Difference between revisions of "Soil moisture Impedance-method (Hydra Probe II)"

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==References==
 
==References==
Blonquist, JM; Jones, SB; Robinson, DA. 2005. Standardizing characterization of electromagnetic water content sensors: Part 2. Evaluation of seven sensing systems. VADOSE ZONE JOURNAL 4 (4): 1059-1069.
+
Blonquist, JM; Jones, SB; Robinson, DA. 2005. Standardizing characterization of electromagnetic water content sensors: Part 2. Evaluation of seven sensing systems. VADOSE ZONE JOURNAL 4(4), 1059-1069.
  
Seyfried, MS; Murdock, MD. 2004. Measurement of soil water content with a 50-MHz soil dielectric sensor. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL 68 (2): 394-403.
+
Seyfried, MS; Murdock, MD. 2004. Measurement of soil water content with a 50-MHz soil dielectric sensor. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL 68(2), 394-403.
  
 
[[Category:Equipment]]
 
[[Category:Equipment]]
 
[[Category: Soil Moisture]]
 
[[Category: Soil Moisture]]

Revision as of 12:31, 18 December 2008

Hydra probe.jpg

Parameter to be measured:

Soil moisture

Method:

Impedance-method

Equipment:

  • Stevens: Hydra Probe II

Advantages:

  • easy and fast measurement of punctual soil moisture
  • manual as well as continuously logged measurements possible

Disadvantages:

  • Each sensor has to be calibrated
  • careful application of probe in stony soils
  • Underestimating of permittivity in media with low permitivity (ε > 40, clay and organic soils)

What to watch out for:

  • Good contact between probe and medium has to be prooved

Problems/Questions:

Links

Other related web sites:

References

Blonquist, JM; Jones, SB; Robinson, DA. 2005. Standardizing characterization of electromagnetic water content sensors: Part 2. Evaluation of seven sensing systems. VADOSE ZONE JOURNAL 4(4), 1059-1069.

Seyfried, MS; Murdock, MD. 2004. Measurement of soil water content with a 50-MHz soil dielectric sensor. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL 68(2), 394-403.