Geochemical processes, weathering, and groundwater recharge in catchments

Cover of: Geochemical processes, weathering, and groundwater recharge in catchments |

Published by Balkema in Rotterdam, Brookfield, Vt., USA .

Written in English

Read online

Subjects:

  • Watersheds.,
  • Hydrogeology.,
  • Groundwater recharge.

Edition Notes

Includes bibliographical references and index.

Book details

Statementedited by Ola M. Saether & Patrice de Caritat.
ContributionsSaether, Ola M., Caritat, Patrice de.
Classifications
LC ClassificationsGB980 .G36 1997
The Physical Object
Paginationxiv, 400 p. :
Number of Pages400
ID Numbers
Open LibraryOL125323M
ISBN 109054106417, 9054106468
LC Control Number99496413
OCLC/WorldCa36657189

Download Geochemical processes, weathering, and groundwater recharge in catchments

Geochemical Processes, Weathering and Groundwater Recharge in Catchments is a specialist book concerned with the natural processes taking place where water interacts with minerals and organic matter at the earth’s surface, in soils or within by: Geochemical processes, weathering and groundwater recharge in catchments.

Responsibility edited by Ola M. Saether & Patrice de Caritat. Imprint collection and analysis of groundwater samples and environmental isotopes as tracers in catchment. (source: Nielsen Book. Geochemical Processes, Weathering and Groundwater Recharge in Catchments is a specialist book concerned with the natural processes taking place where water interacts with minerals and organic matter at the earth’s surface, in soils or within : Book: Geochemical processes, weathering and groundwater recharge in catchments.

+ pp. Abstract: The 13 chapters of this book cover physical and chemical processes in hydrological basins and aspects of catchment analysis and monitoring. Geochemical processes, weathering and groundwater recharge in catchments O. SaetherSP. de Caritat (eds) © Balkema Contents PREFACE H V XIII PARTI: CATCHMENT PROCESSES 1 WEATHERING PROCESSES James LDrever!: V: Definitions of weathering i- ^ iJ: Ji' Types of weathering reaction 4 Congruent dissolution 4.

Description: Geochemical Processes, Weathering and Groundwater Recharge in Catchments is a specialist book concerned with the natural processes taking place where water interacts with minerals and organic matter at the earth’s surface, in soils or within aquifers.

Geochemical Processes, Weathering and Groundwater Recharge in Catchments is a specialist book concerned with the natural processes taking place where water interacts and groundwater recharge in catchments book minerals and organic matter at the earth’s surface, in soils or within aquifers.

Geochemical Processes, Weathering and Weathering Recharge in Catchments: Edited by Ola M. Saether and Patrice de Caritat, A.A. Balkkema Publishers, Old. Lerner DN () Groundwater recharge. In: Saether OM, de Caritat P (eds) Geochemical processes, weathering and groundwater recharge in catchments.

AA Balkema, Rotterdam, pp – Google Scholar Lerner DN, Issar AS, Simmers I () Groundwater recharge, a guide to understanding and estimating natural recharge.

International. Lerner, D.N., Saether, O.M. and Caritat, P.D. () Groundwater Recharge. In Saether, O.M. and de Caritat, P., Eds., Geochemical Processes, Weathering and Groundwater Recharge in Catchments, Balkema, Rotterdam, - References - Scientific Research Publishing.

To support researchers to publish their research Open Access, deals have been negotiated with various publishers. Depending on the deal, a discount is provided for the author on the Article Processing Charges that need to be paid by the author to publish an article Open Access.

bedrock, the much higher subsurface P CO 2 and production of organic acids drives mineral weathering, with associated increases in DIC, pH and Ca 2+. The relatively high solubility of calcite and its contribution to DIC makes carbonate weathering an important process in the evolution of groundwater.

It is with this approach that the chapter discusses the variety of processes occurring within the catchment system, such as weathering and soil production, generation of stormflow and streamflow, movement of soil pore water, groundwater flow, and the overall processes involved with.

