Hydrogeological Studies and Mapping on West Milan Area
|
|
- Peter Lambert
- 6 years ago
- Views:
Transcription
1 Hydrogeological Studies and Mapping on West Milan Area R.Bergamo, W.Danieli, D.de Bartolo, A.P.Gatti ARPA Lombardia, Dipartimento di Milano 1, Area di Tutela Ambientale Via Spagliardi 19, Parabiago (MI) ABSTRACT By means of GIS ArcView software, a map of the territory with wells, classified depending on their depth, was developed; in this way six best drawings for the hydrostratigraphic sections were chosen. The sections obtained enabled us to identify the geometry and the relations among the various groundwater layers in the whole territory. It was then possible to classify the water wells of the territory depending on the aquifer catchment; other maps, showing isolines of the depth of the layers bottom, were also implemented. INTRODUCTION AND PURPOSE This project was conceived and developed in order to define a detailed hydrogeologic structure of the territory of ARPA Lombardia Milano 1, with peculiar interest in the geometry and the relations among the groundwater layers. In fact, even if the whole territory extends in Po plain and is all made up of fluvioglacial and alluvial deposits, there are significant differences in hydrogeological structure of the various zones. So, it is a fundamental requirement, for those who deal with environmental subsoil problems, to have a flexible and preliminary tool, which can give swift and synthetic information on the aquifer geometry. Starting from this point, the aquifer characterization could be further investigated ( hydrodynamical properties, vulnerability, etc.) CHARACTERISTICS OF THE AREA Geology and hydrogeology of the territory This work has been developed starting from the general knowledge of geology and hydrogeology of Lombardy plain and from the wells database of the SIF ( Sistema Informativo Falda Groundwater Information System), a team coordinated by the Provincia of Milan and working with ARPA Milano 1 and various public agencies. The area under study extends in the west Milan Area. The subsoil, at water wells catchment depths, is made up of plio-pleistocenic sediments, which were classified by various authors in lithological or hydrostratigraphic or hydrogeological units (PROVINCIA DI MILANO and POLITECNICO DI MILANO, 1995); summing up, it is possible to see, from bottom to top, a clayey layer of marine origin, a sandy-clay layer of transition and continental origin (Villafranchiano), a conglomerate and sandstone layer (Ceppo), a sandy-gravel layer of fluvioglacial Riss-Mindel origin and a gravellysand layer of fluvioglacial Wurm origin (AVANZINI et al. 1995). Fluvioglacial Wurm deposits outcrop in almost the whole territory and constitute the main level of the plain; recent drifts along the Ticino and Olona river and the Mindel-Riss fluvioglacial terrace, which is located to the north of Garbagnate, almost ten meters high above the plain, are an exception. The Ceppo layer is just observed in the east part of the territory under study. It is possible to notice, passing downstream and increasing the depth, a progressive prevailing of the silty-clay terrain.
2 The plio-pleistocenic sediments are also influenced by deep tectonic structures which concern the premesozoic basement. A series of faults and overthrusts determine a progressive raising of the basement going eastward up to a maximum value in Monza area and whereas the overlying layers, even the pleistocenic ones, grow thinner in connection with the Monza horst (AVANZINI et al. 1995). For the subdivision of the groundwater layers, the classification of the aquifers in hydrostratigraphic units has been adopted (FRANCANI and POZZI, 1981); according to this classification, the first aquifer finds place in the gravelly-sand layer, the second in the sandy-gravel layer and in the Ceppo and the third in the sandy-clay layer. The first and the second aquifer, in such a way defined, constitute the traditional aquifer. In SIF database, about 4000 wells and 1000 piezometers of the territory under study are codified, with data relative to the principal characteristics (stratigraphy, x y coordinates, property, condition of the wells, usage, etc ). Almost 1250 of these points ( 1000 wells and 250 piezometers circa) have x y coordinates and stratigraphy and constitute the basis for this work. GIS APPLICATIONS By means of ArcView GIS software it was possible to develop a map of the whole territory, in which wells and piezometers are located and classified by means of different colors depending on the stratigraphy depth. The deepest well is about 275 m, whereas the most frequent depth class takes place between 100 and 150 m. This map ( see fig. 1 for a detail), enabled us to define the best layout for six stratigraphic sections which cross the whole territory according to the criterion to form a regularly spaced grid with three sections parallel to the principal flow lines (NNW-SSE) and three perpendicular, and to involve the most and deepest wells with known stratigraphy Another criterion which has led to choose the layout, was the intersection with most wells of the three piezometric monitoring SIF networks (first, second and third aquifer layer), because these wells were already classified depending on the water catchment. By utilizing the finding features within a specified distance Arcview function, the wells located within 300 m from the section drawing were selected; among them the most suitable, because of location and depth, were selected to add new data to the six stratigraphic sections. A long and exacting work was done to draw stratigraphic sections and to correlate the lithological levels. In that way the principal aquifers and aquicludes of the territory were located, also by means of a critical comparison with the existing bibliography and the pre-existing classification of the monitoring SIF net wells. The six sections were then schematically developed, by representing only the limits between the aquifer layers, the filter position of each well, and the piezometric level deduced by the piezometric map of the phreatic zone at September 2000 (SIF). Fig. 2 shows a detail of one schematic section. RESULTS AND CONCLUSIONS The study of the sections showed very interesting situations: In the northern part of the territory there are no interbedded silty-clay layers for a nearly 100 m depth; we have just one phreatic aquifer that only downstream divides in first and second aquifer, separated by an impervious layer. This fact is very well shown in fig.2. The bottom of the traditional aquifer (first and second layers) becomes less deep going from north to south.
