solar radiation context/importance of solar radiation measurements –energy available to earth...
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SOLAR RADIATION
• Context/Importance of solar radiation measurements– Energy available to Earth– Atmospheric circulation– Here: microscale energy balance: turbulence generation– Almost 50% of short-wave radiation absorbed by surface and changed into th-IR
• Types of radiation (irradiation W/m2)– Direct solar radiation– Diffuse solar radiation (scattering and recflections)– Global solar radiation
hemispherical (2 steradians)
– Spectral range from 300 to 3000 nm
SENSOR TYPES: AN OVERVIEW OF TECHNOLOGIES
• Direct solar radiation: Pyrheliometers– Tracking of solar position (azimuth and zenith angles)
• Net radiation level: Radiometers– Sum of direct and diffuse solar radiation minus reflected
• PPFD: Quantum sensors– Photosynthetic light spectrum or PPFD
• Total (global) radiation: Pyranometers– Thermopile arrays
• Electrical output prop. to absorbed radiation• Thermocouples in series or in parallel
– Photovoltaic detectors• Si – photodiodes (barrier-layer cell)• Potential at junction between two materials• Rapid response time
OUR CHOICE:THE DAVIS SOLAR RADIATION SENSOR 6450
• General information– Si photodiode with wide spectral response (sealed)– Convection cooling of body, run-off path for water– Cutoff ring for cosine response, level indicater, alignment fins– In-build amplifier
• Manufacturer’s specifications– Power requirements: 3 VDC (10%); 1 mA; 3 mW– Analog output [0,+3VDC]; 1.67 mV per W/m2
– Operating environmental conditions:• Temperature: -40° to +65°C• Temperature corrections: coeff = 0.12% per °C; ref temp = 25°C
– Sensor specifications• Spectral response: 400 (300) to 1100 nm• Output Range: 0 to 1800 W/m2
• Cosine Response 3% (0°-70° i. angle); 10% (70°-80°i.a.)• Accuracy: 5% of full scale (ref: Eppley PSP at 1000 W/m2)• Drift: up to 2% per year
OUR CHOICE:THE DAVIS SOLAR RADIATION SENSOR 6450
• Sensor components and dimensions– Diffuser with ‘excellent’ cosine response– Cable (industrial version: 5 m)– Dimensions: 51 mm x 70 mm x 57 mm– Weight: 226 g
• Mounting– Top of stand– Needs flat surface with holes for fixing– 3 screws and springs for levelling– Fins for optical alignment
CALIBRATION REQUIREMENTSIMPROVED ACCURACY LOW-COST SENSORS
• Studies by King et al. at Sandia National Laboratories– Achieve better accuracy (3%) using photodiodes instead of expensive
thermopile devices (2%)
• Main factors influencing accuracy– Solar spectral influence– Solar angle-of-incidence
• Sensor’s response to direct irradiance influenced by cosine of solar AOI & optical characteristics of front surface
• Significant measurement errors at high AOI
– Operating temperature
• Calibration methodology– Determine AMa and AOI functions (empirical curves)
– Determine calibration constant Cn (in mV) for standardized AMa solar spectra, at a reference temperature To
– Apply corrections for an improved estimate of the total (broadband) irradiance Et:
CALIBRATION REQUIREMENTSIMPROVED ACCURACY LOW-COST SENSORS
• Solar spectral influence– Changes of solar spectral distribution over the day– Compute spectral mismatch parameter M (ASTM)
– Option to relate M to the absolute optical airmass AMa
and obtain a continuous spectral mismatch parameter
• Solar angle-of-incidence– Influence depends on pyranometer’s optical
characteristics (diffuser)– AOI function
• Operating temperature
• Other factors:– Mechanical and optical asymmetries, linearity of
response, path across pyranometer, response time,
stability
CALIBRATION REQUIREMENTSCLASSIFICATION & INDICATIONS
• WMO classification of Davis 6450 pyranometer– Second class pyranometer
• WMO calibration methods (using sun or lab source)– Comparison with standard pyrheliometer– Comparison with standard pyranometer
