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The effects of soil bulk density, clay content and temperature on soil water content measurement using time‐domain reflectometry
Author(s) -
Gong Yuanshi,
Cao Qiaohong,
Sun Zongjia
Publication year - 2003
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.1358
Subject(s) - water content , loam , soil science , bulk density , reflectometry , soil texture , field capacity , soil water , pedotransfer function , environmental science , water retention curve , materials science , geology , geotechnical engineering , time domain , hydraulic conductivity , computer science , computer vision
Time‐domain reflectometry (TDR) is increasingly used for field soil water estimation because the measurement is non‐destructive and less affected by soil texture, bulk density and temperature. However, with the increase in instrument resolution, the influences of soil bulk density and temperature on TDR soil moisture measurements have been reported. The influence is primarily caused by changes in soil and water dielectric permittivity when soil compaction and temperature varies. The objective of this study is to quantify the influence of soil bulk density and temperature, and to provide the corresponding correction methods. Data collected from sand, sandy loam, loam and clay loam show a linear relationship between the square root of dielectric constant of dry soil and bulk density, and a bulk density correction formula has been developed. The dielectric permittivity of soil solids estimated using this formula is close to that of oxides of aluminium, silicon, magnesium and calcium. Data collection from sandy loam show a noticeable decrease in measured soil moisture with increase in temperature when the volumetric soil water content is above 0·30 m 3 m −3 . A temperature‐correction equation has been developed, which could provide the corrected soil moisture based on soil temperature and TDR‐measured moisture. The effect of clay content has been detected, but it is not statistically significant. High clay contents cause the underestimation of soil water content in the low moisture range and overestimation of soil water content in the high moisture range. Copyright © 2003 John Wiley & Sons, Ltd.