土壤水分-基质势-温度复合传感器研制

    Development of a composite sensor for the soil moisture, matric potential and temperature synchronous measurement

    • 摘要: 土壤水分、基质势是描述土壤持水特性的重要参数,不同类型土壤的水分特征曲线存在明显差异。目前在野外环境下通常采用传感器分离测量法测定土壤水分特征曲线,但因土壤的空间异质性导致较大的测量误差。为此,该研究设计了一种可同步测量土壤水分、基质势和温度的复合传感器,主要组成部分包括32位MCU主控芯片、继电器切换模块、介电水分/基质势测量模块和温度测量模块,主控芯片通过控制继电器切换实现土壤水分、基质势和温度的同步测定,同时进行温度校正。采用森林土壤、农田壤土和砂土对复合传感器进行性能测试、标定和观测试验,并与商业化仪器的测量结果进行对比。结果表明:在干燥至近饱和范围内,复合传感器测定的土壤水分和基质势均具有良好的单调性,决定系数R2均大于0.98,土壤体积含水率和基质势的测量范围分别为0~40%和-1 500~-15 kPa,水分和基质势的响应时间分别为450 ms和150 s。采用商业化仪器分离测量方法与本文复合传感器分别同步测定森林土壤、农田壤土和砂土的水分特征曲线,2种方法测得的土壤水分特征曲线的皮尔逊相关系数均大于0.96。本文研制的复合传感器可以实现不同类型土壤水分特征曲线的准确测定,为农业生产和环境监测等领域提供可靠的技术支持。

       

      Abstract: Abstract: Soil moisture content and matric potential are two important parameters for determining soil water characteristic curve (SWCC), which has significant differences for different types of soils. The common method to determine SWCC under field condition is using two separated sensors to measure moisture content and matric potential of the tested soils. However, measurement error may occur due to soil spatial heterogeneity around two sensors. In this study, a novel composite sensor was designed to simultaneously measure soil moisture content, matric potential, and temperature. The composite sensor consists of a 32-bit MCU main control chip, relay switching module, dielectric measurement module for determining soil moisture content and matric potential, and temperature measurement module. The main MCU control chip measures soil moisture content, matric potential, and temperature through controlling the relay switching, and performs temperature correction as well. The performances of the composite sensor were tested for soil moisture content and soil matric potential measurements including monotonicity, calibration, volume of sensitivity, response time, etc. To test the monotonicity of the dielectric mode, the length of high frequency transmission line was gradually increased and the sensor output was recorded when the probes of soil moisture content and soil water potential were moistened from dry to saturation. The three modes, soil moisture content, soil matric potential and temperature were calibrated respectively using forest soil, farmland loam and sandy soil. To determine the volume of sensitivity of the soil moisture content mode, the probe of soil moisture content was installed in a soil sample. The soil sample was gradually removed layer by layer and meanwhile the output of the soil moisture content was recorded. When the output started to decrease, the radius of volume of sensitivity was determined by measuring the thickness of residual soil layer from surface to the probe. To determine the response time of soil moisture content and soil matric potential modes, the composite sensor probe was firstly dried and then put into a saturated soil sample. Meanwhile, the output of the soil moisture content and soil matric potential was recorded as time elapse. When the recorded output of each mode did not remarkedly change, the elapsed time was the response time. Experiments for sensor observation were conducted using forest soil, farmland loam and sandy soil under laboratory condition at 25 ℃. The experimental results were compared with those measured using commercial instruments. The results showed that the composite sensor had a good monotonicity when measuring soil moisture content and matric potential in the range from dry to near saturation. After calibration, the composite sensor can determine soil moisture content, matric potential and temperature with high accuracies, achieving the determination coefficients larger than 0.98. The measurement ranges of volumetric soil water content and soil matric potential were 0-40% and -1 500--15 kPa, respectively, which is feasible for most soil textures. The response time of the soil moisture content and soil matric potential was 450 ms and 150 s, respectively. The temperature coefficient of the circuit board of the composite sensor was yielded to correct the temperature induced output variation. The SWCCs of forest soil, farmland loam and sandy soil were determined using both the commercial instruments and the composite sensor during wetting and drying processes. The hysteresis between soil drying and wetting processes was also observed as expected. The Pearson correlation coefficients between the SWCCs measured by the two methods were larger than 0.96 during wetting and drying processes, i.e., 0.962 and 0.983 for the forest soil, 0.993 and 0.995 for the farmland loam, and 0.979 and 0.998 for the sandy soil. The composite sensor developed in this study can accurately determine soil water characteristic curves of different types of soils.

       

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