(natural conditions)– Comparison on laboratory optical bench– Comparison in laboratory integrating chambers– Calibrate in the normal position of use
• Comparison with reference pyranometer– Simultaneous operation of both instruments– Long period for representative results in typical conditions– Calibration factor: k = R kr (R-response ratio test/reference)– Take temperature into account– Davis sensors individually calibrated against secondary standard – standard
calibrated against Eppley Precision Spectral Pyranometer in natural daylight
SITE SELECTION CONSIDERATIONS
• Site selection– Site should be free from any obstruction above plane of sensing element– Shadow possibilities at any time of year have to be taken into account– Should be away from light-coloured walls or reflective objects– Should not be exposed to artificial radiation sources– Keep at certain distance from buildings or obstructions– Here: these considerations will probably not be taken into account– Avoid vibrations due to high winds, use rigid platform
• Installation– Careful optical levelling of instrument, check plotting irradiance throughout a day– Maximum cable length and weatherproofed junctions
• Operation– Sampling rate– Integration of data
MAINTAINANCE REQUIREMENTS
• Inspection frequencies (ASTM standards)– Daily for cleaning– Semi-annual for inclination angle verification– Annual for recalibration and general deterioration inspection
• Care and maintainance– Wipe dry and clean diffuser using cloth and ethyl alcohol– Gently remove solid deposits: frozen snow, frost or rime
• Recalibration– Observed annual drift of 2%, for higher accuracy, calibrate once a year– Basic calibration procedures should be employed if preserved standards
available– Quality control with long-term plots of solar noon irradiance value during clear
sky conditions
Si Photodiode Visible to UV
• What is a photodiode?
-> A component semiconductor able to detect a radiation, which collects the visible signal and transforms it into electric signal. Family of the active photoreceivers, it requires to be polarized in reverse by an external food.
-> 3 distinct areas are located:
• charging space (ZCE) • Neutral region of type N• Neutral region of type P
Si Photodiode Visible to UV
• Dimensional outlines
-> Side View:
-> Top View:
Width: 5,5 mm
Width window: 3,1 mm
Height: 16,5 mm
Distance connects: 2,55mm
Si Photodiode Visible to UV
• General Characteristics :
- package= 18mm
- Active area size= 1,2 mm2
- Reverse voltage(VRMax)= 30 Volts
- Operating temperature(Topr)= -40 to +100
- Storage temp.(Tstg)= -55 to +125 celsius
-> Analogical dispositif with borosilicate glass
Si Photodiode Visible to UV
• Electrical and optical Characteristics :
-Spectral response range from 320 to 1100 nm
- Peak (sensitivity wave length) lambda= 960 nm « spectral response »
- PhotoSensitivity (S)= 0,6 (A/W) « photosensitivity »
Si Photodiode Visible to UV
Warning: Photodiodes (Ge) have a more significant photosensitivity but their dark current is notable ID = 10 uA. It is thus preferable to use photodiodes (Si) (ID near 10 pA) for the detection of weak illuminations.
-Dark current ID= 2 pA
- Temp. coefficient of ID= 1,12 times / degree
Si Photodiode Visible to UV
• Electrical and optical Characteristics :
- Rise time : 0,4 micro sec. «rise time/ load resistance»
- Terminal capacitance(Ct)= 140 pF
- Shunt resistance (Rsh)= 5 to100 GOhm « shunt
resistance »
This device goes to necessite the use of an amplifier of impedance. About alternative technologies we have: laser, and every works with wavelength.
Si Photodiode Visible to UV
• Precision and accuracy: - Near the microseconde
- High reliability
- High linearity(->relationship between the collected ray and the electrical current product is strictly linear)
• Maintenance requirements
- The cellule must be always clean to intercept radiations clearly with no wrong ways and any shade about objects have to affect our measurements.
