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1

Webber, David F., Manveen Bansal, Steven K. Mickelson, et al. "Assessing Surface Flowpath Interception by Vegetative Buffers Using ArcGIS Hydrologic Modeling and Geospatial Analysis for Rock Creek Watershed in Central Iowa." Transactions of the ASABE 61, no. 1 (2018): 273–83. http://dx.doi.org/10.13031/trans.12350.

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Abstract. Nonpoint-source (NPS) pollution is a major cause of surface water quality degradation due to the transport of chemicals, nutrients, and sediments into lakes and streams. Vegetative buffers comprise several effective landscape best management practices (BMPs) that include vegetative filter strips (VFS) and grassed waterways. However, some BMPs are less effective due to concentrated surface flow, improper cropland-to-VFS area ratios, and surface flowpaths that partially or completely bypass vegetative buffers. The overall objective of this study was to quantify the accuracy of simulate
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2

Wacha, Kenneth, A. Papanicolaou, Christos Giannopoulos, et al. "The Role of Hydraulic Connectivity and Management on Soil Aggregate Size and Stability in the Clear Creek Watershed, Iowa." Geosciences 8, no. 12 (2018): 470. http://dx.doi.org/10.3390/geosciences8120470.

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The role of tillage practices on soil aggregate properties has been mainly addressed at the pedon scale (i.e., soilscape scale) by treating landscape elements as disconnected. However, there is observed heterogeneity in aggregate properties along flowpaths, suggesting that landscape scale hydraulic processes are also important. This study examines this supposition using field, laboratory and modeling analysis to assess aggregate size and stability along flowpaths under different management conditions: (1) tillage-induced abrasion effects on aggregate size were evaluated with the dry mean weigh
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3

Zhang, Peng Wei, Qing Bo Wen, and Li Ming Hu. "Numerical Simulation of Contaminant Dynamic Transfer in Dual-Domain Model." Advanced Materials Research 864-867 (December 2013): 1379–85. http://dx.doi.org/10.4028/www.scientific.net/amr.864-867.1379.

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Preferential flowpaths (PFP) causes highly heterogeneity of soil. In this study a preferential flowpaths generalized model has been established, based on dual-domain model (DDM) which reflects contaminant transport and the dynamic transfer between mobile and immobile domains, quantitatively analyses the contaminant mass transfer in pore scale at three different conditions. Besides, define relative hydraulic conductivity reflect the impact of PFP physical parameters, results show that it can affect the contaminant transport form and the distribution of contaminant concentration.
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4

Datry, Thibault, and Scott T. Larned. "River flow controls ecological processes and invertebrate assemblages in subsurface flowpaths of an ephemeral river reach." Canadian Journal of Fisheries and Aquatic Sciences 65, no. 8 (2008): 1532–44. http://dx.doi.org/10.1139/f08-075.

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We present the first measurements of solutes, invertebrates, and microbial activity in the semi-perched hyporheic, parafluvial, and riparian flowpaths of an ephemeral river channel. Dissolved organic carbon (DOC), nitrogen (DON), and phosphorus (DOP) concentrations decreased as water from an adjacent river mainstem moved through the flowpaths. DOC, DON, and DOP processing rates decreased with increasing mainstem flow and increased with parafluvial zone length. These patterns suggest that the surface water zones of perched river systems are organic nutrient sources to subsurface flowpaths and t
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5

Fisher, Stuart G., Ryan A. Sponseller, and James B. Heffernan. "HORIZONS IN STREAM BIOGEOCHEMISTRY: FLOWPATHS TO PROGRESS." Ecology 85, no. 9 (2004): 2369–79. http://dx.doi.org/10.1890/03-0244.

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6

Hanna, Darrin M., and Richard E. Haskell. "Flowpaths: Compiling stack-based IR to hardware." Microprocessors and Microsystems 30, no. 3 (2006): 125–36. http://dx.doi.org/10.1016/j.micpro.2005.07.001.

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7

Kukemilks, Karlis, and Jean-Frank Wagner. "Detection of Preferential Water Flow by Electrical Resistivity Tomography and Self-Potential Method." Applied Sciences 11, no. 9 (2021): 4224. http://dx.doi.org/10.3390/app11094224.