3 Near the limit of the Mindel-Riss fluvioglacial terrace it is possible to point out a rapid change in aquifers depth. Going eastward it is possible to observe the gradual thinning of the traditional aquifer, because of the raising of its basis. The schematic reconstruction of the hydrogeologic structure, defined along the section drawings, consents to individuate the aquifer caught by all the wells of the territory, depending on the filter positions, even if not included in the sections: during this procedure we realized the need to add 4 hydrogeologic sections: two in the NNW-SSE and two in WSW-ENE direction. Fig. 3 shows, for a part of the territory, the result of the work: the wells which were in the beginning only classified depending on depth, can now be differentiated depending on aquifer catchment. A series of map with isobaths of the limits between aquifers was also developed by means of SURFER interpolation software and then imported by ArcView. The final result is a work tool which consents a rapid framing of the hydrogeologic condition, very useful for the development of the functions of ARPA, for instance: the individuation of the vulnerability degree of the wells in an area in which a spill occurred, the evaluation of the best depth of new catchments, the choice of how to close unused wells, the individuation of the recharge area of deep catchments. REFERENCES AVANZINI, M., BERETTA, G.P., FRANCANI, V., and NESPOLI, M., 1995, Indagine preliminare sull uso sostenibile delle falde profonde nella Provincia di Milano. FRANCANI, V., and POZZI, R., 1981, Condizioni di alimentazione delle riserve idriche del territorio milanese. La rivista della strada, L303, Milano PROVINCIA DI MILANO and POLITECNICO DI MILANO, 1995, Le risorse idriche sotterranee nella Provincia di Milano vol.1 : Lineamenti idrogeologici
4
5
A STUDY OF THE COASTAL AQUIFERS IN EMILIA-ROMAGNA REGION
TECNOLOGÍA DE LA INTRUSIÓN DE AGUA DE MAR EN ACUÍFEROS COSTEROS: PAÍSES MEDITERRÁNEOS IGME. Madrid 2003. ISBN. 84-7840-470-8 Molinari Fabio Carlo li.mo@libero.it Di Dio Gian Marco Tcoppola@regione.emilia-romagna.it
More informationAppendix D. Sediment Texture and Other Soil Data
5 6 7 8 Appendix D. Sediment Texture and Other Soil Data This appendix describes the sediment texture of the aquifer system in the Restoration Area. The contents of this appendix describe the: Importance
More informationPrediction of subsoil subsidence caused by opencast mining
Land Subsidence (Proceedings of the Fifth International Symposium on Land Subsidence, The Hague, October 1995). IAHS Publ. no. 234, 1995. 167 Prediction of subsoil subsidence caused by opencast mining
More informationEnhanced Characterization of the Mississippi River Valley Alluvial Aquifer Using Surface Geophysical Methods
Photo by Shane Stocks, U.S. Geological Survey Enhanced Characterization of the Mississippi River Valley Alluvial Aquifer Using Surface Geophysical Methods Presented by Ryan F. Adams US Geological Survey
More informationLand subsidence due to groundwater withdrawal in Hanoi, Vietnam
Land Subsidence (Proceedings of the Fifth International Symposium on Land Subsidence, The Hague, October 1995). 1AHS Publ. no. 234, 1995. 55 Land subsidence due to groundwater withdrawal in Hanoi, Vietnam
More informationEvolution of the conceptual hydrogeologic and ground-water flow model for Las Vegas Valley, Clark County, Nevada
Evolution of the conceptual hydrogeologic and ground-water flow model for Las Vegas Valley, Clark County, Nevada Geological Society of America Annual Meeting November 14, 2 David J. Donovan Southern Nevada
More information3.4 Typical Soil Profiles
SEI.UoC.0002.11 Figure 4. Streams in central Christchurch as mapped in March 1850, superposed on aerial photography captured on 24 February 2011. Streams digitised from the Black Map of Christchurch (March
More informationMathematical model of Baltic artesian basin
Mathematical model of Baltic artesian basin Juris Sennikovs, Janis Virbulis, and Uldis Bethers Laboratory for Mathematical Modelling of Environmental and Technological Processes UNIVERSITY OF LATVIA Contents
More informationImpact of the Danube River on the groundwater dynamics in the Kozloduy Lowland
GEOLOGICA BALCANICA, 46 (2), Sofia, Nov. 2017, pp. 33 39. Impact of the Danube River on the groundwater dynamics in the Kozloduy Lowland Peter Gerginov Geological Institute, Bulgarian Academy of Sciences,
More information3D Geological modeling of the coastal area in Emilia-Romagna, Italy
8 th EUREGEO 2015, June 15 th -17 th Barcelona 3D geological modeling of the coastal area of Emilia-Romagna, Italy. Calabrese et al. 3D Geological modeling of the coastal area in Emilia-Romagna, Italy
More informationINTRODUCTION Water resources are vitally important for the future of humankind. Groundwater from karst aquifers is among the most important drinking w
Vulnerability Mapping for the Protection of Carbonate (Karst) Aquifers (Ramallah-Al Bireh District) Eng. Amjad da Assi House of fw Water and de Environment May, 2007 INTRODUCTION Water resources are vitally
More informationENVIRONMENTAL EFFECTS OF GROUNDWATER WITHDRAWAL IN SOUTH NYÍRSÉG
PhD thesis ENVIRONMENTAL EFFECTS OF GROUNDWATER WITHDRAWAL IN SOUTH NYÍRSÉG János Szanyi Szeged, 2004 ENVIRONMENTAL EFFECTS OF GROUNDWATER WITHDRAWAL IN SOUTH NYÍRSÉG Preliminaries, the aims of the dissertation
More informationRESISTIVITY IMAGING AND BOREHOLE INVESTIGATION OF THE BANTING AREA AQUIFER, SELANGOR, MALAYSIA. A.N. Ibrahim Z.Z.T. Harith M.N.M.