InfraRed Thermometer (IRT)
• Sensor to get Skin Temperature
Canopy Surfaces(Ground, Wall, Roof, …)
• Anything above «Absolute Zero» radiates in the IR
+ : Everything can be measured
- : Risk of Perturbations
Compounds Infomations
• IR Thermopile Detector Target
Wave Length : 5 m -14 m
Atmospheric Window (H2O, CO2, CH4, …)
• Temperature Sensor Environment
IRT Specifications
• Operating Power Requirements :
• Output Format :
- Voltage Output Conversion (Analog)
(expected ranges : 0 - 10V, 4 - 20 mA)
- CPU (chip) converts Analog signal into Digital
Voltage 3V 4.5V
Current 4 A 6 A
• Range of environmental Conditions :
- Temperature : Measurement Range -33° 220°C Operating Range -10° 50°C
- Emissivity of Materials (Function of T°) : High Emissivity : Plastic, Glass, Ceramics, Water, Soil, … Low Emissivity : Gold, Aluminium, shiny Objects
- Field of View : Distance of Sensor Spot Size on Surface
IRT Specifications
• Accuracy :
Thermopile Depends on neighbourhood Temperature
IRT Specifications
Error on Measurment when ambiant T° = 25°
T°
eM
Relative Measurment Error min : ambiant T° = target T°
+/- 15°
+/- 0.5°
Alternative technologies
• Thermocouple :
2 dissimilar Metals are joined
When Junction is heated (or cooled), a Voltage is produced
• Resistance Temperature Detector (RTD) :Composed of a Material which has well known «Temp – Res» Relationship. Most accurate Sensor, Stability & Sepeatability
Both are contact Sensors, that means they have to be close to the Surface.
Calibrations & Maintenance
• Blackbody Cavity (commercial) :
Standard Method for Calibration (emissivity : ε =1) need to get ε-Target from Tables
• On Field :
Has to be done for specific Surface Properties
use Hand-held with auto ε-compensation system
• Test Calibration Frequency Requirement :
Drift ? Emissivity changes ?
Sites Selection
As many representative Samples as possible…
• Different Exposition Surfaces :
Ground, Wall and Roof
Sunny vs. Shaded Sites
• Different Surface Types (with high ε) :
Concrete, Brick, Asphalt, Glass, Gravels, …
Notices…
• Still no Information about how to fix IRT on Stands
• Many Certifications about the Products (e.g. ISO 9001)
• Not a lot of Specific Informations about the sensor TN0am Difficulty to be informed through the website !!
• References :www.zytemp.com (choosen Instrument)www.apogeeinstruments.comwww.hukseflux.comwww.omega.com
Measurement of Surface Wind
• Wind direction meteorological forecast
• Wind speed Naval war strategy
• Modern wind sensors
– Anemometers based on cooling effect of wind
– Anemometers based on air movement
– Anemometers based on wind force
Wind measurement
• Wind speed
Definition:
- Wind velocity
- Average over 10 min
• Wind direction
Definition:- Direction from which wind
is blowing - Geographical north- Calm
Units: degreesUnits: m/s or knots
Wind Sensors:Davis anemometer
• Direction vane
=> Measures wind direction
• Cup rotor
=> Measures wind speed
Wind speed sensor: Two sub-assemblies
Rotor:• Proportional to wind
speed• Problem with starting
threshold speed• Response to change in
wind speed = distance constant
Signal generator:• Reed switch in
anemometer head unit• Magnet in the wind cup
assembly
=> Circuit closure
N 2RRV (turn/sec) regimerotation N
radius R
elocityrotation v
Wind direction vane: Two sub-assemblies
Vane:• Well-balanced• One-single equilibrium
position
Signal generator:• Shaft angle transducer• 360º Potentiometer• Resistance: 0-20K Ohms• Input Voltage: 3V• Output voltage• Analog signal
Range and Accuracy:Range:• Wind speed 0.9-78 m/s• Wind direction 0-360° or 16 compass points
Accuracy:• Wind speed 5%• Wind direction 7°
Resolution:• Wind speed 1mph• Wind direction 1°
Environmental Conditions
• Freezing Conditions => Use of drip rings
• Hurricane and light breeze => Wind tunnel testing
Maintenance
• No maintenance required
Calibration requirement
• Calibration curve: nature of response to change in wind speed
• Rotation rate: function of wind speed• Usually linear calibration• Specific to each type and instrument
• Overspeeding: overestimation of wind speed
Distance constant: greater for deceleration than for acceleration => depends on the angle of attack
l0U-U
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Considerations about site selection
• Cable length 42 m • International standard recommendation
– Height:– Open terrain
• Obstructions– Buildings– Trees
)]75.4(log656.0233.0[VV 1001h h
=> Ideal recommendation: wind sensors only on open, flat, rural terrain
Conclusion: Why choose a cup anemometer?
