Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...

SSHCZO -- Hydropedologic Properties, Electrical Conductivity -- Shale Hills -- (2009-2013)


Authors:
Owners: This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource.
Type: Resource
Storage: The size of this resource is 167.0 KB
Created: Nov 19, 2019 at 12:06 a.m.
Last updated: Nov 26, 2019 at 7:59 p.m.
Citation: See how to cite this resource
Content types: Single File Content 
Sharing Status: Public
Views: 1789
Downloads: 118
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

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. Electric Conductivity is measured at between 4 and 5 depths at 13 sites. Electric conductivity is measured with HydraProbes manufactured by Stevens Instruments, and by 5TE probes manufactured by Decagon. At 2 sites (15 and 55) electric conductivity is measured with 2 loggers, which have different time stamps.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Susquehanna Shale Hills Critical Zone Observatory, Shale Hills
North Latitude
40.6650°
East Longitude
-77.9047°
South Latitude
40.6640°
West Longitude
-77.9069°

Temporal

Start Date:
End Date:

Content

ReadMe.md

SSHCZO -- Hydropedologic Properties, Electrical Conductivity -- Shale Hills -- (2009-2013)


OVERVIEW

Description/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. Electric Conductivity is measured at between 4 and 5 depths at 13 sites. Electric conductivity is measured with HydraProbes manufactured by Stevens Instruments, and by 5TE probes manufactured by Decagon. At 2 sites (15 and 55) electric conductivity is measured with 2 loggers, which have different time stamps.

Creator/Author

Lin, Henry

CZOs

Shale Hills

Contact

Dr. Henry Lin, Crop and Soil Science, The Pennsylvania State University, 444 Agricultural Sciences and Industries Building, University Park, PA. 814-865-6726 henry.lin@psu.edu

Subtitle

Level 1 - Quality Controlled Data




SUBJECTS

Disciplines

Soil Science / Pedology

Topics

Hydropedologic Properties|Electrical Conductivity

Keywords

soil|water|hydrology|hydropedology|soil science|soil temperature

Variables

Julian Day|Decimal Time of Day|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)

Variables ODM2

Electrical conductivity




TEMPORAL

Date Start

2009-01-01

Date End

2013-12-31




SPATIAL

Field Areas

Susquehanna Shale Hills Critical Zone Observatory

Location

Shale Hills

North latitude

40.6649680616

South latitude

40.6639684182

West longitude

-77.9068646529

East longitude

-77.904664515

alt text



REFERENCE

Citation

The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Shale Hills Susquehanna Critical Zone Observatory.

Publications of this data

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. http://dx.doi.org/10.1016/j.geoderma.2005.03.013

Publications using this data

Graham, C., and Lin, H.S. (2011). Controls and Frequency of Preferential Flow Occurrence: A 175-event Analysis. Vadose Zone Journal 10:816-831 http://dx.doi.org/10.2136/vzj2010.0119

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, http://dx.doi.org/10.2136/vzj2010.0133

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. http://dx.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. http://dx.doi.org/10.2136/vzj2005.0058

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, http://dx.doi.org/10.2136/vzj2010.0134

CZO ID

2602




COMMENTS

Comments

Probe Depths at each site, in cm:

Site A4: 5, 20, 36; Site 3: 10, 20, 30, 40, 50; Site 6: 60, 40, 30, 20, 10; Site 8: 10, 20, 30, 40, 50; Site 11: 11, 36, 66, 11, 24, 36, 51; Site 12: 10, 48, 81, 11, 27, 48, 64; Site 15: 5, 13, 20, 41, 41, 52, 73, 73; Site 55: 5, 8, 14, 14, 30

Additional Metadata

Name Value
czos Shale Hills
czo_id 2602
citation The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Shale Hills Susquehanna Critical Zone Observatory.
comments Probe Depths at each site, in cm: Site A4: 5, 20, 36; Site 3: 10, 20, 30, 40, 50; Site 6: 60, 40, 30, 20, 10; Site 8: 10, 20, 30, 40, 50; Site 11: 11, 36, 66, 11, 24, 36, 51; Site 12: 10, 48, 81, 11, 27, 48, 64; Site 15: 5, 13, 20, 41, 41, 52, 73, 73; Site 55: 5, 8, 14, 14, 30
keywords soil, water, hydrology, hydropedology, soil science, soil temperature
subtitle Level 1 - Quality Controlled Data
variables Julian Day, Decimal Time of Day, Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m)
disciplines Soil Science / Pedology

Related Resources

This resource is referenced by 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. http://dx.doi.org/10.1016/j.geoderma.2005.03.013

How to Cite

Lin, H. (2019). SSHCZO -- Hydropedologic Properties, Electrical Conductivity -- Shale Hills -- (2009-2013), HydroShare, http://www.hydroshare.org/resource/4cefa72017ce4f128de6b7e61efae487

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

Comments

There are currently no comments

New Comment

required