JOURNAL OF ENVIRONMENTAL HYDROLOGY The Electronic Journal of the International Association for Environmental Hydrology On the World Wide Web at http://www.hydroweb.com VOLUME 11 2003 RESISTIVITY IMAGING
More information11/22/2010. Groundwater in Unconsolidated Deposits. Alluvial (fluvial) deposits. - consist of gravel, sand, silt and clay
Groundwater in Unconsolidated Deposits Alluvial (fluvial) deposits - consist of gravel, sand, silt and clay - laid down by physical processes in rivers and flood plains - major sources for water supplies
More information' International Institute for Land Reclamation and Improvement. 2 Groundwater Investigations. N.A. de Ridder'? 2.1 Introduction. 2.
2 Groundwater Investigations N.A. de Ridder'? 2.1 Introduction Successful drainage depends largely on a proper diagnosis of the causes of the excess water. For this diagnosis, one must consider: climate,
More informationLand subsidence induced by groundwater extraction in the Alto Guadalentín aquifer, SE Spain.
Land subsidence induced by groundwater extraction in the Alto Guadalentín aquifer, SE Spain. Pablo Ezquerro, Marta Béjar-Pizarro, Gerardo Herrera, José A. Fernández Merodo, Roberto Tomás, Carolina Guardiola-Albert,
More informationFinal Report on Development of Deep Aquifer Database and Preliminary Deep Aquifer Map
4 CHAPTER Final Report on Development of Deep Aquifer Database and Preliminary Deep Aquifer Map 31 Chronostragraphic Mapping 4.1 Introduction The analysis of geological logs was conducted during the project
More informationProposed Cemetery Thornhill Road. Tier One Hydrogeological Risk Assessment. Peter Mitchell Associates
Proposed Cemetery Thornhill Road Tier One Hydrogeological Risk Assessment Peter Mitchell Associates January 2015 Executive Summary This report uses a desk-based risk assessment technique published by the
More informationG. Barrocu G. Ranieri Faculty of Engineering, University of Cagliari, Italy. In the region of Muravera, south-east coast of Sardinia, the trend of
HYDROGEOLOGICAL AND GEOPHYSICAL INVESTIGATIONS FOR EVALUATING SALT INTRUSION PHENOMENA IN SARDINIA G. Barbieri G. Barrocu G. Ranieri Faculty of Engineering, University of Cagliari, Italy Abstract In the
More informationFoundations on Deep Alluvial Soils
Canterbury Earthquakes Royal Commission Hearings 25 October 2011, Christchurch GEO.CUB.0001.1-35.1 Foundations on Deep Alluvial Soils Misko Cubrinovski, Ian McCahon, Civil and Natural Resources Engineering,
More informationEvaluation of Subsurface Formation of Pabna District, Bangladesh
IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG) e-issn: 2321 0990, p-issn: 2321 0982.Volume 1, Issue 4 (Sep. Oct. 2013), PP 30-36 Evaluation of Subsurface Formation of Pabna District, Bangladesh
More informationHYDROGYEOLOGICAL CONDITIONS IN EGYPT REGWA
HYDROGYEOLOGICAL CONDITIONS IN EGYPT REGWA Introduction The purpose of this report is to present a summary of hydrogeological condition in Egypt. The main water-bearing formation in Egypt are the extensive
More informationBulletin of Earth Sciences of Thailand
Quantitative Seismic Geomorphology of Early Miocene to Pleistocene Fluvial System of Northern Songkhla Basin, Gulf of Thailand Oanh Thi Tran Petroleum Geoscience Program, Department of Geology, Faculty
More informationInverting hydraulic heads in an alluvial aquifer constrained with ERT data through MPS and PPM: a case study
Inverting hydraulic heads in an alluvial aquifer constrained with ERT data through MPS and PPM: a case study Hermans T. 1, Scheidt C. 2, Caers J. 2, Nguyen F. 1 1 University of Liege, Applied Geophysics
More informationPROCEEDINGS PIT IAGI YOGYAKARTA 2012 The 41 st IAGI Annual Convention and Exhibition
EG-25 COMPARING QUALITATIVE AND QUANTITATIVE METHOD TO DETERMINE EARTHQUAKE SUSCEPTIBILITY LEVEL AT KULON PROGO, YOGYAKARTA by: Deasy Rimanda Cahyaningtyas (1), Prof. Dr. Kirbani Sri Brotopuspito (2) Salahuddin
More informationHYBRID DETERMINISTIC AND STOCHASTIC HYDROSTRATIGRAPHIC MODELING OF A COMPLEX GLACIAL AQUIFER SYSTEM
HYBRID DETERMINISTIC AND STOCHASTIC HYDROSTRATIGRAPHIC MODELING OF A COMPLEX GLACIAL AQUIFER SYSTEM Lawrence D. Lemke, Andrew L. Frahm, Lena K. Pappas Department of Geology, Wayne State University, Detroit,
More informationGeology (Mellow) Hike, Santa Lucia Memorial Park February 16, I. Overview of Santa Lucia Range geology and tectonic history
Geology (Mellow) Hike, Santa Lucia Memorial Park February 16, 2015 I. Overview of Santa Lucia Range geology and tectonic history A. Basement Rocks 1. Salinian Block Rocks Sierra Nevada Type, continental
More informationIPMO2-1. Groundwater Modelling of Chiang Rai Basin, Northern Thailand. Sattaya Intanum* Dr.Schradh Saenton**
IPMO2-1 Groundwater Modelling of Chiang Rai Basin, Northern Thailand Sattaya Intanum* Dr.Schradh Saenton** ABSTRACT Chiang Rai basin, situated in Chiang Rai and Phayao provinces covering an area of 11,000