Advantages:• Robust assembling• Comfortable handling• Competitive price• Easy measurement
technique
Inconvenients:• Horizontal speed• Slow response to wind
variation• Constraining siting
=> Cup anemometers are simple and convenient instruments!
One device for measuring both relative humidity and temperature
MEASUREMENT OF TEMPERATURE AND RELATIVE HUMIDITY
MEASUREMENT OF TEMPERATURE AND RELATIVE HUMIDITY
• Sensor SHT75 (total weight = 168 mg)
Fig.: www.sensirion.com/humidity
SPECIFICATIONS OF SHT75
• Power requirements
- VOLTAGE supply is between : 2.4 and 5.5 V
- Maximum supply CURRENT depends on the conditions :
- when it is measuring : 550 A - in average : 28 A
(with one measurement of 12bit per second)
SPECIFICATIONS OF SHT75
• For sending a command, we have to do the following steps :- initiate a transmission- enter the code for the command
- measurement sequence for RH and T
Fig.: www.sensirion.com/humidity
SPECIFICATIONS OF SHT75
• How do we do practically for sending command ?
Fig.: www.sensirion.com/humidity
Fig.: www.sensirion.com/humidity
SPECIFICATIONS OF SHT75
• Output format
- Digital output for both temperature and relative humidity (there is a 14bit analog to digital converter)
• Converting Output to physical values
- We need to use 2 formula with five coefficients to convert from digital readout to temperature and to relative humidity.
SPECIFICATIONS OF SHT75
• Converting Output to physical values- for relative humidity :
Fig.: www.sensirion.com/humidity
SPECIFICATIONS OF SHT75
• Converting Output to physical values- for temperature :
Fig.: www.sensirion.com/humidity
SPECIFICATIONS OF SHT75
• Range of environmental conditions for proper operation:
In our case, there is no specific problem…
… except for the extreme values for both RH and T.
Fig.: www.sensirion.com/humidity
SPECIFICATIONS OF SHT75
• Precision and accuracy
Fig.: www.sensirion.com/humidity
SPECIFICATIONS OF SHT75
• Alternative technologie :- the most accurate humidity measurement instruments that exist on the market are the chilled mirror hygrometers.
- However, these instruments are very expensive.
Fig.: www.sensirion.com/humidity
CALIBRATION REQUIREMENTS
• Each of our sensors (SHT75) are already calibrated in a precision humidity chamber.
SITE SELECTION CONSIDERATIONS
• Our operating conditions in any case on the campus, are fully included in the recommended conditions. Therefore there is no restriction for selecting the sites.
• (We must still be careful with the areas near the laboratories of air pollution because the chemical vapors may interfere with the polymers used for capacitive humidity sensors. High levels of pollutants could cause permanent damage to the sensing polymer.)
MAINTENANCE REQUIREMENTS
• There is an “end of battery” function that detects voltages below 2.47 V.
• No specific maintenance.
WIRED RAIN METERWS-7048U
LA CROSSETECHNOLOGY
Blablabla…
INTRODUCTION
• Floods have become a more and more frequent phenomenon. They are responsible for high human and financial losses.
