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Measurement of soil water content in a hyper-arid environment using time-domain reflectometry sensors
Time‐domain reflectometry (TDR) sensors have been widely used in many fields for measurement of soil water content. However, few TDR sensors have been used in a hyper‐arid environment (e.g. less than 0·05 m3 m−3), and such sensor applicability is not yet confirmed. In this study we examine θ − t and...
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Published in: | Hydrological processes 2005-12, Vol.19 (19), p.3911-3920 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Time‐domain reflectometry (TDR) sensors have been widely used in many fields for measurement of soil water content. However, few TDR sensors have been used in a hyper‐arid environment (e.g. less than 0·05 m3 m−3), and such sensor applicability is not yet confirmed. In this study we examine θ − t and θ − εbulk relations and temperature dependency for natural sand and glass beads in a laboratory using commercially available TDR sensors. As a result, this study clarifies that TDR sensors are applicable even in a hyper‐arid environment when calibration was properly made. We also focus on a specific range of soil water content, which leads to a highly precise calibration equation. Copyright © 2005 John Wiley & Sons, Ltd. |
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ISSN: | 0885-6087 1099-1085 |
DOI: | 10.1002/hyp.5989 |