IMPROVED CALIBRATION OF TIME-DOMAIN REFLECTOMETRY SOIL-WATER CONTENT MEASUREMENTS

被引:263
作者
DIRKSEN, C [1 ]
DASBERG, S [1 ]
机构
[1] ARO,VOLCANI CTR,INST SOILS & WATER,BET DAGAN,ISRAEL
关键词
D O I
10.2136/sssaj1993.03615995005700030005x
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Time domain reflectometry (TDR) is becoming a widely used method to determine volumetric soil water content, theta, from measured effective relative dielectric constant (permittivity), epsilon, using the empirical theta(epsilon) Topp-Davis-Annan calibration equation. This equation is not adequate for all soils. The purpose of this study was to compare the Topp calibration equation with a theoretical (Maxwell-De Loor) and an empiricial (fitting exponent alpha) mixing model for the four components: solid phase (s), tightly bound water (bw), free water, and air. Water content permittivity were measured, gravimetrically and by TDR, on packed columns of 11 soils ranging from loess to pure bentonite. Measured specific surfaces were S = 25 to 665 m2 g-1 and bulk densities rho(b) = 0.55 to 1.65 g cm-3. Topp yielded accurate epsilon(theta) values only for the four soils with rho(b) > 1.30 g cm-3, including illite (S = 147 m2 g-1). Maxwell-De Loor gave similar accuracy for seven soils, including attapulgite (S = 270 m2 g-1, rho(b) = 0.55 g cm-3), assuming a monomolecular tightly bound water layer (thickness delta = 3 x 10(-10) m; theta(bw) = delta rho(b)S), epsilon(bw) = 3.2, and epsilon(s) = 5.0. The epsilon(theta) curve of these soils had the same shape as Topp. Two gibbsite soils with dissimilar curves required epsilon(bw) = 3.2 and epsilon(s) = 16 to 18, and two smectite soil materials required epsilon(bw) = 30 to 50 and epsilon(s) = 5.0, to obtain good fits. Deviations from Topp appear generally due more to the lower rho(b) and thus higher air volume fraction at the same theta associated with fine-textured soils than to tightly bound water with low epsilon. Both effects, as well as apparent anomalous behavior such as decreasing effective epsilon with increasing epsilon(s), can be accomodated by the Maxwell-De Loor equation. This makes it a better calibration equation than Topp. The empirical a model is sensitive to the unpredictable value of a and cannot accomodate anomalous behavior.
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页码:660 / 667
页数:8
相关论文
共 26 条
[11]   TIME DOMAIN REFLECTOMETRY CALIBRATION FOR UNIFORMLY AND NONUNIFORMLY WETTED SANDY AND CLAYEY LOAM SOILS [J].
DASBERG, S ;
HOPMANS, JW .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1992, 56 (05) :1341-1345
[12]  
DELOOR GP, 1964, APPL SCI RES B, V3, P479, DOI DOI 10.1007/BF02919923
[13]  
DELOOR GP, 1990, BCRS9013 TNO PHYS EL
[14]  
DIRSKEN C, 1992, AGRONOMY ABSTRACTS, P214
[15]   MICROWAVE DIELECTRIC BEHAVIOR OF WET SOIL .2. DIELECTRIC MIXING MODELS [J].
DOBSON, MC ;
ULABY, FT ;
HALLIKAINEN, MT ;
ELRAYES, MA .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1985, 23 (01) :35-46
[16]   ELECTRICAL DOUBLE-LAYER THEORY .2. POISSON-BOLTZMANN EQUATION INCLUDING HYDRATION FORCES [J].
GUR, Y ;
RAVINA, I ;
BABCHIN, AJ .
JOURNAL OF COLLOID AND INTERFACE SCIENCE, 1978, 64 (02) :333-341
[17]   A COMPUTER-CONTROLLED 36-CHANNEL TIME DOMAIN REFLECTOMETRY SYSTEM FOR MONITORING SOIL-WATER CONTENTS [J].
HEIMOVAARA, TJ ;
BOUTEN, W .
WATER RESOURCES RESEARCH, 1990, 26 (10) :2311-2316
[18]   AUTOMATIC, REAL-TIME MONITORING OF SOIL-MOISTURE IN A REMOTE FIELD AREA WITH TIME DOMAIN REFLECTOMETRY [J].
HERKELRATH, WN ;
HAMBURG, SP ;
MURPHY, F .
WATER RESOURCES RESEARCH, 1991, 27 (05) :857-864
[19]  
ISRAELACHVILI JN, 1984, J COLLOID INTERF SCI, V98, P500
[20]   EMPIRICAL-EVALUATION OF THE RELATIONSHIP BETWEEN SOIL DIELECTRIC-CONSTANT AND VOLUMETRIC WATER-CONTENT AS THE BASIS FOR CALIBRATING SOIL-MOISTURE MEASUREMENTS BY TDR [J].
ROTH, CH ;
MALICKI, MA ;
PLAGGE, R .
JOURNAL OF SOIL SCIENCE, 1992, 43 (01) :1-13