The Effect of Lithology and Agriculture at the Susquehanna Shale Hills Critical Zone Observatory

The footprint of the Susquehanna Shale Hills Critical Zone Observatory was expanded in 2013 from the forested Shale Hills subcatchment (0.08 km) to most of Shavers Creek watershed (163 km) in an effort to understand the interactions among water, energy, gas, solute, and sediment. The main stem of Sh...

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Main Authors: Li Li, Roman A. DiBiase, Joanmarie Del Vecchio, Virginia Marcon, Beth Hoagland, Dacheng Xiao, Callum Wayman, Qicheng Tang, Yuting He, Perri Silverhart, Ismaiel Szink, Brandon Forsythe, Jennifer Z. Williams, Dan Shapich, Gregory J. Mount, Jason Kaye, Li Guo, Henry Lin, David Eissenstat, Ashlee Dere, Kristen Brubaker, Margot Kaye, Kenneth J. Davis, Tess Russo, Susan L. Brantley
Format: Article
Language:English
Published: Wiley 2018-10-01
Series:Vadose Zone Journal
Online Access:https://dl.sciencesocieties.org/publications/vzj/articles/17/1/180063
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spelling doaj-75d07f251f254ca9b5dc6777b8519e472020-11-25T03:29:38ZengWileyVadose Zone Journal1539-16632018-10-0117110.2136/vzj2018.03.0063The Effect of Lithology and Agriculture at the Susquehanna Shale Hills Critical Zone ObservatoryLi LiRoman A. DiBiaseJoanmarie Del VecchioVirginia MarconBeth HoaglandDacheng XiaoCallum WaymanQicheng TangYuting HePerri SilverhartIsmaiel SzinkBrandon ForsytheJennifer Z. WilliamsDan ShapichGregory J. MountJason KayeLi GuoHenry LinDavid EissenstatAshlee DereKristen BrubakerMargot KayeKenneth J. DavisTess RussoSusan L. BrantleyThe footprint of the Susquehanna Shale Hills Critical Zone Observatory was expanded in 2013 from the forested Shale Hills subcatchment (0.08 km) to most of Shavers Creek watershed (163 km) in an effort to understand the interactions among water, energy, gas, solute, and sediment. The main stem of Shavers Creek is now monitored, and instrumentation has been installed in two new subcatchments: Garner Run and Cole Farm. Garner Run is a pristine forested site underlain by sandstone, whereas Cole Farm is a cultivated site on calcareous shale. We describe preliminary data and insights about how the critical zone has evolved on sites of different lithology, vegetation, and land use. A notable conceptual model that has emerged is the “two water table” concept. Despite differences in critical zone architecture, we found evidence in each catchment of a shallow and a deep water table, with the former defined by shallow interflow and the latter defined by deeper groundwater flow through weathered and fractured bedrock. We show that the shallow and deep waters have distinct chemical signatures. The proportion of contribution from each water type to stream discharge plays a key role in determining how concentrations, including nutrients, vary as a function of stream discharge. This illustrates the benefits of the critical zone observatory approach: having common sites to grapple with cross-disciplinary research questions, to integrate diverse datasets, and to support model development that ultimately enables the development of powerful conceptual and numerical frameworks for large-scale hindcasting and forecasting capabilities.https://dl.sciencesocieties.org/publications/vzj/articles/17/1/180063
collection DOAJ
language English
format Article
sources DOAJ
author Li Li
Roman A. DiBiase
Joanmarie Del Vecchio
Virginia Marcon
Beth Hoagland
Dacheng Xiao
Callum Wayman
Qicheng Tang
Yuting He
Perri Silverhart
Ismaiel Szink
Brandon Forsythe
Jennifer Z. Williams
Dan Shapich
Gregory J. Mount
Jason Kaye
Li Guo
Henry Lin
David Eissenstat
Ashlee Dere
Kristen Brubaker
Margot Kaye
Kenneth J. Davis
Tess Russo
Susan L. Brantley
spellingShingle Li Li
Roman A. DiBiase
Joanmarie Del Vecchio
Virginia Marcon
Beth Hoagland
Dacheng Xiao
Callum Wayman
Qicheng Tang
Yuting He
Perri Silverhart
Ismaiel Szink
Brandon Forsythe
Jennifer Z. Williams
Dan Shapich
Gregory J. Mount
Jason Kaye
Li Guo
Henry Lin
David Eissenstat
Ashlee Dere
Kristen Brubaker
Margot Kaye
Kenneth J. Davis
Tess Russo
Susan L. Brantley
The Effect of Lithology and Agriculture at the Susquehanna Shale Hills Critical Zone Observatory
Vadose Zone Journal
author_facet Li Li
Roman A. DiBiase
Joanmarie Del Vecchio
Virginia Marcon
Beth Hoagland
Dacheng Xiao
Callum Wayman
Qicheng Tang
Yuting He
Perri Silverhart
Ismaiel Szink
Brandon Forsythe
Jennifer Z. Williams
Dan Shapich
Gregory J. Mount
Jason Kaye
Li Guo
Henry Lin
David Eissenstat
Ashlee Dere
Kristen Brubaker
Margot Kaye
Kenneth J. Davis
Tess Russo
Susan L. Brantley
author_sort Li Li
title The Effect of Lithology and Agriculture at the Susquehanna Shale Hills Critical Zone Observatory
title_short The Effect of Lithology and Agriculture at the Susquehanna Shale Hills Critical Zone Observatory
title_full The Effect of Lithology and Agriculture at the Susquehanna Shale Hills Critical Zone Observatory
title_fullStr The Effect of Lithology and Agriculture at the Susquehanna Shale Hills Critical Zone Observatory
title_full_unstemmed The Effect of Lithology and Agriculture at the Susquehanna Shale Hills Critical Zone Observatory
title_sort effect of lithology and agriculture at the susquehanna shale hills critical zone observatory
publisher Wiley
series Vadose Zone Journal
issn 1539-1663
publishDate 2018-10-01
description The footprint of the Susquehanna Shale Hills Critical Zone Observatory was expanded in 2013 from the forested Shale Hills subcatchment (0.08 km) to most of Shavers Creek watershed (163 km) in an effort to understand the interactions among water, energy, gas, solute, and sediment. The main stem of Shavers Creek is now monitored, and instrumentation has been installed in two new subcatchments: Garner Run and Cole Farm. Garner Run is a pristine forested site underlain by sandstone, whereas Cole Farm is a cultivated site on calcareous shale. We describe preliminary data and insights about how the critical zone has evolved on sites of different lithology, vegetation, and land use. A notable conceptual model that has emerged is the “two water table” concept. Despite differences in critical zone architecture, we found evidence in each catchment of a shallow and a deep water table, with the former defined by shallow interflow and the latter defined by deeper groundwater flow through weathered and fractured bedrock. We show that the shallow and deep waters have distinct chemical signatures. The proportion of contribution from each water type to stream discharge plays a key role in determining how concentrations, including nutrients, vary as a function of stream discharge. This illustrates the benefits of the critical zone observatory approach: having common sites to grapple with cross-disciplinary research questions, to integrate diverse datasets, and to support model development that ultimately enables the development of powerful conceptual and numerical frameworks for large-scale hindcasting and forecasting capabilities.
url https://dl.sciencesocieties.org/publications/vzj/articles/17/1/180063
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