scholarly journals Simulated effect of a forest road on near-surface hydrologic response: redux

2006 ◽  
Vol 32 (1) ◽  
pp. 126-142 ◽  
Author(s):  
Benjamin B. Mirus ◽  
Brian A. Ebel ◽  
Keith Loague ◽  
Beverley C. Wemple
Keyword(s):  
Hydrologic Response ◽  
Near Surface ◽  
Forest Road ◽  
Simulated Effect

Simulated effect of a forest road on near-surface hydrologic response and slope stability

2005 ◽  
Vol 30 (3) ◽  
pp. 325-338 ◽  
Author(s):  
Anona L. Dutton ◽  
Keith Loague ◽  
Beverley C. Wemple
Keyword(s):  
Slope Stability ◽  
Hydrologic Response ◽  
Near Surface ◽  
Forest Road ◽  
Simulated Effect

Simulated effect of soil depth and bedrock topography on near-surface hydrologic response and slope stability

2012 ◽  
Vol 38 (2) ◽  
pp. 146-159 ◽  
Author(s):  
Cristiano Lanni ◽  
Jeff McDonnell ◽  
Luisa Hopp ◽  
Riccardo Rigon
Keyword(s):  
Slope Stability ◽  
Soil Depth ◽  
Hydrologic Response ◽  
Near Surface ◽  
Bedrock Topography ◽  
Simulated Effect

Near-surface hydrologic response for a steep, unchanneled catchment near Coos Bay, Oregon: 2. Physics-based simulations

2007 ◽  
Vol 307 (4) ◽  
pp. 709-748 ◽  
Author(s):  
B. A. Ebel ◽  
K. Loague ◽  
J. E. Vanderkwaak ◽  
W. E. Dietrich ◽  
D. R. Montgomery ◽  
...  
Keyword(s):  
Hydrologic Response ◽  
Near Surface ◽  
Coos Bay

Near-surface hydrologic response for a steep, unchanneled catchment near Coos Bay, Oregon: 1. Sprinkling experiments

2007 ◽  
Vol 307 (10) ◽  
pp. 1194-1195
Author(s):  
B. A. Ebel ◽  
K. Loague ◽  
W. E. Dietrich ◽  
D. R. Montgomery ◽  
R. Torres ◽  
...  
Keyword(s):  
Hydrologic Response ◽  
Near Surface ◽  
Coos Bay

Near-surface hydrologic response for a steep, unchanneled catchment near Coos Bay, Oregon: 1. sprinkling experiments

2007 ◽  
Vol 307 (4) ◽  
pp. 678-708 ◽  
Author(s):  
B. A. Ebel ◽  
K. Loague ◽  
W. E. Dietrich ◽  
D. R. Montgomery ◽  
R. Torres ◽  
...  
Keyword(s):  
Hydrologic Response ◽  
Near Surface ◽  
Coos Bay

Rapid simulated hydrologic response within the variably saturated near surface

2008 ◽  
Vol 22 (3) ◽  
pp. 464-471 ◽  
Author(s):  
Brian A. Ebel ◽  
Keith Loague
Keyword(s):  
Hydrologic Response ◽  
Near Surface

scholarly journals Physics-based continuous simulation of long-term near-surface hydrologic response for the Coos Bay experimental catchment

2008 ◽  
Vol 44 (7) ◽  
Author(s):  
Brian A. Ebel ◽  
Keith Loague ◽  
David R. Montgomery ◽  
William E. Dietrich
Keyword(s):  
Hydrologic Response ◽  
Near Surface ◽  
Continuous Simulation ◽  
Coos Bay

Benthic foraminiferal zonation in deep-water carbonate platform margin environments, northern Little Bahama Bank

1988 ◽  
Vol 62 (01) ◽  
pp. 1-8 ◽  
Author(s):  
Ronald E. Martin
Keyword(s):  
Deep Water ◽  
Benthic Foraminifera ◽  
Carbonate Platform ◽  
Sedimentary Facies ◽  
Depositional Environments ◽  
Near Surface ◽  
Sediment Gravity Flows ◽  
Gravity Flows ◽  
Platform Margin ◽  
Water Carbonate

The utility of benthic foraminifera in bathymetric interpretation of clastic depositional environments is well established. In contrast, bathymetric distribution of benthic foraminifera in deep-water carbonate environments has been largely neglected. Approximately 260 species and morphotypes of benthic foraminifera were identified from 12 piston core tops and grab samples collected along two traverses 25 km apart across the northern windward margin of Little Bahama Bank at depths of 275-1,135 m. Certain species and operational taxonomic groups of benthic foraminifera correspond to major near-surface sedimentary facies of the windward margin of Little Bahama Bank and serve as reliable depth indicators. Globocassidulina subglobosa, Cibicides rugosus, and Cibicides wuellerstorfi are all reliable depth indicators, being most abundant at depths >1,000 m, and are found in lower slope periplatform aprons, which are primarily comprised of sediment gravity flows. Reef-dwelling peneroplids and soritids (suborder Miliolina) and rotaliines (suborder Rotaliina) are most abundant at depths <300 m, reflecting downslope bottom transport in proximity to bank-margin reefs. Small miliolines, rosalinids, and discorbids are abundant in periplatform ooze at depths <300 m and are winnowed from the carbonate platform. Increased variation in assemblage diversity below 900 m reflects mixing of shallow- and deep-water species by sediment gravity flows.

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