• Good predictions of rain can allow to avoid such losses by building protection in key places for example.
• Predictions are based on previous rain measurements.
That’s why it is important to make good measurements in many different places. We can do them using our wired rain meter.
POWER REQUIREMENTS
• 2x AA, IEC LR6 1.5V batteries.
• Life time of a battery: about one year.
SPECIFIC FEATURES
• 3 displays of rainfall quantities.• Transmission of rainfall data through a connected wired
rain gauge.• Rainfall unit display in inch or in millimeters (1inch =
25.4mm).• Manual and auto reset of rainfall data.• Auto off function (after 12 hours).• Wall mounting or table standing.
DISPLAY OF RAINFALL DATA (1/ 2)
• 1 auto display : the rain quantity data will be displayed an added to the previous recorded data in the auto counter.
• If no rain is recorded during 2 hours, the auto counter will
display the last recorded data. The auto counter will
automatically reset to 0.0 mm when rain begins again.
• The rain data of auto counter cannot be reset manually.
DISPLAY OF RAINFALL DATA (2/ 2)
• 2 manual displays : the rain quantity data will be displayed in counter 1 and 2. New rain data will be added to the previous records and unless the counters are manually reset by pressing reset 1 or reset 2 key, the rain data will increase continuously to a maximum of 9999.9 mm.
ACCURACY
• The rain sensor features a self emptying tipping bucket that measures 0.01 inch per tip.
• So accuracy is 0.01 inch = 0.254 mm.
CALIBRATION REQUIREMENTS
• There is no need for calibration.• We can imagine improving the precision by comparing
the measurement with a graduated recipient during a rain period.
SITE SELECTION CONSIDERATIONS
• We must place the rain gauge in a site where the rain cannot be intercepted before falling into the sensor.
• Wire length is 10 meters, the rain meter must be placed under shelter. So the rain gauge will be placed at a maximal distance of 10 meters from a sheltered location.
PROBLEMS THAT MAY OCCUR
• Something can fall into the rain gauge and disturb the measurements.
• If it is snowing the measurements won’t be correct.
• Even if snow is alternating with rain, the measurments will be affected.
END
Soil Moisture
The ECH2O Probe
Atmospheric Turbulent Flow in Urban Environments , V. Silva 2005
Plan
Introduction
Specifications
Calibration requirements
Site selection considerations
Maintenance requirements
Applications notes
Synthesis
Introduction
soil moisture
>> when to irrigate, how much water to apply,…
>> transport and storage of dissolved nutrients and pollutants
The Ech2o Probe
dielectric permittivity
>> sensitive measure of water content
ECH2O Probes in both 4” and 8” lengths
Specifications
Echo probe diagram
Specifications
Power
Requirements: 2.5VDC @ 2mA to 5VDC @ 7mA
Specifications
Output format
Analog : 10-40% of excitation voltage (250-1000mV) at 2500mV excitation.
Specifications
Accuracy
Typically ± (± 3%)With soil-specific calibration ± (± 1%)
Resolution
0.002m3/m3 (0.1%)
Allowable environmental conditions
Operating Environment
0 to 50º C
Range of Measurement
0 to saturated volumetric water content
Calibration requirements
ECHO probe : pre-calibrated for most soil types
• Soil type with high sand or salt content : standard calibration not accurate
>> specific calibrations
Calibration requirements
stability on sand soils
Calibration requirements
standard calibration (2500mV excitation)
(ECHO-20) :
(m3/m3) = 0.000695mv - 0.29
(ECHO-10) :
(m3/m3) = 0.000936mv - 0.376
volumetric water content
mv millivolt output
Site selection considerations
soil adjacent to the probe surface
>> strongest influence on the probe reading
air gaps or excessive soil compaction
>> profoundly influence the readings
Site selection considerations
large metal objects
>> attenuate the probe’s electromagnetic field
Site selection considerations
install the ECHO probe
>> pilot hole in the soil
the entire length of the probe
must
be covered
Site selection considerations
Orientation
>> flat side perpendicular to the surface
Maintenance requirements
Removing the Probe
not pull it out of the soil by the cable !