More informationSITE INVESTIGATION STRATEGY (SIS) FOR NORISC. Checklist (ver 2.0)
FOR NORISC Checklist (ver 2.0) Ulf Qvarfort*, Gerhard Schwarz* and the NORISC group *) Geological Survey of Sweden Contents Pre-Investigation Phase: Site characterisation and target definition Investigation
More informationINTERNATIONAL JOURNAL OF GEOMATICS AND GEOSCIENCES Volume 5, No 2, 2014
INTERNATIONAL JOURNAL OF GEOMATICS AND GEOSCIENCES Volume 5, No 2, 2014 Copyright by the authors - Licensee IPA- Under Creative Commons license 3.0 Research article ISSN 0976 4380 Disposition of aquifer
More informationSECTION 4 TABLES. 1 Summary of Hydrogeologic Parameters for Various Stratigraphic Units FIGURES
SECTION 4 4.0 OVERVIEW OF GEOLOGY AND HYDROGEOLOGY... 13 4.1 Comparison of East and West Sides of Study Area... 15 4.2 Bedrock Sequence... 17 4.3 Mancos Shale (Upper Cretaceous)... 18 4.4 Mesaverde Formation
More informationdepression above scarp scarp
1 LAB 1: FIELD TRIP TO McKINLEYVILLE AND MOUTH OF THE MAD RIVER OBJECTIVES: a. to look at geomorphic and geologic evidence for large scale thrust-faulting of young sediments in the Humboldt Bay region
More informationLAND SUBSIDENCE IN THE AREA OF MODENA, PO VALLEY, NORTHERN ITALY
LAND SUBSIDENCE IN THE AREA OF MODENA, PO VALLEY, NORTHERN ITALY A. Colombetti, R. Gelmini - Institute of Geology, Univ. of Modena, Italy M. Pellegrini - Dept. Earth Sciences, Univ. of Bologna, Italy N.
More informationChapter 8 Fetter, Applied Hydrology 4 th Edition, Geology of Groundwater Occurrence
Chapter 8 Fetter, Applied Hydrology 4 th Edition, 2001 Geology of Groundwater Occurrence Figure 8.42. Alluvial Valleys ground-water region. Fetter, Applied Hydrology 4 th Edition, 2001 Fetter, Applied
More informationThe Milan agglomeration Strategic Noise Map
Edinburgh, Scotland EURONOISE 2009 October 26-28 The Milan agglomeration Strategic Noise Map Giovanni Zambon a Simone Radaelli b Università degli Studi di Milano-Bicocca, Dipartimento di Scienze dell Ambiente
More informationEnvrionmental impact assessment of urban development plan by vulnerability model application
International Journal of Environmental Science & Technology Vol., No., pp. 7-, Spring Environmental impact assessment Envrionmental impact assessment of urban development plan by vulnerability model application
More informationV S and N SPT Measures for Seismic Characterization of Soils
V S and Measures for Seismic Characterization of Soils 218 Giovanna Vessia, Mario Luigi Rainone, and Patrizio Signanini Abstract Seismic classification of soils for designing purposes can be addressed
More information2. REGIS II: PARAMETERIZATION OF A LAYER-BASED HYDROGEOLOGICAL MODEL
HYDRAULIC PARAMETERIZATION OF 3D SUBSURFACE MODELS: FROM MEASUREMENT-SCALE TO MODEL-SCALE Jan L. Gunnink, Jan Stafleu, Denise Maljers and Jan Hummelman TNO Geological Survey of the Netherlands, P.O. Box
More informationInternational Workshop on Groundwater Systems in Europe, August, 2013 Berlin
Hydrogeological Mapping in Albania From the IHME contribution to larger scale national maps R. Eftimi, I. Tafilaj, G. Bisha & Xh. Sheganaku Mali me Gropa karst plateau Selita spring The hydrogeological
More informationA NOVEL APPROACH TO GROUNDWATER MODEL DEVELOPMENT. Thomas D. Krom 1 and Richard Lane 2
A NOVEL APPROACH TO GROUNDWATER MODEL DEVELOPMENT Thomas D. Krom 1 and Richard Lane 2 1 Touch Water Ltd., P.O. Box 143, Lincoln, Christchurch, New Zealand; email: touchwater@gmail.com 2 Applied Research
More informationGOVERNMENT OF NEPAL MINISTRY OF IRRIGATION GROUND WATER RESOURCES DEVELOPMENT BOARD BABARMAHAL, KATHMANDU, NEPAL
GOVERNMENT OF NEPAL MINISTRY OF IRRIGATION GROUND WATER RESOURCES DEVELOPMENT BOARD BABARMAHAL, KATHMANDU, NEPAL GIS Based Updating of Groundwater Level Siraha District Final Report Submitted to Ground
More informationAssessing the Ground Response to Urbanization in the Fiumicino area by Combining Geological and Geotechnical Data with Satellite InSAR Data
Assessing the Ground Response to Urbanization in the Fiumicino area by Combining Geological and Geotechnical Data with Satellite InSAR Data P. Mazzanti F. Bozzano, C. Esposito, M. Patti, A. Rocca La Missione
More informationSequence Stratigraphy as a tool for water resources management in alluvial coastal aquifers: application to the Llobregat delta (Barcelona, Spain)
Sequence Stratigraphy as a tool for water resources management in alluvial coastal aquifers: application to the Llobregat delta (Barcelona, Spain) Desiré Gàmez Torrent December 2007 CHAPTER 1: Introduction
More informationA method for three-dimensional mapping, merging geologic interpretation, and GIS computation
A method for three-dimensional mapping, merging geologic interpretation, and GIS computation Soller, David R., U.S. Geological Survey, 908 National Center, Reston, VA 20192 and Richard C. Berg, Illinois
More informationINVESTIGATING AND UNDERSTANDING THE GROUND WHY BOTHER?
