Estimating soil water content using site-specific calibration of capacitance measurements from sentek EnviroSCAN systems

被引:0
|
作者
Jabro, JD
Leib, BG
Jabro, AD
机构
[1] USDA ARS, No Plains Agr Res Lab, Sidney, MT 59270 USA
[2] Univ Tennessee, Dept Biosyst Engn & Environm Sci, Knoxville, TN USA
[3] Robert Morris Univ, Moon Township, PA USA
关键词
soil; sensor water content; capacitance; irrigation; calibration;
D O I
暂无
中图分类号
S2 [农业工程];
学科分类号
0828 ;
摘要
Newly developed sensors, including the EnviroSCAN capacitance system have the potential to monitor and estimate soil moisture content continuously at various depths. A simple site calibration of the sensors is required to obtain accurate soil water content because these sensors are shipped with a default (uncalibrated) equation to the user Therefore, our research objectives were: 1) to calibrate the EnviroSCAN capacitance system versus soil moisture values estimated by a neutron probe calibrated with gravimetrically measured water contents, then 2) statistically compare the calibrated soil water content results with those estimated by the uncalibrated equation using three years of field data. Both the EnviroSCAN capacitance and the neutron probe were installed in a Warden silt loam soil planted to alfalfa. The average water contents of the soil profile estimated by the EnviroSCAN capacitance was used to develop a site specific calibration equation by comparing the sensors' scaled frequencies for 1998 with the soil water content of the neutron probe. The site calibration equation was then statistically validated using both 1999 and 2000 soil water contents. The statistical analyses indicated that discrepancies existed between soil water contents of the site calibration equation and those estimated by the uncalibrated equation. For instance, the RRMSE values of soil water content produced from the calibrated equation were 7%, 41%, and 40%, compared with uncalibrated RRMSE values of 68%, 59%, and 66%, for 1998, 1999, and 2000, respectively. These results support that the site calibration equation was found to give more accurate estimates of individual values (low RRMSE) of volumetric soil water content compared to those obtained from the uncalibrated equation.
引用
收藏
页码:393 / 399
页数:7
相关论文
共 4 条
  • [1] Field measurements of the water content in the top soil using a new capacitance sensor with a flat sensitive volume
    Ruth, B
    Munch, JC
    JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, 2005, 168 (02) : 169 - 175
  • [2] Accurate Measurements of Forest Soil Water Content Using FDR Sensors Require Empirical In Situ (Re)Calibration
    De Vos, Bruno
    Cools, Nathalie
    Verstraeten, Arne
    Neirynck, Johan
    APPLIED SCIENCES-BASEL, 2021, 11 (24):
  • [3] Laboratory Calibration and Field Validation of Soil Water Content and Salinity Measurements Using the 5TE Sensor
    Zemni, Nessrine
    Bouksila, Fethi
    Persson, Magnus
    Slama, Fairouz
    Berndtsson, Ronny
    Bouhlila, Rachida
    SENSORS, 2019, 19 (23)
  • [4] Feasibility analysis of using inverse modeling for estimating field-scale evapotranspiration in maize and soybean fields from soil water content monitoring networks
    Foolad, Foad
    Franz, Trenton E.
    Wang, Tiejun
    Gibson, Justin
    Kilic, Ayse
    Allen, Richard G.
    Suyker, Andrew
    HYDROLOGY AND EARTH SYSTEM SCIENCES, 2017, 21 (02) : 1263 - 1277