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    • 3. 发明公开
    • SPECIFICATION DEVICE FOR WATER STATUS OF SOIL, AND METHOD FOR SAME
    • VORRICHTUNG ZUR BESTIMMUNG DES WASSERSTATUS IM BODEN UND VERFAHRENDAFÜR
    • EP2584348A1
    • 2013-04-24
    • EP11795717.5
    • 2011-06-14
    • National University Corporation Toyohashi University of Technology
    • FUTAGAWA, MasatoSAWADA, Kazuaki
    • G01N27/06G01N27/22
    • G01N27/048G01N33/182G01N33/246
    • When the water content is determined, the electric conductivity has an effect on the water content. On the other hand, when the electric conductivity is determined, the water content has an effect on the electric conductivity. Accordingly, even if each characteristic is measured independently, each obtained value includes the error.
      Contacting a pair of electrodes with soil, applying an alternate current input electric signal to one of the pair of electrodes, comparing a phase of an output electric signal from the other of the pair electrodes with a phase of the input electric signal; and determining the concentration of the ionic solute included in the solvent according to a difference of the phases. The difference of the phases is not dependent on the water content. An electrical conductivity is proportional to a water content and ion concentration, thereby, the water content of soil is available according to the measured electrical conductivity, while determining the ion concentration.
    • 当确定含水量时,电导率对含水量有影响。 另一方面,当确定电导率时,含水量对电导率有影响。 因此,即使独立地测量每个特性,每个获得的值包括误差。 将一对电极与土壤接触,向一对电极之一施加交流电流输入电信号,将输出电信号中的另一个的输出电信号的相位与输入电信号的相位进行比较; 并根据相的差异确定溶剂中包含的离子溶质的浓度。 相的差异不取决于含水量。 电导率与含水量和离子浓度成比例,从而根据测得的电导率,确定土壤的含水量,同时确定离子浓度。