Catálogo de publicaciones - revistas
Hydrogeology Journal
Resumen/Descripción – provisto por la editorial en inglés
Hydrogeology Journal has acquired a large worldwide readership since its inception in 1992. A mainstream paper in Hydrogeology Journal integrates subsurface hydrology and geology with the other supporting disciplines (such as geochemistry, geophysics, geomorphology, geobiology, surface-water hydrology, tectonics, mathematics, numerical modeling, economics, and sociology) to explain phenomena observed in the field.Palabras clave – provistas por la editorial
No disponibles.
Disponibilidad
| Institución detectada | Período | Navegá | Descargá | Solicitá |
|---|---|---|---|---|
| No detectada | desde ene. 1997 / hasta dic. 2023 | SpringerLink |
Información
Tipo de recurso:
revistas
ISSN impreso
1431-2174
ISSN electrónico
1435-0157
País de edición
Alemania
Fecha de publicación
1995-
Cobertura temática
Tabla de contenidos
The conceptualization model problem?surprise
John Bredehoeft
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. 37-46
Hydrogeology of an arid endorheic basin (Tsagaan Els, Dornogobi, Mongolia): field data and conceptualization, three-dimensional groundwater modeling, and water budget
Pierre Grizard
; Jean-Michel Schmitt; Patrick Goblet
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. 145-160
Estimating the specific yield of the Pampeano aquifer, Argentina, using superconducting gravimeter data
Jonatan E. Pendiuk; Luis Guarracino; Marvin Reich; Claudio Brunini; Andreas Güntner
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. 2303-2313
Constant-head and variable-head injection tests for determining the hydraulic parameters of an aquitard
Yawen Xin; Zhifang Zhou; Zhi Dou; Mingwei Li; Jun Ma
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. 2359-2372
Inversion of hydrogeological parameters based on an adaptive dynamic surrogate model
Yong Liu; Jiannan Luo; Yu Xiong; Yeifei Ji; Xin Xin
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Inverse unsaturated-zone flow modeling for groundwater recharge estimation: a regional spatial nonstationary approach
Mohammad Karamouz; Hadi Meidani; Davood Mahmoodzadeh
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Groundwater recharge pathways to a weathered-rock aquifer system in a dryland catchment in Burkina Faso
Radegonde Rusagara; Mahamadou Koïta; Valérie Plagnes; Anne Jost
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Application of airborne and ground geophysics to unravel the hydrogeological complexity of the Deccan basalts in central India
Sahebrao Sonkamble; Subash Chandra; Paras R. Pujari
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
A dual-continuum model (TOUGH2) for characterizing flow and discharge in a mechanically disrupted sandstone overburden
Diego Bedoya-Gonzalez; Timo Kessler; Thomas Rinder; Maria-Theresia Schafmeister
<jats:title>Abstract</jats:title><jats:p>Underground hard coal mining usually disrupts the mechanical equilibrium of rock sequences, creating fractures within minor permeable rocks. The present study employs a dual-continuum model to assess how both fractured and porous sandstone media influence the percolation process in postmining setups. To test the approach, the software TOUGH2 was employed to simulate laminar fluid flow in the unsaturated zone of the Ibbenbüren Westfield mining area. Compared to other coal mining districts in Germany, this area is delineated by the topography and local geology, leading to a well-defined hydrogeological framework. Results reveal good agreement between the calculated and measured mine water discharge for the years 2008 and 2017. The constructed model was capable of reproducing the bimodal flow behavior of the adit by coupling a permeable fractured continuum with a low-conductivity rock matrix. While flow from the fractured continuum results in intense discharge events during winter months, the rock matrix determines a smooth discharge limb in summer. The study also evaluates the influence of individual and combined model parameters affecting the simulated curve. A detailed sensitivity analysis displayed the absolute and relative permeability function parameters of both continua among the most susceptible variables. However, a strong a priori knowledge of the value ranges for the matrix continuum helps to reduce the model ambiguity. This allowed for calibration of some of the fractured medium parameters for which sparse or variable data were available. However, the inclusion of the transport component and acquisition of more site-specific data is recommended to reduce their uncertainty.</jats:p>
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Groundwater-level recovery following closure of open-pit mines
Caglar Bozan; Ilka Wallis; Peter G. Cook; Shawan Dogramaci
<jats:title>Abstract</jats:title><jats:p>Open-pit mining has increased substantially over the past two decades. Many currently operating open-pit mines are facing the end of mine-life over the next few decades and, increasingly, focus is shifting towards mine-closure planning that provides evidence on available closure options under the given geological, hydro(geo)logical and climatic conditions. This study uses synthetic groundwater modelling to build basic process understanding of closure options and how these will determine the formation of pit lakes. This governs the long-term pit lake water quality and how postmining landscapes may be utilised. Simulations show that the recovery time of postmining groundwater levels increases with decreasing aquifer transmissivity. Final postmining water tables are predominantly controlled by the implemented mine closure options and climatic conditions. The most important decision is, thereby, whether to backfill the pit to above the water table or allow a pit lake to develop. Under moderately transmissive aquifer settings, backfilling of pits leads to rapidly rising groundwater levels within the first decade after mining, with water-table recoveries of above 70%. If mine voids remain unfilled, evaporation from the pit lake surface becomes a governing factor in determining whether the unfilled mine pit becomes a terminal sink for groundwater. Lake levels may remain subdued by several 10s of metres in arid to semiarid climates. If surplus surface water can be diverted into open pits, rapid filling can accelerate groundwater recovery of open pits in regions of low permeability. This is a less successful management option in transmissive aquifers.</jats:p>
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible