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Title	Susquehanna Shale Hills CZO - Imaginary Time Imaginary Dialetric Constant Data
Date	2012
Abstract	The Real-Time Soil Moisture Monitoring Network provides integrated observation of water, energy and temperature in the soils of the Shale Hills Susquehanna Critical Zone Observatory watershed. Dialetric Constant is measured at 4 depths at 2 sites. Imaginary Dialetric Constant is measured with HydraProbes manufactured by Stevens Instruments.
Metadata	Click here for full metadata
Data DOI	doi:10.26208/61XM-1W08

Researchers

Lin, H. S. Penn State Ecosystem Science Management

Lin, H. S.
Penn State Ecosystem Science Management

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Additional Information

http://www.czo.psu.edu/

http://www.czo.psu.edu/

References

Graham, C., and H.S. Lin. 2011. Controls and frequency of preferential flow occurrence at the Shale Hills Critical Zone Observatory: A 175 event analysis of soil moisture response to precipitation. Vadose Zone Journal. 10:3, 816-831. https://doi.org/10.2136/vzj2010.0119
Takagi, K. and H.S. Lin. (2011): Temporal Dynamics of Soil Moisture Spatial Variability in the Shale Hills Critical Zone Observatory. Vadose Zone Journal 10:832-842. https://doi.org/10.2136/vzj2010.0134
Takagi, K. and H.S. Lin. (2012). Changing controls of soil moisture spatial organization in the Shale Hills Catchment. Geoderma.173-174: 489-302. https://doi.org/10.1016/j.geoderma.2011.11.003
Andrews, D.M., H. Lin, Q. Zhu, L. Jin, S.L. Brantley. (2011): Hot Spots and Hot Moments of Dissolved Organic Carbon Export and Soil Organic Carbon Storage in the Shale Hills Critical Zone Observatory. Vadose Zone Journal 10:943-954. https://doi.org/10.2136/vzj2010.0149
Jin, L., Andrews, D.M., Holmes, G.H., Lin, H., and Brantley, S.L. (2011): Opening the "Black Box": Water Chemistry Reveals Hydrological Controls on Weathering in the Susquehanna Shale Hills Critical Zone Observatory. Vadose Zone Journal 10:928-942. https://doi.org/10.2136/vzj2010.0133
Zhang, J. H.S. Lin, and J. Doolittle. 2011. Subsurface Lateral Flow as Revealed by Combined Ground Penetrating Radar and Real-Time Soil Moisture Monitoring. Submitted to Hydrological Processes.
Zhu, Q., and Lin, H.S. (2010): Comparing Ordinary Kriging and Regression Kriging for Soil Properties in Contrasting Landscapes. Pedosphere 20:594-606. https://doi.org/10.1016/S1002-0160(10)60049-5
Lin, H.S., and Zhou, X. (2008): Evidence of Subsurface Preferential Flow Using Soil Hydrologic Monitoring in the Shale Hills Catchment . European Journal of Soil Science 59:34–49. https://doi.org/10.1111/j.1365-2389.2007.00988.x
Lin, H.S. (2006): Temporal stability of soil moisture spatial pattern and subsurface preferential flow pathways in the Shale Hills Catchment. Vadose Zone Journal 5:317-340. https://doi.org/10.2136/vzj2005.0058
Lin, H.S., Kogelmann, W., Walker, C., and Bruns, M.A. (2006): Soil moisture patterns in a forested catchment: A hydropedological perspective. Geoderma 131:345-368. https://doi.org/10.1016/j.geoderma.2005.03.013

Graham, C., and H.S. Lin. 2011. Controls and frequency of preferential flow occurrence at the Shale Hills Critical Zone Observatory: A 175 event analysis of soil moisture response to precipitation. Vadose Zone Journal. 10:3, 816-831. https://doi.org/10.2136/vzj2010.0119

Takagi, K. and H.S. Lin. (2011): Temporal Dynamics of Soil Moisture Spatial Variability in the Shale Hills Critical Zone Observatory. Vadose Zone Journal 10:832-842. https://doi.org/10.2136/vzj2010.0134

Takagi, K. and H.S. Lin. (2012). Changing controls of soil moisture spatial organization in the Shale Hills Catchment. Geoderma.173-174: 489-302. https://doi.org/10.1016/j.geoderma.2011.11.003

Andrews, D.M., H. Lin, Q. Zhu, L. Jin, S.L. Brantley. (2011): Hot Spots and Hot Moments of Dissolved Organic Carbon Export and Soil Organic Carbon Storage in the Shale Hills Critical Zone Observatory. Vadose Zone Journal 10:943-954. https://doi.org/10.2136/vzj2010.0149

Jin, L., Andrews, D.M., Holmes, G.H., Lin, H., and Brantley, S.L. (2011): Opening the "Black Box": Water Chemistry Reveals Hydrological Controls on Weathering in the Susquehanna Shale Hills Critical Zone Observatory. Vadose Zone Journal 10:928-942. https://doi.org/10.2136/vzj2010.0133

Zhang, J. H.S. Lin, and J. Doolittle. 2011. Subsurface Lateral Flow as Revealed by Combined Ground Penetrating Radar and Real-Time Soil Moisture Monitoring. Submitted to Hydrological Processes.

Zhu, Q., and Lin, H.S. (2010): Comparing Ordinary Kriging and Regression Kriging for Soil Properties in Contrasting Landscapes. Pedosphere 20:594-606. https://doi.org/10.1016/S1002-0160(10)60049-5

Lin, H.S., and Zhou, X. (2008): Evidence of Subsurface Preferential Flow Using Soil Hydrologic Monitoring in the Shale Hills Catchment . European Journal of Soil Science 59:34–49. https://doi.org/10.1111/j.1365-2389.2007.00988.x

Lin, H.S. (2006): Temporal stability of soil moisture spatial pattern and subsurface preferential flow pathways in the Shale Hills Catchment. Vadose Zone Journal 5:317-340. https://doi.org/10.2136/vzj2005.0058

Lin, H.S., Kogelmann, W., Walker, C., and Bruns, M.A. (2006): Soil moisture patterns in a forested catchment: A hydropedological perspective. Geoderma 131:345-368. https://doi.org/10.1016/j.geoderma.2005.03.013

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