Abstract
The Cordillera Blanca in Northwestern Peru is home to a quarter of the world's tropical glaciers, where hydrologic regimes are rapidly changing due to warming- induced glacier recession. Proglacial alpine meadows are storing a significant portion of annual basin discharge, and buffer dry season low flows as glaciers continue to lose their influence on the regional hydrologic cycle. We used integrated seismic (refraction, H/V passive seismic) and electrical (2D ERT and 1D soundings) in conjunction with borehole data to characterize the nature of proglacial talus aquifers in alpine meadows at elevations above 3500 masl. The meadow subsurface exhibits a transition from relatively slow (400-800 m/s) to fast (~2500 m/s) seismic p-wave velocity at depths of 4 to 8m, coinciding with the top of a composite layer of buried talus boulders, according to borehole data. Artesian pressure head in piezometers screened at the boulders indicate the presence of an aquifer confined by clay sediments. Resistivity profiles suggest that the upper most portions of the buried talus deposit are infilled with saturated clay, which dissipates with depth where sediments become more electrically resistive. Passive seismic and 1D electrical soundings suggest that total sediment thickness extends deeper than 20 m, allowing for first estimates of talus aquifer storage volumes and groundwater residence times. Based on the results from this study, we present a refined conceptual model of talus aquifers, from their formation to hydrologic function. Throughout the Cordillera Blanca, buried talus aquifers have the potential to store between 7 and 20% of annual basin discharge, which will allow for future predictions of dry season base flow for the region's principal river.
| Original language | English (US) |
|---|---|
| Title of host publication | 24th European Meeting of Environmental and Engineering Geophysics |
| Publisher | European Association of Geoscientists and Engineers, EAGE |
| ISBN (Electronic) | 9789462822634 |
| DOIs | |
| State | Published - Jan 1 2019 |
| Event | 24th European Meeting of Environmental and Engineering Geophysics - Porto, Portugal Duration: Sep 9 2018 → Sep 13 2018 |
Other
| Other | 24th European Meeting of Environmental and Engineering Geophysics |
|---|---|
| Country | Portugal |
| City | Porto |
| Period | 9/9/18 → 9/13/18 |
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ASJC Scopus subject areas
- Geotechnical Engineering and Engineering Geology
- Geochemistry and Petrology
- Energy Engineering and Power Technology
Cite this
Integrating multiple geophysical methods to understand groundwater storage and discharge in tropical proglacial catchments. / Glas, R.; Lautz, Laura K; McKenzie, J.; Moucha, Robert; Mark, B.
24th European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists and Engineers, EAGE, 2019.Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Integrating multiple geophysical methods to understand groundwater storage and discharge in tropical proglacial catchments
AU - Glas, R.
AU - Lautz, Laura K
AU - McKenzie, J.
AU - Moucha, Robert
AU - Mark, B.
PY - 2019/1/1
Y1 - 2019/1/1
N2 - The Cordillera Blanca in Northwestern Peru is home to a quarter of the world's tropical glaciers, where hydrologic regimes are rapidly changing due to warming- induced glacier recession. Proglacial alpine meadows are storing a significant portion of annual basin discharge, and buffer dry season low flows as glaciers continue to lose their influence on the regional hydrologic cycle. We used integrated seismic (refraction, H/V passive seismic) and electrical (2D ERT and 1D soundings) in conjunction with borehole data to characterize the nature of proglacial talus aquifers in alpine meadows at elevations above 3500 masl. The meadow subsurface exhibits a transition from relatively slow (400-800 m/s) to fast (~2500 m/s) seismic p-wave velocity at depths of 4 to 8m, coinciding with the top of a composite layer of buried talus boulders, according to borehole data. Artesian pressure head in piezometers screened at the boulders indicate the presence of an aquifer confined by clay sediments. Resistivity profiles suggest that the upper most portions of the buried talus deposit are infilled with saturated clay, which dissipates with depth where sediments become more electrically resistive. Passive seismic and 1D electrical soundings suggest that total sediment thickness extends deeper than 20 m, allowing for first estimates of talus aquifer storage volumes and groundwater residence times. Based on the results from this study, we present a refined conceptual model of talus aquifers, from their formation to hydrologic function. Throughout the Cordillera Blanca, buried talus aquifers have the potential to store between 7 and 20% of annual basin discharge, which will allow for future predictions of dry season base flow for the region's principal river.
AB - The Cordillera Blanca in Northwestern Peru is home to a quarter of the world's tropical glaciers, where hydrologic regimes are rapidly changing due to warming- induced glacier recession. Proglacial alpine meadows are storing a significant portion of annual basin discharge, and buffer dry season low flows as glaciers continue to lose their influence on the regional hydrologic cycle. We used integrated seismic (refraction, H/V passive seismic) and electrical (2D ERT and 1D soundings) in conjunction with borehole data to characterize the nature of proglacial talus aquifers in alpine meadows at elevations above 3500 masl. The meadow subsurface exhibits a transition from relatively slow (400-800 m/s) to fast (~2500 m/s) seismic p-wave velocity at depths of 4 to 8m, coinciding with the top of a composite layer of buried talus boulders, according to borehole data. Artesian pressure head in piezometers screened at the boulders indicate the presence of an aquifer confined by clay sediments. Resistivity profiles suggest that the upper most portions of the buried talus deposit are infilled with saturated clay, which dissipates with depth where sediments become more electrically resistive. Passive seismic and 1D electrical soundings suggest that total sediment thickness extends deeper than 20 m, allowing for first estimates of talus aquifer storage volumes and groundwater residence times. Based on the results from this study, we present a refined conceptual model of talus aquifers, from their formation to hydrologic function. Throughout the Cordillera Blanca, buried talus aquifers have the potential to store between 7 and 20% of annual basin discharge, which will allow for future predictions of dry season base flow for the region's principal river.
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U2 - 10.3997/2214-4609.201802464
DO - 10.3997/2214-4609.201802464
M3 - Conference contribution
AN - SCOPUS:85060512950
BT - 24th European Meeting of Environmental and Engineering Geophysics
PB - European Association of Geoscientists and Engineers, EAGE
ER -