| Services Available | |
|---|---|
| Repair | 不 |
| 校准 | 不 |
| Free Support | Yes |
The CWS655 is a wireless version of our CS655 soil water reflectometer. It has 12 cm rods and monitors soil volumetric water content, bulk electrical conductivity, and temperature. This reflectometer has an internal 900 MHz spread-spectrum radio that transmits data to a CWB100 Wireless Base Station or to another wireless sensor. The internal radio's frequency is commonly used in the US and Canada.
Read More这促使uct will be discontinued as of 10 April 2017. Please review theCWS-Series and CWB-Series Discontinuation Noticefor further details.
CWS655具有12厘米杆,可以插入土壤中。它测量传播时间,信号衰减和温度。然后从这些原始值中得出介电介电常数,体积水含量和块状电导率。
Measured signal attenuation is used to correct for the loss effect on reflection detection and thus propagation time measurement. This allows accurate water content measurements in soils with bulk ≤3.7 dS m-1不执行土壤特异性校准。
土壤颗粒电导率也派生from the attenuation measurement. A thermistor in thermal contact with a probe rod near the epoxy surface measures temperature. Horizontal installation of the sensor provides accurate soil temperature measurement at the same depth as the water content measurement. For other orientations, the temperature measurement will be that of the region near the rod entrance into the epoxy body.
There are situations when it is desirable to make measurements in locations where the use of cabled sensors is problematic. Protecting cables by running them through conduit or burying them in trenches is time consuming, labor intensive, and sometimes not possible. Local fire codes may preclude the use of certain types of sensor cabling inside of buildings. In some applications measurements need to be made at distances where long cables decrease the quality of the measurement or are too expensive. There are also times when it is important to increase the number of measurements being made but the data logger does not have enough available channels left for attaching additional sensor cables.
| Measurements Made | Soil electrical conductivity (EC), relative dielectric permittivity, volumetric water content, soil temperature |
| Water Content Accuracy | ±3% VWC typical in mineral soils, where solution EC ±10 dS/m |
| 所需的设备 | CWB100 |
| Rods | 不t replaceable |
| Sensors | 不t interchangeable |
| 天气抵抗 | 传感器和电池组的IP67等级(必须正确安装电池组。每个传感器都经过泄漏测试。) |
| Operating Temperature Range | -25°至 +50°C |
| Operating Relative Humidity Range | 0 to 100% |
| Power Source | 2 AA batteries with a battery life of 1 year assuming sensor samples taken every 10 minutes. (Optional solar charging available.) |
| Average Current Drain | 300 μA (with 15-minute polling) |
| Rod Diameter | 3.2 mm (0.13 in.) |
| Rod Length | 12 cm (4.7 in.) |
| Dimensions | 14.5 x 6 x 4.5 cm (5.7 x 2.4 x 1.77 in.) |
| Weight | 216 g (7.6 oz) |
Measurement Accuracies |
|
| Volumetric Water Content | 在具有溶液电导率≤10ds/m的矿物土壤中,±3%VWC典型。使用TOPPS方程(M3/m3). |
| 相对介电介电常数 |
|
| Bulk Electrical Conductivity | ±(5% of reading + 0.05 dS/m) |
| Soil Temperature | ±0.5°C |
内部25 MW FHSS广播 |
|
| Frequency | 902 to 918 MHz |
| Where Used | US and Canada |
| FHSS Channel | 50 |
| Transmitter Power Output | 25 mW (+14 dBm) |
| Receiver Sensitivity | -110 dBm (0.1% frame error rate) |
| Standby Typical Current Drain | 3 μA |
| 接收典型的电流排水 | 18 MA(全奔跑) |
| 传输典型电流流量 | 45 mA |
| Average Operating Current | 15 μA (with 1-second access time) |
| Quality of Service Management | RSSI |
| 附加的功能 | GFSK调制,数据交织,正向误差校正,数据争夺,RSSI报告 |
The Wireless Sensor Planner is a tool for use with Campbell Scientific wireless sensors. It assists in designing and configuring wireless sensor networks.
