Temporal variability of soil organic carbon transport in the Enxoé agricultural watershed
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  • 作者:T. B. Ramos ; S. Rodrigues ; M. A. Branco ; A. Prazeres…
  • 关键词:DOC ; Hysteresis ; POC ; Mediterranean region ; Temporary rivers
  • 刊名:Environmental Earth Sciences
  • 出版年:2015
  • 出版时间:May 2015
  • 年:2015
  • 卷:73
  • 期:10
  • 页码:6663-6676
  • 全文大小:1,581 KB
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  • 作者单位:T. B. Ramos (1)
    S. Rodrigues (2)
    M. A. Branco (2)
    A. Prazeres (2)
    D. Brito (1)
    M. C. Gon?alves (2)
    J. C. Martins (2)
    M. L. Fernandes (2)
    F. P. Pires (2)

    1. MARETEC, Instituto Superior Técnico, University of Lisbon, Av. Rovisco Pais, no 1, 1049-001, Lisboa, Portugal
    2. INIAV, Instituto Nacional de Investiga??o Agrária e Veterinária, Oeiras, Portugal
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:None Assigned
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1866-6299
文摘
The temporal variability of particulate (POC) and dissolved (DOC) organic carbon concentrations was analyzed in the Enxoé temporary river, southern Portugal, between September, 2010 and August, 2013. The overall aim was to study the variability of those elements during storm events, and determine their origin and the main transfer mechanisms to the river. Twenty-one flood events were observed. An empirical model was used to describe changes in solute concentrations, and the magnitude and rotational patterns of the hysteretic loops during flood events. POC and DOC concentrations varied between 0.49-8.93 and 0.25-5.75?mg L?, respectively. POC and DOC annual yields varied between 0.06-.15 and 0.03-.47 t km?, respectively. Flood events had greater effect in POC than in DOC variability. POC had mostly a terrestrial origin, with exports being related to soil erosion and runoff. POC revealed a flushing behavior during the entire monitored period, and clockwise or anticlockwise trajectory loops whenever the predominant origin of the exports was in river bed deposits or arable lands, respectively. DOC had also a terrestrial origin, but it revealed a contrasting dilution behavior and, in general, anticlockwise hysteresis loops. DOC showed a delay in the arrival of solutes to the river, consistent with mass flow through subsurface flow. DOC exports were thus associated with soil weathering and crop mineralization. This work highlights the main processes involved in POC and DOC loads in a temporary river during flood events, with a precise quantification of those elements.

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