Global warming is a big environment. Under such circumstances, the area of ​​drought disasters is continuously expanding. With the development of social modernization, the economic losses caused by drought have also increased year by year. The characteristics of the drought monitoring work also determine the number of drought monitoring sites, scattered locations, data collection difficulties, and high efficiency and cost. The soil drought monitoring system can achieve real-time data collection of soil moisture content, evaporation, precipitation, and temperature, and report the collected data to the central station through the GPRS wireless network; drought severity ranking based on BP neural network algorithm through the central station The model assesses the drought situation data reported by the telemetering terminal in real time and realizes drought forecasting and forecasting, which provides a basis for timely and effective prevention and control measures for local drought resistance.
The monitoring of drought by the soil drought monitoring system is mainly about the collection of soil moisture content. The steps for the detection of farmland soil moisture content are as follows:
(1) Choose a place that is flat, soil is more uniform, away from the gully, or a place that is significantly moister or drier than the surrounding soil as a test point, then dig a 0.5m or so earth pit, and select the soil where the pit wall is dense. 10cm, 20cm and 40cm small depth installation of soil moisture sensor. At the same time, 3 test soil samples were collected on the horizontal layer of each inserted sensor with a ring knife, poured into an aluminum box and marked.
(2) Connect the soil moisture sensor to the RTU with the set parameters, and use the weight of the soil sample with the accuracy of O.lg to weigh the soil sample as the wet weight M of the soil sample. The soil samples were baked in an oven at 105 °C for 6} 8 h until constant weight. The ten soil masses were then determined. The ten samples were recorded as soil samples.
Through comparison of the soil drought monitoring system, it was found that the average soil moisture content at 10cm and 40cm was larger than the mean soil moisture content at 20cm, and the law of soil moisture content in the intercropping fields; the maximum and minimum deviations of field measurements in each soil layer. Changes in a certain range, which is related to soil water distribution at the monitoring site of Xiaotong, but the soil moisture content of the entire soil layer is within a certain range; the field measured value at each site is slightly different from the measured value of the drying method, and the field measurement value is small. Basically follow the ten baked method measurements.
The monitoring of drought by the soil drought monitoring system is mainly about the collection of soil moisture content. The steps for the detection of farmland soil moisture content are as follows:
(1) Choose a place that is flat, soil is more uniform, away from the gully, or a place that is significantly moister or drier than the surrounding soil as a test point, then dig a 0.5m or so earth pit, and select the soil where the pit wall is dense. 10cm, 20cm and 40cm small depth installation of soil moisture sensor. At the same time, 3 test soil samples were collected on the horizontal layer of each inserted sensor with a ring knife, poured into an aluminum box and marked.
(2) Connect the soil moisture sensor to the RTU with the set parameters, and use the weight of the soil sample with the accuracy of O.lg to weigh the soil sample as the wet weight M of the soil sample. The soil samples were baked in an oven at 105 °C for 6} 8 h until constant weight. The ten soil masses were then determined. The ten samples were recorded as soil samples.
Through comparison of the soil drought monitoring system, it was found that the average soil moisture content at 10cm and 40cm was larger than the mean soil moisture content at 20cm, and the law of soil moisture content in the intercropping fields; the maximum and minimum deviations of field measurements in each soil layer. Changes in a certain range, which is related to soil water distribution at the monitoring site of Xiaotong, but the soil moisture content of the entire soil layer is within a certain range; the field measured value at each site is slightly different from the measured value of the drying method, and the field measurement value is small. Basically follow the ten baked method measurements.
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