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Title	Susquehanna Shale Hills CZO - Real Time Soil Matric Potential Data - 229
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. Soil Matric Potential is measured at between 3 and 13 depths at 7 sites. Matric potential is measured with 229 probes manufactured by Campbell Scientific.
Metadata	Click here for full metadata
Data DOI	doi:10.26208/ZMHJ-AN07

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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