基于FDR原理的凍土測量方法
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中國氣象局河南省農業氣象保障與應用技術重點實驗室開放研究基金項目(AMF201603)、河南省氣象局項目(KM201715、KM201815)、公益性行業(氣象)科研專項(GYHY201106042)資助


A Method for Measuring Frozen Soil Based on Frequency Domain Reflectometry Principle
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    摘要:

    在我國地面氣象觀測中,凍土的自動觀測一直未能實現,為了解決這一問題,本文基于頻域反射(Frequency Domain Reflectometry,FDR)測量原理,通過測量土壤介電常數變化實現凍土測量的方法,設計了一種基于平面電容傳感器分層檢測凍土的傳感器,土壤凍結時,其內部水分會相變為冰,水的介電常數遠大于冰,利用水凍結相變后引起介電常數急劇變化的特性,建立了基于土壤介電常數、地溫反演凍土的數學模型,并進行了典型土壤實驗室凍結試驗及外場對比觀測試驗,結果表明:凍土傳感器能正確分辨土壤凍結狀態,測量數據與人工觀測趨勢一致,相關系數可達099以上,平均測量誤差小于3 cm,基于介電特性的凍土傳感器可以準確連續測量土壤的凍結深度及其生消變化。

    Abstract:

    In meteorological observation projects, the automatic observation of frozen soil has not been realized. In order to solve this problem, this paper presents a method for measuring frozen soil by means of the changes of soil dielectric constant, based on the planar capacitive sensor. When the soil is frozen, the internal moisture will turn into ice, and for the dielectric constant of water is much larger than that of ice, the dielectric constant changes drastically after water freezing (phase transformation). Based on the characteristic of soil dielectric constant and ground temperature, the mathematical model to retrieve frozen soil is established, and a typical soil laboratory freezing test is carried out. The field comparison test results show that the frozen soil sensor can correctly distinguish the soil freezing state; the measured data and manual observation are of the same trend; the correlation coefficient is up over 099; the average measurement error is less than 3 cm. The sensor based on the dielectric characteristics of the frozen soil can accurately and continuously measure the soil freezing depth and various changes.

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陳海波,李鵬,李翠娜,師麗魁,謝婷婷,余國河.基于FDR原理的凍土測量方法[J].氣象科技,2018,46(6):1081~1086

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  • 收稿日期:2017-11-06
  • 定稿日期:2018-09-11
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  • 在線發布日期: 2018-12-27
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