In‐situ probe spacing calibration improves the heat pulse method for measuring soil heat capacity and water content
In‐situ probe spacing calibration improves the heat pulse method for measuring soil heat capacity and water content
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DOI:
10.1002/saj2.20124
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发表时间:
2020-09
影响因子:
2.9
通讯作者:
Meng Zhang;Yili Lu;T. Ren;R. Horton
中科院分区:
文献类型:
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作者:
Meng Zhang;Yili Lu;T. Ren;R. Horton
Heat pulse (HP) sensors have been used extensively to measure soil thermal properties and volumetric water content (θ) simultaneously. Probe spacing (R), the distance between heater probe and temperature probe, is routinely calibrated in agar solution before making HP measurements. In reality,Rmay change due to probe deflection at insertion into soil, causing uncertainties in HP measured volumetric heat capacity (C) and θ. In this paper, we present a simple on‐site calibration method for determining in‐situRby using theoreticalCvalues estimated from soil bulk density and θ values of intact soil cores collected near the sensor locations at the end of experiment. The proposed approach was tested on two field soils whereCand θ were monitored continuously. Inconsistent results were observed between agar‐calibratedRvalues (Ragar) andRvalues obtained from in‐situ calibration (Rin‐situ). Maximum difference betweenRagarandRin‐situreached 20% ofRagar. Compared to TDR measured θ, usingRagarled to root mean square errors (RMSEs) of 0.26 MJ m−3K−1inCand 0.06 m3m−3in θ on average. ForRin‐situ, the RMSE ofCwas less than 0.16 MJ m−3K−1and RMSE of θ was within 0.04 m3m−3. Thus, the use of in‐situ probe spacing calibration improved the accuracies of HP measuredCand θ.