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Miquel Mir-Gual, Guillem X. Pons, Irene Delgado-Fernández and Thomas A. G. Smyth
Blowouts are integral features of coastal dune fields. Their presence enhances both geomorphological and ecological diversity and enables the movement of sand by wind. Their role as a ?transport corridor? may be, however, considered negative from a coast...
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Jasper Knight and Mohamed A. M. Abd Elbasit
Remote sensing of coastal sediments for the purpose of automated mapping of their physical properties (grain size, mineralogy and carbonate content) across space has not been widely applied globally or in South Africa. This paper describes a baseline stu...
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Elisa Leone, Nobuhisa Kobayashi, Antonio Francone, Samuele De Bartolo, Davide Strafella, Felice D?Alessandro and Giuseppe Roberto Tomasicchio
Dune recovery interventions that integrate natural, sustainable, and soft solutions have become increasingly popular in coastal communities. In the present study, the reliability of an innovative non-toxic colloidal silica-based solution for coastal sand...
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Alejandro Montes,Fernando Santiago,Mónica Salemme,Ramiro López
Pág. 61 - 76
Laguna Las Vueltas (LLV) area retains the morphology of a late Pleistocene watershed that was flooded during a mid-Holocene marine transgression. Sediments associated with a paleosol dated at 22,582 cal yr BP reflect subaerial exposure of the area prior ...
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Oliver M. Lopez, Khan Z. Jadoon and Thomas M. Missimer
Planning for use of a dune field aquifer for managed aquifer recharge (MAR) requires that hydraulic properties need to be estimated over a large geographic area. Saturated hydraulic conductivity of dune sands is commonly estimated from grain size distrib...
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Iqra Mughal, Khan Z. Jadoon, P. Martin Mai, Samir Al-Mashharawi and Thomas M. Missimer
A component of designing a managed aquifer recharge system in a dune aquifer is the control of diffusive evaporative loss of water which is governed by the physical properties of the sediments and the position of the water table. A critical water table p...
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Cesar E. Gazzera,Luis A. Spalletti
Pág. 131 - 151
ABSTRACT. The lowermost section of a thick Albian(?)-Campanian redbed sequence in the central part of the Neuquen Basin is composed of fine sandstones and pelites with subordinated extra and intraformational conglomerates. Several facies and sedimentary ...
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