Análisis del estado de la capa activa en el emplazamiento de la base antártica española Gabriel de Castilla, Isla Decepción, Antártida

  1. M. A. de Pablo 1
  2. A. Molina 1
  3. C. Recio 2
  4. M. Ramos 1
  5. G. Goyanes 3
  6. M. A. Ropero 4
  1. 1 Universidad de Alcalá
    info
    Universidad de Alcalá

    Alcalá de Henares, España

    ROR https://ror.org/04pmn0e78

    Geographic location of the organization Universidad de Alcalá
  2. 2 Universidad Politécnica de Madrid
    info
    Universidad Politécnica de Madrid

    Madrid, España

    ROR https://ror.org/03n6nwv02

    Geographic location of the organization Universidad Politécnica de Madrid
  3. 3 Instituto Antártico Argentino
    info
    Instituto Antártico Argentino

    Buenos Aires, Argentina

    ROR https://ror.org/02vyk6z19

    Geographic location of the organization Instituto Antártico Argentino
  4. 4 Laboratorio de Ingenieros del Ejército "General Marvá" - INTA. Ministerio de Defensa
Journal:
Boletín geológico y minero

ISSN: 0366-0176

Year of publication: 2017

Volume: 128

Issue: 1

Pages: 69-92

Type: Article

DOI: 10.21701/BOLGEOMIN.128.1.004 DIALNET GOOGLE SCHOLAR

More publications in: Boletín geológico y minero

Sustainable development goals

Abstract

The degradation of permanent frozen ground (permafrost) and the increase in the thickness of the active layer may be caused both by natural processes (such as global climate change) and by anthropic activity, which changes the natural environmental conditions that allow its existence, as has been widely reported to occur in the northern polar and subpolar regions. In the case of Antarctica, some scientific research stations are located in areas with permafrost, such as the Spanish Antarctic station “Gabriel de Castilla” on Deception Island. In the place where the station is located, an important increase in erosion has been observed in recent years, including the excavation of new gullies and the erosion of the coastal cliffs. In order to develop an initial analysis of the possible effects of the station on the permafrost degradation, ground temperature has been monitored since 2012 and the thickness and of the active layer and the temperature, both inside and beneath the station, have also been sporadically measured. Here we show the results and discuss how the station reduces the freezing of the ground during the winter when the station is closed and facilitates the warming of the ground during the living periods of the station in the Antarctic summer. Those initial results and conclusions make necessary to continue the study of the permafrost and the active layer in the station site by systematic monitoring of the ground temperature and the thickness of the active layer.

Funding information

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