2013
DOI: 10.1007/s12665-013-2694-3
|View full text |Cite
|
Sign up to set email alerts
|

Building a 3D geomodel for water resources management: case study in the Regional Park of the lower courses of Manzanares and Jarama Rivers (Madrid, Spain)

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
3
0

Year Published

2015
2015
2023
2023

Publication Types

Select...
7
2

Relationship

0
9

Authors

Journals

citations
Cited by 18 publications
(6 citation statements)
references
References 8 publications
0
3
0
Order By: Relevance
“…The basement of the aquifer and its sidewalls are formed by Tertiary sedimentary units, which consist mainly of gypsum with intercalated beds of carbonate rocks and mudstones (Fig. 2) (Calvo et al 1989;Carreño Conde et al 2014). The aquifer has an average thickness of 10.97m and is characterized by a storage coe cient and a transmissivity of 0.07 and 700 m 2 /d, respectively (Bardají et al, 1990).…”
Section: Study Areamentioning
confidence: 99%
See 1 more Smart Citation
“…The basement of the aquifer and its sidewalls are formed by Tertiary sedimentary units, which consist mainly of gypsum with intercalated beds of carbonate rocks and mudstones (Fig. 2) (Calvo et al 1989;Carreño Conde et al 2014). The aquifer has an average thickness of 10.97m and is characterized by a storage coe cient and a transmissivity of 0.07 and 700 m 2 /d, respectively (Bardají et al, 1990).…”
Section: Study Areamentioning
confidence: 99%
“…The "Aluviales Jarama-Tajuña" aquifer is uncon ned, according to lithological sections (Fig. 2b) and pumping test (Carreño Conde et al 2014). Therefore, 100% of study area is uncon ned aquifer and the map of groundwater occurrence (G) is de ned by a single value equal to one (1) according to GOD method.…”
Section: God Vulnerability Analysismentioning
confidence: 99%
“…Geologically, the Parque Regional del Sureste is characterized by the presence of two fundamental lithological domains: the Neogene tertiary and the Quaternary [25]. The geological location of the settling pond is the Vega Baja del Jarama, characterized by the development of a large number of stream terraces, associated with Quaternary climatic oscillations, isostatic uplift tectonics and block adjustments, and lithological-structural controls [26]. The main lithology of these terraces is formed by gravel bars and/or sand with limited sand fraction [27], besides alterations in the conglomerate, silt and clay.…”
Section: Settling Ponds Descriptionmentioning
confidence: 99%
“…In recent years, domestic and foreign scholars have absorbed theories and technologies such as computer visualization and graphic imaging to conduct research on the theory and methods of true three-dimensional geoscience modeling. At the same time, scholars have conducted beneficial explorations in the expression and organization of topological relationships among geological objects [6][7][8][9][10] . It should be noted that 3D visualization of geological modeling and 3D geographic information systems are two high-tech fields that are currently developing in parallel within the field of geosciences.…”
Section: Introductionmentioning
confidence: 99%