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This study explores the hydrogeological conditions of a landslide-prone hillslope in the Upper Mosel valley, Luxembourg. The investigation program included the monitoring of piezometer wells, hydrogeological field tests, analysis of drillcore records, and geophysical surveys. Monitoring and field testing in some of the observation wells indicated very pronounced preferential flow. Electrical resistivity tomography (ERT) and self-potential geophysical methods were employed in the study area for exploration of the morphology of preferential flowpaths. Possible signals associated with flowing gro
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8

Gardner, John R., Scott H. Ensign, Jeffrey N. Houser, and Martin W. Doyle. "Light exposure along particle flowpaths in large rivers." Limnology and Oceanography 65, no. 1 (2019): 128–42. http://dx.doi.org/10.1002/lno.11256.

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9

Elsenbeer, Helmut. "Hydrologic flowpaths in tropical rainforest soilscapes?a review." Hydrological Processes 15, no. 10 (2001): 1751–59. http://dx.doi.org/10.1002/hyp.237.

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10

Georgiadis, Nicholas J., Dennis A. Yoder, Manan A. Vyas, and William A. Engblom. "Status of turbulence modeling for hypersonic propulsion flowpaths." Theoretical and Computational Fluid Dynamics 28, no. 3 (2014): 295–318. http://dx.doi.org/10.1007/s00162-013-0316-z.

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11

Jung, Hyejung, Dong-Chan Koh, Yun Kim, Sung-Wook Jeen, and Jeonghoon Lee. "Stable Isotopes of Water and Nitrate for the Identification of Groundwater Flowpaths: A Review." Water 12, no. 1 (2020): 138. http://dx.doi.org/10.3390/w12010138.

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Nitrate contamination in stream water and groundwater is a serious environmental problem that arises in areas of high agricultural activities or high population density. It is therefore important to identify the source and flowpath of nitrate in water bodies. In recent decades, the dual isotope analysis (δ15N and δ18O) of nitrate has been widely applied to track contamination sources by taking advantage of the difference in nitrogen and oxygen isotope ratios for different sources. However, transformation processes of nitrogen compounds can change the isotopic composition of nitrate due to the
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12

Jaunat, J., F. Huneau, A. Dupuy, H. Celle-Jeanton, and P. Le Coustumer. "Coupling hydrology, geochemistry and hydrodynamics towards rational management of discontinuous aquifers: application to the Ursuya massif (Basque Country, France)." Proceedings of the International Association of Hydrological Sciences 364 (September 16, 2014): 386–91. http://dx.doi.org/10.5194/piahs-364-386-2014.

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Abstract. The metamorphic massif of Ursuya (French Basque Country) is a strategic aquifer for the water supply of southwestern France. A multidisciplinary approach, conducted between 2009 and 2013, has led to understanding of the behaviour of this system made of discontinuous media. Isotopic and geochemical characteristics of rainwater were studied together with groundwater geochemistry, to delineate the water–rock interactions along the underground flowpaths. The chemical characteristics of groundwater, the residence times (less than 10 years to more than 50 years) and the associated mixing p
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13

Milligan, Ryan T., Dean R. Eklund, J. Mitch Wolff, Mark Gruber, and Tarun Mathur. "Dual-Mode Scramjet Combustor: Numerical Analysis of Two Flowpaths." Journal of Propulsion and Power 27, no. 6 (2011): 1317–20. http://dx.doi.org/10.2514/1.b34178.

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14

Jones, Thomas A. "Using flowpaths and vector fields in object-based modeling." Computers & Geosciences 27, no. 2 (2001): 133–38. http://dx.doi.org/10.1016/s0098-3004(00)00085-6.

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15

Pfister, Laurent, Carlos E. Wetzel, Núria Martínez-Carreras, et al. "Examination of aerial diatom flushing across watersheds in Luxembourg, Oregon and Slovakia for tracing episodic hydrological connectivity." Journal of Hydrology and Hydromechanics 63, no. 3 (2015): 235–45. http://dx.doi.org/10.1515/johh-2015-0031.