INVESTIGATING AND UNDERSTANDING THE GROUND WHY BOTHER? Dr Jacqueline Skipper Geotechnical Consulting Group WHAT IS UNDERSTANDING THE GROUND? Site Good enough ground model for successful project construction
More informationGIS Ostrava Surface models for geosciencesjanuary , 2012, Ostrava
A CONCEPTUAL HYDROGEOLOGICAL MODEL FOR THE OPEN PIT MINE POLJE E (KOLUBARA COAL BASIN, SERBIA) Dragoljub, Bajić 1, Dušan, Polomčić 2 1 Department of hydrogeology, Faculty of mining and geology, University
More informationGROUNDWATER OCCURRENCE IN KENYA
GROUNDWATER OCCURRENCE IN KENYA Steven Okoth Owuor Ministry of Water and Sanitation Sunday, January 20, 2019 1 Geography INTRODUCTION The Republic of Kenya is located in East Africa The total area of the
More informationOn the sources of salinity in groundwater under plain areas. Insights from δ 18 O, δ 2 H and hydrochemistry in the Azul River basin, Argentina
On the sources of salinity in groundwater under plain areas. Insights from δ 18 O, δ 2 H and hydrochemistry in the Azul River basin, Argentina M.E. Zabala a, M. Manzano b, M. Varni a, P. Weinzettel a a
More informationBuried-valley Aquifers: Delineation and Characterization from Reflection Seismic and Core Data at Caledon East, Ontario
Buried-valley Aquifers: Delineation and Characterization from Reflection Seismic and Core Data at Caledon East, Ontario Russell, H.A.J. 1, S.E. Pullan 1, J.A. Hunter 1, D.R. Sharpe 1, and S. Holysh 2 1
More informationTHE ROLE OF 3-D GEOLOGIC MODELING AND DATABASE SOLUTIONS IN THE VIRTTAANKANGAS ARTIFICIAL RECHARGE PROJECT, SOUTHWESTERN FINLAND
THE ROLE OF 3-D GEOLOGIC MODELING AND DATABASE SOLUTIONS IN THE VIRTTAANKANGAS ARTIFICIAL RECHARGE PROJECT, SOUTHWESTERN FINLAND Artimo, A. 1, S. Saraperä 2, and I. Ylander 1 1 Turku Region Water Ltd.,
More informationGEOLOGICAL AND HYDROGEOLOGICAL CONSIDERATIONS ON THE PHREATIC AQUIFER OF THE TARNAVA MICA RIVER FLOOD PLAIN AND TERRACES
GEOLOGICAL AND HYDROGEOLOGICAL CONSIDERATIONS ON THE PHREATIC AQUIFER OF THE TARNAVA MICA RIVER FLOOD PLAIN AND TERRACES E. RADU 1, M. RADESCU, C. RADU, A. PANDELE, M. MINCIUNA ABSTRACT. Geological and
More informationAPPLICATION OF THE TRUNCATED PLURIGAUSSIAN METHOD TO DELINEATE HYDROFACIES DISTRIBUTION IN HETEROGENEOUS AQUIFERS
XIX International Conference on Water Resources CMWR 2012 University of Illinois at Urbana-Champaign June 17-22, 2012 APPLICATION OF THE TRUNCATED PLURIGAUSSIAN METHOD TO DELINEATE HYDROFACIES DISTRIBUTION
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 14: Sedimentary Rocks Part 2: Alluvial Fans and Rivers Instructor: Dr. Douglas W. Haywick Last Time 1) Types of Sediment 2) Sedimentary Rock
More informationAWRA PMAS Engineers Club of Philadelphia. A Geologic Perspective on Stormwater
AWRA PMAS Engineers Club of Philadelphia A Geologic Perspective on Stormwater Toby J. Kessler, P.G. Hydrogeologist Trevor G. Woodward, P.G. Engineering Geologist September 10, 2014 Gilmore & Associates,
More informationDrift Filled Hollows Examples from Crossrail. John Davis Crossrail Chief Engineer s Group
Drift Filled Hollows Examples from Crossrail John Davis Crossrail Chief Engineer s Group The Crossrail route in Central London Crossrail route with the northern Thames Tributaries & some major geological
More informationGeology and Soils. Technical Memorandum
Geology and Soils Technical Memorandum TO: FDOT FROM: HDR, Inc. DATE: February 2013 PROJECT: St Johns River Crossing FPID No: 208225-3-21-01 Clay, Duval, and St. Johns Counties; Florida Geology and soils
More informationIntegrated geological approach to the study of coastal subsidence in Emilia-Romagna. Luisa PERINI Calabrese Lorenzo, Luciani Paolo, Severi Paolo,
Integrated geological approach to the study of coastal subsidence in Emilia-Romagna Luisa PERINI Calabrese Lorenzo, Luciani Paolo, Severi Paolo, Subsidence hazard of Emilia-Romagna coastal plain Caputo
More informationCRITERIA FOR DEFINING THE SERIES (DAR, 2006)