Number of FAQs related toCWS655:34
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大量的电导率(EC)测量是沿传感器杆进行的,它是在土壤前12厘米上的EC平均读数。
Damage to the CWS655 electronics or rods cannot be repaired because these components are potted in epoxy. A faulty or damaged sensor needs to be replaced. For more information,refer to theRepair and Calibrationpage.
The volumetric water content reading is the average water content over the length of the sensor’s rods.
不. The equation used to determine volumetric water content in the firmware for the CWS655 is the Topp et al. (1980) equation, which works for a wide range of mineral soils but not for organic soils. In organic soils, the standard equations in the firmware will overestimate water content.
When using a CWS655 in organic soil, it is best to perform a soil-specific calibration.有关执行土壤特异性校准的详细信息,refer to “The Water Content Reflectometer Method for Measuring Volumetric Water Content” section in theCS650/CS655手册. A linear or quadratic equation that relates period average to volumetric water content will work well.
The equation used to determine volumetric water content in the firmware for the CWS655 is the Topp et al. (1980) equation, which works for a wide range of mineral soils but not necessarily for artificial soils that typically have high organic matter content and high clay content. In this type of soil, the standard equations in the firmware will overestimate water content.
When using a CWS655 in artificial soil, it is best to perform a soil-specific calibration. For details on performing a soil-specific calibration,refer to “The Water Content Reflectometer Method for Measuring Volumetric Water Content” section in theCS650/CS655手册. A linear or quadratic equation that relates period average to volumetric water content will work well.
There is not an easy way to correct CWS655 readings for temperature. The CWS655 temperature sensor is located inside the sensor’s epoxy head next to one of the sensor rods. The stainless-steel rods are not thermally conductive, causing the reported soil temperature reading to be the temperature of the sensor head near the soil surface. Because the sensor is installed vertically with the sensor head above ground, the soil temperature reading is not representative of the temperature over the length of the 12 cm rods, but the reading is closer to the temperature of the soil surface. Performing a temperature correction requires a separate temperature sensor to be buried at approximately 6 cm deep and combines that data with the values reported by the CWS655.
不. The abrupt permittivity change at the interface of air and saturated soil causes a different period average response than would occur with the more gradual permittivity change found when the sensor rods are completely inserted in the soil.
For example, if a CWS655 was inserted halfway into a saturated soil with a volumetric water content of 0.4, the probe would provide a different period average and permittivity reading than if the probe was fully inserted into the same soil when it had a volumetric water content of 0.2.
否。温度传感器位于传感器杆之一旁边的传感器的环氧头部内部。不锈钢杆不是热导电的,因此报道的土壤温度读数实际上是在土壤表面附近的传感器头的温度。
因为传感器是在接地上方的传感器头垂直安装的,所以土壤温度读数不能代表12 cm杆的长度,但读数更接近土壤表面的温度。由于温度读数不能代表水含量测量的土壤的整个厚度,因此没有尝试纠正温度变化的水含量读数。
Yes, but the pots would have to be large. The CWS655 can detect water as far away as 10 cm (4 in.) from the rods. If the pot has a diameter smaller than 20 cm (8 in.), the CS655 could potentially detect the air around the pot, which would underestimate the water content. In addition, potting soil is typically high in organic matter and clay, causing the probably need for a soil-specific calibration.
Period average and electrical conductivity readings were taken with several CWS655 probes in solutions of varying permittivity and varying electrical conductivity at constant temperature. Coefficients were determined for a best fit of the data. The equation is of the form
Ka(σ,τ) = C0*σ3*τ2+ c1*σ2*τ2+ c2*σ*τ2+ c3*τ2+ c4*σ3*τ + C5*σ2*τ + C6*σ*τ + C7*τ + C8*σ3+ c9*σ2+ c10*σ + C11
where Kais apparent dielectric permittivity, σ is bulk electrical conductivity (dS/m), τ is period average (μS), and C1到c11are constants.
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