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Abstract Hydrological processes research remains a field that is severely measurement limited. While conventional tracers (geochemicals, isotopes) have brought extremely valuable insights into water source and flowpaths, they nonetheless have limitations that clearly constrain their range of application. Integrating hydrology and ecology in catchment science has been repeatedly advocated as offering potential for interdisciplinary studies that are eventually to provide a holistic view of catchment functioning. In this context, aerial diatoms have been shown to have the potential for detecting
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16

Shrestha, Rajesh R., Karsten Osenbrück, and Michael Rode. "Assessment of catchment response and calibration of a hydrological model using high-frequency discharge–nitrate concentration data." Hydrology Research 44, no. 6 (2013): 995–1012. http://dx.doi.org/10.2166/nh.2013.087.

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This study uses a high-frequency discharge and nitrate concentration dataset from the Weida catchment in Germany for the catchment scale hydrologic response analysis. Nitrate transport in the catchment is mostly conservative as indicated by the nitrate stable isotope (δ15N and δ18O) analysis. Discharge–nitrate concentration data from the catchment show distinctive patterns, suggesting flushing and dilution response. A self-organizing feature map-based methodology was employed to identify such patterns or cluster in the datasets. Based on knowledge of the catchment conditions and prevailing und
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17

Cheon, Enok, Seung-Rae Lee, and Deuk-Hwan Lee. "Hazard Assessment Based on the Combination of DAN3D and Machine Learning Method for Planning Closed-Type Barriers against Debris-Flow." Water 12, no. 1 (2020): 170. http://dx.doi.org/10.3390/w12010170.

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If a slope located near a densely populated region is susceptible to debris-flow hazards, barriers are used as a mitigation method by placing them in flow channels; i.e., flowpaths. Selecting the location and the design of a barrier requires hazard assessment to determine the width, volume, and impact pressure of debris-flow at the moment of collision. DAN3D (Three-Dimensional Dynamic Analysis), a 3D numerical model for simulating debris-flow, has been widely used to perform hazard assessment; however, solely using DAN3D would be both insufficient and inefficient in finding the optimal barrier
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18

Banks, Eddie W., Margaret A. Shanafield, and Peter G. Cook. "Induced Temperature Gradients to Examine Groundwater Flowpaths in Open Boreholes." Groundwater 52, no. 6 (2014): 943–51. http://dx.doi.org/10.1111/gwat.12157.

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19

Sappa, Giuseppe, Stefania Vitale, and Flavia Ferranti. "Identifying Karst Aquifer Recharge Areas using Environmental Isotopes: A Case Study in Central Italy." Geosciences 8, no. 9 (2018): 351. http://dx.doi.org/10.3390/geosciences8090351.

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Water resources management is one of the most important challenges worldwide because water represents a vital resource for sustaining life and the environment. With the aim of sustainable groundwater management, the identification of aquifer recharge areas is a useful tool for water resources protection. In a well-developed karst aquifer, environmental isotopes provide support for identifying aquifer recharge areas, residence time and interconnections between aquifer systems. This study deals with the use of environmental isotopes to identify the main recharge area of a karst aquifer in the Up
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20

Dole-Olivier, Marie-José. "The hyporheic refuge hypothesis reconsidered: a review of hydrological aspects." Marine and Freshwater Research 62, no. 11 (2011): 1281. http://dx.doi.org/10.1071/mf11084.

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The hyporheic zone (HZ) is thought to serve multiple functions for lotic invertebrates, but its role in the persistence of benthic assemblages after disturbances (‘hyporheic refuge hypothesis’, HRH) has never been clearly demonstrated since its initial proposal in 1953. Water exchanges through the HZ appear to be crucial in determining most hyporheic processes and subsequently, in controlling directly or indirectly the distribution of hyporheic assemblages. At present, it seems that the distribution of hyporheic refugia would also be controlled by hyporheic flowpaths, explaining the non-unifor
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21

Sobczak, William V., and Stuart Findlay. "VARIATION IN BIOAVAILABILITY OF DISSOLVED ORGANIC CARBON AMONG STREAM HYPORHEIC FLOWPATHS." Ecology 83, no. 11 (2002): 3194–209. http://dx.doi.org/10.1890/0012-9658(2002)083[3194:vibodo]2.0.co;2.

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22

Jones, T. "FP2VF: Fortran 90 program to generate a vector field from flowpaths." Computers & Geosciences 29, no. 2 (2003): 209–14. http://dx.doi.org/10.1016/s0098-3004(02)00109-7.

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23

Schreiber, M. E., G. R. Moline, and J. M. Bahr. "Using Hydrochemical Fades to Delineate Ground Water Flowpaths in Fractured Shale." Groundwater Monitoring & Remediation 19, no. 1 (1999): 95–109. http://dx.doi.org/10.1111/j.1745-6592.1999.tb00192.x.

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24

Elsenbeer, Helmut, and Andreas Lack. "Hydrometric and hydrochemicai evidence for fast flowpaths at La Cuenca, Western Amazonia." Journal of Hydrology 180, no. 1-4 (1996): 237–50. http://dx.doi.org/10.1016/0022-1694(95)02889-7.

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25

Collins, Bridget M., William V. Sobczak, and Elizabeth A. Colburn. "Subsurface flowpaths in a forested headwater stream harbor a diverse macroinvertebrate community." Wetlands 27, no. 2 (2007): 319–25. http://dx.doi.org/10.1672/0277-5212(2007)27[319:sfiafh]2.0.co;2.

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26

Toran, Laura, Ellen K. Herman, and William B. White. "Comparison of Flowpaths to a Well and Spring in a Karst Aquifer." Ground Water 45, no. 3 (2007): 281–87. http://dx.doi.org/10.1111/j.1745-6584.2007.00287.x.

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27

Voytek, Emily B., Caitlin R. Rushlow, Sarah E. Godsey, and Kamini Singha. "Identifying hydrologic flowpaths on arctic hillslopes using electrical resistivity and self potential." GEOPHYSICS 81, no. 1 (2016): WA225—WA232. http://dx.doi.org/10.1190/geo2015-0172.1.

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Shallow subsurface flow is a dominant process controlling hillslope runoff generation, soil development, and solute reaction and transport. Despite their importance, the location and geometry of these flow paths are difficult to determine. In arctic environments, shallow subsurface flow paths are limited to a thin zone of seasonal thaw above permafrost, which is traditionally assumed to mimic the surface topography. We have used a combined approach of electrical resistivity tomography (ERT) and self-potential (SP) measurements to map shallow subsurface flow paths in and around water tracks, dr
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28

Lewis, David Bruce, Nancy B. Grimm, Tamara K. Harms, and John D. Schade. "Subsystems, flowpaths, and the spatial variability of nitrogen in a fluvial ecosystem." Landscape Ecology 22, no. 6 (2007): 911–24. http://dx.doi.org/10.1007/s10980-007-9078-6.

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29

Pfeiffer, Shaili M., Jean M. Bahr, and Richard D. Beilfuss. "Identification of groundwater flowpaths and denitrification zones in a dynamic floodpain aquifier." Journal of Hydrology 325, no. 1-4 (2006): 262–72. http://dx.doi.org/10.1016/j.jhydrol.2005.10.019.

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30

Asano, Yuko, Jana E. Compton, and M. Robbins Church. "Hydrologic flowpaths influence inorganic and organic nutrient leaching in a forest soil." Biogeochemistry 81, no. 2 (2006): 191–204. http://dx.doi.org/10.1007/s10533-006-9036-4.

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31

Shaughnessy, Andrew R., Xin Gu, Tao Wen, and Susan L. Brantley. "Machine learning deciphers CO<sub>2</sub> sequestration and subsurface flowpaths from stream chemistry." Hydrology and Earth System Sciences 25, no. 6 (2021): 3397–409. http://dx.doi.org/10.5194/hess-25-3397-2021.

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Abstract. Endmember mixing analysis (EMMA) is often used by hydrogeochemists to interpret the sources of stream solutes, but variations in stream concentrations and discharges remain difficult to explain. We discovered that machine learning can be used to highlight patterns in stream chemistry that reveal information about sources of solutes and subsurface groundwater flowpaths. The investigation has implications, in turn, for the balance of CO2 in the atmosphere. For example, CO2-driven weathering of silicate minerals removes carbon from the atmosphere over ∼106-year timescales. Weathering of
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32

Del Rosario, Rosalie B., and Vincent H. Resh. "Interstitial invertebrate assemblages associated with small-scale subsurface flowpaths in perennial and intermittent California streams." Fundamental and Applied Limnology 150, no. 4 (2001): 629–40. http://dx.doi.org/10.1127/archiv-hydrobiol/150/2001/629.