Geochemical Processes, Weathering and Groundwater Recharge in Catchments is a specialist book concerned with the natural processes taking place where water interacts with minerals and. Abstract. Stable isotope (18 O and 2 H) and geochemical signatures are used to gain some insight into recharge processes and groundwater salinization mechanisms in a semi-arid rangeland catchment.

The km 2 catchment is underlain by fractured lower Beaufort sandstones and mudstones and is intruded by several dolerite dykes. Chloride and isotopic relationships suggest that chloride ions in. Cristobal Padilla, Yuichi Onda, Tomoyuki Iida, Interaction between runoff – bedrock groundwater in a steep headwater catchment underlain by sedimentary bedrock fractured by gravitational deformation, Hydrological Processes, /hyp, 29, 20, (), ().

In book: Geochemical Processes, Weathering and Groundwater Recharge in Catchments (pp). The use of mathematical models to depict changes at the catchment scale is examined in the context of geochemical processes, weathering, and recharge in catchments.

A case study conducted at Plynlimon, Wales, UK to study the effects of forestry management on stream water quality is described. The hydrochemistry of the atmospheric inputs, stream draining undisturbed forest, and stream draining.

Geochemical techniques have been used to estimate groundwater recharge and its spatial variability in basement terrain in a semi-arid area of southern Zimbabwe. Recharge rates estimated by chloride mass balance have been determined in the Romwe Catchment, a small ( km2) headwater catchment.

Groundwater (GW) depletion and recurring floods have become a major concern among researchers and planners across the world. To rejuvenate stressed aq. View our complete catalog of authoritative Geographic Information Systems related book titles and textbooks published by Routledge and CRC Press.

Geochemical Processes, Weathering and Groundwater Recharge in Catchments. O.M. Saether, P. de Caritat. Jan. 1st, Sedimentology.

Cojan, M. Renard. Book Chapter: Saether OM. de Caritat P. Geochemical Processes, Weathering and Groundwater Recharge in Catchments. Taylor & Francis, Leiden, The Netherlands R (Final) not available: Book Chapter (3) Meeting: Macalady DL. Properties of natural organic matter relevant to pollutant transport and transformations.

Jakub Jankovec, Tomáš Vitvar, Martin Šanda, Takuya Matsumoto and Liang-Feng Han, Groundwater recharge and residence times evaluated by isotopes of hydrogen and oxygen, noble gases and CFCs in a mountain catchment in the Jizera Mts., northern Czech Republic, GEOCHEMICAL JOURNAL, /geochemj, 51, 5, (), ().

Groundwater downgradient from Trandum municipallandfill was investigated in summerwith a viewto assessing the distribution of redox-sensitivespecies. The water table at Trandum is 10–26 metersbelow the surface. Monitoring well filters have beeninstalled at depths of up to 15 m below water table,covering an area of m by m.

Groundwaterinfluenced by the landfill seems to be. The variations of Na +, Ca 2+, Mg 2+, and were derived from natural weathering reactions, which suggested that the same geochemical processes occurred in the rock weathering reactions that released Na +, Ca 2+, Mg 2+, and into the groundwater along the flow path.

This interpretation is consistent with the water-rock interaction equation for. Volume 5 has several objectives. The first is to present an overview of the composition of surface and ground waters on the continents and the mechanisms that control the compositions.

The second is to present summaries of the tools and methodologies used in modern studies of the geochemistry of surface and ground waters. The third is to present information on the role of weathering. A contrast in the 87 Sr/ 86 Sr ratio of atmospherically derived Sr (∼) and Sr from regional bedrock (>) allows quantification of the proportions of precipitation recharge and groundwater discharge into peat columns of bogs and fens in the Glacial Lake Agassiz Peatlands.

Two contrasting bog‐fen pairs were studied: the Lost River peatland located over a regional groundwater. The chemical characteristics of surface water, base flow and groundwater in a first-order catchment in the wheatbelt of Western Australia were used to study the weathering process and its relationship to the development of groundwater and stream salinity.