CRITERIA FOR DEFINING THE SERIES (DAR, 2006) On the Soils Map of Catalonia (1:25 000), the soil series are defined on the basis of the following hierarchically organised criteria. Classification at the
More informationREGIONAL GEOLOGY IN KHMER BASIN
CONTENTS 1-Khmere Basin 2-Regional Geology Khmer Basin 3-Regime Tectonic 4-Seismic Database -a/ Acquisition Data -b/ Prospect Angkor -C/ Cross Section Seismic 5-Play Type -a/ Play Schematic -b/ Structure
More informationStructural Style and Tectonic Evolution of the Nakhon Basin, Gulf of Thailand
Structural Style and Tectonic Evolution of the Nakhon Basin, Gulf of Thailand Piyaphong Chenrai Petroleum Geoscience Program, Department of Geology, Faculty of Science, Chulalongkorn University, Bangkok
More informationVu Ngoc Ky Academy of Mining and Geology Hanoi, Vietnam
HYDROGEOLOGICAL CONDITIONS IN TiiE MAIN COAL BASINS OF VIETNAM Vu Ngoc Ky Academy of Mining and Geology Hanoi, Vietnam ABSTRACT Three problems are presented in the following paper: l.distribution and general
More informationHYDROGEOLOGICAL PROPERTIES OF THE UG2 PYROXENITE AQUIFERS OF THE BUSHVELD COMPLEX
R. Gebrekristos, P.Cheshire HYDROGEOLOGICAL PROPERTIES OF THE UG2 PYROXENITE AQUIFERS OF THE BUSHVELD COMPLEX R. Gebrekristos Digby Wells Environmental P. Cheshire Groundwater Monitoring Services Abstract
More informationDETECTION OF GROUNDWATER POLLUTION USING RESISTIVITY IMAGING AT SERI PETALING LANDFILL, MALAYSIA
JOURNAL OF ENVIRONMENTAL HYDROLOGY The Electronic Journal of the International Association for Environmental Hydrology On the World Wide Web at http://www.hydroweb.com VOLUME 8 2000 DETECTION OF GROUNDWATER
More informationCorrelation of gravel deposits from trenching project on Alder Creek fluvial terrace near Point Arena, California
Correlation of gravel deposits from trenching project on Alder Creek fluvial terrace near Point Arena, California Aletha Lee Department of Geology and Geography, West Virginia University, White Hall, Morgantown,
More information- Cased-hole geophysical well logs - Airborne geophysics - Seismic data - LiDAR. GeoConvention 2015: New Horizons 1
Thermal Effects and Quaternary Hydrogeology: Making Good Decisions in a Complex Geologic Setting Timothy Johnsen, Phd, Quaternary Specialist (tjohnsen@matrix-solutions.com) Alex Haluszka, MSc, P.Geol.,
More informationLower Mainland Surficial Geology From Wisconsin Ice Age to Protocol 21
Lower Mainland Surficial Geology From Wisconsin Ice Age to Protocol 21 BCEIA BEST Conference 2018 Whistler, BC Kalina Malowany and Virginie Brunetaud Presentation Outline 1. Surficial Geology it s more
More informationVertical Electrical Sounding Survey for Groundwater Exploration in Parts of Anyigba and its Environs, in the Anambra Basin of Nigeria
British Journal of Applied Science & Technology 4(): 978-988, 204 SCIENCEDOMAIN international www.sciencedomain.org Vertical Electrical Sounding Survey for Groundwater Exploration in Parts of and its Environs,
More informationBasin Analysis Applied to Modelling Buried Valleys in the Great Lakes Basin
EARTH SCIENCES SECTOR GENERAL INFORMATION PRODUCT 35 Basin Analysis Applied to Modelling Buried Valleys in the Great Lakes Basin Sharpe, D R; Russell, H A J 2004 Originally released as: Basin Analysis
More informationThe Geology of Sebago Lake State Park
Maine Geologic Facts and Localities September, 2002 43 55 17.46 N, 70 34 13.07 W Text by Robert Johnston, Department of Agriculture, Conservation & Forestry 1 Map by Robert Johnston Introduction Sebago
More informationAPPLICATION OF ELECTRICAL RESISTIVITY TOMOGRAPHY FOR SAND UNDERWATER EXTRACTION
International Scientific Conference GEOBALCANICA 2018 APPLICATION OF ELECTRICAL RESISTIVITY TOMOGRAPHY FOR SAND UNDERWATER EXTRACTION Maya Grigorova Ivaylo Koprev University of Mining and Geology St. Ivan
More information1-D Electrical Resistivity Survey For Groundwater In Ketu-Adie Owe, Ogun State, Nigeria.
IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG) e-issn: 2321 0990, p-issn: 2321 0982.Volume 3, Issue 5 Ver. I (Sep. - Oct. 2015), PP 75-82 www.iosrjournals.org 1-D Electrical Resistivity Survey
More informationAirborne Geophysics to Map Groundwater. Bill Brown
Airborne Geophysics to Map Groundwater Bill Brown bb@skytem.com A 6 borehole represents 1 millionth of an acre Aquifer Materials An aquifer is an underground layer of water bearing permeable rock, rock
More informationPRELIMINARY. Select Geophysical Methods and Groundwater Modeling: Examples from USGS studies. Claudia Faunt and a cast of others
Select Geophysical Methods and Groundwater Modeling: Examples from USGS studies Claudia Faunt and a cast of others Current Preliminary Studies Stanford Water in the West Groundwater Data Workshop Series:
More informationGalilee Basin. Galilee Basin Hydrogeological Investigations. Briefing to RAPAD Longreach, 16 May rpsgroup.com.au
Galilee Basin Galilee Basin Hydrogeological Investigations Briefing to RAPAD Longreach, 16 May 20116 1 The Galilee Basin Geologically & hydrogeological diverse sedimentary Covers 247,000 km 2 The Galilee
More informationLocation of protection zones along production galleries: an example of methodology
Tracers and Modelling in Hydrogeology (Proceedings of the TraM'2000 Conference held at Liège, Belgium, May 2000). IAHS Publ. no. 262, 2000. 141 Location of protection zones along production galleries:
More informationFrom 2D Seismic to Hydrodynamic Modelling
From 2D Seismic to Hydrodynamic Modelling A Complex Study of Turbidites in a Petroleum-Bearing Basin Marcell Lux, HC Exploration Geologist Ahmed Amran, HC Exploration Advisor Marianna Vincze, Geomodel
More informationDewatering tests results for underground C Line stations construction
Geotechnical Aspects of Underground Construction in Soft Ground Viggiani (ed) 12 Taylor & Francis Group, London, ISBN 978--415-68367-8 Dewatering tests results for underground C Line stations construction
More informationEVALUATION OF AQUIFER CHARACTERISTICS FOR SELECTED NEW METHOD OF THE UM RUWABA FORMATION: NORTH KORDOFAN STATE, SUDAN
EVALUATION OF AQUIFER CHARACTERISTICS FOR SELECTED NEW METHOD OF THE UM RUWABA FORMATION: NORTH KORDOFAN STATE, SUDAN ELHAGA.B *1; ELZIENS.M*2 ANDLISSANN.H*3 *1Department of C i v i l E n g i n e e r i
More informationGroundwater in Bayfield County
Groundwater in Bayfield County Presented to Bayfield County Large Scale Livestoc Study Committee April 23, 2015 Madeline Gotowitz Hydrogeologist Groundwater in Bayfield County Groundwater basics Hydrogeology
More informationObjectives. to map land subsidence at a basin scale through spaceborne
Dipartimento di Scienze della Terra www.geo.unifi.it Tele-Rilevamento Europa TRE, a POLIMI spin-off company Land subsidence mapping and monitoring through PSInSAR: examples from the Arno river basin (Italy)
More informationAssessing Groundwater Vulnerability and Contaminant Pathways at MCAS Beaufort, SC
Assessing Groundwater Vulnerability and Contaminant Pathways at MCAS Beaufort, SC James M. Rine, John M. Shafer, Elzbieta Covington Abstract A project to assess the vulnerability of groundwater resources
More informationURBAN HYDROLOGY: WATER IN THE CITY OF TSHWANE Plant Sciences Auditorium, University of Pretoria January 2014 URBAN HYDROGEOLOGY
URBAN HYDROLOGY: WATER IN THE CITY OF TSHWANE Plant Sciences Auditorium, University of Pretoria 23 24 January 2014 URBAN HYDROGEOLOGY MATTHYS A. DIPPENAAR DEPARTMENT GEOLOGY, UNIVERSITY OF PRETORIA HYDROGEOLOGY
More informationDipartimento di Ingegneria Civile, Edile-Architettura e Ambientale, Università degli Studi dell Aquila, Italy 2
Comparison between shallow geology, resonance frequency and buildings damage due to the April 6, 2009 Mw 6.1 and the February 2, 1703 Mw 6.7 earthquakes at L Aquila historical downtown M. Tallini 1, F.
