TY - JOUR
T1 - Relating land surface, water table, and weathering fronts with a conceptual valve model for headwater catchments
AU - Brantley, Susan L.
AU - Lebedeva, Marina I.
N1 - Funding Information:
National Science Foundation, Grant/Award Numbers: EAR13‐31726, EAR12‐39285; U.S. Department of Energy, Grant/Award Number: DOE OBES DE‐FG02‐05ER15675 Funding information
Funding Information:
Funding is acknowledged from DOE OBES DE‐FG02‐05ER15675, and NSF Critical Zone Observatory grants EAR 12‐39285 and 13‐31726 to S.L.B. Work at Shale Hills (Figure 5c,d ) is facilitated by the College of Agricultural Sciences, Pennsylvania State University and Department of Ecosystem Science and Management as part of Penn State's Stone Valley Forest. Conversations with X. Gu and F. Reis and an insightful review by. C. Harman and anonymous reviewers are acknowledged.
Funding Information:
Funding is acknowledged from DOE OBES DE-FG02-05ER15675, and NSF Critical Zone Observatory grants EAR 12-39285 and 13-31726 to S.L.B. Work at Shale Hills (Figure 5c,d) is facilitated by the College of Agricultural Sciences, Pennsylvania State University and Department of Ecosystem Science and Management as part of Penn State's Stone Valley Forest. Conversations with X. Gu and F. Reis and an insightful review by. C. Harman and anonymous reviewers are acknowledged.
Publisher Copyright:
© 2020 John Wiley & Sons Ltd
PY - 2021/2
Y1 - 2021/2
N2 - Knowing little about how porosity and permeability are distributed at depth, we commonly develop models of groundwater by treating the subsurface as a homogeneous black box even though porosity and permeability vary with depth. One reason for this depth variation is that infiltrating meteoric water reacts with minerals to affect porosity in localized zones called reaction fronts. We are beginning to learn to map and model these fronts beneath headwater catchments and show how they are distributed. The subsurface landscapes defined by these fronts lie subparallel to the soil-air interface but with lower relief. They can be situated above, below, or at the water table. These subsurface landscapes of reaction are important because porosity developed from weathering can control subsurface water storage. In addition, porosity often changes at the weathering fronts, and when this affects permeability significantly, the front can act like a valve that re-orients water flowing through the subsurface. We explore controls on the positions of reaction fronts under headwater landscapes by accounting for the timescales of erosion, chemical equilibration, and solute transport. One strong control on the landscape of subsurface reaction is the land surface geometry, which is in turn a function of the erosion rate. In addition, the reaction fronts, like the water table, are strongly affected by the lithology and water infiltration rate. We hypothesize that relationships among the land surface, reaction fronts, and the water table are controlled by feedbacks that can push landscapes towards an ‘ideal hill’. In this steady state, reaction-front valves partition water volumes into shallow and deep flowpaths. These flows dissolve low- and high-solubility minerals, respectively, allowing their reaction fronts to advance at the erosion rate. This conceptualization could inform better models of subsurface porosity and permeability, replacing the black box.
AB - Knowing little about how porosity and permeability are distributed at depth, we commonly develop models of groundwater by treating the subsurface as a homogeneous black box even though porosity and permeability vary with depth. One reason for this depth variation is that infiltrating meteoric water reacts with minerals to affect porosity in localized zones called reaction fronts. We are beginning to learn to map and model these fronts beneath headwater catchments and show how they are distributed. The subsurface landscapes defined by these fronts lie subparallel to the soil-air interface but with lower relief. They can be situated above, below, or at the water table. These subsurface landscapes of reaction are important because porosity developed from weathering can control subsurface water storage. In addition, porosity often changes at the weathering fronts, and when this affects permeability significantly, the front can act like a valve that re-orients water flowing through the subsurface. We explore controls on the positions of reaction fronts under headwater landscapes by accounting for the timescales of erosion, chemical equilibration, and solute transport. One strong control on the landscape of subsurface reaction is the land surface geometry, which is in turn a function of the erosion rate. In addition, the reaction fronts, like the water table, are strongly affected by the lithology and water infiltration rate. We hypothesize that relationships among the land surface, reaction fronts, and the water table are controlled by feedbacks that can push landscapes towards an ‘ideal hill’. In this steady state, reaction-front valves partition water volumes into shallow and deep flowpaths. These flows dissolve low- and high-solubility minerals, respectively, allowing their reaction fronts to advance at the erosion rate. This conceptualization could inform better models of subsurface porosity and permeability, replacing the black box.
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U2 - 10.1002/hyp.14010
DO - 10.1002/hyp.14010
M3 - Article
AN - SCOPUS:85098129848
SN - 0885-6087
VL - 35
JO - Hydrological Processes
JF - Hydrological Processes
IS - 2
M1 - e14010
ER -