QT-1021 evapotranspiration station is designed based on the potential evapotranspiration method (ETO method). Designed for agriculture and irrigation control. This station can calculate the potential evapotranspiration (ETO) according to the Penman-Monteith equation, the total water loss from soil evaporation and plant transpiration. ETO results in favorable irrigation control; efficient use of water resources.
QT-1021 Evapotranspiration Station
Principle introduction
Penman-Monteith is based on the theory of energy balance and water vapor diffusion, that is, considering the effects of aerodynamics and radiation terms, as well as the physiological characteristics of the crop, it is considered that the underside crop canopy surface cannot be viewed even under sufficient water supply. It is a saturated layer, and the surface resistance parameter is introduced in its calculation formula to characterize the resistance of leaf stomata and surface soil to water vapor transmission during crop physiological processes. The applicable conditions of this equation are stable conditions, that is, the temperature, atmospheric pressure, and wind speed distributions approximately meet adiabatic conditions (no heat exchange). If the equation is used for a small period of time (1 hour or less), a stable correction is required. However, when the reference surface ET0 is used to estimate the sufficient water supply, the heat exchange is small and generally no stable correction is required. The Penman-Monteith formula comprehensively considers the influence of various meteorological factors on ET0, and it is a mechanism formula with a reliable physical basis and has been widely used in many countries and regions in the world. After decades of theoretical research and practical application, this formula has been recognized as a standard method for calculating ET0.
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Penman-Monteith formula:
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System Features:
l Suitable for agricultural production, scientific research and standard measurement
l Easy to install and maintain
l Built-in calculation formula can directly obtain evapotranspiration value
l Data collection density can be set by yourself
l Status monitoring
l Support AC / solar power supply
l Maintenance-free, suitable for field applications
lSingle-station application or network deployment, wireless data transmission
l Large-capacity data storage
Network management software (optional):
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a) Management function: It has functions of hierarchical management of data and management of monitoring points.
b) Collection function: collect the soil moisture monitoring data at the monitoring point.
c) Alarm function: data alarm function.
d) Query function: The monitoring system software can query various historical records.
e) Storage function: The front-end monitoring equipment has a large capacity data storage function; the monitoring center database can record all historical data.
f) Analysis function: The data can generate curves and reports for trend analysis.
Technical Parameters
CR1000
Data collector
Technical Parameters
Maximum sampling frequency
100Hz
Analog channel
8 differential channels (16 single-ended channels)
Pulse channel
2
Control output
8
Excitation channel
3 voltage channels
Other ports
4 SDI-12 or 4 RS232 (shared with 8 control output interfaces)
Data communication port
1 CS I / O; 1 RS-232; 1 parallel peripheral
Signal input range
± 5000mV
A / D conversion accuracy
13-bit analog / digital conversion
Measurement resolution
0.33 µV
measurement accuracy
± (reading * 0.06% + offset), 0 ~ 40 ℃
Built-in storage space
4M
Supply voltage
9.6 ~ 16VDC
Power consumption
Sleep mode: 0.6mA, 1Hz acquisition frequency: 4.2mA
size
23.9 × 10.2 × 6.1cm
Operating temperature
-25 ~ 50 ℃; -55 ~ 85 ℃ (extended)
CS215 temperature and humidity sensor
CS215
Technical Parameters
Temperature Sensor
Measuring range
-40 ~ 70 ℃
measurement accuracy
± 0.3 ℃ (at 25 ℃), ± 0.4 ℃ (5 ~ 40 ℃), ± 0.9 ℃ (-40 ~ 70 ℃)
Response time
<120 s
Output resolution
0.1 ℃
Relative humidity sensor
Measuring range
0 ~ 100% RH (at -20 ~ 60 ℃)
measurement accuracy
(At 25 ℃): ± 2% (10 ~ 90% RH); ± 4% (0 ~ 100% RH)
Temperature dependence
Better than ± 2% (at 20 ~ 60 ℃)
Short-term lag
< 1.0% RH
Long-term stability
Better than ± 1% RH / year
Response time
<10 s (63%, wind speed 1m / s)
calibration
NIST, NPL
Other technical parameters
Supply voltage
6 ~ 16VDC (12VDC interface of data collector is recommended)
Current consumption
120μA at rest, 1.7mA at measurement (for 0.7 seconds)
Operating temperature
-40 ~ 70 ℃
size
18cm in length, 1.2cm / 1.8cm in diameter (probe end / cable end)
weight
150g
TE525 rainfall
TE525
Technical Parameters
sensor type
Magnetic reed switch
Output
Switch signal
Accuracy
1.0% up to 2 "/ hr (50 mm / hr)
Collector size
24.5cm diameter x 29.21cm high
Collector area
214cm2
Operating temperature
0 ~ 50 ℃
cable length
12 meters
material
Anodized aluminum
03002 wind speed and direction sensor
03002
Technical Parameters
Wind speed measurement range
0-50 m / s
Wind direction measurement range
360 degree mechanical, 355 degree electronic.
Wind speed measurement accuracy
± 0.49 m / s
Wind direction measurement accuracy
± 5 degrees
Wind speed
1.1 m / s
Damping ratio
0.2
Wind speed signal output
Electromagnetically induced AC sinusoidal voltage, 1 pulse per loop.
Wind direction signal output
10K potentiometer, linearity: 0.5%
Potentiometer excitation
5-15VDC
Linear adapter
12-30VDC
Mounting rod diameter
34mm
Sensor net weight
0.7Kg
SP-110 total radiation sensor
SP-110
Technical Parameters
Cosine response
(45-degree angle)
± 1%
Cosine response
(75 degree angle)
± 4%
Absolute measurement accuracy
± 5%
Uniformity
± 3%
Repeatability
± 1%
Sensitivity
0.200 mV per W m-2
Linear range
0-350 mV (0 ~ 1,750 W m-2)
Power consumption
no
working environment
-40 ° C ~ + 70 ° C; 0 ~ 100%
material
Anodized aluminum, acrylic plexiglass lens
cable
3 m shielded cable
size
2.4cm diameter, 2.75cm high
weight
70 g
Origin: United States