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Acta agriculturae Slovenica, 85 - 2, november 2005 str. 359 – 374
Agrovoc Descriptors: soil, moisture content, soil water content, sensors,
measurement, clay soils, silty soils, sandy soils
Agris Category Codes: P33
COBISS code 1.01
Comparison of laboratory TDR soil water measurements
Vesna ZUPANC
1
, Gregor ADAM
2
, Marina PINTAR
3
Received: 10- 9-2005, accepted 10-10-2005
Delo je prispelo: 10- 9-2005, sprejeto 10-10-2005
ABSTRACT
Reliable soil moisture sensors are essential for agricultural application. Time Domain
Reflectometry (TDR) is a useful method for nondestructive, continuous measurements of soil
water content. Laboratory measurements of soil volumetric water content by the TDR 100
Time Domain Reflectometer were compared to gravimetric measurements in three soils, Clay
Loam, Silt Loam and Sand soil. Comparison between original and homemade 10 cm and 20
cm rods was made. TDR 100 gave good results in Clay Loam and Silt Loam soil and over
estimated VWC in Sand soil. Results showed little or no difference between original and
homemade sensor measurements.
Key words: volumetric water content, soil moisture sensor, TDR
IZVLEČEK
PRIMERJAVA LABORATORIJSKIH MERITEV VODE V TALNEM SUBSTRATU S TDR
Zanesljivi senzorji za merjenje vlage v tleh so v kmetijstvu nujni. Time Domain Reflectometry
(TDR) je metoda, ki omogoča kontinuirano merjenje vlage v tleh brez rušenja talnega profila.
Laboratorijske meritve volumske vsebnosti vode, izvedene s TDR 100 Reflectometrom, smo
primerjali z gravimetrično metodo v glinasto ilovnatih, meljasto ilovnatih ter peščenih tleh.
Primerjali smo meritve narejene z izvirnimi ter doma narejenimi 10 cm in 20 cm sondami.
TDR 100 je pokazal dobre rezultate v glinasto ilovnatih in meljasto ilovnatih tleh, v peščenih
tleh so bile izmerjene vrednosti višje od standarda. Rezultati kažejo malo ali nič razlik med
meritvami, opravljenimi z izvirnimi in doma narejnimi sondami.
Ključne besede: volumska vsebnost vode, senzor za merjenje vlage v tleh, TDR
1 INTRODUCTION
Many plant-soil-water and hydrological investigations depend on accurate
measurement of soil water content. Often undergoing study of the processes requires
continuous measurement. Time Domain Reflectometry (TDR) became known as a
1
Assist., PhD., Biotechnical faculty, Department for Agronomy, Center for agrohydrology
and land reclamation, Jamnikarjeva 101, 1000 Ljubljana, Slovenia vesna.zupanc@bf.uni-
lj.si
2
ADACHEM doo, Ulica generala Levičnika 34i 6000Koper
3
Assist. Prof., PhD., Biotechnical faculty, Department for Agronomy, Center for
agrohydrology and land reclamation, Jamnikarjeva 101, 1000 Ljubljana, Slovenia
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Résumé du contenu

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Acta agriculturae Slovenica, 85 - 2, november 2005 str. 359 – 374 Agrovoc Descriptors: soil, moisture content, soil water content, sensors, measure

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Acta agriculturae Slovenica, 85 - 2, november 2005 368 Comparison of the TDR 100 measurements and gravimetrically determined VWC (Figure 4)

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ZUPANC, V. in sod.: Comparison of laboratory TDR soil water measurements 3690102030405001020304050Gravimetric Method (Vol %)Sensor Measurements (V

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Acta agriculturae Slovenica, 85 - 2, november 2005 370 010203040500 1020304050Gravimetric Method (Vol %)Sensor Measurements (Vol %)TDR 100 20b Figure

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ZUPANC, V. in sod.: Comparison of laboratory TDR soil water measurements 3710102030405001020304050Gravimetric Method (Vol %)Sensor Measurements (V

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Acta agriculturae Slovenica, 85 - 2, november 2005 372 0102030405001020304050Gravimetric Method (Vol %)Sensor Measurements (Vol %)TDR 100 20a Figure

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ZUPANC, V. in sod.: Comparison of laboratory TDR soil water measurements 3734 CONCLUSIONS TDR 100 Reflectometer measurements were compared to g

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Acta agriculturae Slovenica, 85 - 2, november 2005 374 Topp, G.C, Davis, J.L. and Annan, A.P. 1980. Electromagnetic determination of soil water cont

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Acta agriculturae Slovenica, 85 - 2, november 2005 360 useful method for nondestructive, continuous measurements of soil water content and bulk elec

Page 10 - Sensor Measurements (Vol %)

ZUPANC, V. in sod.: Comparison of laboratory TDR soil water measurements 361 Figure 1: Scheme of TDR 100 experiment set, connections of PC with TD

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Acta agriculturae Slovenica, 85 - 2, november 2005 362 buried at any orientation to the surface (Campbell Scientific, 2004). The measureme

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ZUPANC, V. in sod.: Comparison of laboratory TDR soil water measurements 363Table 1: Measurements of soil VWC TDR 100 Time Domain Reflectometer fo

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Acta agriculturae Slovenica, 85 - 2, november 2005 364 Table 2: Measurements of soil VWC TDR 100 Time Domain Reflectometer for four different soil

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ZUPANC, V. in sod.: Comparison of laboratory TDR soil water measurements 365Table 3: Measurements of soil VWC TDR 100 Time Domain Reflectometer fo

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Acta agriculturae Slovenica, 85 - 2, november 2005 366 0102030405001020304050Gravimetric Method (Vol %)Sensor Measurements (Vol %)TDR 100 10a Figure

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ZUPANC, V. in sod.: Comparison of laboratory TDR soil water measurements 3670102030405001020304050Gravimetric Method (Vol %)Sensor Measurements (V

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