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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
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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
Analyzing spatio-temporal mechanisms of land subsidence in the Parowan Valley, Utah, USA
Jiawei Li
; Ryan Smith; Katherine Grote
<jats:title>Abstract</jats:title><jats:p>Parowan Valley, Utah (USA), is an agricultural region experiencing rapid subsidence due to extensive groundwater extraction from aquifers with a significant portion of fine-grained sediments. To analyze the subsidence spatio-temporally, time-series Interferometric Synthetic Aperture Radar (InSAR) of 155 Sentinel-1 C-band scenes were processed. These data showed approximately 30 cm of ground subsidence in Parowan Valley from 2014 to 2020. Because of the high temporal sampling rate of the Sentinel-1 satellite (12-day cycle), it is possible to determine the seasonal changes of ground deformation and relate this to groundwater extraction. To better understand the relationship between ground deformation and groundwater extraction in the Parowan Valley, temporal changes in hydraulic head data from US Geological Survey observation wells were monitored. Additionally, well logs were analyzed and used to construct a map that showed the percentage of fine-grained material in the subsurface. The investigation of hydraulic head and geology, together with InSAR-derived ground displacement data, indicates that the most subsidence occurs where there is a co-occurrence of high groundwater demand and a high percentage of fine-grained sediments, but recharge likely plays a role in mitigating subsidence in some areas. The subsidence developed in Parowan Valley shows a long-term trend as well as seasonal variation and appears to be influenced by both agricultural activity and annual precipitation.</jats:p>
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Correction: Groundwater and climate change: threats and opportunities
Tibor Y. Stigter; Jodie Miller; Jianyao Chen; Viviana Re
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
A framework for assessing the 4th rank dispersivity tensor under anisotropic axial symmetries
Xiang Fan; Donald M. Reeves
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Combining harmonic pumping with a tracer test for fractured aquifer characterization
Arezou Dodangeh; Mohammad Mahdi Rajabi; Marwan Fahs
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Analysis of water inrush at Dongyu coal mine in China from an old water-logged goaf associated with a syncline fractured zone
Kai Ma; Tianhong Yang; Wenxue Deng; Xiangang Hou; Zhenshuan Li; Yong Zhao; Yilong Liu; Yuan Gao; Dongdong Sun; Junxu Hou
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Quantification of normal and sustainable management practices for groundwater resources: example of the arid Najafabad alluvial aquifer in Isfahan Province, Iran
Mostafa Naderi; Mohammad Hajiketabi
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Analysis of groundwater flow through low-latitude alpine permafrost by model simulation: a case study in the headwater area of Yellow River on the Qinghai-Tibet Plateau, China
Shuhui Gao; Huijun Jin; Qingbai Wu; Victor F. Bense; Dongliang Luo; Qingfeng Wang; Yuzhong Yang; Wenwen Chang
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
The impact of groundwater recharge on land subsidence: a case study from the Cangzhou test area, Hebei Province, China
Xin Wang; Zujiang Luo; Zhao Li; Qian Zhao; Jing Dai
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Correction: The 21st century water quality challenges for managed aquifer recharge: towards a risk-based regulatory approach
Yan Zheng; Joanne Vanderzalm; Niels Hartog; Enrique Fernández Escalante; Catalin Stefan
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible
Distribution of tritium-helium groundwater ages in a large Cenozoic sedimentary basin (North German Plain)
Annika Desens; Georg Houben; Jürgen Sültenfuß; Vincent Post; Gudrun Massmann
<jats:title>Abstract</jats:title><jats:p>The travel time of groundwater plays a major role in the understanding of hydrogeological systems; however, large data sets necessary for regional studies of groundwater age are rare. In this study, a unique large data set of groundwater samples analysed for tritium and helium isotopes collected over the last 20 years from Cenozoic aquifers of the North German Plain is explored. Hereby, the variety of natural and technical influences on the tritium-helium age, including screen depth and length, groundwater recharge rate and climatic effects, are investigated. To a sampling depth of ~40 m below ground level, the median tritium-helium age increases almost linearly with depth, reaching a maximum of 40 years. Below, the portion of older, tritium-free water rises. The tritium-helium ages of the tritium-bearing portion increase only slightly to a maximum of about 46 years. The depth distribution of the tritium-helium age shows a dependency on groundwater recharge rates. Considering the same depth level, younger ages are related to higher groundwater recharge rates as compared to groundwater that infiltrated in areas with lower recharge rates. This is especially observed for shallow depths. Tritium-helium ages younger than 40 years are reflected well in the atmospheric tritium input curves, while deviations from it can be related to anthropogenic influences such as input from nuclear power plants and irrigation with deep, tritium-poor groundwater. The regional distribution for shallow wells indicates increasing tritium-helium ages from west to east, corresponding to decreasing groundwater recharge rates due to the more continental climate in the east.</jats:p>
Palabras clave: Earth and Planetary Sciences (miscellaneous); Water Science and Technology.
Pp. No disponible