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33

Garvelmann, J., C. Külls, and M. Weiler. "A porewater – based stable isotope approach for the investigation of subsurface hydrological processes." Hydrology and Earth System Sciences Discussions 8, no. 5 (2011): 9089–112. http://dx.doi.org/10.5194/hessd-8-9089-2011.

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Abstract. Predicting and understanding subsurface flowpaths is still a crucial issue in hydrological research. We present an experimental approach to reveal present and past subsurface flowpaths of water in the unsaturated and saturated zone. Two hillslopes in a humid moutainous catchment have been investigated. The H2O(liquid) – H2O(vapor) equilibration laser spectroscopy method was used to obtain high resolution δ2H vertical depth profiles of porewater at various points along a fall line of a pasture hillslope in the southern Black Forest, Germany. The Porewater Stable Isotope Profile (PSIP)
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34

Mulholland, Patrick J. "Hydrometric and stream chemistry evidence of three storm flowpaths in Walker Branch Watershed." Journal of Hydrology 151, no. 2-4 (1993): 291–316. http://dx.doi.org/10.1016/0022-1694(93)90240-a.

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35

Johnson, Mark S., Johannes Lehmann, Eduardo Guimarães Couto, João Paulo Novães Filho, and Susan J. Riha. "DOC and DIC in Flowpaths of Amazonian Headwater Catchments with Hydrologically Contrasting Soils." Biogeochemistry 81, no. 1 (2006): 45–57. http://dx.doi.org/10.1007/s10533-006-9029-3.

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36

Deemy, James B., and Todd C. Rasmussen. "Hydrology and water quality of isolated wetlands: Stormflow changes along two episodic flowpaths." Journal of Hydrology: Regional Studies 14 (December 2017): 23–36. http://dx.doi.org/10.1016/j.ejrh.2017.10.001.

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37

Garvelmann, J., C. Külls, and M. Weiler. "A porewater-based stable isotope approach for the investigation of subsurface hydrological processes." Hydrology and Earth System Sciences 16, no. 2 (2012): 631–40. http://dx.doi.org/10.5194/hess-16-631-2012.

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Abstract. Predicting and understanding subsurface flowpaths is still a crucial issue in hydrological research. We present an experimental approach to reveal present and past subsurface flowpaths of water in the unsaturated and saturated zone. Two hillslopes in a humid mountainous catchment have been investigated. The H2O(liquid) – H2O(vapor) equilibration laser spectroscopy method was used to obtain high resolution δ2H vertical depth profiles of pore water at various points along two fall lines of a pasture hillslope in the southern Black Forest, Germany. The Porewater-based Stable Isotope Pro
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38

BACCHUS, S. T. "Discriminating Sources and Flowpaths of Anthropogenic Nitrogen Discharges to Florida Springs, Streams and Lakes." Environmental and Engineering Geoscience 11, no. 4 (2005): 347–69. http://dx.doi.org/10.2113/11.4.347.

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39

Kukshinov, N. V., and S. N. Batura. "Numerical simulation of hydrogen combustion in oxidizer supersonic flow in flowpaths of various configurations." Journal of Physics: Conference Series 1359 (November 2019): 012064. http://dx.doi.org/10.1088/1742-6596/1359/1/012064.

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40

Costa, Diogo, and John W. Pomeroy. "Preferential meltwater flowpaths as a driver of preferential elution of chemicals from melting snowpacks." Science of The Total Environment 662 (April 2019): 110–20. http://dx.doi.org/10.1016/j.scitotenv.2019.01.091.

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41

Klepikova, Maria, Bernard Brixel, and Mohammadreza Jalali. "Transient hydraulic tomography approach to characterize main flowpaths and their connectivity in fractured media." Advances in Water Resources 136 (February 2020): 103500. http://dx.doi.org/10.1016/j.advwatres.2019.103500.

