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Published online 16 November 2005
Published in Vadose Zone J 4:1011-1019 (2005)
DOI: 10.2136/vzj2004.0108
© 2005 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Time Domain Reflectometry Range of Accuracy for High Surface Area Soils

Sally Logsdon*

National Soil Tilth Laboratory, 2150 Pammel Dr., Ames, IA 50011


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Fig. 1. Specific surface area for the different depths of Sites 1, 2, 3, and 4.

 


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Fig. 2. Comparison of bulk densities for field sites and corresponding repacked laboratory calibration.

 


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Fig. 3. Laboratory waveforms for (a) Site 3, 43-cm depth, 0.326 m3 m–3 and for (b) Site 4, 96-cm depth, 0.379 m3 m–3.

 


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Fig. 4. Field data for Site 3, 35-cm depth, 1996 season, showing good quality TDR data.

 


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Fig. 5. Field data for Site 1, 58-cm depth, 1996 season, showing noisy TDR data.

 


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Fig. 6. Fairly good agreements between laboratory and field raw data for (a) Site 3, 35-cm depth, but field data were offset to higher values for (b) Site 4, 35-cm depth. The laboratory excludes data points with incorrect internal waveform analysis, and only the good field data were included in the calibration.

 


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Fig. 7. Comparison of measured and calculated water content for laboratory data showing each site-depth regression (overlapping) without and with a temperature correction, and compared with Topp's (1980) equation.

 


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Fig. 8. Comparison of measured and calculated water content for field data showing each site–depth regression (overlapping) without and with a temperature correction, and compared with Topp's (1980) equation.

 


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Fig. 9. Calculated water content from TDR, with and without a temperature term, and water content from neutron probe for 1996, Site 3, 35-cm depth.

 


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Fig. 10. Calculated water content from TDR, with and without a temperature term, and water content from neutron probe for 1996, Site 1, 58-cm depth.

 


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Fig. 11. Calculated water content from TDR, with and without a temperature term, and water content from neutron probe for 1997, Site 1, 58-cm depth.

 





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