Matches in SemOpenAlex for { <https://semopenalex.org/work/W2137192643> ?p ?o ?g. }
- W2137192643 endingPage "3574" @default.
- W2137192643 startingPage "3556" @default.
- W2137192643 abstract "Abstract To obtain a better understanding of water's journey from the hillslope to the stream, water level time series from 26 groundwater wells in a hillslope–riparian study area in the Panola Mountain Research Watershed, Georgia, USA, were examined with respect to the occurrence of perched groundwater and groundwater flow directions. A connected groundwater table was taken as an indication of a hydrologic connection between the hillslope and the stream. Flow directions were determined based on observed water levels at different combinations of three neighbouring wells. The analyses indicated that the hillslope was disconnected from the stream most of the time but that almost the entire hillslope became connected to the stream during large rainfall events. This coincided with more sustained streamflow during these events. There were clear differences in the timing of the groundwater response between the upper hillslope, lower hillslope and riparian zone, with water levels near the stream and on the upper hillslope rising earlier than on the midslope. The flow directions were generally downslope and were most variable around a bedrock depression on the midslope. On the hillslope, the direction of the water table followed the local bedrock topography when the water level was low at the start and end of an event and the overall surface topography when water levels were high. In the riparian zone, flow directions either did not change significantly during events or turned from a more downstream (i.e. downvalley) direction to a more downslope (i.e. towards the stream) direction. These results highlight the competing influence of surface and bedrock topography on hillslope flow directions and improve our understanding of hillslope–riparian‐stream connectivity. Copyright © 2015 John Wiley & Sons, Ltd." @default.
- W2137192643 created "2016-06-24" @default.
- W2137192643 creator A5023484674 @default.
- W2137192643 creator A5028147456 @default.
- W2137192643 creator A5071760047 @default.
- W2137192643 date "2015-05-26" @default.
- W2137192643 modified "2023-10-14" @default.
- W2137192643 title "Hillslope-riparian-stream connectivity and flow directions at the Panola Mountain Research Watershed" @default.
- W2137192643 cites W1481494297 @default.
- W2137192643 cites W1501999399 @default.
- W2137192643 cites W1503982519 @default.
- W2137192643 cites W1509397625 @default.
- W2137192643 cites W1513772660 @default.
- W2137192643 cites W1562924588 @default.
- W2137192643 cites W1587773806 @default.
- W2137192643 cites W1588540824 @default.
- W2137192643 cites W1662707998 @default.
- W2137192643 cites W1668564613 @default.
- W2137192643 cites W1671483852 @default.
- W2137192643 cites W1763321171 @default.
- W2137192643 cites W1885855140 @default.
- W2137192643 cites W1897507705 @default.
- W2137192643 cites W1964124143 @default.
- W2137192643 cites W1978530899 @default.
- W2137192643 cites W1980499810 @default.
- W2137192643 cites W1980602747 @default.
- W2137192643 cites W1980658138 @default.
- W2137192643 cites W1987899762 @default.
- W2137192643 cites W1992789834 @default.
- W2137192643 cites W1993601481 @default.
- W2137192643 cites W1995646567 @default.
- W2137192643 cites W1995724908 @default.
- W2137192643 cites W1995848841 @default.
- W2137192643 cites W2002287531 @default.
- W2137192643 cites W2005943143 @default.
- W2137192643 cites W2009086755 @default.
- W2137192643 cites W2013193588 @default.
- W2137192643 cites W2014391803 @default.
- W2137192643 cites W2016901841 @default.
- W2137192643 cites W2025829064 @default.
- W2137192643 cites W2029205420 @default.
- W2137192643 cites W2030183079 @default.
- W2137192643 cites W2032239372 @default.
- W2137192643 cites W2036537516 @default.
- W2137192643 cites W2038848584 @default.
- W2137192643 cites W2050727042 @default.
- W2137192643 cites W2051026334 @default.
- W2137192643 cites W2052509795 @default.
- W2137192643 cites W2053787544 @default.
- W2137192643 cites W2054451705 @default.
- W2137192643 cites W2054821304 @default.
- W2137192643 cites W2054971855 @default.
- W2137192643 cites W2055978418 @default.
- W2137192643 cites W2063332389 @default.
- W2137192643 cites W2063606949 @default.
- W2137192643 cites W2068280848 @default.
- W2137192643 cites W2071888783 @default.
- W2137192643 cites W2081743863 @default.
- W2137192643 cites W2093475078 @default.
- W2137192643 cites W2094512748 @default.
- W2137192643 cites W2097058572 @default.
- W2137192643 cites W2105251015 @default.
- W2137192643 cites W2112655628 @default.
- W2137192643 cites W2115838363 @default.
- W2137192643 cites W2118651358 @default.
- W2137192643 cites W2118992670 @default.
- W2137192643 cites W2122410232 @default.
- W2137192643 cites W2122877606 @default.
- W2137192643 cites W2123729643 @default.
- W2137192643 cites W2129629964 @default.
- W2137192643 cites W2135689040 @default.
- W2137192643 cites W2136690550 @default.
- W2137192643 cites W2139744610 @default.
- W2137192643 cites W2142891982 @default.
- W2137192643 cites W2143127109 @default.
- W2137192643 cites W2143359154 @default.
- W2137192643 cites W2145513521 @default.
- W2137192643 cites W2146184050 @default.
- W2137192643 cites W2150524457 @default.
- W2137192643 cites W2151526862 @default.
- W2137192643 cites W2155097344 @default.
- W2137192643 cites W2158572362 @default.
- W2137192643 cites W2159948926 @default.
- W2137192643 cites W2165833683 @default.
- W2137192643 cites W2168153241 @default.
- W2137192643 cites W2169622957 @default.
- W2137192643 cites W2171292418 @default.
- W2137192643 cites W2500262678 @default.
- W2137192643 doi "https://doi.org/10.1002/hyp.10508" @default.
- W2137192643 hasPublicationYear "2015" @default.
- W2137192643 type Work @default.
- W2137192643 sameAs 2137192643 @default.
- W2137192643 citedByCount "52" @default.
- W2137192643 countsByYear W21371926432015 @default.
- W2137192643 countsByYear W21371926432016 @default.
- W2137192643 countsByYear W21371926432017 @default.
- W2137192643 countsByYear W21371926432018 @default.
- W2137192643 countsByYear W21371926432019 @default.