Towards a better understanding of riparian zone water table response to precipitation: surface water infiltration, hillslope contribution or pressure wave processes?

2012 ◽  
Vol 26 (21) ◽  
pp. 3207-3215 ◽  
Author(s):  
Philippe Vidon
Keyword(s):  
Surface Water ◽  
Water Table ◽  
Pressure Wave ◽  
Riparian Zone ◽  
Water Infiltration ◽  
Wave Processes ◽  
Zone Water

scholarly journals A Hydrologic Landscapes Perspective on Groundwater Connectivity of Depressional Wetlands

Water ◽  
2019 ◽  
Vol 12 (1) ◽  
pp. 50 ◽  
Author(s):  
Brian P. Neff ◽  
Donald O. Rosenberry ◽  
Scott G. Leibowitz ◽  
Dave M. Mushet ◽  
Heather E. Golden ◽  
...  
Keyword(s):  
Surface Water ◽  
Water Table ◽  
Conceptual Knowledge ◽  
Groundwater Discharge ◽  
Depressional Wetlands ◽  
Hydrologic Connectivity ◽  
Site Specific ◽  
Depressional Wetland ◽  
Resource Managers ◽  
Flow Through

Research into processes governing the hydrologic connectivity of depressional wetlands has advanced rapidly in recent years. Nevertheless, a need persists for broadly applicable, non-site-specific guidance to facilitate further research. Here, we explicitly use the hydrologic landscapes theoretical framework to develop broadly applicable conceptual knowledge of depressional-wetland hydrologic connectivity. We used a numerical model to simulate the groundwater flow through five generic hydrologic landscapes. Next, we inserted depressional wetlands into the generic landscapes and repeated the modeling exercise. The results strongly characterize groundwater connectivity from uplands to lowlands as being predominantly indirect. Groundwater flowed from uplands and most of it was discharged to the surface at a concave-upward break in slope, possibly continuing as surface water to lowlands. Additionally, we found that groundwater connectivity of the depressional wetlands was primarily determined by the slope of the adjacent water table. However, we identified certain arrangements of landforms that caused the water table to fall sharply and not follow the surface contour. Finally, we synthesize our findings and provide guidance to practitioners and resource managers regarding the management significance of indirect groundwater discharge and the effect of depressional wetland groundwater connectivity on pond permanence and connectivity.

Mineralogical and textural evolution of the economic manganese mineralisation in western Rhodope massif, N. Greece

1991 ◽  
Vol 55 (380) ◽  
pp. 423-434 ◽  
Author(s):  
M. K. Nimfopoulos ◽  
R. A. D. Pattrick
Keyword(s):  
Surface Water ◽  
Water Table ◽  
Fault Zones ◽  
Hydrothermal Fluids ◽  
Mineral Paragenesis ◽  
Textural Evolution ◽  
Mn Oxide ◽  
Alkaline Earths ◽  
Mn Oxides ◽  
Hydrothermal Veins

AbstractThe western Rhodope massif contains a significant number of ‘battery grade’ Mn-oxide deposits which are best developed in the area near Kato Nevrokopi, Drama district, N. Greece. Economic Mn-oxide ore concentrations are confined to fault zones and related karsts in marbles. The mineralisation has formed by weathering of hydrothermal veins that were genetically related to Oligocene magmatism.At Kato Nevrokopi, progressive and continuous weathering of primary, hydrothermal veins of rhodochrosite, mixed sulphide, quartz and ‘black calcite’ (calcite and todorokite) has resulted in the formation of the assemblage MnO-gel-(amorphous Mn-oxide)-todorokite-azurite-goethite-cerussite in the veins and the assemblage MnO-gel-nsutite-chalcophanite-birnessite-cryptomelane-pyrolusite and malachite and amorphous Fe-oxides in karstic cavities.The fs2 and fO2 of the hydrothermal fluids increased with time. The breakdown of the hypogene Mn-carbonate was aided by the production of an acidic fluid due to the oxidation of sulphides. Precipitation of the supergene ores was caused by neutralisation of the fluids due to reaction with the host marble and to mixing of relatively reduced fluids with oxygenated surface water in a fluctuation water table regime. Zinc was also mobile during weathering and became concentrated in the intermediate Mn-oxides, effectively stabilising their structures. The mineral paragenesis records the progressive oxidation of the ore and the appearance of less hydrated Mn-oxides, low in alkalis and alkaline earths.

scholarly journals A New Conceptual Model for Slope-Infiltration

Water ◽  
2019 ◽  
Vol 11 (4) ◽  
pp. 678 ◽  
Author(s):  
Renato Morbidelli ◽  
Corrado Corradini ◽  
Carla Saltalippi ◽  
Alessia Flammini ◽  
Jacopo Dari ◽  
...  
Keyword(s):  
Surface Water ◽  
Conceptual Model ◽  
Soil Type ◽  
Unsolved Problem ◽  
Threshold Value ◽  
Water Velocity ◽  
Water Infiltration ◽  
Infiltration Process ◽  
Wide Range ◽  
Steep Slopes

Rainfall infiltration modeling over surfaces with significant slopes is an unsolved problem. Even though water infiltration occurs over soil surfaces with noticeable gradients in most real situations, the typical mathematical models used were developed for infiltration over horizontal surfaces. In addition, recent investigations on infiltration over sloping surfaces have provided conflicting results, suggesting that our understanding of the process may still be lacking. In this study, our objective is to specifically examine if the surface water velocity that is negligible over near horizontal soil surfaces can affect the infiltration process over steep slopes. A new conceptual model representing a wide range of experimental results is proposed. The model represents water flow as an ensemble of infinitesimal “particles” characterized by specific velocities and assumes that only “particles” with velocity less than a threshold value can contribute to the infiltration process. The velocity distribution and the threshold value depend on slope and soil type, respectively. This conceptual model explains observed results and serves as a foundation for developing further experiments and refining models that offer more realistic representations of infiltration over sloping surfaces.

