Brantley, S., Jin, L., Andrews, D., Holmes, G., Holleran, M., Williams, J., Herndon, E., Sullivan, P. 2013. Susquehanna Shale Hills Critical Zone Observatory Porewater Chemistry (2008), Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.1594/IEDA/100235.
Susquehanna Shale Hills Critical Zone Observatory Porewater Chemistry (2008)
Soil water chemistry collected from nested-suction lysimeters (Soil water samplers, 1900 series, SoilMoisture Equipment Corp., Santa Barbara, CA) along a South (S) Planar (P) and South (S) Swale (S) hillsope transect in the Susquehanna Shale Hills Critical Zone Observatory in 2008. Lysimeter nests were located at three different positions along the hillslope elevational gradient; with the most elevated site located at the Ridge Top (RT) followed by the Mid Slope (MS) and lowest site at the Valley Floor (VF). As the lysimeters were installed to the depth of augering refusal, first lysimeters were installed at a depth 10 cm with subsequent lysimeters installed every 10 cm.
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Susquehanna Shale Hills, Pennsylvania
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, doi:10.2136/vzj2010.0133.
Andrews, D.M., H. Lin, Q. Zhu, L. Jin, S.L. Brantley. "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, doi:10.2136/vzj2010.0149.
User Contributed Keyword(s):
oil water geochemistry, major ions, DOC, trace elements, catchment, hillslope, ridge top, valley floor
National Science Foundation: 0725019
Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC BY-NC-SA 3.0]