximity to communications (near an
antenna or antenna wiring), it may be necessary to alternate the data recording and data transmitting functions
(i.e., measurements should not be made when data are being transmitted wirelessly). If EMI is suspected, place a
tinfoil cap over the front of the sensor and monitor the signal voltage from the detector. The signal voltage should
remain stable at (or very near) zero.