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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2018-10-01
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Series: | Vadose Zone Journal |
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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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