Meteoric water infiltrates through the unsaturated zone to the water table aquifer and through the aquifer outcrop in the case of a confined. Groundwater Geochemistry and Isotopes provides the theoretical understanding and interpretive methods and contains a useful chapter presenting the basics of sampling and analysis.

This text teaches the thermodynamic basis and principal reactions involving the major ions, gases and isotopes during groundwater recharge, weathering and redox Reviews: 3.

Patrice De Caritat is the author of Geochemical Processes, Weathering and Groundwater Recharge in Catchments ( avg rating, 0 ratings, 0 reviews, publi. Groundwater recharge; a guide to understanding and estimating natural recharge.

International Contributions to Hydrogeology vol. Heise, Hannover, FRG. pages. In alpine catchments, groundwater recharge mainly occurs by snowmelt. Thus, to capture the seasonal groundwater storage amplitude, we quantify the groundwater storage increase between the peak of snow accumulation and the moment when snow has completely melted within the catchment.

Geochemical Processes {And to get the book you'd like, you simply ought to style and hunt for it, then click the name to visit a web page with detailed details. After that, it is possible to click on its name all over again and strike “GET†to download the eBook.

Topics covered: Geochemical record of terrestrial environmental change, and global geochemical cycles; Chemical weathering and climate, river catchment studies; Environmental geochemistry of the terrestrial environment and its effect on health; Organic geochemistry; Marine and sedimentary geochemistry; Mineralogy, microbes and chemistry of weathering; Geochemical thermodynamics.

The objective of this paper is to assess quantitatively the potential recharge of shallow aquifers in the Senegal River delta in context of semi-arid climate, of massive irrigation development and of modification of hydrologic and hydrogeological characters after dams building.

Quantitative estimation of recharge potentialities have been based on hydrological balance and groundwater table. Geochemical research on natural weathering has often been directed towards explanations of the chemical composition of surface water and ground water resulting from subsurface water-rock interactions.

These interactions are often defined as the incongruent dissolution of primary silicates, such as feldspar, producing secondary weathering products, such as clay minerals and oxyhydroxides, and. The groundwater geochemistry of the Saloum delta aquifer: Importance of silicate weathering, recharge and mixing processes Serigne Faye1*, Mamadou Issa Ba 1, Moctar Diaw1 and Seyni Ndoye2 1Department of Geology, Faculty of Science and Technology, University Cheikh Anta Diop (UCAD), P.

Box Dakar-Fann, Senegal. geochemical processes in systems contaminated with acid mine drainage, and ; Natural organic matter in catchments, in: Geochemical Processes, Weathering and Recharge in Catchments, in O. M Saether and P. de Caritat, eds.

Geochemical Processes, Weathering and Groundwater Recharge in Catchments. Groundwater; nitrate; Sugarcane; Tropics, Sulphate; Denitrification; Soil Chemistry; Environmental Chemistry; Water Geochemistry; Contaminant Transport; Geochemistry. In the Sahel region in Africa, and in most arid regions, groundwater is the crucial source for water supply since surface water is scarce.

This study aimed to understand a complex geochemical mechanism controlling the mineralization process in the Taoudeni Basin.

A thousand randomly distributed groundwater samples acquired from different aquifers were used for this research. Society memberships: Geochemical Society, Geological Society of America (fellow), International Association for Geochemistry and Cosmochemistry, Mineralogical Society of America (fellow).

PUBLICATIONS: Books Drever, J.I. () (editor) Surface and Ground Water, Weathering. Al-Atraf field, is located southwest of Kuwait City, the groundwater is produced from the Kuwait Group aquifer. The objectives are to identify aquifer type and its characteristics.

The major geochemical processes operating in the aquifer have to be revealed. In addition, to evaluate the groundwater quality and its suitability of drinking and agriculture usage, an investigation was carried .The geochemical conditions, occurrence of selected trace elements, and processes controlling the occurrence of selected trace elements in groundwater were investigated in groundwater basins of the Desert and Basin and Range (DBR) hydrogeologic provinces in southeastern California as part of the Priority Basin Project (PBP) of the Groundwater Ambient Monitoring and Assessment (GAMA) Program.

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