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  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Mines and mineral resources. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (177 pages)
    Edition: 1st ed.
    ISBN: 9789401791441
    Series Statement: Environmental Science and Engineering Series
    DDC: 333.8
    Language: English
    Note: Intro -- Preface -- Acknowledgments -- Contents -- Figures -- Plates -- Tables -- 1 Introduction -- Abstract -- 1.1…Introduction -- 1.2…Mining: The Historical Perspective -- 1.3…River Sand Mining: Environmental Issues -- 1.4…Sand: Ecological Values and Uses -- 1.5…Origin of Sand -- 1.6…Scope of the Present Study -- References -- 2 Rivers-Structure and Functions -- Abstract -- 2.1…Introduction -- 2.2…The River Ecosystem -- 2.3…Geological Work of Rivers -- 2.4…River Sediments and Channel Processes -- 2.5…River Classification -- 2.6…Concepts in Riverine Studies -- 2.6.1 River Continuum Concept -- 2.6.2 Nutrient Spiraling Concept -- 2.6.3 Flood Pulse Concept -- 2.7…Human Interventions -- References -- 3 River Sand Mining and Mining Methods -- Abstract -- 3.1…Introduction -- 3.2…Types of Alluvial Sand Extraction -- 3.2.1 Instream Mining -- 3.2.2 Floodplain Mining -- 3.2.3 Terrace Mining -- 3.3…Methods of Sand Extraction -- 3.3.1 Active Channels -- 3.3.2 Floodplains and Terraces -- 3.4…Manual and Mechanical Mining -- References -- 4 Impacts of River Sand Mining -- Abstract -- 4.1…Introduction -- 4.2…Changes in Bed Forms -- 4.3…Changes in Sediment Characteristics -- 4.4…Changes in Water Quality and Quantity -- 4.5…Changes in Biological Environment -- 4.6…Changes in Socioeconomic Environment -- 4.7…Vegetation Effects -- 4.8…Damage to Infrastructure Facilities -- 4.9…Flood Plain Pits Capturing -- 4.10…Impacts of River Sand Mining on Coastal Marine Environment -- References -- 5 Sand Mining: The World Scenario -- Abstract -- 5.1…Introduction -- 5.2…Arizona and California -- 5.3…Italy -- 5.4…Kenya -- 5.5…Jamaica and Costa Rica -- 5.6…Malaysia -- 5.7…China -- 5.8…Sri Lanka -- 5.9…Nepal -- 5.10…Maldives -- 5.11…India -- 5.12…Summary -- References -- 6 Environmental Case Studies from SW India -- Abstract -- 6.1…Introduction -- 6.2…Manimala River. , 6.2.1 Instream Sand Mining -- 6.2.2 Floodplain Sand Mining -- 6.2.3 Channel Incision -- 6.3…Periyar River -- 6.3.1 Sand Mining from Periyar River -- 6.3.2 Channel Incision -- 6.4…Drivers of Change -- 6.5…Environmental Implications of Sand Mining -- References -- 7 EIA of River Sand Mining -- Abstract -- 7.1…Introduction -- 7.2…Environmental Impact Assessment -- 7.3…General Methodologies of EIA: An Overview -- 7.3.1 Ad hoc Method -- 7.3.2 Checklist Method -- 7.3.3 Matrix Method -- 7.3.4 Networks -- 7.3.5 Overlays -- 7.3.6 Simulation and Modeling Workshop -- 7.3.7 Rapid Impact Assessment Matrix -- 7.4…Methodology Adopted -- 7.5…EIA of Sand and Gravel Mining -- 7.5.1 Impact Assessment Using Matrix Method -- 7.5.2 Rapid Impact Assessment Matrix -- 7.5.2.1 Assessment Criteria -- 7.5.2.2 Assessment Results -- 7.5.3 Physical and Chemical Components -- 7.5.3.1 Land/River Channel -- 7.5.3.2 Air and Water -- 7.5.4 Biological Components -- 7.5.5 Social Components -- 7.6…Discussion -- References -- 8 Mining Strategies and Management -- Abstract -- 8.1…Introduction -- 8.2…Environmental Laws Pertaining to Sand Mining -- 8.3…Purpose of the Guidelines -- 8.4…A Framework for Action -- 8.5…The Importance of Channel Maintenance Processes -- 8.6…Management Options and Extraction Control Measures -- 8.7…Restoration and River Management -- 8.8…Management Plan -- 8.8.1 Instream Mining -- 8.8.2 Floodplain Mining -- 8.9…General Guidelines -- References -- 9 River Sand Auditing: An Example from SW India -- Abstract -- 9.1…Introduction -- 9.2…River Sand Auditing -- 9.3…Methodology -- 9.3.1 Resource Estimation -- 9.3.2 Resource Allocation -- 9.3.3 Performance Evaluation/Sand Resource Accounting -- 9.3.4 Estimation of Unauthorized Sand Mining: An Example -- References -- 10 Sand: The Fine Aggregate -- Abstract -- 10.1…Introduction -- 10.2…Sand: The Fine Aggregate. , 10.3…Usefulness of Aggregates -- 10.4…Aggregates for Constructions -- 10.5…Fine Aggregate for Making Concrete -- 10.5.1 Sand for Mortars and Plasters -- 10.5.2 Sand for Filling -- 10.6…Storing and Handling of Aggregates -- 10.7…Aggregate Resource Protection -- References -- 11 Sources of Sand and Conservation -- Abstract -- 11.1…Introduction -- 11.2…Sand: River Sources -- 11.3…Non-river Sources -- 11.3.1 Dune Sands -- 11.3.2 Glacial Outwash Sand -- 11.3.3 Sand in Lakes and Backwaters -- 11.3.4 Beach Sands -- 11.3.5 Reservoir Sand -- 11.3.6 Marine Sand -- 11.4…Sand: Artificial -- 11.4.1 Crushed Rock Sand (Manufactured Sand) -- 11.4.2 Secondary Sand -- 11.5…Conservation of Sand -- References -- Subject Index.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Environmental geology 25 (1995), S. 270-276 