More informationThe Nubian Sandstone Aquifer System. Martina Müller Claudia Dengler Felix Leicht
The Nubian Sandstone Aquifer System Martina Müller Claudia Dengler Felix Leicht Geography Transboundary groundwater system beneath the north-eastern Sahara total extension of over 2.2 Mio km² Shared between
More informationGroundwater Dynamics and Quality Assessment in an Agricultural Area
American Journal of Environmental Sciences 7 (4): 354-361, 2011 ISSN 1553-345X 2011 Science Publications Groundwater Dynamics and Quality Assessment in an Agricultural Area Stefano Lo Russo, Adriano Fiorucci
More information4.3. Geomorphologic route along the Urasalakh River
The Expedition Lena-Anabar 2003 4 Periglacial studies around Cape Mamontov Klyk 4.3. Geomorphologic route along the Urasalakh River Dimitri Bolshiyanov and Alexander Makarov 4.3.1 Structure of Quaternary
More informationGPR survey and field work summary in Siilinjärvi mine during July 2014
GEOLOGICAL SURVEY OF FINLAND Groundwater Espoo 21.6.2016 67/2016 GPR survey and field work summary in Siilinjärvi mine during July 2014 Samrit Luoma, Juha Majaniemi, Tiina Kaipainen, and Antti Pasanen
More informationAnalysis of the temporal and spatial variations of the chloride concentration in the Río Mojotoro basin
Analysis of the temporal and spatial variations of the chloride concentration in the Río Mojotoro basin Jacqueline Köhn, Eduardo Kruse & Jerónimo Ainchil Facultad de Ciencias Astronómicas y Geofísicas
More informationLand subsidence due to groundwater withdrawal from the semi-confined aquifers of southwestern Flanders
Land Subsidence (Proceedings of the Fifth International Symposium on Land Subsidence, The Hague, October 1995). IAHS Publ. no. 234, 1995. 47 Land subsidence due to groundwater withdrawal from the semi-confined
More informationApplication of Aquifer Vulnerability Index (AVI) method to assess groundwater vulnerability to contamination in Semarang urban area
Application of Aquifer Vulnerability Index (AVI) method to assess groundwater vulnerability to contamination in Semarang urban area Thomas Triadi Putranto 1*, Narulita Santi 1, Dian Agus Widiarso 1, and
More informationA hydrogeological study of the Nhandugue River, Mozambique A major groundwater recharge zone
A hydrogeological study of the Nhandugue River, Mozambique A major groundwater recharge zone Arvidsson, Kristina; Stenberg, Li; Chirindja, Farisse; Owen, Richard; Dahlin, Torleif Published in: Physics
More informationSeepage Analysis for Shurijeh Reservoir Dam Using Finite Element Method. S. Soleymani 1, A. Akhtarpur 2
Seepage Analysis for Shurijeh Reservoir Dam Using Finite Element Method S. Soleymani 1, A. Akhtarpur 2 1 Group of Dam Construction, Toossab Company, P.O. Box 917751569, Mashhad City, Iran, PH (+98) 511-7684091;
More informationPROANA A USEFUL SOFTWARE FOR TERRAIN ANALYSIS AND GEOENVIRONMENTAL APPLICATIONS STUDY CASE ON THE GEODYNAMIC EVOLUTION OF ARGOLIS PENINSULA, GREECE.
PROANA A USEFUL SOFTWARE FOR TERRAIN ANALYSIS AND GEOENVIRONMENTAL APPLICATIONS STUDY CASE ON THE GEODYNAMIC EVOLUTION OF ARGOLIS PENINSULA, GREECE. Spyridoula Vassilopoulou * Institute of Cartography
More informationGroundwater Sequence Stratigraphy:
Groundwater Sequence Stratigraphy: A Geology-based Approach for Developing Accurate and Representative Hydrogeologic Conceptual Models for Successful Groundwater Sustainability Plans Rick Cramer, Burns
More informationOak Ridges Moraine Aquifer Vulnerability Mapping
Accompanying Document to the Reference Map for Ontario Regulation 140/02 (Oak Ridges Moraine Conservation Plan) March 2004 2 1. Purpose of Report Accompanying Document to the Reference Map for Ontario
More informationiii CONTENTS vii ACKNOWLEDGMENTS EXECUTIVE SUMMARY INTRODUCTION Study Area Data Sources Preparation of Geologic Maps
CONTENTS ACKNOWLEDGMENTS EXECUTIVE SUMMARY INTRODUCTION Study Area Data Sources Preparation of Geologic Maps GEOLOGY Bedrock Geology Succession and Distribution Structural Features Description of Bedrock
More information3.0 GEOLOGY AND HYDROGEOLOGY
3.0 GEOLOGY AND HYDROGEOLOGY 3.1 Methodology The Geological Survey of Ireland (GSI) publication Geology of South Cork was consulted to establish the nature of the bedrock lithology and Quaternary sediments.
More informationNewcastle West GWB: Summary of Initial Characterisation.
Newcastle West GWB: Summary of Initial Characterisation. Hydrometric Area Local Authorities 24 - Deel/ Shannon Estuary Limerick Co. Co. Topography Associated surface water features Rivers: Deel, Daar,
More informationQUATERNARY SEQUENCE GRID-BASED HYDROSTRATIGRAPHIC 3D MODELLING BY THE RELATIVE METHOD, CHÂTEAUGUAY RIVER WATERSHED, QUEBEC
QUAERNARY SEQUENCE GRID-BASED HYDROSRAIGRAPHIC 3D MODELLING BY HE RELAIVE MEHOD, CHÂEAUGUAY RIVER WAERSHED, QUEBEC ommy remblay 1, Miroslav Nastev 2, Michel Lamothe 1 1 UQAM, Département des Sciences de
More informationSequence Stratigraphy. Historical Perspective
Sequence Stratigraphy Historical Perspective Sequence Stratigraphy Sequence Stratigraphy is the subdivision of sedimentary basin fills into genetic packages bounded by unconformities and their correlative
More information