scholarly journals Using Wavelet Coherence to Characterize Surface Water Infiltration into a Low‐Lying Karst Aquifer

Ground Water ◽  
2020 ◽  
Author(s):  
Philip Schuler ◽  
Èlia Cantoni ◽  
Léa Duran ◽  
Paul Johnston ◽  
Laurence Gill
Keyword(s):  
Surface Water ◽  
Karst Aquifer ◽  
Water Infiltration ◽  
Wavelet Coherence

scholarly journals Assessment of river water infiltration conditions based on both chloride mass-balance and hydrogeological setting: the Krajkowo riverbank filtration site (Poland)

Geologos ◽  
2021 ◽  
Vol 27 (1) ◽  
pp. 35-41
Author(s):  
Jozef Gorski ◽  
Krzysztof Dragon ◽  
Roksana Kruc-Fijalkowska ◽  
Magdalena Matusiak
Keyword(s):  
Surface Water ◽  
River Water ◽  
Water Infiltration ◽  
Riverbank Filtration ◽  
Superficial Zone ◽  
Well Production ◽  
Lower Chloride ◽  
Average Contribution ◽  
Strong Erosion ◽  
Chloride Concentrations

Abstract In the present work measurements of chloride concentrations were used to assess the variability of infiltration conditions and contributions of surface water and local groundwater to the discharge of wells at Krajkowo riverbank filtration site (western Poland). Tests were performed on samples from 26 wells located in a well gallery close to the River Warta. Due to higher chloride concentrations in river water in comparison with local groundwater, significant differences in concentrations in samples from individual wells were noted. In particular, lower chloride concentrations in 11 wells were recorded, which can be linked to the local occurrence of low-permeability deposits in the superficial zone; a locally higher degree of riverbed sediment clogging in the highly convex meandering zone, where strong erosion of the riverbed occurred, which in turn led to increased clogging; the occurrence of a more intensive groundwater inflow into the river valley due to water infiltration from a smaller river entering the River Warta valley, as well as unfavourable conditions for the infiltration of surface water to the lower part of the aquifer with a greater thickness. Differences in chloride concentrations observed were also used to quantify approximately river water contribution to the well production. The average contribution of the River Warta to the recharge of the entire well gallery was estimated at 59.8%.

Reactivation of a huge ancient landslide by surface water infiltration

2019 ◽  
Vol 16 (4) ◽  
pp. 806-820 ◽  
Author(s):  
Guo-xiang Tu ◽  
Da Huang ◽  
Hui Deng
Keyword(s):  
Surface Water ◽  
Water Infiltration ◽  
Ancient Landslide

The effect of a pressure wave on a rigid wall covered with a porous layer

2006 ◽  
Vol 4 ◽  
pp. 156-165 ◽  
Author(s):  
S.V. Lukin
Keyword(s):  
Porous Layer ◽  
Pressure Wave ◽  
Continuum Model ◽  
Solid Wall ◽  
Rigid Wall ◽  
Saturated Liquid ◽  
Wave Processes ◽  
Porous Substance ◽  
Step Type ◽  
Type Pressure

The influence of the non-stationary Basset-Boussinesq forces on the reflection of a step-type pressure wave from a solid surface coated with a porous layer, a saturated liquid or a gas is investigated. The study of wave processes is carried out within the framework of the multi-velocity continuum model. A comparative analysis of the properties of porous screens saturated with a liquid or gas is carried out. The degree of influence of the non-stationary Basset-Boussinesq force on reflection of a wave from a solid wall covered with a porous substance is established.

scholarly journals Impact of Sea-Level Rise on the Hydrologic Landscape of the Mānā Plain, Kaua‘i

Water ◽  
2021 ◽  
Vol 13 (6) ◽  
pp. 766
Author(s):  
Basil Gomez
Keyword(s):  
Surface Water ◽  
Sea Level Rise ◽  
Sea Level ◽  
Water Table ◽  
Root Zone ◽  
Storm Runoff ◽  
Transient Event ◽  
Gravity Flows ◽  
Operational Ability ◽  
Event Based

The Mānā Plain is a land apart, buffered from oceanographic influences by ~3–35 m high backshore deposits, and drained by an intricate, >100-y-old ditch system and modern, large-capacity pumps. Quantifying present and prospective inputs and outputs for the hydrologic landscape suggests that, although sea-level rise (SLR) will begin to impact ditch system operations in 2040, transient, event-based flooding caused by rainfall, not SLR induced, multi-mechanism flooding, will continue to pose the most immediate threat. This is because as sea level rises the ability of gravity flows to discharge storm runoff directly into the ocean will diminish, causing floodwater to pond in low-lying depressions. Estimates of the volume of water involved suggests the risk of flooding from surface water is likely to extend to 5.45 km2 of land that is presently ≤ 1 m above sea level. This land will not be permanently inundated, but weeks of pumping may be required to remove the floodwater. Increasing pumping capacity and preserving some operational ability to discharge storm runoff under the influence of gravity will enhance the ditch system’s resilience to SLR and ensure it continues to fulfill its primary functions, of maintaining the water table below the root zone and diverting storm runoff away from farmland, at least until the end of this century.

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