    ISSN: 1432-0495
    Keywords: Sedimentation ; Geochemistry ; Tropical river ; Physical fractionation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Geochemical characteristics of Fe and Mn in sand, silt, and clay fractions as well as in bulk sediments of the tropical perennial Muvattupuzha river and the Central Vembanad estuary of the southwest coast of India have been studied and discussed. The results of a physical fractionation study of Fe and Mn indicated a substantial increase in the content of these metals in silt and clay fractions above that in sand. The riverine silt and clay fractions account for two to three times the enrichment of Fe and Mn than the corresponding sand fraction; the estuarine counterparts indicate four to eight times the enrichment. The observed enrichment of Fe and Mn towards the more finer size grades is mainly due to the increased surface area of the finer clastics, which in turn increase the absorptive ability. However, the mineralogical diversities of the three size fractions also influence the enrichment of Fe and Mn. The spatial distribution of Fe and Mn indicates a marked decrease in the content of the latter than the former towards the high saline zones of the river and the estuary. This variation could be due to the higher solubility of Mn towards the high saline zones of the aquatic environment where reducing condition prevails most of the year.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-0495
    Keywords: Key words Geochemistry ; Trace metals ; Granulometric partitioning
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Geochemical characteristics of six trace metals – Cu, Co, Ni, Zn, Cd and Cr – in the bulk sediment and sand, silt and clay fractions of a tropical estuary on the southwest coast of India have been studied and discussed. In bulk sediment, the trace metal concentration is controlled mainly by the textural composition of the sample. Mud, sandy mud and sandy silt register higher concentrations of trace metals than that in sand-dominant sediments. The granulometric partitioning studies also re-affirmed the role of particle size in enriching the trace metals. The silt and clay fractions exhibit 7–8 times the enrichment of Cu and Cd compared to that in sand. The enrichment factors of Zn, Cr, Ni and Co in the silt and clay fractions, compared to that in sand, are 5–6, 4–5, 2–5 and 2–3 times, respectively. The trace metals in the sand fraction, particularly Ni and Cr, exhibit strong positive correlation with the heavy mineral content of the samples. It clearly indicates a heavy mineral pathway to the trace metals in the sand fraction. Cu and Co in silt and clay fractions exhibit a marked decrease towards the high saline zones of the estuary. This is attributed to the desorption of Cu and Co from particulate phases during estuarine mixing. Contrary to Cu and Co, the content of Zn in the clay fraction shows a marginal increase towards the estuarine mouth. This could be explained by the influx of Zn-rich contaminant discharges from Zn-smelting industries located slightly north of the estuarine mouth. The released Zn will effectively be held in the lattices of the clay mineral montmorillonite, which also exhibits a marked increase towards the estuarine mouth. The anomalously high values of Cd in some places of the Central Vembanad estuary is attributed to the local pollution.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1432-0495
    Keywords: Key words Sedimentation ; Geochemistry ; Mangrove environment