Maintenance requirements
durability of the Echo Probe wires at low temperatures :
breaking point : between -35° C and -45° C
Maintenance requirements
problems with rodents
>> chewing on the ECHOprobe cables
Application notes
Application notes
Application notes
An ECH2O Radio Logger in Southeastern Idaho potato field
>> multiple-depth
soil moisture readings
and precipitation
data
Synthesis
benefits• High resolution allows daily or hourly
tracking of water use.
• Voltage output proportional to water content.
• Low-cost dielectric water content sensor
• Very low power requirement.
Synthesis
inconvenients• Sensitivity to salt and temperature.
Model 264Very Low Differential Pressure
Transducer
Measuring a PRESSURE DIFFERENCES (unidirectional or
bidirectional)
Model 264Very Low Differential Pressure Transducer
What does it do?
It measures the pressure difference between two pressures (measured from two different medias at the same time), converting it to a proportional electrical output. Scale can be set for either unidirectional (i.e. 0 to maxp) or bidirectional (i.e. –maxp to maxp) pressure differences.
Models with different scale (maximum pressures) ranges are available Measuring either low or very low pressures.
Model 264Very Low Differential Pressure Transducer
Power requirement & Output format
Mode A – VOLTAGE
In: 9-30 VDC, current not specified
Out: 0 to 5 VDC (analog pressure indication)
Mode B – CURRENT
In: 9-30 VDC
Circle: 4-20mA (analog pressure indication), to any external load of 0-800 ohms
Uses 9-30 V, DC. ANALOG. Two models are available: Voltage and Current
Output: Signal (Voltage resp. Current) proportional to pressure
Internal Regulation permits use with unregulated power supplies
Model 264Very Low Differential Pressure Transducer
Conditions for proper operationPressure ranges:
- Measurement:
•Unidirectional: 0 – 0.00025 atm to 0 – 0.25 atm
•Bidirectional: 0 – 0.0012 atm to 0 – 0.12 atm
- Allowed overpressure: 0.7 atm in both directions
Temperature:
-18 to 79°C (error compensated for -18 to 65°C)
NO LIQUIDS OR CORROSIVE GASES
Sensor is quite robust to substances in the atmosphere; However, very aggressive compounds like chloric or sulfuric acid however could cause damage, and exposure to moisture or contaminants can lead to performance losses.
Model 264Very Low Differential Pressure Transducer
Precision & accuracy
Standard accuracy: ±1.0% full scale (i.e. 2.5E-6 to 2.5E-3 atm, depending on scale)
Higher accuracies available
Signal is temperature compensated to 0.033% FullScale/°C thermal error over the temperature range of -18 to 65°C
Model 264Very Low Differential Pressure Transducer
Alternative technologies
Virtually all modern pressure sensors, pressure is measured by monitoring a diaphragm which is being subjected to the test pressure on one side, and the specified reference pressure (varying or fixed through a hermetically sealed vacuum) on the other side.
In Setra Model 264, both sides of the diaphragms are accessible to external pressures Pressure DIFFERENCES are measured; the alternate method are instruments for absolute measurements.
Model 264Very Low Differential Pressure Transducer
Calibration requirements
No field calibration required (factory calibrated)
Mounting position effects < 0.0025 atm
•factory calibrated for vertical position
Manual zero & span adjustment possible
(open both ports to atmosphere -> adjust zero-screw, then apply full pressure and adjust FS-signal with span-screw)
However, setra recommends software correction
Model 264Very Low Differential Pressure Transducer
Site selection considerations
No special conditions (suitable for any air or nonconductive gases)
Exceeding moisture should be prevented from entering the instrument
Model 264Very Low Differential Pressure Transducer
Maintenance requirements
No special maintenance required
No indication of durability
Model 264Very Low Differential Pressure Transducer
Tubing recommendations
Diameter of ideal tubes depend primarily on length:
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