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42

Toosi, Ehsan R., John P. Schmidt, and Michael J. Castellano. "Land use and hydrologic flowpaths interact to affect dissolved organic matter and nitrate dynamics." Biogeochemistry 120, no. 1-3 (2014): 89–104. http://dx.doi.org/10.1007/s10533-014-9983-0.

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43

Chaves, Joaquín, Christopher Neill, Sonja Germer, et al. "Nitrogen Transformations in Flowpaths Leading from Soils to Streams in Amazon Forest and Pasture." Ecosystems 12, no. 6 (2009): 961–72. http://dx.doi.org/10.1007/s10021-009-9270-4.

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44

Williams, Mark W., Mark Rikkers, and W. Tad Pfeffer. "Ice Columns and Frozen Rills in a Warm Snowpack, Green Lakes Valley, Colorado, U.S.A." Hydrology Research 31, no. 3 (2000): 169–86. http://dx.doi.org/10.2166/nh.2000.0011.

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Here we provide information on ice columns and frozen rills found in late-season snowpacks in and near the Green Lakes Valley of the Colorado Front Range, USA. The presence of ice columns and frozen rills in late season snowpacks may provide insights with which to understand the spatial distribution of preferential flowpaths in melting snowpacks. In July and August of 1996 and 1997 we found ice columns in every one of the more than 50 snow fields we investigated. The ice columns showed a consistent morphology; each column was approximately 75 cm in vertical extent, with about 5 cm projecting a
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45

de Graaf, I. E. M., E. H. Sutanudjaja, L. P. H. van Beek, and M. F. P. Bierkens. "A high resolution global scale groundwater model." Hydrology and Earth System Sciences Discussions 11, no. 5 (2014): 5217–50. http://dx.doi.org/10.5194/hessd-11-5217-2014.

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Abstract. Groundwater is the world's largest accessible source of fresh water. It plays a vital role in satisfying needs for drinking water, agriculture and industrial activities. During times of drought groundwater sustains baseflow to rivers and wetlands, thereby supporting ecosystems. Most global scale hydrological models (GHMs) do not include a groundwater flow component, mainly due to lack of geohydrological data at the global scale. For the simulation of lateral flow and groundwater head dynamics a realistic physical representation of the groundwater system is needed, especially for GHMs
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46

Vatne, G., and T. D. L. Irvine-Fynn. "Morphological dynamics of an englacial channel." Hydrology and Earth System Sciences Discussions 12, no. 8 (2015): 7615–64. http://dx.doi.org/10.5194/hessd-12-7615-2015.

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Abstract. Despite an interest in the hydraulic functioning of supraglacial and englacial channels over the last four decades, the processes and forms of such ice-bounded streams have remained poorly documented. Recent glaciological research has demonstrated the potential significance of so-called "cut and closure" streams, where englacial or subglacial flowpaths are created from the long-term incision of supraglacial channels. These flowpaths are reported to exhibit step-pool morphology, comprising knickpoints and/or knickzones, albeit exaggerated in dimensions in comparison to their supraglac
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47

Ribot, Miquel, Susana Bernal, Myrto Nikolakopoulou, et al. "Enhancement of carbon and nitrogen removal by helophytes along subsurface water flowpaths receiving treated wastewater." Science of The Total Environment 599-600 (December 2017): 1667–76. http://dx.doi.org/10.1016/j.scitotenv.2017.05.114.

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48

Wallace, Carlington, Gregory McCarty, Sangchul Lee, et al. "Evaluating Concentrated Flowpaths in Riparian Forest Buffer Contributing Areas Using LiDAR Imagery and Topographic Metrics." Remote Sensing 10, no. 4 (2018): 614. http://dx.doi.org/10.3390/rs10040614.

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49

Eshleman, Keith N., John S. Pollard, and Anne K. O'Brien. "Interactions between groundwater and surface water in a virginia coastal plain watershed. 1. Hydrological flowpaths." Hydrological Processes 8, no. 5 (1994): 389–410. http://dx.doi.org/10.1002/hyp.3360080503.

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50

Zheng, Chunmiao, and Steven M. Gorelick. "Analysis of Solute Transport in Flow Fields Influenced by Preferential Flowpaths at the Decimeter Scale." Ground Water 41, no. 2 (2003): 142–55. http://dx.doi.org/10.1111/j.1745-6584.2003.tb02578.x.

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