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The textural and geochemical aspects of the sediments of a tropical mangrove ecosystem have been studied and discussed. The sediments are characterized by the abundance of silt and sand with minoramounts of clay. The mean size of the sediment ranges from 0.205 mm to 0.098 mm (fine to very fine grained sand). The sediments are very poorly sorted, negatively to very negatively skewed, and platy to extremely leptokurtic in nature. The organic carbon content of the sediments ranges from 0.33% to 4.93%, which is controlled by the particle size of the sediments. The CaCO3 content is five times the enrichment of organic carbon. This enhanced CaCO3 content of the mangrove sediments might be a result of the abundance of shell fragments in the sediments. The shell mining activities in the estuarine bed adjoining the Kumarakam mangroves also contribute a substantial amount of lime muds to the mangrove area, which in turn add CaCO3 to the sediments. The relative concentrations of heavy metals are Fe〉Mn〉Cr〉Zn〉Ni〉Cu. All heavy metals other than Fe show an increase in concentration compared to the other parts of the estuarine bed. Cluster analysis indicates that the contents of organic C, Fe and Mn have a marked bearing on the Cr, Zn, Ni, and Cu levels of the mangrove sediments.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1432-0495
    Keywords: Key words Interstitial water geochemistry ; Nutrients ; Early diagenesis ; Tropical estuaries ; Southwest coast of India
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The concentrations of N, P and Fe in surface sediments and interstitial and overlying (bottom and surface) waters of the Ashtamudi estuary located in the southwest coast of India are reported along with the various chemical species of N (NO2–N, NO3–N, NH3–N and total N) and P (organic P, inorganic P and total P) in interstitial and overlying waters and discussed in terms of the physico-chemical environment of the system. The interstitial water exhibits higher salinity values compared to bottom and surface waters, indicating the coupled effects of salt-wedge phenomena and gravitational convection of more saline-denser marine water downward through surface sediments. N, P and Fe as well as their chemical forms are enriched in the interstitial water compared to bottom and surface waters. However, the dissolved oxygen (DO) shows an opposite trend. The marked enrichment of NH3–N in the interstitial water and its marginal presence in bottom and surface waters, together with the substantial decrease in the DO concentrations of bottom water and consequent increase in the concentrations of NO2–N and NO3–N in interstitial and bottom waters, points to the nitrification process operating in the sediment-water interface of the Ashtamudi estuary. The enrichment of total N, P and Fe in the interstitial water compared to the overlying counterparts and the positive correlation of sediment N, P and Fe with mud contents as well as organic carbon indicate that these elements are liberated during the early diagenetic decomposition of organic matter trapped in estuarine muds.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1432-0495
    Keywords: Sedimentation ; Geochemistry ; Mangrove environment
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The textural and geochemical aspects of the sediments of a tropical mangrove ecosystem have been studied and discussed. The sediments are characterized by the abundance of silt and sand with minor amounts of clay. The mean size of the sediment ranges from 0.205 mm to 0.098 mm (fine to very fine grained sand). The sediments are very poorly sorted, negatively to very negatively skewed, and platy to extremely leptokurtic in nature. The organic carbon content of the sediments ranges from 0,33% to 4.93%, which is controlled by the particle size of the sediments. The CaCO3 content is five times the enrichment of organic carbon. This enhanced CaCO3 content of the mangrove sediments might be a result of the abundance of shell fragments in the sediments. The shell mining activities in the estuarine bed adjoining the Kumarakam mangroves also contribute a substantial amount of lime muds to the mangrove area, which in turn add CaCO3 to the sediments. The relative concentrations of heavy metals are Fe 〉 Mn 〉 Cr 〉 Zn 〉 Ni 〉 Cu. All heavy metals other than Fe show an increase in concentration compared to the other parts of the estuarine bed. Cluster analysis indicates that the contents of organic C, Fe and Mn have a marked bearing on the Cr, Zn, Ni, and Cu levels of the mangrove sediments.
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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